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Roy Ward (1984)
On the response to precipitation of headwater streams in humid areasJournal of Hydrology, 74
J. Martinec (1975)
Subsurface flow from snowmelt traced by tritiumWater Resources Research, 11
R. Linsley, M. Kohler, J. Paulhus (1958)
Hydrology for engineers
G. Pinder, John Jones (1969)
Determination of the ground‐water component of peak discharge from the chemistry of total runoffWater Resources Research, 5
T. Dinçer, B. Payne, T. Florkowski, J. Martinec, E. Tongiorgi (1970)
Snowmelt runoff from measurements of tritium and oxygen‐18Water Resources Research, 6
A. Rodhe (1981)
Spring Flood Meltwater or GroundwaterHydrology Research, 12
M. Anderson, T. Burt (1982)
The contribution of throughflow to storm runoff: An evaluation of a chemical mixing modelEarth Surface Processes and Landforms, 7
M. Davis, M. Ford (1982)
Sediment focusing in Mirror Lake, New Hampshire1Limnology and Oceanography, 27
N. Johnson, C. Driscoll, J. Eaton, G. Likens, W. McDowell (1981)
‘Acid rain’, dissolved aluminum and chemical weathering at the Hubbard Brook Experimental Forest, New HampshireGeochimica et Cosmochimica Acta, 45
(1981)
Standard Methods for the Examination of Water and WastewaterEarth Surf Processes
M. G. Anderson, T. P. Burt (1982)
The contribution of throughflow to storm runoff: An evaluation of a chemical mixing modelLimnol. Oceanogr., 7
M. Sklash, R. Farvolden (1979)
The Role Of Groundwater In Storm RunoffJournal of Hydrology, 43
D. Pilgrim, D. Huff, T. Steele (1979)
Use of specific conductance and contact time relations for separating flow components in storm runoffWater Resources Research, 15
V. Kennedy (1971)
Silica Variation in Stream Water with Time and Discharge
As part of the construction of a simulation model to test an acid precipitation neutralization mechanism, the stream hydrograph was separated into its base flow and event water components using stable environmental isotopes of water, naturally occurring conservative tracer. Three snowmelt events and one storm event during the winter and spring of 1984 were studied at an instrumented watershed in the Hubbard Brook Experimental Forest, New Hampshire. Conditions for use of the isotopic tracer were not always met, however. During the latter part of the snowmelt and the storm the isotopic content of the groundwater and event water were not distinguishable. Furthermore, the isotopic content of the meltwater varied considerably over time, thereby reducing the precision of the hydrograph separation. Frequent sampling of the meltwater is mandatory to assess this variability. Because the concentration of major cations and anions was measured as well, chemical tracers could be compared to the isotopic tracer, when the isotopic hydrograph separation was reliable, to test whether the chemical tracer was conservative. Dissolved silica was found to act as a conservative tracer for this watershed.
Water Resources Research – Wiley
Published: Sep 1, 1986
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