Sediment, nitrate, and ammonium in surface runoff from two Tahoe Basin soil types
1994
Naslas, G.D. | Miller, W.W. | Blank, R.R. | Gifford, G.F.
Few studies have addressed the natural pollution potential of pristine subalpine forested watersheds on a site-specific basis. Consequently, specific source and amounts of nutrient discharge to tributaries of the Tahoe Basin are difficult to identify. The sediment content and nitrate and ammonium levels in surface runoff from two soil types (Meeks and Umpa), four plot conditions (wooded natural and disturbed, open natural and disturbed), and three slopes (gentle, moderate, and steep) were studied using rainfall simulation that applied a 9 cm h-1, 1-h event. A significant (P < 0.005) two-way interaction between soil type and plot condition affected runoff nitrate concentration. Runoff from natural or disturbed open plots contained significantly (P = 0.05) greater nitrate than wooded plots. Peak concentrations of nitrate commonly occurred during early runoff, suggesting that peak nitrate discharge to Lake Tahoe tributaries can be expected during early runoff from snowmelt and summer precipitation events. The highest nitrate runoff concentration and 1-h cumulative loading from the 0.46 m2 plots were 6.7 mg L-1 (Umpa, open natural, 15-30 percent slope), and 0.7 mg (Umpa, open natural, > 30 percent slope), respectively. Ammonium in surface runoff was generally below detection limits (< 0.05 micrograms L-1). No statistical relationship between runoff nitrate and sediment discharge was detected.
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