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Titlebook: Biogeochemical Monitoring in Small Catchments; Refereed papers from Ji?í ?erny,Martin Novák,R. Kelman Wieder Book 1995 Springer Science+Bus

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發(fā)表于 2025-3-25 05:15:39 | 只看該作者
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Randomized Intervention Analysis of the Response of the West Bear Brook Watershed, Maine to Chemicall acidification and therefore provided an objective basis for determining whether changes in the geochemical behavior of West Bear Brook were temporally associated with the chemical manipulation. RIA analysis using weekly data yielded higher probabilities of stream water chemistry effects being temp
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發(fā)表于 2025-3-25 15:59:25 | 只看該作者
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發(fā)表于 2025-3-25 20:53:05 | 只看該作者
Biotic and Abiotic Processes Controlling Water Chemistry During Snowmelt at Rabbit Ears Pass, Rocky en ion was hypothesized to be generated from nitrification in overlying soils, and subsequently exchanged with other cations, particularly Ca...Solute concentrations in streamwater also decreased as snowmelt progressed. Variations in groundwater levels and solute concentrations indicate that most of
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發(fā)表于 2025-3-26 01:43:16 | 只看該作者
The Relationship Between Dissolved Organic Matter and Percolation Water Chemistry in Northern Finlan cm in the percolation water. Organic matter thus plays an important role as an anion in percolation water, and regulates water pH in the surface soil. A high proportion of dissolved Al was in the form of organic complexes. Total dissolved Al levels were well below the toxic limits for pine.
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Sulfur and Oxygen Isotope Ratios in Sulfate During an Acidification Reversal Study at Lake G?rdsj?n,f sprinlding water S with a larse reservoir of Sin the catchment. Oxygen isotopes in SO. suggest that less than one third of the SO.in runoff is secondary SO. formed within the soil profile. This is, however, no evidence for net mineralization of S. The SO.in runoff in the roofed catchment is a mixt
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