At this site, real-time estimates of water quality depend on the availability of instantaneous discharge and specific conductivity measurements. During winter months, real-time water quality estimates may not be available for this site due to effects of ice.
Model Form #1
ln(LDS) =
- 6.8461 + 1.0045 ln(Q)
+ 1.0597 ln(SC)
where:
- LDS is computed load diss. solids, in tons per day
- Q is computed discharge, stage-discharge rating curve, in cubic feet per second
- SC is specific conductance at 25 degrees Celsius, in microsiemens per centimeter
Model Calibration
Basic Data
Number of measurements: | 88 |
---|---|
Mean squared error: | 0.97891236 |
Multiple R2: | 0.9891 |
Bias correction (smearing) factor: | 1.0003 |
Explanatory Variables
Variable | Value | Standard error |
---|---|---|
Intercept | -6.8461 | 0.3913 | ln(Q) | 1.0045 | 0.0205 | ln(SC) | 1.0597 | 0.0318 |
Correlation Matrix
Intercept | ln(Q) | ln(SC) | |
---|---|---|---|
Intercept | 1 | -0.9942 | -0.996 |
ln(Q) | -0.9942 | 1 | 0.9805 |
ln(SC) | -0.996 | 0.9805 | 1 |
Reference
- Linard, J.I., Schaffrath, K.R., 2014, Regression models for estimating salinity and selenium concentrations at selected sites in the upper Colorado River Basin, Colorado: 2009 - 2012 (in publication process): U.S. Geological Survey Open File Report 2014-1015, 28 p.