Anion
exchange separation of trace level of thorium and uranium from
zirconium matrix: ICP-AES and laser fluorimetric
determination of uranium and thorium in zircon mineral
A
rapid method for determination of trace elements in hydrogeochemical
samples and saline waters using ICP–AES after
copper–diethyldithiocarbamate co-precipitation
Assessment
of moisture content in the steam generated by steam generator of
a nuclear power plant by determining the sodium content in the
condensate by flame emission spectrometer
Synthesis
of immobilized used green tea leaves on silica gel and its application
in separation / pre concentration of uranium and trace elements
in hydrogeochemical samples
Wavelength
dispersive x-ray fluorescence vis-à-vis inductively coupled
plasma- optical emission spectrometry of major and trace elements
in silicate rocks
Chanchal Sarbajna, Smeer Durani, V.Rajagopalan and D.S.R.Murthy
Wavelength-dispersive
x-ray fluorescence spectrometric determination of some rare-earth
elements in columbite-tantalite using their k-spectra and an LiF
420 analysing crystal
B.N.
Tikoo, Anjan Chaki, Yamuna Singh, and S. Viswanathan
Standardization
of a particle induced gamma ray emission (PIGE) method for fluorine
determination at FOTIA, BARC and its application to borosilicate
glass samples
R.
Acharya, R. Tripathi, K. Sudarshan, A.V.R. Reddy, R. G. Thomas,
S. Santra, S.K. Gupta, R.K. Choudhury, R.K. Mishra,
V.G. Katarni, C.P. Kaushik
Characterization
of Selenium (IV) and Selenium (VI) in water samples using diaminobenzidine
and estimation by graphite furnace atomic absorption spectroscopy
Quantitative
electron probe micro analysis of uranium minerals in Proterozoic
quartzites and basal granitoids of Damarcherla area, Palnadu Sub-Basin
of Cuddapah basin, Nalgonda district, Andhra Pradesh, India
V.Rajagopalan,
A.K.Paul, S.V.S.Reddy and H.K.Sabot
CHEMICAL CHARATERTIZATION
OF REFRACTORY MINERALS FOR MAJOR ELEMENTS BY MICROWAVE ASSISTED DIGESTION
AND FLAME-AAS
Smeer Durani, Neeraja Mathur, D.S.R.Murty
Chemistry laboratory,
Atomic Minerals Directorate for Exploration and Research,
Begumpet, Hyderabad-500016
Abstract
A simple, convenient
and rapid dissolution method resulting in a single solution for determination
of major impurities in hi-tech minerals
is described. Six mineral samples i.e., ilmenite, rutile, garnet, zircon,
monazite and sillimanite were dissolved by microwave assisted digestion
procedures and major element impurities such as Al, Fe, Ca, Mg, Mn,
Na, K, P were determined by Flame AAS & UV-VIS spectrophotometry.
The validity / performance of Microwave assisted digestion (MDS) method
was compared with the conventional analytical methods of hot plate
digestion / fusion. MDS requires only two hours of sample dissolution
time, much shorter than required for conventional digestion in an open
vessel and also results in very less amount of dissolved salts. The
recoveries were in the range of 85 – 110%.
Keywords: Chemical characterization; Refractory minerals; Flame-AAS;
Microwave digestion
A NEW SAMPLE DECOMPOSITION PROCEDURE FOR THE BARYTE BEARING ROCKS AND
PEGMATITE MINERALS: ELEMENTAL CHARACTERISATION USING ICP-AES AND
FAAS
A. Premadas and Anitha Mary Thomas
Chemistry Laboratory, Southern Region
Atomic Minerals Directorate for Exploration and Research
Department of Atomic Energy, Nagarbhavi, Bangalore-560072, India.
apremadas.amd@gov.in
Abstract
This paper proposes a new sample decomposition procedure for the baryte
bearing rocks and baryte bearing pegmatite refractory minerals for
the preparation of a single sample solution. Samples are completely
decomposed by fusion with a mixture of di-sodium hydrogen phosphate
and di-hydrogen sodium phosphate, the cooled melt is completely extracted
in distilled water. The solution after suitable dilution is used for
the ICP-AES and FAAS estimation of essentially Ba, Ti, Al, Fe, Mn,
Ca, and Mg and also some other elements like Sr, Cr, Mo, V, Nb and
Ta. Uranium is determined by the laser fluorimetric method. A lithium
meta-borate fusion for the sample decomposition is also optimized.
The results obtained by the two methods are compared with the conventional
acid digestion and sodium carbonate fusion. Validity of the proposed
method is established by analyzing some Canadian Certified Reference
samples like SY-2, SY-3, SO-2, MRG-1 and FeR-1 doped with milligram
quantities of barium sulphate and synthetic samples prepared from high
purity oxides. The proposed procedure is simple, accurate and precise.
A RAPID DISSOLUTION PROCEDURE FOR THE FLUORIMETRIC DETERMINATION OF
URANIUM IN CALCRETE SAMPLES OF
WESTERN RAJASTHAN
A. Thangaraj, M.K. Ganguly, P.N. Bangroo, K.Ramesh Kumar and L. K.
Nanda
Western Region, Atomic Minerals Directorate for Exploration and Research,
Department of Atomic Energy, Jaipur
Abstract
The calcrete samples
in Rajasthan have shown positive uranium concentration in a set of
samples in Lachhri area. Since these samples contain high
calcium, the opening of the samples by hydrofluoric acid becomes difficult
due to formation of insoluble calcium and magnesium fluorides. In order
to circumvent this problem, boric acid was used along with nitric acid
to break the fluorides and remove fluoride. The recovery of uranium
in the presence of boric acid was studied and found to be quantitative.
Based on this a procedure of sample opening of calcrete samples and
estimation of uranium is presented in this work.
RAPID DECOMPOSITION AND DISSOLUTION OF TIN SLAG SAMPLES FOR DIRECT
DETERMINATION OF URANIUM BY LASER INDUCED FLUORIMETRY
P.L. Mahanta, G. Chakrapani*, R. Radhamani and P. Murugesan
Chemistry Laboratory, Atomic Minerals Directorate for Exploration
and Research Central Region, Nagpur-440001
*chakrapanigotur@yahoo.com
Abstract
A
simple and rapid decomposition method has been developed for application
to dissolution
of tin slag
samples for determination of uranium at
ppm levels by Laser Induced Fluorimetry. Tin slag samples were treated
with HF and HClO4,
fumed to dryness, fused with flux (Sodium dihydrogen orthophosphate
and di-sodium hydrogen ortho phosphate in the ratio 1:1)
and dissolved in distilled water for the analysis of uranium by laser
induced fluorimetry (LIF). The main advantage of this method is sample
decomposition is simple, no separation stage is involved and analysis
could be carried out directly. The flux (phosphate mixture) used for
decomposition itself acts as fluorescence enhancing buffer unlike other
complexing agents like Oxalic, Tartaric and Citric acids (used in various
sample decomposition procedures involving variety of fluxes) as these
reagents acts as strong quenchers of uranium fluorescence and hence
separation is required before analysis. The accuracy of the method
is evaluated by analyzing synthetic samples and comparing the values
obtained by present method with pellet fluorimetry. In both the cases
the results obtained are well within the experimental error. The RSD
of the method is ± 10% at 100 ppm level. The method is successfully
applied to numerous tin slag samples received from Rare Metal and Rare
Earth Investigation Groups.
Keywords: Uranium, Tin slag, Phosphate flux, Laser Fluorimetry.
DEVELOPMENT OF METHOD FOR RAPID DIGESTION OF SILICEOUS URANIUM ORES
OF SINGHBHUM SHEAR ZONE
S.K. Singh and *A.K. Singh
Control Research and Development Department,
Uranium Corporation of India Limited, Turamdih
*anand_ucil@rediffmail.com
Abstract
Singhbhum shear zone (SSZ) of Jharkhand state is known as the treasure
house of many minerals of economic importance. The zone also hosts
the lion’s share of Indian uranium reserves spread in a number of small
to medium deposits. Jaduguda, the first uranium deposit to be discovered
in the country is located almost at the centre of this 180 km long
shear zone. The host rock of the uranium-mineralized sector of SSZ
is rich in silica content and its digestion by conventional open vessel
digestion method is very tedious and time-consuming. It calls for the
development of a rapid and effective method for digestion of this type
of ore. Experiments were carried out to digest the siliceous uranium
ores by Microwave digester and the method has now been standardized
for regular application.
A SIMPLE, RAPID AND ACCURATE DETERMINATION OF URANIUM IN MONAZITE MINERAL,
Th AND REE-RICH MATRIX USING LASER FLUORIMETER AND ICP-AES
A.Premadas*, Nishma Ojha and Dhilshathu Beegam
Chemistry Laboratory, Southern Region
Atomic Minerals Directorate for Exploration and Research
Department of Atomic Energy, Nagarabhavi, Bangalore-560072, India.
*apremadas.amd@gov.in
Abstract
An
accurate, simple, rapid and direct laser fluorimetric determination
of trace level
of uranium
in monazite mineral, thorium and rare earth
elements rich matrix is reported with a determination limit of 1µg
g-1 uranium in ThO2 matrix using laser fluorimeter. Sample solution
is prepared by fusing the sample with a mixture of Na4P2O7 and
NaH2PO4 and
the solution is prepared in distilled water, and few drops of hydrogen
peroxide were added in case of monazite mineral. Suitable aliquot is
taken for the direct laser fluorimetric determination of uranium using
sodium pyrophosphate solution (pH ~ 7) as fluorescence enhancing reagent.
