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Featured researches published by M. S. Rathi.


X-Ray Spectrometry | 2000

Evaluation of energy‐dispersive x‐ray fluorescence spectrometry in the rapid analysis of silicate rocks using pressed powder pellets

N. K. Saini; P. K. Mukherjee; M. S. Rathi; P. P. Khanna

Energy-dispersive x-ray fluorescence (EDXRF) spectrometry was used for the analysis of silicate rocks using pressed powder pellets. It is observed that with this low-cost, simple and fast technique, trace elements such as V, Cr, Co, Ni, Cu, Zn, Ga, Pb, Th, Rb, Sr, U, Y, Zr and Nb can be determined along with 10 major oxides of Na, Mg, Al, Si, P, K, Ca, Ti, Mn and Fe with reasonably good accuracy and precision, depending upon the elemental abundance, analyte matrix and analytical conditions. Performance parameters such as minimum detection limit, accuracy and precision were estimated for these elements in silicate rocks under optimized analytical conditions. The technique is useful when a large number of samples are to be routinely analysed with sufficient accuracy and precision. Selection of operating parameters is discussed for the simultaneous analysis of several elements in a group. Copyright


Talanta | 1991

Determination of ten rare-earth elements and yttrium in silicate rocks by ICP—AES without separation and preconcentration

M. S. Rathi; P. P. Khanna; Pulok Kumar Mukherjee

Lanthanum, cerium, neodymium, samarium, europium, gadolinium, dysprosium, erbium, ytterbium, lutetium and yttrium have been determined in 8 international rock standards by inductively coupled plasma atomic emission spectrometry (ICP-AES) without prior ion-exchange separation and preconcentration. The results for La, Ce, Nd, Eu, Dy, Yb and Y were in good agreement with the reported values, whereas those for Sm, Gd, Er and Lu were less accurate. However, the results for Sm, Gd, Er and Lu can also be used for studies of petrogenesis.


Journal of Trace and Microprobe Techniques | 2002

Trace element estimation in soils: An appraisal of ED-XRF technique using group analysis scheme

N. K. Saini; P. K. Mukherjee; M. S. Rathi; P. P. Khanna; K. K. Purohit

ABSTRACT The nondestructive nature, easier sample preparation and simultaneous multi-element analysis capability of the Energy Dispersive X-ray Fluorescence (ED-XRF) Spectrometry, makes it an attractive technique for the elemental analysis of a wide range of materials. Optimised operating conditions enhance the detection efficiency and improve the minimum detection limits for several elements analysed in a group. The present study shows the performance of an ED-XRF system in analysing 15 important trace elements (V, Cr, Co, Ni, Cu, Zn, Ga, Pb, Th, Rb, U, Sr, Y, Zr, and Nb) in soils and sediment samples. These elements were divided into two groups and were analysed at different operating conditions suitably optimized for each group. The grouping of the elements was done keeping in view the optimum excitation and detection condition requirement for each group of elements. The medium-Z elements (V, Cr, Co, Ni, Cu, Zn, and Ga) were called as group “A” elements, while the rest were taken into group “B.” Well characterised soil and sediment reference samples were used to estimate the quality (precision and accuracy) of the analysis data produced by ED-XRF. Optimisation of the analysis procedure and achievable Minimum Detection Limits were studied. The analysis scheme may prove useful when a large number of soil and sediment samples are required to be analysed.


Talanta | 1983

Analytical applications of Zr(IV) and Ti(IV) arsenophosphates as ion-exchangers

K.G. Varshney; S. Agrawal; K. Varshney; A. Premedas; M. S. Rathi; P.P. Khanna

The distribution of 27 metal ions between zirconium and titanium arsenophosphate and demineralized water, perchloric acid and nitric acid has been studied. On the basis of the results, several binary and ternary separations can be designed. The data have been used in application of these materials to the analysis of certain alloys and rocks.


Journal of Trace and Microprobe Techniques | 2002

Trace element characteristics of a new silicate reference material from Himachal Himalaya (India)

P. K. Mukherjee; P. P. Khanna; M. S. Rathi; N. K. Saini; K. K. Purohit

ABSTRACT Geological rocks and soils involve complex matrix compositions and their characterization is very difficult. Analysis of trace elements in soils and other silicate rocks seriously suffer due to the lack of availability of suitable silicate reference materials. Environmentally sensitive elements are of particular concern. In this paper, we discuss the procedures for characterization of the 27 trace elemental abundance in a new silicate reference sample of granitic composition (named as DG-H). A total number of about 2500 units of data for more than 50 trace elements were received from as many as 44 laboratories. The element wise data sets were subjected to rigorous statistical treatment to identify the outliers and subsequent rejection. Rest of the data, called “qualified data,” are therefore, used to estimate five estimators of central tendency, robust, as well as non-robust, viz., Mean, Median, Geometric Mean, Gastwirth Median, and Trimean. The arithmetic mean, called Preferred Mean (PM) of the above five estimates is assigned as Working Value or Recommended Value. As many as 23 elements are assigned recommended values, whereas rest four elements are found marginally less characterized. This reference sample would benefit the potential analytical community engaged in analysis of trace elements silicate in materials like rocks and soils.


Journal of Geological Society of India | 1998

A New Geochemical Reference Sample of Granite (DG-H) from Dalhousie, Himachal Himalaya

N. K. Saini; P. K. Mukherjee; M. S. Rathi; P. P. Khanna; K. K. Purohit


Environmental Earth Sciences | 2001

Heavy metal distribution and environmental status of Doon Valley soils, Outer Himalaya, India

K. K. Purohit; P. K. Mukherjee; P. P. Khanna; N. K. Saini; M. S. Rathi


Geochemical Journal | 2007

A stream sediment geochemical survey of the Ganga River headwaters in the Garhwal Himalaya

P. K. Mukherjee; K. K. Purohit; N. K. Saini; P. P. Khanna; M. S. Rathi; A. E. Grosz


Journal of The Geological Society of India | 1998

Geochemistry and Petrogenesis of a Supracrustal Granite from Dalhousie, Himachal Himlaya

P. K. Mukherjee; K. K. Purohit; M. S. Rathi; P. P. Khanna


Journal of Geological Society of India | 1994

Working Values for Major, Minor and Trace Elements for Meta-Basic Reference Sample (MB-H)

M. S. Rathi; P. P. Khanna; P. K. Mukherjee; K. K. Purohit; N. K. Saini

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P. P. Khanna

Wadia Institute of Himalayan Geology

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P. K. Mukherjee

Wadia Institute of Himalayan Geology

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K. K. Purohit

Wadia Institute of Himalayan Geology

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N. K. Saini

Wadia Institute of Himalayan Geology

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A. Premedas

Aligarh Muslim University

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K. Varshney

Aligarh Muslim University

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K.G. Varshney

Aligarh Muslim University

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P.P. Khanna

Wadia Institute of Himalayan Geology

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Pulok Kumar Mukherjee

Wadia Institute of Himalayan Geology

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S. Agrawal

Aligarh Muslim University

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