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A Comparison of Methods for Deriving Solute Flux Rates Using Long-Term Data from Streams in the Mirror Lake Watershed |
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| Authors: | Bukaveckas PA Likens GE Winter TC Buso DC |
| Institution: | 1. Water Resources Laboratory, University of Louisville, Louisville, KY 40292, USA 2. Institute of Ecosystem Studies, Box AB, Millbrook, NY, 12545, USA 3. U.S. Geological Survey, Denver Federal Center, Denver, CO, 80225, USA 4. Institute of Ecosystem Studies, Box AB, Millbrook, NY, 12545, USA |
| Abstract: | Calculation of chemical flux rates for streams requires integration of continuous measurements of discharge with discrete measurements of solute concentrations. We compared two commonly used methods for interpolating chemistry data (time-averaging and flow-weighting) to determine whether discrepancies between the two methods were large relative to other sources of error in estimating flux rates. Flux rates of dissolved Si and SO4 2- were calculated from 10 years of data (1981-1990) for the NW inlet and outlet of Mirror Lake and for a 40-day period (March 22 to April 30, 1993) during which we augmented our routine (weekly) chemical monitoring with collection of daily samples. The time-averaging method yielded higher estimates of solute flux during high-flow periods if no chemistry samples were collected correponding to peak discharge. Concentration-discharge relationships should be used to interpolate stream chemistry during changing flow conditions if chemical changes are large. Caution should be used in choosing the appropriate time-scale over which data are pooled to derive the concentration-discharge regressions because the model parameters (slope and intercept) were found to be sensitive to seasonal and inter-annual variation. Both methods approximated solute flux to within 2-10% for a range of solutes that were monitored during the intensive sampling period. Our results suggest that errors arising from interpolation of stream chemistry data are small compared with other sources of error in developing watershed mass balances. |
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