Unlike in the pellet fluorimetric determination of uranium, fluorescence
quenching is not observed either due to thorium or rare earth elements
in the concentration range studied (5-200 µg ml-1)
by this method. Analytical problems encountered in the determination
of uranium in
monazite mineral by the pellet fluorimetric method after the ethyl
acetate solvent extraction separation is also discussed. A spectral
interference-free ICP-AES uranium determination procedure in monazite
mineral is optimized after the solvent extraction separation of uranium
from acidified sodium polyphosphate medium using ethyl acetate, tri-n-butyl
phosphate (TBP) and tri-n-octyl phosphine oxide (TOPO) as individual
extractant. The proposed uranium determination methods are validated
by estimating uranium in (i) monazite in-house reference sample (ii)
synthetic sample prepared by mixing high purity oxides of Th and some
REE, doped with known trace amounts of uranium and, (iii) by the standard
addition technique. The laser fluorimetric determination is used for
the determination of uranium at trace level, and ICP-AES at the percentage
level. The RSD of the method at 1µg g-1 uranium in ThO2 matrix
is 7% (n=4) and at 0.35% uranium in monazite mineral RSD is 4% (n=4)
using ICP-AES.
ANION EXCHNAGE SEPARATION OF TRACE LEVEL OF THORIUM AND URANIUM FROM
ZIRCONIUM MATRIX: ICP-AES AND LASER FLUORIMETRIC DETERMINATION OF URANIUM
AND THORIUM IN ZIRCON MINERAL
A. Premadas and B. Gomathyamma
Chemistry Laboratory, Southern Region
Atomic Minerals Directorate for Exploration and Research
Department of Atomic Energy, Nagarabhavi, Bangalore-560072, India.
apremadas.amd@gov.in
Abstract
A simple, selective and quantitative anion exchange separation procedure
for Th and U at trace level from Zr-rich matrix has been developed.
Both Th and U are adsorbed on an anion exchanger, Dowex-1 X8, (100-200
mesh size) quantitatively, leaving the Zr un-adsorbed, facilitating
the complete separation of Th and U from Zr-rich matrix, thus providing
an interference-free ICP-AES determination of Th and U at trace level.
The procedure is applied to zircon mineral sample. A simple, rapid
and direct laser fluorimetric determination of U in zircon sample is
also developed, and the tolerance level of Zr and oxalate salts are
quantified. The proposed methods are accurate and the reproducible.
Atomic Minerals Directorate for Exploration and Research,
Department of Atomic Energy Begumpet Hyderabad - 500 629
Abstract
Estimation
of Uranium in geological rock samples, is carried out by gamma ray
spectrometry measuring 1.76 MeV gamma emitted by daughter
product 214Bi
of the Uranium series with an assumption that Uranium series is in
equilibrium with its daughter products. In present attempt,
estimation of Uranium has been done by measuring 63.3 keV and 92.38
keV gamma rays emitted by nuclide 234Th
(immediate daughter product of 238U)
using High Purity Germanium detector. Interestingly this technique
does not need apriori any conditions of equilibrium or disequilibrium
in the Uranium series - an advantage.
Keywords: Uranium; Direct estimation; HPGe detector; Geological samples
DETERMINATION
OF URANIUM CONCENTRATION AND FREE ACID IN URANYL NITRATE SOLUTIONS
BY TWO-END POINT pH TITRATION
Binoj Nair, P. Shanmugavelu, T.M. Sudhakar and S.Sarkar
Analytical Control Laboratory, Chemical Technology Group,
Bhabha Atomic Research Centre, Mumbai, India
Abstract
A simple analytical method has been described for measuring the
free acidity and uranium concentration in uranium bearing process
stream
samples for uranium refining industry. The method involves acid-base
titration using standardised NaOH as titrant at two pre-set end
points i.e. pH-3 and pH-4, which corresponds to the free acid
and the hydrolyzing
reaction of uranium. The volume of titrant consumed in back titration
can be calculated to yield the free acidity and uranium concentration
of the sample aliquot. The calibration is performed using a standard
uranyl nitrate solution where the uranium concentration is 30 g/L
with a free acidity of 0.3 N. Relative standard deviation of less
than 2 % has been obtained for both uranium and free acidity measurements
by the proposed method. The results are compared with those obtained
by potentiometry and the results are found to be satisfactory.
ESTIMATION OF LOW LEVELS OF URANIUM IN ACTIVE EFFLUENTS AND SOLID WASTE
FROM URANIUM PROCESSING FACILITIES USING AUTOMATIC VOLUMETRIC ANALYZER
Shanmugavelu.P, Prabhakar.M.S, Pavithran. M.V., Sudhakar. T.M and
Sarkar.S
Analytical Control Laboratory, Chemical Technology Group,
Bhabha Atomic Research Centre, Mumbai, India
Abstract
A simple, fast
and accurate analytical method for estimating low level of uranium
in active effluents
and solid waste originating from uranium
processing industries is described here. The method involves complete
automation of analysis using computer controlled titrator as per standard
Davis & Gray volumetric method. The method is tested for its performance
and validated by analyzing different standard solutions. It is found
that samples having uranium concentration above 200 ppm can be analysed
with the acceptable limit of precision and accuracy.
ANALYSIS OF URANIUM – A COMPARATIVE STUDY USING ICP-MS
AND LASER FLUORIMETRY
Shailaja Pandey, Niyoti S. Shenoy and Sanjukta A. Kumar
Analytical Chemistry Division, Bhabha Atomic Research Centre,
Mumbai 400085, India
Abstract
Uranium in ultratrace level has been determined in seawater using
ICP-MS and Laser Fluorimetry. A matrix separation is carried
out using Poly Hydroxamic
Acid as solid phase extractant in the case of ICP-MS to remove the high
salt content. In laser fluorimetry a nitric acid treatment
was done to eliminate
the quenching effect. The values obtained by both the techniques are in
good agreement.
TRACE ELEMENT ANALYSIS OF URANIUM SAMPLES:
ROUTINE ANALYSIS METHODOLOGY
S.Chandramouleeswaran and J.C.Upadya
Analytical Chemistry Division,
Bhabha Atomic Research Centre, Trombay, Mumbai 400 085
Abstract
The analysis of
trace levels of iron and aluminium in uranium are routinely carried
out and around
1900 samples have been analyzed over
the last five years. The matrix is removed by solvent extraction method
using tributyl phosphate (TBP). The separated aqueous phase containing
iron and aluminium were analyzed using both spectrophotometry and ICP-AES.
The spectrophotometric method has a detection limit of 0.04 µg/
mL whereas that for ICP-AES is 0.1 µg/ mL. Because of the large
sample throughput, the use of ICP-AES is more suited for the regular
analysis.
DETERMINATION
OF %235U
IN DEPLETED URANIUM SAMPLES USING NAI(TL)-GAMMA RAY SPECTROMETER
IN COMBINATION WITH REDOX TITRIMETRY
R. Vasantha, U. Bharati Misra, B. Narasimha Murty and R.B. Yadav
Control Laboratory, Nuclear Fuel Complex, Hyderabad, India- 500 062
Abstract
The present paper describes an analytical method based on combination
of Gamma Ray Spectrometry cum Redox Titrimetry to determine the content
of 235U
in depleted uranium materials. The content of in depleted uranium
samples is calculated by measuring the count rates
pertaining to photo
peak of 185.7 keV of sample solution and that of the natural uranium
standard solution having the same concentration of uranium. The count
rates are measured by using gamma ray spectrometer equipped with
a NaI(Tl) detector and the concentration of uranium in the
solutions
is determined by redox titrimetric method. The variance in the calculated
content of %235U is
expressed in terms of variance in the count rates at the 185.7 keV
photo peak pertaining to sample and natural uranium
standard solutions using the basic statistical concept of propagation
of errors.
The present method in determination of %235U has
relative standard deviation of 1% (n=10) at 0.590 % 235U
in depleted uranium samples. The content
of %235U determined
in various uranium dioxide powders of depleted uranium material using
the present method are compared well with those values
obtained by thermal ionization mass spectrometry.
Keywords: Depleted uranium; Redox titration; Gamma ray spectrometer
DIFFERENTIAL PULSE POLAROGRAPHIC DETERMINATION
OF URANIUM IN LEACH LIQUORS
A. A. Patwardhan
Chemistry Laboratory, Atomic Minerals Directorate for Exploration
and Research,
Central Region, AMD Complex, Civil Lines, Nagpur-440 001
Abstract
Leaching of Uranium ores is an initial and intrinsic step towards
its beneficiation and conversion into nuclear fuel .The “leach liquors”
are the process solutions produced during the beneficiation operation
and require frequent and rapid monitoring for their uranium content.
However, most of the existing analytical procedures viz. fluorimetric
technique and ICP-AES require pre-separation of uranium owing to possible
matrix interferences.
Present
communication describes a direct (without any pre- separation), rapid
and selective method for determination of uranium in leach liquors
by Differential Pulse Polarography. A mixture of Sulphuric acid (0.05M)
and ascorbic acid (2%w/v) has been used as supporting electrolyte.
Uranium, under the conditions, exhibits a reduction peak at – 0.228
v. Vs Ag/AgCl reference electrode. The lowest limit of quantitation
achieved by the proposed method is 5 ppm of U3O8 (RSD
+ 3%) in presence of large amount of iron(U :Fe ratio =1: 10000)
The
two major advantages of the proposed method are (i) absence of any
separation or pre-concentration step and (ii) the use of 0.05
M H2SO4 as
supporting electrolyte, which, is the very medium used as leaching
agent in the acid leaching of uranium ores. Other experimental
parameters viz. effect of supporting electrolyte, effect of ascorbic
acid concentration ,effect of presence of other ions, possibility
of simultaneous determination of other cations etc. has also been
studied
in detail . Routine samples of leach liquors received were analysed
by the proposed method, and the method has been validated by analysing
international rock standards namely SY-2 and SY-3.
COMPARISON
OF CLASSICAL AND INSTRUMENTAL TECHNIQUES FOR THE ANALYSIS OF HIGH GRADE URANIUM ORES AND PROCESS SAMPLES
N. Balachandran, R. R. Venkitakrishnan and A. S. Navale
Mineral Processing Division, BARC, AMD Complex, Hyderabad
Abstract
The uranium content in Indian uranium ores is quite low. The analysis
of uranium in these ores is commonly carried out by pellet fluorimetriy.
