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- W2276243622 abstract "The long-term studies of water and chemical budgets in the Hubbard Brook watershed, White Mountains, New Hampshire, have assumed that the underlying bedrock is watertight and that all of the liquid water discharged from the experimental subcatchment areas was measured using stream gauging instrumentation. This paper reviews the evidence used by past workers to support this assumption. In a reanalysis of the reported relationship between precipitation inputs and stream outputs of chloride, the mean annual groundwater discharge beneath the stream gauging stations was computed to be at least 5–10% of the mean annual precipitation. Groundwater discharge of this quantity would change both the evapotranspiration and the rock-weathering rates reported for the Hubbard Brook watershed. On-site hydrogeological field tests are recommended in all watersheds that are assumed to be underlain by watertight bedrock. [Key words: forested ecosystems, groundwater hydrology, bedrock fractures, water budgets, evapotranspirati..." @default.
- W2276243622 created "2016-06-24" @default.
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- W2276243622 date "1993-09-01" @default.
- W2276243622 modified "2023-09-26" @default.
- W2276243622 title "EVALUATION OF THE ASSUMPTION OF WATERTIGHT BEDROCK UNDERLYING AN EXPERIMENTAL WATERSHED" @default.
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- W2276243622 doi "https://doi.org/10.1080/02723646.1993.10642492" @default.
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