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- W22382000 abstract "A watershed of almost 6 km/sup 2/ in the White Knob Mountains of central Idaho contains 3 well-defined but unique wetlands. During the dry season, these 3 wetlands and several smaller ones contribute over 35% of the watershed's flow while comprising less than 20% of the drainage area. Except for iron and sulfate, the wetlands contribute a smaller proportion of the load of each of the major dissolved chemicals than their contribution of water, probably indicating that they serve as storehouses for spring snowmelt which they release slowly throughout the dry season. However, the chemical composition of water in the wetlands differs markedly from snowmelt. Examination of each of the 3 major wetlands reveals significant differences in their contributions related to their hydrogeology. The highest of these wetlands contributes 20% of the watershed's flow. At the same time, it provides 13% of the total dissolved solids load, but 30% of the sulfate load. A second wetland, the smallest of the three, is dominated by a small tarn, making its effects indistinguishable from surface flow. The largest and lowest of the 3 wetlands contains a deep spring system contributing over 12% of the watershed's total flow and disproportionate amounts of ironmore » and sulfate. This latter situation may indicate close hydraulic connection with mineralized zones in the bedrock below the wetland.« less" @default.
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- W22382000 date "1985-01-01" @default.
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- W22382000 title "Role of wetlands in the flow and chemical loads of an alpine watershed" @default.
- W22382000 hasPublicationYear "1985" @default.
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