Recently, a high grade uranium ore sample was received in our laboratory
having uranium content more than 20%. The process stream samples from
this ore also are high in uranium content. The classical methods like
volumetry and gravimetry are employed for analysis of such high grade
samples. But these classical methods are time consuming and sample
throughput is considerably low. Studies were carried out to adopt pellet
fluorimetric technique for such high grade ore and compare the results
with those from classical methods. The results showed that it is possible
to obtain results comparable to the classical methods and that the
fluorimetric method can be applied to the analysis of both high and
low grade samples without loss in accuracy.
A RAPID METHOD FOR DETERMINATION OF TRACE ELEMENTS IN HYDROGEOCHEMICAL
SAMPLES AND SALINE WATERS USING ICP – AES AFTER COPPER – DIETHYLDITHIOCARBAMATE
CO-PRECIPITATION
Roopa Bose and K.Satyanarayana
Chemistry Laboratory,Southern Region,
Atomic Minerals Directorate for Exploration and Research,
AMD Complex,Nagarbhavi,Bangalore.
Abstract
A
method for the determination of trace amounts of Bi, Cd, Co, Cr,
Hf, Ni, Pb, Th,
Zn and Zr in
hydrogeochemical samples and saline waters
by Inductively Coupled Plasma Atomic Emission Spectrometry after co-precipitation
by using diethyldithiocarbamate as a chelating agent and copper as
a carrier element is described. Different factors including pH of the
sample solution, chelating agent conc., carrier element conc. and time
of contact were optimized for achieving quantitative recovery of the
traces at µgl-1 levels. The method developed was applied for
estimation of traces in hydrogeochemical samples received from different
field areas pertaining to uranium exploration programmes. The optimized
procedure was also successfully applied to recover trace elements from
spiked samples of reconstituted sea water at 5 – 10 µgl-1 conc.
The
recoveries varied from 98 % to 105 % according to the trace elements
determined except in the case of Bi where the recovery was varied
between 85% to 88%. The limits of determination by the proposed method
in natural
water samples are 5 µgl-1 for
Bi and Hf; 4 µgl-1 for
Pb and Th; 2 µgl-1 for
Co, Ni, Zr and 1 µgl-1 for
Cd, Cr and Zn by ICP - AES. By flame AAS the limits of determination
were 6 µgl-1 for
Pb; 3 µgl-1 for
Co and Ni; 1 µgl-1 for
Cd and 0.5 µgl-1 for
Zn. The RSD of the present procedure as a whole ( n = 3) is about
6 – 8% at 5 µgl-1 level.
Keywords: Co-precipitation; Sodium diethyldithiocarbamate; Water samples;
ICP-AES
SELECTIVE METHOD FOR DETERMINATION OF PESTICIDE RESIDUES IN ENVIRONMENTAL
WATER SAMPLES USING CAPILLARY GAS CHROMATOGRAPH AND MASS SPECTROMETRY
K. Rama Mohan*, A. Keshav Krishna, N. N. Murthy, A. Santosh Kumar,
G. Machender
Environmental Geochemistry Division, National Geophysical Research
Institute
(Council of Scientific & Industrial Research, India)
Uppal Road, Hyderabad 500606, India
*krmohan@ngri.res.in
Abstract
A selective method
for the determination of organochlorine pesticide (OCP) residues
in water
samples was reported. Liquid-Liquid-Extraction
(LLE) method was evaluated in optimizing the extraction procedure for
the analysis of pesticides. Florisil column chromatography was adopted
for clean-up the extracts. The dichloromethane gave the best results
of all the extracting solvents used. The percentage of recoveries ranged
from 90.12±7.12 (Dieldrin) to 101.25±2.84% (d-BHC). The
Limits of detection for the OCPs vary between 0.4 and 1.6µg/l.
The residues were determined by gas chromatographic separation and
GC quadrupole–MS detection. The determination of 16 OCPs was achieved
in about 23 min. The LLE method was applied to groundwater samples
collected from Kazipalli Industrial Area, Hyderabad that receives run-offs
from agricultural lands and effluents from industries. The levels of
OCPs levels detected ranged from 0.5 (Dieldrin) to 111.6µg/l
(d-BHC) which include some endocrine disrupting pesticides.
Keywords: Determination; Organochlorine pesticide (OCP); GC-MS; Water
samples
*Corresponding author
SURFACE TENSION OF WATER, SATURATED (0-100%) WITH
TRI-n-BUTYL PHOSPHATE AT 298.15 K
Shekhar Kumar*, Rajnish Kumar and S.B. Koganti
Reprocessing Research and Development Division
Reprocessing Group, IGCAR, Kalpakkam 603102, India
*shekhar@igcar.gov.in
Abstract
The surface tension of water with varying concentration of TBP (0-100%
saturation) was measured at 298.15 K and 0.1 MPa. The experimental
data could be modeled by the Tamura’s method. However for modeling
of experimental data by Szyszkowski equation, need for a correction
in the basic equation was observed as the “constant” ac was found to
be composition dependent for the TBP-water system. An extended Szyszkowski
equation has been proposed in this work, possibly for the first time
in literature.
ASSESSMENT OF MOISTURE CONTENT IN THE STEAM GENERATED BY STEAM GENERATOR
OF A NUCLEAR POWER PLANT BY DETERMINING THE SODIUM CONTENT IN THE CONDENSATE
BY FLAME EMISSION SPECTROMETER
P.K.Pal and R.C.Bohra
Rajasthan Atomic Power Station, Kota, Rajasthan
Abstract
This
paper describes a procedure to assess the content of moisture indirectly
in the steam generated by a steam generated used in a nuclear
power plant which is an important parameter for the smooth functioning
of the steam generator. The procedure involves generation of steam
with use of boiler water containing known quantity of sodium followed
by the determination of content of sodium in the condensate water using
flame emission technique. As the moisture content in the steam can
result only due to carry over of the boiler water containing sodium,
the presence of sodium in the water condensate which otherwise would
have been nil is an indirect measure of moisture content in the steam.
Thus, the fraction of moisture content in the steam is simply the ratio
of contents of content of sodium in the water condensate to content
of sodium in the boiler water.
Keywords:
Moisture content; Determination; Sodium in condensate; Flame emission
spectrometer
SYNTHESIS OF IMMOBILIZED USED GREEN TEA LEAVES ON SILICA GEL AND ITS
APPLICATION IN SEPARATION / PRE CONCENTRATION OF URANIUM AND TRACE
ELEMENTS IN HYDROGEOCHEMICAL SAMPLES
Vijay Kumar, Satya Prakash and P.N. Bangroo
Chemistry Laboratory, Western Region, Atomic Minerals Directorate
for Exploration and Research, Department of Atomic Energy, Jaipur
Abstract
A simple and sensitive
method has been developed for the separation and pre concentration
of trace elements like copper, cobalt, nickel,
zinc and uranium by means of Used Green Tea Leaves (UGTLs), immobilized
over the silica gel using a 25mm x 10mm sorbent column. The pre concentrated
elements have been determined by Inductively Coupled Plasma-Optical
Emission Spectrometer (Jobin Yuon, Horiba Ultima2), Flame Atomic Absorption
Spectrometer (Analytik Jena novAA 300)and uranium by Fluorimeter (model
Galvanek and Morrison) /Laser Induced Fluorimeter (Fabricated by RRCAT,
Indore).The pre concentration studies have been carried out at different
pH (2-7) conditions so as to arrive at optimization and the quantitative
recovery of analytes by eluting with 1 mol/L of HCl solution at the
flow rate of 1.5 ml/min. The validity of the method was checked with
synthetic mixture and standard addition technique. The method has been
tested in a number of effluents and hydrogeochemical samples. Accuracy
achieved was ±10% at 10ppb level for trace elements and 0.1ppb
for uranium with the enrichment factor of 10.
A RAPID METHOD FOR MAJOR AND TRACE ELEMENT DETERMINATION IN WATERS
USING PLASMA EMSSION SPECTROMETRY
Smeer Durani and D. S. R. Murty
Atomic Minerals Directorate for Exploration and Research,
Department of Atomic Energy, Begumpet, Hyderabad-500016
Abstract
For hydrogeochemical exploration studies, water plays a key role as
the mediator of many processes, as well as being the principle medium
for the solubilisation and transport of material. Hence, its composition
is intensively studied for geochemical interpretation. Direct analysis
of water is the simplest application of ICP-OES in practice. A large
number of hydrogeochemical samples are analysed for major and trace
elements. Quick analytical feed back for field interpretation is required.
Therefore, an Inductively Coupled Plasma Optical emission spectrometry
is used for multi elemental determination of major and trace elements
without pre-concentration. The present equipment utilized has advantage
of low detection limits, excellent sensitivity and high sample throughput.
Keywords: Determination; Hydrogeochemical samples; ICP-OES; Trace
elements
DETERMINATION OF INDIUM IN NIOBATE/ TANTALATE AND
GEOLOGICAL SAMPLES BY ICP- AES AFTER ACID HYDROLYSIS
SEPARATION AND SOLVENT EXTRACTION
A simple, precise
and accurate solvent extraction method is described for the separation
and estimation of Indium in geological materials.
Solvent extraction of Indium from 6 M HCl medium using tri-n-butyl
phosphate, selectively separates Indium from accompanying elements
in different type of geological samples. Acid hydrolysis of Nb/Ta samples
separates Indium from major matrix elements like Nb and Ta. The remaining
elements do not influence the selective extraction and preconcentration
of In and its subsequent determination by ICP-AES or flame AAS. The
silica rich geological samples are decomposed by HF-H2SO4-HCl
treatment followed by dissolution in 6M HCl before applying solvent
extraction
procedure. In Nb/Ta type of samples, Indium was separated from Nb and
Ta by acid hydrolysis, involving fusion with Na2O2,
dissolution in HCl followed by NH4OH
precipitation and hydrolysis in HCl. The oxychloride
precipitates of Nb and Ta are filtered off and subjected to solvent
extraction using TBP. The proposed method has been applied to some
international reference standards (IGS-33 and ASK-3) and to some Nb/Ta
type samples and the results are compared by ICP-AES as well flame
AAS techniques. The method is simple, rapid and accurate showing a
relative standard deviation of 2% (at 170 µg/g) to 7.0% (at 16 µg/g
) and the method can be applied down to 1 µg/g .
