Stream Phosphorus Transport in the Lake Tahoe Basin, 1989–1996

  title={Stream Phosphorus Transport in the Lake Tahoe Basin, 1989–1996},
  author={Lorin K. Hatch and John E. Reuter and Charles Remington Goldman},
  journal={Environmental Monitoring and Assessment},
Lake Tahoe is undergoing the initial stages of culturaleutrophication due to human alteration of the airshed andwatershed. The lake's switch from nitrogen (N) to phosphorus (P)limitation has been attributed primarily to atmospheric Nloading. This places an increased importance on controllingwatershed movement of P to the lake. A stream water qualitymonitoring data set consisting of nine streams in the Lake Tahoebasin has been analyzed to characterize the spatiotemporalvariation of P delivery to… 
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Use of turbidometry to characterize suspended sediment and phosphorus fluxes in the Lake Tahoe basin, California, USA
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Soil Phosphorus Speciation and Availability in Meadows and Forests in Alpine Lake Watersheds With Different Parent Materials
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Transport and Transformation of Phosphorus in a Forest Stream Ecosystem
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Atmospheric deposition of nitrogen and phosphorus in the annual nutrient load of Lake Tahoe (California‐Nevada)
Atmospheric deposition provides most of the dissolved inorganic nitrogen (DIN) and total nitrogen in the annual nutrient load of Lake Tahoe. Deposition also contributes significant amounts of soluble
Long-term change in Lake Tahoe (California-Nevada, U.S.A.) and its relation to atmospheric deposition of algal nutrients
Bounds for the doubling times of the TN pool and the TN: TP ratio demonstrate that loading is fast enough to cause the observed changes, and suggest that interannual variability in nitrate and total acid-hydrolyzable phosphorus is large enough to disguise trends of the expected magnitude.
Origins and scale dependence of temporal variability in the transparency of Lake Tahoe, California–Nevada
Secchi depth has been measured in Lake Tahoe an average of every 12 d since July 1967. Because of the unusual clarity of the lake, Secchi depth measurement is responsive to small changes in
Primary productivity, nutrients, and transparency during the early onset of eutrophication in ultra‐oligotrophic Lake Tahoe, Califomia‐Nevada1
For more than half a century, the trophic status of water bodies has been of interest to Iimnologists and oceanographers alike. This report demonstrates the close, inverse relationship between
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Streambed sediments and the bryophyte community are sites of retention and processing of dissolved phosphorus (DP) in Bear Brook, an undisturbed headwater stream in the Hubbard Brook Experimental