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dc.contributor.authorShirodkar, P.V.
dc.contributor.authorYingkai, X.
dc.date.accessioned2009-01-12T09:08:30Z
dc.date.available2009-01-12T09:08:30Z
dc.date.issued1997
dc.identifier.citationCurrent Science, Vol.72; 74-77p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/2035
dc.description.abstractThe abundance and isotopic compositions of boron in sediments from the salt lakes of Qaidam Basin, China have been determined by thermal ionization mass spectrometry of cesium borate. The results show large variations in the isotopic compositions of boron. The observed variations of delta sup(11)B, ranging from - 25.2 ppt to + 26.08 ppt (relative to NBS SRM 951) indicate both an enrichment and depletion in the lighter isotope (sup(11)B) in the lake sediments. The lower delta sup(11)B values of sediments are mostly closer to the boron isotopic composition of minerals. Such low delta sup(11)B values are attributed to the presence of borates, ulexite and other carbonate minerals in sediments of the salt lakes of Qaidam Basin.
dc.language.isoen
dc.publisherCurrent Science Association, Bangalore
dc.rightsCopyright [1997]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectboron
dc.subjectisotopes
dc.subjectsediments
dc.subjectanalytical techniques
dc.subjectdepletion
dc.subjectcarbonate minerals
dc.titleIsotopic compositions of boron in sediments and their implications
dc.typeJournal Article


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