DETERMINATION OF As, Se AND Mo IN GEOLOGICAL SAMPLES
BY ICP-AES AFTER SULFIDE CO-PRECIPITATION AND
PRECONCENTRATION USING Cu AS CARRIER
K. Satyanarayana, Usha Nathan and A.K. Rai
Chemistry Laboratory, Southern Region
Atomic Minerals Directorate for Exploration and Research
Department of Atomic Energy, Nagarabhavi, Bangalore-560072, India.
Abstract
A simple and rapid inductively coupled plasma atomic emission spectrometric
method for the determination of As, Se and Mo in a variety of geological
materials is described. The samples are treated with a mixture
of acids like HF, HNO3,
HClO4 and
H2SO4.
Copper carrier solution is added to the clear solution to act
as a co-precipitant before the
addition of sodium sulfide solution in 10% v/v HCl solution. The
precipitates are dissolved in aqua-regia and H2SO4 with
final dissolution in 10% v/v H2SO4 acid
solution and is aspirated into the plasma for optical emission
measurements. The method is accurate and
precise,
offering a relative standard deviation ranging from 2-7.0 % for
all the three elements studied. The method was applied to different
types
of international reference standards, viz., SY-3, FER-1, FER-2,
SO-2, SO-3, SO-4, ASK-2, and ASK-3 besides some geological
materials including
iron rich pit samples, pyrite rich and limestone samples for all
the elements and measured at their most sensitive emission lines
viz.193.759nm for As(I), 196.090nm for Se(I), and 202.030nm for
Mo(II). The values obtained are compared well with the certified
values for
all the three elements. The method allows the determination of
As, Se and Mo down to 1µg/gm in different types of geological samples.
ANALYSIS
OF Cm-247 SUPERCAST ALLOY FOR Au, Hg, In and Pd by ICP-AES
G. Satyanarayana, R. Ethiraj, Y. Balaji Rao* and R.B. Yadav
Control Laboratory, Nuclear Fuel Complex, Department of Atomic Energy,
ECIL Post, Hyderabad 500062
*ybr@nfc.gov.in
Abstract
The
present paper discusses a new method developed for estimation of
Gold (Au), Mercury
(Hg),
Indium (In) and Palladium (Pd) in Nickel
based Cm-247 super alloy by Inductively Coupled Plasma Atomic Emission
Spectrometer (ICP-AES). The present procedure employs the dissolution
of alloy in a mixture of Sulphuric acid, Nitric acid and HF and subsequent
analysis by sequential ICP-AES (Model JY Ultima 2C HR, France).This
procedure is being developed as a nodal procedure for indigenously
development of alloy for secondary standards purpose. A Relative Standard
Deviation of less than ± 5% has been achieved for all the elements.
DETERMINATION OF ARSENIC BY ICP-OES WITH CONCOMITANT METALS ANALYSER
(CMA) – AN ASSESSMENT.
Alok Pandey, G. S. Chowdary and Adarsh Kumar
Chemistry Laboratory,
Atomic Minerals Directorate for Exploration and Research,
Department of Atomic Energy
Northern Region, New Delhi-110 066
Abstract
Arsenic was determined by ICP-OES model JY2000(2) in combination with
Concomitant Metal Analyser (CMA) in order to assess its performance
and its actual utility. Water samples as well as rock samples were
analysed. CMA gives improvement in the signal (10-15 times), but it
depends on the oxidation state of arsenic . The efficiency of hydride
generation is not the same for Arsenic (III) and Arsenic (V) both in
acidic and in alkaline conditions. In acidic conditions the difference
is less. So presenting As in single form in samples similar to that
of the solution used for calibration is important for accurate analysis.
In the continuous generation of hydrides only a small portion of sample
enters the spray chamber. No pre-concentration of analyte from whole
of the sample is possible as in discrete hydride generators used with
atomic absorption spectrometers. For rock samples hydrochloric acid
concentration of hydride generator has to be increased to prevent precipitation
of hydroxides of concomitant elements in spray chamber.
Keywords:
Arsenic; Hydride generation; Sodium borohydride; Pre-concentration;
water
and rock samples
DETERMINATION OF NEPTUNIUM IN DISSOLVER SOLUTION OF
SPENT PHWR FUEL BY INDUCTIVELY COUPLED
PLASMA ATOMIC EMISSION SPECTROMETRY
1PREFRE
Plant, Nuclear Recycle Group, Bhabha Atomic Research Centre,Tarapur-401502 2Radiochemistry
Division, Bhabha Atomic Research Centre, Mumbai-400085
Abstract
A method has
been standardized for the determination of Np in the dissolver solution
of the spent
PHWR fuel. The method involves the
quantitative separation of Np from the dissolver solution by solvent
extraction with 0.5 M thenoyltrifluoroacetone - xylene (TTA) and its
determination by ICP-AES after stripping Np from the organic phase
into the aqueous medium with 8M HNO3.
The reliability of the method is checked by standard addition technique.
The method is precise and
accurate yielding Np analytical recovery of 99.8 ±1%. The Np
concentration of dissolver solution of the spent PHWR fuel is found
to be in the range of 8- 10 mg/L.
DETERMINATION OF YTTRIUM, RARE EARTH ELEMENTS, ZIRCONIUM AND THORIUM
IN COMPLEX GEOLOGICAL SAMPLES BY ICP-OES
Beena Sunilkumar, G. S. Chowdary and Adarsh Kumar
Chemistry Laboratory, Atomic Minerals Directorate for Exploration
and Research,
Department of Atomic Energy
Northern Region, New Delhi-110 066
Abstract
Three methods of sample solution preparation for the determination
of yttrium, rare earth elements and thorium in complex geological samples
by ICP-OES using JY2000(2), were compared and assessed for their environmental
friendliness , ease of handling time required for the analysis.
Atomic Minerals Directorate for Exploration and Research
Department of Atomic Energy, Northern Region, New Delhi
Abstract
Gamma
ray logging of boreholes is a method of measuring naturally occuring
gamma radiation to characterize the rock or sediment in a
borehole. It is most commonly used for finding the grade and depthwise
extension of uranium anomaly located on the surface . Gamma-ray measurements
detect variations in the natural radioactivity originating from changes
in concentrations of the trace elements uranium (U) and thorium (Th)
as well as changes in concentration of the major rock forming element
potassium (K). Since the concentrations of these naturally occurring
radioelements vary between different rock types, natural gamma-ray
logging provides an important tool for lithologic mapping and stratigraphic
correlation, for detecting alteration zones. For example, in sedimentary
rocks, sandstones can be easily distinguished from shales due to the
low potassium content of the sandstones compared to the shales.
In
AMD, point-by-point logging method is used to determine eU3O8 concentration
up to 20 ppm level using scintillation dtecetor ( NaI(Tl) : 1/2” X 2” size).
However as the surface manifestations of uraniums deposits are becoming sparse,
a need is being felt that eU3O8 data
below 20 ppm is required for picking up alteration zones which will help
in conceptual geological modelling,
enabling
discovery of concealed uranium deposits.
The
authors have developed, designed and fabricated a new high sensitivity
logging probe which provides ppm eU3O8 data
at 3ppm level with a precision of 10%. The probe houses two NaI(Tl) detectors
(1/2” X 2”) connected head-to-head,
increasing both the detector and sample volume and thereby enhancing sensitivity
and accuracy. The highlight of the probe is its sensitivity of 8 cps / ppm
eU3O8.The
probe also provides better average grade of in-situ sample. The use of two
detectors provides the flexibility of variable sample volume which
can be further increased by increasing the detector separation. An additional
feature is a passive mixer electronic circuit used in connecting two detectors
to minimise the counting losses. This probe is well integrated with existing
logging equipment.
This paper describes the characteristics of high sensitivity logging probe
and the favourable results obtained with its use in some boreholes of Pisnari
prospect.
Keywords:
Gamma ray logging; Boreholes; eU3O8 ;
Rock samples
DEVELOPMENT
OF AN INDIGENOUS ECHELLE SPECTROMETER WITH PIXEL PROFILING FOR SIMULTANEOUS
SPECTRO-CHEMICAL ANALYSIS
D. V. Udupa, B. J. Shetty, N. Omana, P. B. Patil, Sanjiva Kumar and
Ajaya Kumar
Spectroscopy Division, Bhabha Atomic Research Centre, Mumbai 400 085
Abstract
An indigenously
developed echelle grating spectrometer has been used for simultaneous
analysis
of eight impurities in aluminium using an
ICP source of excitation. An improvement in the signal / background
ratio is observed when the analysis is carried out by profiling of
the lines, so as to get the pixel with the peak intensity on the CCD
every time before starting the analysis as compared to analysis without
profiling. The instrument uses a 2-D CCD detector for recording the
spectrum in the range of 2100 – 4000 Å with wavelength resolution
of 0.2 Å at 3000 Å.
ANALYTICAL INSTRUMENTATION FOR IN-SITU RADIOACTIVITY MEASUREMENTS
IN MINERAL EXPLORATION
S.Kannan* , C.V.R.Sarma
Atomic Minerals Directorate for Exploration and Research
Department of Atomic Energy, India
Abstract
Radioactivity measurement in boreholes, core and powder samples is
essential for exploration of radioactive minerals. With the recent
advancements in technology, the design of instrumentation for these
measurements resulted in miniaturization, low power consumptions and
additional user friendly features.
A Portable micro controller based Digital count rate meter was designed
and developed for gamma ray bore-hole logging employing Geiger Muller
/Scintillation detectors. The features of in-situ calibration and evaluation
of data resulted in quick and rapid logging of boreholes and processing
of data.
Instrumentation required for Radioactivity measurement of the borehole
core and powder samples were also designed, developed with similar
state of art technology employing microcontrollers for in-situ estimation
of results. The battery operated and portable Micro controller based
Core and radiometric analysis systems with storage memory acquires
and stores the data and display the evaluated results on panel mounted
alphanumeric Liquid Crystal display(LCD). Further the data may be retrieved
and downloaded to a computer for further analysis. In-situ printing
of data without the additional requirement of personal Computer would
assist the geoscientist in quick evaluation of results for further
interpretation.
