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Lunt Lunt (1932)
Profile characteristics of New England forest soilsBull. Conn. Agr. Exp. Sta., 342
F. Bormann, G. Likens, D. Fisher, R. Pierce (1968)
Nutrient Loss Accelerated by Clear-Cutting of a Forest EcosystemScience, 159
C. Johnson, P. Needham (1966)
Ionic Composition of Sagehen Creek, California, Following an Adjacent FireEcology, 47
Bormann (1967)
Nutrient cyclingScience, 155
G. Likens, F. Bormann, N. Johnson, R. Pierce (1967)
The Calcium, Magnesium, Potassium, and Sodium Budgets for a Small Forested Ecosystem.Ecology, 48 5
D. Fisher, A. Gambell, G. Likens, F. Bormann (1968)
Atmospheric Contributions to Water Quality of Streams in the Hubbard Brook Experimental Forest, New HampshireWater Resources Research, 4
N. Johnson, G. Likens, F. Bormann, R. Pierce (1968)
Rate of chemical weathering of silicate minerals in New HampshireGeochimica et Cosmochimica Acta, 32
W. Durum (1953)
Relationship of the mineral constituents in solution to stream flow, Saline River near Russell, KansasEos, Transactions American Geophysical Union, 34
Langbein Langbein, Dawdy Dawdy (1964)
Occurrence of dissolved solids in surface waters in the United StatesU. S. Geol. Surv. Prof. Pap., 501‐D
G. Hart, R. Leonard, R. Pierce (1962)
Leaf fall, humus depth, and soil frost in a northern hardwood forest, 131
G. Pinder, John Jones (1969)
Determination of the ground‐water component of peak discharge from the chemistry of total runoffWater Resources Research, 5
Franz Juang, N. Johnson (1967)
Cycling of chlorine through a forested watershed in New EnglandJournal of Geophysical Research, 72
Stream water chemistry varies hyperbolically with stream discharge through four decades of discharge change within the Hubbard Brook Experimental Forest, New Hampshire. This dilution process is most simply explained by the mixing of rain water or surface water with deeper soil water. The resultant mixture of waters subsequently appears as stream water. Sodium and silica concentrations in stream water are markedly diluted during high discharge periods while hydrogen ion, aluminum, and nitrate concentrations are increased. Magnesium, calcium, sulfate, chloride and potassium concentrations are changed very little by stream discharge variations. During the summer, biologic activity measurably reduces the concentration of nitrate and potassium in stream water.
Water Resources Research – Wiley
Published: Dec 1, 1969
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