2022
DOI: 10.1016/j.jhazmat.2022.129017
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Arsenic and uranium contamination of Orog Lake in the Valley of Gobi Lakes, Mongolia: Field evidence of conservative accumulation of U in an alkaline, closed-basin lake during evaporation

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Cited by 13 publications
(4 citation statements)
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“…After the removal of protein by 10% trifluoroacetic acid and centrifugation, the supernatant was passed through a 0.22-μm filter. The filtrate was used to measure the trace minerals in their plasma by inductively coupled plasma mass spectrometry (X7, Thermo Inc., Waltham, MA, USA) 50 .…”
Section: Methodsmentioning
confidence: 99%
“…After the removal of protein by 10% trifluoroacetic acid and centrifugation, the supernatant was passed through a 0.22-μm filter. The filtrate was used to measure the trace minerals in their plasma by inductively coupled plasma mass spectrometry (X7, Thermo Inc., Waltham, MA, USA) 50 .…”
Section: Methodsmentioning
confidence: 99%
“…Olgoy Lake (46°33′48″N, 100°6′29″E) is an alkaline lake at about 2100 m elevation in Mongolia, south of the Khangai Mountains, with a salinity of 1−2 g/kg and a pH of 9−10 (Figure 1). 4,13,20 Its average depth is about 1 m, and its surface area is about 1.55 km 2 . The lake has no permanent outlet, and inflowing streams form temporarily during the rainy season, typically from April to October.…”
Section: ■ Materials and Methodsmentioning
confidence: 99%
“…These observations possibly suggest that CO 2 can be absorbed into lake water and converted to carbonate mineral during evaporation in alkaline saline lakes. 20 To assess the applicability of carbonate formation in alkaline saline lakes to NETs, it is necessary to better understand the relationship between the water chemistry of alkaline saline lakes and the formation of authigenic carbonate minerals, for which a full understanding of carbonate mineral equilibria in solution is essential. The important authigenic carbonate minerals in alkaline saline lakes are MHC and AMC.…”
Section: ■ Introductionmentioning
confidence: 99%
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