2014
DOI: 10.1007/s40010-014-0181-1
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Hydrogeochemistry of Meltwater of the Chaturangi Glacier, Garhwal Himalaya, India

Abstract: A hydrochemical analysis of meltwater draining from Chaturangi glacier was conducted to determine the dissolved ions chemistry and to evaluate the geochemical processes controlling major ions chemistry of the study area. Ca 2? , Mg 2? and SO 4 2-are the dominant ions in the glacier meltwater. The ratio of (Ca ? Mg) versus TZ ? varied from 0.79 to 0.86 with an average value of 0.82 ± 0.02 indicating larger contribution of Ca and Mg to the total cations. (Ca ? Mg)/(Na ? K) ratio is also high, varying from 3.77 t… Show more

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Cited by 11 publications
(8 citation statements)
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“…Also, evaporite dissolution is small in glacierised basin in the Himalaya comparing to CD and sulphide oxidation (e.g. Sharma and others, 2013; Singh and others, 2015a, b).…”
Section: Resultsmentioning
confidence: 99%
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“…Also, evaporite dissolution is small in glacierised basin in the Himalaya comparing to CD and sulphide oxidation (e.g. Sharma and others, 2013; Singh and others, 2015a, b).…”
Section: Resultsmentioning
confidence: 99%
“…The Satopanth and Bhagirathi glaciers were sampled during the middle of the summer ablation period from 17 to 23 August 1989, and towards the end of the ablation period from 11 to 19 October 1991 (Chauhan and Hasnain, 1993). Sampling of meltwater at the Bara Shigri glacier was carried out during the ablation period of July and September 2012 and from August to September 2013 (Singh and others, 2015a; b). The Chaturangi glacier meltwater was sampled during August and September 2008 (Singh and others, 2015b).…”
Section: Methodsmentioning
confidence: 99%
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