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State Space Analysis of Soil Water and Salinity Regimes in a Loam Soil Underlain by Shallow Groundwater

L. Wu*,a, T. H. Skaggsb, P. J. Shouseb and J. E. Ayarsc

a Dep. of Environmental Sciences, Univ. of California, Riverside, CA 92507
b George E. Brown, Jr. Salinity Lab., 450 W. Big Springs Rd., Riverside, CA 92507
c USDA-ARS, Water Management Research Lab., Fresno, CA 93727



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Fig. 1. (A) Field measured profile-averaged water content, k, (B) bulk electrical conductivity, b, (C) irrigation input, and (D) estimated evapotranspiration (ET) during the growing season, 1997.

 


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Fig. 2. Observed and regression lines of groundwater recharge (+) and discharge (-) as a function of profile-averaged soil water content.

 


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Fig. 3. (A) Time domain reflectometry measured and Kalman filter estimated profile-averaged soil water content (WC) and its estimation error and (B) Kalman filter estimated salt concentration (mg cm-3 soil) and its estimation error with weekly measurement update. The diamond symbol indicates the weekly water content measurement used to update the filter.

 


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Fig. 4. Estimated (A) daily groundwater flux and (B) salt flux.

 


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Fig. 5. Time domain reflectometry measured and Kalman filter (KF) estimated soil water electrical conductivity (ECw) and electrical conductivity of saturated extract (ECe) with weekly measurement update.

 


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Fig. 6. (A) Time domain reflectometry measured and Kalman filter estimated profile-averaged soil water content (WC) and its estimation error and (B) Kalman filter estimated salt concentration (mg cm-3 soil) and its estimation error with biweekly measurement update. The diamond symbol indicates the biweekly water content measurement used to update the filter.

 


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Fig. 7. Time domain reflectometry measured and Kalman filter (KF) estimated soil water electrical conductivity (ECw) and electrical conductivity of saturated extract (ECe) with biweekly measurement update.

 





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