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• W23257013 abstract "The east central Sierra Nevada received acid precipitation (pH 3.7 to 4.9) during convective storms interspersed through the dry season of 1981. Sulfuric acid contributed about twice the acidity of nitric acid. In contrast, late autumn, winter, and early spring snow (1981-1982) ranged in pH from 5.2 to 6.1 (mean 5.7) and had low ammonium, nitrate, and sulfate concentrations. As of 1981 most of the alpine lakes of the Sierra Nevada remain very weakly buffered, bicarbonate lakes that receive a small loading of acid precipitation and a large annual input of snowmelt uncontaminated by strong acids. If the acidity of the precipitation increases, the pH of the lakes will decrease rapidly because the lakes and their basins have extremely low buffer capacity especially when runoff peaks during snow melt. 27 references." @default.
• W23257013 created "2016-06-24" @default.
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• W23257013 date "1982-01-01" @default.
• W23257013 modified "2023-09-28" @default.
• W23257013 title "Acid precipitation and buffer capacity of lakes in the Sierra Nevada, California" @default.
• W23257013 hasPublicationYear "1982" @default.
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