The above Instrumentation was successfully deployed at several field
areas in the country for radioactive mineral exploration program of
Atomic Minerals Directorate.
The present paper describes the design and fabrication details, software
modules developed for the above Instrumentation.
WAVELENGTH
DISPERSIVE X-RAY FLUORESCENCE VIS-À-VIS INDUCTIVELY
COUPLED PLASMA- OPTICAL EMISSION SPECTROMETRY OF MAJOR AND TRACE ELEMENTS
IN SILICATE ROCKS
Chanchal Sarbajna, Smeer Durani, V.Rajagopalan and D.S.R.Murthy
Atomic Minerals
Directorate for Exploration & Research
Department of Atomic Energy
1-10-153, Begumpet, Hyderabad-500629, A.P.
Abstract
A simple, precise, accurate and rapid technique is described for
the analysis of major (Na, Mg, Al, Si, K, Ca and Fe, P, Ti and
Mn) and selected trace elements
(V, Cr, Co, Ni, Cu, Zn, Ga, Rb, Sr, Y, Zr, Nb, Ba, Pb, Ce, U and Th) by WDXRFS
and ICP-OES techniques in geo-materials, especially silicate rocks. The state
of art MagiX-PRO Wavelength Dispersive X-ray Fluorescence Spectrometer and
ULTIMA-2 Inductively Coupled Plasma- Optical Emission Spectrometer have been
used in the present study as an indispensable geo-analytical tool for the
analysis of major and selected trace elements at ppm to percentage
level, with high
precision and relatively better accuracy. However, the more thrust is being
laid in developing an analytical methodology that gives a user friendly procedure
with the availability of integrated software and matrix interference algorithms.
The standard reference material (G-2) was analyzed following the method developed
by both the techniques and the results obtained are in good agreement with
the recommended values. The relative accuracy and precision of both the proposed
methods are excellent for most of the elements.
Keywords:
Wavelength dispersive X-ray fluorescence; ICP-OES; Major and trace
elements;
Silicate rocks
WAVELENGTH-DISPERSIVE X-RAY FLUORESCENCE SPECTROMETRIC DETERMINATION
OF SOME RARE-EARTH ELEMENTS IN COLUMBITE-TANTALITE USING THEIR K-SPECTRA
AND AN LiF 420 ANALYSING CRYSTAL
B.N. Tikoo*, Anjan Chaki+, Yamuna Singh, and S. Viswanathan
Atomic Minerals Directorate for Exploration and Research, Department
of AtomicEnergy,
Government of India, 1-10-153-156, Begumpet, Hyderabad-500 016,
India
amdhyd@ap.nic.in
Abstract
The paper proposes a simple, accurate, precise, rapid, and non-destructive
unconventional wavelength-dispersive x-ray fluorescence spectrometric
technique for determining Ce, Nd, Sm, and Gd in rare-earth element
(REE) concentrates chemically extracted from columbite-tantalite.
The method uses the K x-ray spectra of Ce, Nd, Sm, and Gd and
an LiF 420
analysing crystal to overcome the problems inherent in the conventional
method which uses their complex L x-ray spectra with troublesome
spectral-line coincidences and overlaps.
In
the present method the achievable coefficient of variations (n =
4) in an admixture containing the elements at the specified
levels
respectively. The coefficient of variation obtained in the case
of Ce, Nd, Sm and Gd respectively is 6.7, 7.6, 3.2, and 3% in
analysing four synthetic samples containing Ce, Nd, Sm and Gd respectively
955,
488, 3929 and 1002 µg/g. The precision is excellent (within
3% for Gd and within 3.2% for Sm) and very good (within 6.7%
for Ce and
within 7.6% for Nd).
For a single analysis total time taken for determining Ce, Nd,
Sm, and Gd in a batch of twentyfour samples, in quadruplicate using
a manual spectrometer
is twenty hours.
AN X-RAY DIFFRACTION STUDY OF URANINITE FROM
THE KARIMNAGAR GRANULITE BELT, ANDHRA PRADESH, INDIA,
WITH ANOMALOUS UNIT-CELL DIMENSION
R. Viswanathan, Yamuna Singh, M. Sai Baba, Anjan Som, K.
Shiv Kumar, and K. Umamaheswar
Atomic Minerals Directorate for Exploration and Research,
Department of Atomic Energy, Begumpet, Hyderabad-500 016
Abstract
The
paper presents the results of an x-ray diffraction (XRD) study of
uraninite from
the
Karimnagar granulite belt (KGB) of Andhra Pradesh,
with its compositional characteristics. It is observed that the unit-cell
parameter (a0 =
5.4729Å) of uraninite in the granulite is higher
than the value (a0 =
5.4682Å) given in ICDD Card No. 5-550 for
uraninite standard. This unit-cell size of the investigated uraninite
in the granulite is even higher than the ideal unit-cell size of 5.4700Å given
for uraninite. Therefore, the unit-cell size of the investigated uraninite
belongs to the category of anomalous unit-cell size. The anomalous
unit-cell dimension (a0 =
5.4729Å) of the investigated uraninite
from the granulite of the KGB, as against the reference value of 5.4682Å,
is interpreted to be due to extensive substitution of U by Th. This
interpretation is supported by the fact that the uraninites from the
granulite of the KGB contain high amounts of thorium (5.99-7.12% ThO2;
av. 6.62% ThO2).
Furthermore, extensive substitution of U by Th has also resulted in
low contents of U (53.16-59.62% UO2,
av. 56.23% UO2)
in uraninite. In contrast, the unit-cell parameter (a0 =
5.4658Å)
of uraninite from the gneiss, with its oxygen content in the formula-unit
(FU), i.e., UO2.04,
is nearly the same as given in ICDD Card No. 5-550 for uraninite standard
(a0 =
5.4682Å; FU = UO2.03).
The normal unit-cell dimension of uraninite from the gneiss is due
to its low
thorium (0.10% ThO2)
and REE (0.94%) contents.
SPECTROPHOTOMETRIC DETERMINATION OF NITROGEN IN NIOBIUM METAL
A.Narsing Rao, K. Madhava Krishna, Vijaya Ram Mohan and R.B. Yadav
Control Laboratory, Nuclear Fuel Complex,
ECIL Post, Hyderabad 500 062
rby@nfc.gov.in
Abstract
This paper describes the analytical procedure for the spectrophotometric
determination of trace quantities of nitrogen in niobium metal that
finds extensive application as strategic material in nuclear and space
industries.
The method entails boiling a known quantity of sample with concentrated
sulphuric acid in the presence of potassium sulphate and copper sulphate.
After the mineralisation, the acidic solution is carefully diluted
with water and made alkaline with excess of sodium hydroxide during
which ammonia is generated. This is steam distilled and collected as
the condensate. When Nessler’s reagent is added to the distillate,
a brownish yellow complex is formed that has the maximum absorbance
at 400 nm thus facilitating its quantification by photometric measurement.
The results obtained have been compared with that obtained by nitrogen
analyzer (inert gas fusion coupled with thermal conductivity measurement)
and the values are found to be in good agreement.
Replicate analysis performed on the sample gave a RSD of ± 10% at 100
ppm level.
Keywords:
Determination; Nitrogen; Spectrophotometry; Nessler’s reagent; Niobium
metal samples
STANDARDIZATION OF A PARTICLE INDUCED GAMMA RAY EMISSION (PIGE) METHOD
FOR FLUORINE DETERMINATION AT FOTIA, BARC AND ITS APPLICATION TO
BOROSILICATE GLASS SAMPLES
R. Acharya1*,
R. Tripathi1,
K. Sudarshan1,
A.V.R. Reddy1,
R. G. Thomas2,
S. Santra2,
S.K. Gupta2,
R.K. Choudhury2,
R.K. Mishra3,
V.G. Katarni3,
C.P. Kaushik3
1Radiochemistry Division, 2Nuclear
Physics Division, 3Waste
Management Division Bhabha Atomic Research Centre, Trombay, Mumbai 400 085
racharya@barc.gov.in
Abstract
A
particle induced gamma ray emission (PIGE) method has been standardized
to determine fluorine non-destructively in percentage to trace concentrations
using proton beam of 4 MeV at FOTIA, BARC. Samples of NaF mixed with
cellulose were palletized and used to obtain calibration plot for F.
The method was validated by determining F in synthetic samples and
then applied to determine F in barium borosilicate glass samples, which
was otherwise difficult by other analytical techniques. Irradiation
times were kept in the range of 30 min – 5 h depending on F concentrations.
The current was monitored using a thin gold foil. The prompt gamma
rays of 110 and 197 keV from 19F(p, p'gamma)19F
reaction, measured by a high resolution gamma ray spectrometer, were
used for calculation of
F concentrations. The measured F concentrations in four borosilicate
glass samples were in the range of 0.6-4 wt%. Detection limit for fluorine
in the present experiments was 60 mg kg-1 using 197 keV gamma-ray.
DETERMINATION OF TRACE AMOUNTS OF BORON
IN GRAPHITE USING ICP-AES
G.A.Tambe, K. Venkatesh and P.V. Ravindran
Analytical Chemistry Division,
Bhabha Atomic Research Centre, Trombay, Mumbai-85
Abstract
Determination of trace amounts of boron was carried out in graphite
powder samples using ICP-AES. The possible loss of boron during the
sample dissolution stage was overcome by fixing boron as barium borate.
Analytical parameters were optimized for quantitative recovery of boron
from the sample matrix. Over triplicate analyses, the co-efficient
of variation was found to be ±6%. This method was adopted for the routine
analysis of graphite samples for the boron content.
