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Extent of snowpack influence on water chemistry in a North Cascades lake

Journal Article · · Water Resour. Res.; (United States)
Integrated snowpack samples and lake water samples were collected from a low-alkalinity watershed in the North Cascades in 1984 and 1985 and analyzed for inorganic chemical parameters. Mean concentrations of NO/sub 3//sup -/ and SO/sub 4//sup -2/ from North Cascades snowpack were near 4.5 and 5.5 ..mu..eq L/sup -1/, respectively. Mean pH was 5.2-5.3. During melting, anion levels in the snowpack decreased and pH increased. By July, mean NO/sub 3//sup -/ and SO/sub 4//sup -2/ concentrations were 0.32 and 1.73 ..mu..eq L/sup -1/, respectively, and mean pH was 5.48. Acid neutralizing capacity at the lake outlet during snow melt was diluted to 50% of April premelt values. During snow melt runoff there was no apparent neutralization of bicarbonate by strong acids. By comparing lake water NO/sub 3//sup -/ concentrations to snowpack concentrations, over 75% of the NO/sub 3//sup -/ in the lake could be attributed to a snowpack source. An estimated 30% of the SO/sub 4//sup -2/ in the lake was derived from the snowpack.
Research Organization:
Western Washington Univ., Bellingham (USA)
OSTI ID:
7040883
Journal Information:
Water Resour. Res.; (United States), Journal Name: Water Resour. Res.; (United States) Vol. 24:5; ISSN WRERA
Country of Publication:
United States
Language:
English