DETERMINATION
OF 10B-ENRICHMENT
IN THE CaF2-BF3 COMPLEX
PREPARED BY HEAVY WATER BOARD, DAE
A.M. Shaikh, S.S. Desai and M. Padalakshmi
Solid State Physics Division,
Bhabha Atomic Research Centre, Mumbai 400 085, India
shaikham@barc.gov.in
Abstract
The paper gives detailed account of generation of BF3 gas
by thermal decomposition of CaF2-BF3 complex
prepared by Heavy Water Board(HWB) and its purification. The BF3 gas
obtained is used for making neutron detectors and various tests are
carried out to check its performance.
The 10B-enrichment in the complex is determined by comparing the
performance of this neutron detector with that made using gas from
imported complex with 10B-enrichment of 93 ± 1 %. The 10B-enrichment
in HWB complex is estimated to 89 ± 2 %.
APPLICATION OF GAS CHROMATOGRAPHY IN GEOCHEMICAL PROSPECTING OF HYDROCARBONS
T. Madhavi, G. Kalpana, M. Lakshmi and A.M. Dayal
National Geophysical Research Institute
(Council of Scientific and Industrial research)
Uppal Road, Hyderabad-500606
madhavit19@gmail.com
Abstract
Gas Chromatography
is employed for adsorbed soil gas analyses of light gaseous hydrocarbons
which
serve as direct indicators in surface geochemical
prospecting of hydrocarbons. Light gaseous hydrocarbons from the subsurface
oil and natural gas reservoirs seep to the surface soils through the
process of diffusion, effusion & buoyancy and get adsorbed to the
soil particles. These hydrocarbons are desorbed from the soil particles
by acid extraction and measured by Gas Chromatograph-Flame Ionization
Detector (GC-FID). The concentrations of the hydrocarbons are subjected
to statistical evaluation which gives information on anomalous hydrocarbon
zones, origin of the gases and oil & gas association of the area.
This paper presents the results of adsorbed soil gas survey conducted
in part of Cuddapah Basin.
Keywords: Gas Chromatography; Geochemical prospecting; Hydrocarbons
APPLICATION OF GC-C-IRMS IN GEOCHEMICAL EXPLORATION OF HYDROCARBONS
Anu Radha .B*., Srinu. D., Patil. D. J. and Dayal.A.M.
National Geophysical Research Institute
(Council of Scientific & Industrial Research),
Hyderabad-500 606.
*annnudin@gmail.com
Abstract
Geochemical exploration for hydrocarbons is a search for chemically
identifiable surface or near-surface occurrences of hydrocarbons, which
serve as clues to the location of undiscovered oil and gas accumulations.
Surface geochemical methods assume that hydrocarbons generated and
trapped at depth leak in varying and detectable quantities to the surface.
Geochemical exploration techniques can be direct or indirect. In indirect
techniques seepage-induced changes in soil, sediment or vegetation
are studied. In direct techniques small quantities of hydrocarbons
that occur in pore space of soil, is desorbed and injected in to a
Gas Chromatograph – Combustion interface coupled with IRMS. This facilitates
the analysis of even the minute amount of sample, typically of the
order of 1nmole.
Analytical Chemistry Division, Bhabha Atomic Research Centre,
Mumbai 400085, India.
Abstract
An
effort is made to adopt methods to determine elements like C, H,
N, S and O in organics
and
organometallic samples. Simultaneous analysis
of C, H, N and S in solid as well as liquid samples by using milligram
size samples has been carried out using established technique. Samples
are subjected to high temperature in presence of oxygen and the gases
formed after oxidation and reduction processes are separated and determined.
Introducing vertical sample loading and coupling of combustion gas
chromatography could make determinations faster compared to classical
methods. Introduction of micro TCD made the determinations more sensitive.
On the other hand Oxygen in samples were determined in a separate run
by pyrolysis. Over the last two-years, about 200 samples have been
analyzed. Statistical analysis of data showed that the method is reliable.
Considering 3sigma of blank, 21µg is detectable. However, due
to weighing difficulties, 100µg is taken as the detection limit.
Keywords:
Determination; C, H, N, S and O elements; Organic and Organometallic
samples;
Thermal conductivity
LIQUID-LIQUID EXTRACTION AND SPECTROPHOTOMETRIC DETERMINATION OF SCANDIUM(III)
WITH HEXAACETATO
CALIX(6)ARENE
C. M. Swamidoss1,
S. M. Khopkar2,
D. D. Malkhede3
1Department of Chemistry, Sant Gadge Baba Amravati University, India, 2Indian Institute of Technology, Mumbai, India, 3Department of Chemistry, University of Pune, India.
Abstract
A
method is proposed for the extraction of Scandium(III) using Hexaacetato
Calix(6)arene. The optimum extraction conditions are evaluated from
a critical study of the effect of pH, concentration of extractant,
shaking time, concentration of various mineral acids used as stripping
agents, different types of polar and non polar diluents and effect
of diverse ions. Solvent extraction of Scandium(III) was carried out
using Hexaacetato Calix(6)arene in Toluene. Scandium(III) is quantitatively
extracted with 1 x 10-4 M
of the ligand in Toluene at pH 5 when equilibrated for 12 minutes.
Scandium in the organic phase was stripped with 1 M
Nitric acid and determined spectrophotometrically by the Arsenazo(III)
method at 675 nm. The metal loading capacity of the reagents is also
studied. The extraction of Sc(III) was carried out in the presence
of various ions to ascertain the tolerance limit of individual ions.
The method can be extended for the determination of Scandium in real
samples.
DETERMINATION OF TITANIUM IN SPECIAL STEELS BY FLAME ATOMIC ABSORPTION
SPECTROMETRY
S. Raju, Y. Balaji Rao* and R.B. Yadav
Control Laboratory, Nuclear Fuel Complex,
Dept.
of Atomic Energy, Govt. of India, ECIL Post, Hyderabad 500062
ybr@nfc.gov.in
Abstract
The
present paper describes a FlameAtomic Absorption Spectrometric method
for the determination of Ti in various grades of special stainless
steels
like SS-321,
D-9, Oxide
Dispersed strengthened steel (ODS), SS-316 Ti, etc. The samples are
dissolved in aquaregia and Hydrofluoric acid. Ti Free SS-304 grade
samples solution is prepared for stock solution, from which matching
standards are prepared. The samples are analysed by AAS (Model GBC-902).
The absorbance is measured at 365.4 nm using reducing Nitrous Oxide-Acetylene
flame. The proposed method is compared with the earlier method (H2O2)
and found to be in excellent agreement. A relative standard deviation
of ± 5% has been achieved.
CHARACTERIZATION OF SELENIUM (IV) AND SELENIUM (VI) IN WATER SAMPLES
USING DIAMINOBENZIDINE AND ESTIMATION BY GRAPHITE FURNACE ATOMIC ABSORPTION
SPECTROSCOPY
Suvarna Sounderajan, G. Kiran Kumar, A.C.Udas*
Analytical Chemistry Division,
Bhabha Atomic Research Center,
Mumbai - 400 085.
Abstract
Selenium
(IV) is known to form stable yellow-colored piazselenol complex by
reaction of Se (IV) with 3, 3’-diaminobenzidine
hydrochloride (DAB),
which is then quantitatively extracted in organic solvent. . In
the present work stable yellow-colored piazselenol extracted in toluene
is used for quantification of Se (IV). Microwave digestion protocol
is optimized for converting selenium (VI) to selenium (IV) by digesting
samples with 4 M HCl. Total Se is then estimated. Concentration
of
Se (VI) in the sample solutions could be calculated by the difference
in total selenium and selenium (IV). The characterization of selenium
was carried out by GFAAS using Pd as modifier. The EPA permissible
level of Se (total) in water is 50 µg/L -1 as
a consequence the concentration of individual species is much lower.
Optimization of
the experimental conditions and instrumental parameters was investigated
in detail. Recoveries of (90-110%) were obtained in the spiked
samples. The detection limit was 1µg L-1,
and an enrichment factor of 20 was obtained. The proposed method
was successfully
applied
for
the determination of trace amounts of selenium (IV) and selenium
(VI) in
process water samples.
AN IMPROVED METHOD FOR ULTRA-TRACE DETERMINATION OF GOLD IN GEOLOGICAL
SAMPLES BY GRAPHITE FURNACE-ATOMIC ABSORPTION SPECTROPHOTOMETRY
S.K.Pradhan and P.K.Tarafder*
Regional Centre for Exploration and Research
Department of Atomic Energy
AMD Complex, Khasmahal
P.O. Tatanagar, Jamshedpur-831002, India
Abstract
A simple, precise, rapid and improved method is developed for the
ultra trace determination of gold in geological samples by Graphite
Furnace Atomic Absorption Spectrophotometry (GF-AAS). After aqua regia
treatment and hydrochloric acid digestion of the sample, gold passes
into solution along with other impurities. The metal is extracted into
MIBK (Methyl Iso-Butyl Ketone) and then stripped back into aqueous
phase with HBr. Gold is then determined by GF-AAS coupled with an auto
sampler. The RSD of this method is ± 10% at 10 ppb concentration level.
This method has been applied to various geological samples for gold
determinations.
SENSING OF SO2 GAS
IN BINARY MIXTURE WITH N2 GAS
USING ULTRASONIC GAS SENSOR AND ITS COMPARISON WITH OTHER STANDARD
METHODS
*J.C. Vyas 1,
A.M. Banerjee 2,
A.K. Tripathi 2,
K.A. Jadhav 3,
V. Nataraju 3,
and S.K. Gupta 1
1Technical
Physics & Prototype
Engineering Division, 2Chemistry
Division, 3Vacuum Physics and Instrumentation Division,
Bhabha Atomic Research Centre, Mumbai 400 085, India
vyas@barc.gov.in
Abstract
Quantitative determination of a given gas in mixed form with a
background gas has important applications for control and monitoring
of chemical
processes. SO2 gas
is a highly reactive gas used in several laboratory / industrial
processes and in particular it is used at an intermediate
step in some chemical methods for conversion of thermal energy
into chemical energy in the form of hydrogen. We measured composition
of this gas in binary mixtures with nitrogen as background, using
ultrasonic gas sensor (UGS). This sensor works non-invasively,
and
the gas concentration is determined by measurement of time of flight
(TOF) of ultra-sound. For calibration and testing of UGS, binary
gas mixtures were prepared by using rotameters, and gas compositions
were determined by UGS, and for comparison purpose by gas chromatography
and an indigenously fabricated mass spectrometer. The SO2 gas
mixtures in nitrogen were prepared in 0 – 10% (by volume) range,
and it
was found that the TOF has approximately linear dependence
with SO2 gas
concentration within the explored range. The SO2 gas
concentrations measured by UGS agreed well with results obtained
by gas chromatography.
However, the gas concentrations obtained by mass spectrometry differed
by a numerical multiplication factor. A tentative explanation for
this discrepancy has been provided.
Keywords: Ultrasonic gas sensor; SO2 gas;
Determination; Time of flight(TOF) of ultra-sound
*Corresponding
author
A REFRACTIVE INDEX BASED METHOD FOR ESTIMATION OF D2O
CONCENTRATION IN D2O-H2O
MIXTURES
Shekhar Kumar*, Pranay Kumar Sinha, Rajnish Kumar, D. Sivakumar, M.
Balamurugan, M. Samapth and S.B. Koganti
Reprocessing R&D
Division,
Indira Gandhi Centre for Atomic Research, Kalpakkam 603102.
*shekhar@igcar.gov.in
Abstract
Refractive index of pure D2O
and aqueous solutions of D2O
was determined experimentally. These experimental values were correlated
and an excellent
agreement between predicted and experimental values was observed. Based
on these results, one simple method (based on refractive index) is
proposed for estimating the D2O
content in the D2O-H2O
mixtures at 298.15 K.
SEQUENTIAL DETERMINATION OF FREE MAGNESIUM AND FREE ZIRCONIUM IN REDUCTION
RESIDUE BY GAS VOLUMETRIC METHOD
M. Koteshwar Rao, Vinay Buche, T. Amar Prakash,
Vijaya Ram Mohan and R.B.Yadav
Control Laboratory, Nuclear Fuel Complex,
ECIL Post, Hyderabad 500062
rby@nfc.gov.in
Abstract
This paper describes a simple and effective method for the sequential
determination of free magnesium (Mg) and free zirconium (Zr) in the
reduction residue generated in the Zirconium Sponge Plant during the
production of reactor grade zirconium sponge by the Kroll’s process.
As the residue cannot be recycled and being pyrophoric, the amount
of free Mg and free Zr in the sample is very vital for its safe disposal.
The proposed method involves the measurement of volume of hydrogen
gas generated by dissolution of known quantity of sample in HCl and
HF added in succession.
A relative standard deviation of ± 5% is obtained at less than 0.5%
concentration of the analytes.
Keywords: Determination; Magnesium; Zirconium; Gas Volumetric method
HIGHLY SENSITIVE, SIMPLE AND COST-EFFECTIVE
ANALYTICAL INSTRUMENTAL METHOD FOR THE DETERMINATION OF SELENIUM IN
ENVIRONMENTAL SAMPLES
B.P. Dayananda and T.N. Kiran Kumar
Department of Chemistry (PG), Maharani’s Science College for Women,
JLB Road, Mysore 570 005, Karnataka State
Abstract
Highly sensitive and simple spectrophotmetric determination of
selenium is described for the determination of selenium(IV)
using a new reagent
Safranine-O. The method is based on the reaction of selenium with
potassium iodide in an acid medium to liberate iodine. The liberated
iodine bleaches the color of safranine-O and cause decrease in
absorbance at 532 nm. This decrease in absorbance is directly
proportional to
selenium concentration obeying Beer’s law in the range 0.5 – 5.0 µg
of Se in a final volume of 10 mL. The molar absorption coefficient
and Sandell’s sensitivity of the method were found to be 8.21 '
104 L mol-1 cm-1 and
0.001 µg cm-2,
respectively. The proposed analytical procedure has been successfully
applied to the determination
of selenium in real samples of water, soil, and plant material.
The results were compared to those obtained with the reference
method.
Statistical analysis of the results confirms the precision and
accuracy of the proposed method. In addition, the developed method
is cost-effective
and involves easily accessible instrumentation technique which
can be used by ordinary research laboratories.
NEW
IMPROVED SYSTEM FOR IN-SITU PRE-CONCENTRATION OF 137Cs
IN COASTAL MARINE ENVIRONMENT
M. B. Pote#;
P. Lenka, S. Sartandel, S. Gothankar, S. Bara,
S. K. Jha*, V. D. Puranik
Environmental Assessment Division
Bhabha Atomic Research Centre, Mumbai #mbpote@barc.gov.in; *skjha@barc.gov.in
Abstract
A new improved system was designed, fabricated and used in evaluating
the 137Cs fallout activity around the coastal environment of Gujarat.
This system allows rapid in-situ pre-concentration from large volume
of sea water samples and is based on copper ferrocyanide [Cu2Fe(CN)6]
coated ion-exchanger resin. The 90-95% recovery was observed, using
dual cartridge exchanger, by passing 1000 liters of seawater at the
flow rate of 15 liters/min. Considering the constrain experienced in
the field experiment, the system was modified to incorporate new features
in order to precisely measure 137Cs
fallout activity in coastal marine environment. Environmental Assessment
Division at present engaged in
establishing the baseline data on fallout 137Cs
in coastal marine environment of India. Recently the system was used
to measure the activity at three
different locations in coastal region of Gujarat and the data presented
here.
Keywords: Preconcentration; 137Cs; Marine environment; Copper ferrocyanide;
Ion exchanger
SIGNIFICANCE OF ANALYTICAL CHEMISTRY AND PRODUCT CHARACTERIZATION TECHNIQUES
IN NUCLEAR WASTE MANAGEMENT
S.Rajasekaran1,
A.S.Pente2,
M.Ramchandran2,
C.P.Kaushik2*
and Kanwar Raj2
1Waste
Immobilization Plant, Nuclear Recycle Group Projects, Kalpakkam 2Waste
Immobilization Plant, Waste Management Division, Nuclear Recycle Group
Bhabha Atomic Research Centre, Mumbai
cpk@barc.gov.in
Abstract
Analytical chemistry
plays a vital role in day-to-day activities at radioactive waste
management
plants by way of meeting the requirements
pertinent to process realization, troubleshooting and relevant research & development.
Successful implementation of scientific activities depends upon the
support of a variety of chemistry disciplines like radiochemistry,
radiation chemistry, analytical chemistry, materials chemistry, separation
chemistry, geochemistry, etc. Present paper highlights the importance
of analytical chemistry and product characterization techniques deployed
in waste management plants. An attempt has been made to summarize the
contribution of compositional characterization of raw materials, nuclear
waste, process streams and plant products as well as in process control
and troubleshooting areas.
Keywords: Waste management; Characterization of materials; Nuclear
waste
*Corresponding
Author
Pb-Pb STEPWISE LEACHING TECHNIQUE: A RELIABLE
GEOCHRONOMETER FOR VARIOUS ROCKS AND MINERALS.
Veena Krishna, B.K.Pandey, D.V.L.N. Sastry
Geochronology Laboratory, Atomic Minerals Directorate for Exploration
and Research, Department of Atomic Energy, Govt. of India, Begumpet, Hyderabad-500629.
Abstract
The Lead Stepwise Leaching (PbSL) procedure has been applied successfully
to date a variety of rock forming minerals. Stepwise leaching aids
in the selective extraction of radiogenic and common lead in successive
stages, which make it possible to obtain age information from a single
phase of the sample. This paper gives a brief account of its application
to different minerals and rock types. It also discusses the application
of this procedure to the dating of banded hematite quartzites from
the Morar formation, Gwalior
Keywords: Geochronometer; Leaching; Radiogenic; Lead
AN OVERVIEW OF THE THERMAL IONIZATION MASS SPECTROMETRY (TIMS) PRESENT
STATUS AND FUTURE PROSPECTS.
B.K.Pandey, Veena Krishna, U.K.Pandey, D.V.L.N. Sastry and Girija
Srinivasan
The TIMS instrument is used for geochronological studies which require
a very precise determination of isotopic composition of elements
like Sr, Nd and Pb. During seventies work was carried out using indigenously
developed instruments and a number of age determinations by Rb-Sr
and U-Pb methods were carried out. Later a modern TIMS, VG354, was
imported and installed in March 1984. This instrument was capable
of accurate isotopic analyses with precision better than 0.003% for
Sr and Nd. During the past 25 years the VG354 TIMS has been used
extensively for a number of age determination studies. Some typical
applications are described briefly. The first ever Sm-Nd age determination
in an Indian laboratory was made on the soda granites of Singhbhum
which yielded depleted mantle model age of around 2.5 Ga. Looking
at the future needs for more precise isotopic measurements of presently
established procedures and also to introduce new techniques of dating
such as Re-Os and U-series disequilibrium dating, a TIMS instrument
with advanced features is under fabrication at the Vacuum and Prototype
Instrumentation Division, BARC, Mumbai.
Keywords:
Thermal ionization mass spectrometry (TIMS); Geochronological;
isotopic;
Singhbhum
VOLTAMMETRIC ANALYSIS OF SCORODITE MINERAL
P.K.Tamrakar and A.K.Sarangi
Uranium Corporation of India Limited
Jaduguda-832 102, Distt. East Singhbhum (Jharkhand)
pk_tamrakar@rediffmail.com
Abstract
Electroanalytical
method i.e. Differential pulse polarography (DPP) and Differential
pulse anodic stripping Voltammetry (DPASV) were developed
for the trace determination of osmium and other metals in scorodite
mineral samples. The analysis of trace metals was performed in two
different supporting electrolytes viz. 0.1M (NH4)2 tartrate
and 0.1M HCl. The results indicated the presence of Tl+, Sb3+,
Zn2+,
Os8+ and
As3+ in
the sample. The method of standard addition was used for quantitative
analysis. The accuracy of the methods was verified by comparing the
observed results with those obtained using atomic absorption spectrometric(AAS)
technique.
APPLICATION OF SPECTROSCOPIC TECHNIQUES FOR IDENTIFICATION OF MINERALS
FROM THE BEACH ROCKS OF TAMILNADU, INDIA
R.Ravisankar
Department of Physics, SSN College of Engineering,
Kalavakkam- 603110,Tamilnadu, India
Abstract
Beach rock is a peculiar type of formation when compared to other
types of rock formations. It needs intensive and extensive investigation
on its formation. Beach rock samples were collected from a vast area
extending from Rameswaram to Kanyakumari of South East Coast of Tamilnadu
and were subjected to spectroscopic studies. The qualitative identification
of the minerals in beach rock samples were carried out by using FT-IR
and XRD techniques. The infrared study on these beach rocks was found
to be highly useful in identifying the various minerals in beach rocks.
The minerals present in beach rocks were further confirmed by the X-ray
diffraction(XRD) technique. Results are discussed and conclusion is
drawn.
Keywords: Beach Rock; Mineral Analysis; FT-IR; XRD techniques
METHOD
DEVELOPMENT FOR THE CHEMICAL CHARACTERIZATION OF Ni, Mn, Ga, A
MAGNETO-CALORIC EFFECT MATERIAL
S. S. Kalyan Kamal*, J. Vimala, P. K. Sahoo, P. Bhasker Rao and L.
Durai
In this report a method development procedure for the analysis of a
new magnetocaloric effect material (NiMnGa) using Inductively Coupled
Plasma Optical Emission Spectrometry (ICP-OES) is discussed. The process
of method validation was carried out using various analytical techniques
like conventional wet chemical techniques and instrumental techniques
such as Atomic Absorption Spectrometry (AAS), and Electron Probe Micro
Analyzer (EPMA). All the techniques show a close agreement in values,
thus this method could be applied for regular analysis of NiMnGa alloys.
Keywords: Chemical characterization; ICP-OES; NiMnGa alloys.
*corresponding author
INAA FOR TRANSPORT OF METAL IONS FROM SIMULATED HIGH LEVEL WASTE ACROSS
HOLLOW FIBER SUPPORTED LIQUID MEMBRANE
D.R. Raut, R. Acharya, P.K. Mohapatra and V.K. Manchanda*
Radiochemistry Division, Bhabha Atomic Research Centre,
Trombay, Mumbai-400085
*vkm@barc.gov.in
Abstract
Transport behaviour of metal ions (including lanthanides) from Simulated
High Level Waste (SHLW) of PHWR (Pressurized Heavy Water Reactor) was
investigated using hollow fiber supported liquid membrane (HFSLM) containing
0.1M TODGA + 0.5M DHOA in NPH as the carrier. Elemental concentrations
were determined by Instrumental Neutron Activation Analysis (INAA)
which involves irradiation of samples using nuclear reactors and radioactive
assay using high resolution gamma spectrometry. The % transport for
both unirradiated and irradiated TODGA samples was obtained. The %
transport of elements viz. La, Ce, Sm, Cr, Ba, Mo and Cs were determined
by INAA and compared with that obtained earlier by ICP-AES technique.
QUANTITATIVE
ELECTRON PROBE MICRO ANALYSIS OF URANIUM MINERALS IN PROTEROZOIC
QUARTZITES AND BASAL GRANITOIDS OF DAMARCHERLA AREA, PALNADU SUB-BASIN
OF CUDDAPAH BASIN, NALGONDA DISTRICT, ANDHRA PRADESH, INDIA
V.Rajagopalan,
A.K.Paul, S.V.S.Reddy and H.K.Sabot
Atomic
Minerals Directorate for Exploration & Research
Department of Atomic Energy, Government of India
1-10-153, Begumpet, Hyderabad-500629, A.P.India
Abstract
The
representative borehole core and grab samples comprising quartzites
of the Proterozoic Palnad basin (PPB) and basement granitoids from
Damarcherla and adjoining areas of Andhra Pradesh in southern Peninsular
India are investigated for knowing the nature of uranium mineralisation.
The quartzites over the unconformity and dominantly the basal granitoids,
with few variants, form the mineralized horizon in the area. the
mineralized host lithounits essentially contain a number of primary
and secondary uranium minerals besides other associated phases like
monazite, zircon and pyrite. The radioactive phases, mainly different
uranium phases, after identification under back scattered electron
imaging and supplemented by the optical microscopy, were spectrally
scanned and qualitatively investigated for a number of major and
minor elements. Selected probe compatible grains were quantitatively
analyzed by electron micro probe, using a number of EPMA standards,
for U, Th, Pb, Ca, Ti, Mn, Fe, Al, Si, P, Y, La, Ce, Pr, Nd, Sm,
Gd, Tb, dy, Ho, Er, Tm, Yb, Lu and Lu and computed as respective
oxides. Thus, the radioactive phases, essentially as discrete grains
of varying shape and size, were analyzed.
The
accrued multi-elemental analytical data has been mineralo-chemically
sifted, synthesized and finally characterized as uraninite, pitchblende,
coffinite, kasolite, autunite and U-Si (tending towards coffinite),
U-Si-Ti, U-Pb-Si complexes. Most of the identified uranium phases,
excluding uraninite and kasolite are occurring as veins, cavity/fracture/grain
boundary fillings. The secondary phases invariably occur as smear
on phenocrysts of the granitoid. The varying mineral chemistry of
radioactive phases represent multi-phase and the physical occurrence
of discrete U-phases with associated petro-mineralogical and geochemical
characters throw light on multi-episodic radioactive mineralization
in the host rock domain. Detailed study on spatially distributed
radioactive and non-radioactive core samples shall reveal the mineralogical
and geochemical guides for uranium exploration in this part of the
country.
Key
words: Uranium, electron probe micro analysis, Quartzites, Granitoids
LARGE SAMPLE ANALYSIS OF COAL AND URANIUM ORE USING K0-BASED
INTERNAL MONO STANDARD NAA METHOD
R. Acharya1,
K. K. Swain2,
T. N. Newton1,
R. Tripathi1,
K. Sudarshan1,
P. K. Pujari1,
A. V. R. Reddy2*
Radiochemistry Division, *Analytical Chemistry Division,
Bhabha Atomic Research Centre, Trombay, Mumbai 400 085
*avreddy@barc.gov.in
Abstract
The k0-based internal mono standard neutron activation analysis (IM-NAA)
method was used to analyze larger size (20-32 g) samples of coal and
uranium ore. Samples were irradiated in the thermal column position
of the Apsara reactor. In order to arrive at representative sample
size, six small size samples (50-1000 mg) of coal were also irradiated
using core position of Apsara reactor. Using in-situ relative efficiency
elemental concentrations were determined by IM-NAA. The element Na
was used as the mono standard and IAEA RM SL-1 was used as the reference
standard.
NATURAL RADIOACTIVITY MEASUREMENT IN SEDIMENT SAMPLES IN AND AROUND
THARANGAMBADI, TAMILNADU
R.Ravisankar1,
A.Rajalakshmi1,
M.Suresh1,
A. Chandrasekaran1,
A.Senthilkumar2 V.Gajendiran3and
V.Meenakshisundaram3
1Department of Physics, SSN College of Engineering,
SSN Nagar, Kalavakkam - 603110, Tamilnadu, India 2Department
of physics, Thangavelu Engineering College,
Karapakkam, Chennai Tamilnadu 3Radiological Safety Division, Safety Group,
Indira Gandhi Centre for Atomic Research (IGCAR), Kalpakkam – 603102,
ravisankarr@ssn.edu.in
Abstract
Thorium
(232Th),
Uranium (238U)
and Potassium (40K)
concentration in sediment samples of Tharagambadi,
Tamilnadu is measured using NaI(Tl)
detector based gamma ray spectrometer. The specific activity for 232Th,
238U
and 40K
are in the range 119.92 to 860.64 Bq/kg 23.11 to 205.38 Bq/kg and 186.44
to 644.52 Bq/kg respectively. The measured activity
concentrations for these radionuclides were compared to world average
activity of soil. The average activity concentration of 232Th
and 238U
in the present study is 27.12 and 2.01 times higher than world median
value while the activity of 40K
is found to be lower. This increased activity level of U & Th might
be due to the coastal processes involving onshore and offshore movements
and the long shore currents
for the transportation of heavies in these places.
Keywords: Natural Radioactivity; Gamma ray Spectrometer; Sediment
samples.
GEO-MICROBIAL PROSPECTING STUDIES OF SURFACE SEDIMENT FROM PETROLIFEROUS
REGION OF THE MEHSANA BLOCK,
NORTH CAMBAY BASIN, INDIA
Rasheed, M.A*. Veena Prasanna, M. Kalpana, G. Patil, D.J. and Dayal
A.M.
Microbiology Laboratory, Surface Geochemical Prospecting of Hydrocarbons
Division, National Geophysical Research Institute
(Council of Scientific & Industrial Research), Hyderabad- 500 606
*rasheedmicro@rediffmail.com
Abstract
Geo-microbial prospecting studies has been carried out to test its
efficacy as surface geochemical methods as regional evaluation tools
in petroliferous region of the Mehsana block, North Cambay Basin and
to investigate whether the geo-microbial anomalies that can establish
an upward migration of hydrocarbons from the deep subsurface source
on correlation with adsorbed soil gas method. A set of 135 sub-soil
samples collected, were analyzed for indicator hydrocarbon oxidizing
bacteria and adsorbed light gaseous hydrocarbons. The microbial prospecting
studies showed the presence of high population of propane oxidizing
bacteria in soil samples. The microbial prospecting studies carried
out in existing Oil and Gas fields of Mehasana, Cambay basin, Gujarat
showed high concentrations of propane oxidizing bacteria in the soils.
This paper reports the results of microbial prospecting studies, adsorbed
light gaseous hydrocarbon analysis of samples collected over petroliferous
region of the Mahesana block, north Cambay basin. The aim of the present
work is to define the geo-microbial signatures, and to investigate
whether the geo-microbial anomalies that can establish an upward migration
of hydrocarbons from the deep subsurface source on correlation with
adsorbed soil gas method over oil and gas proven areas.