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Water Budget Approach to Quantify Corn Grain Yields Under Variable Rooting Depths

D. J. Timlin*,a, Y. Pachepskyb, V. A. Snyderc and R. B. Bryantd

a USDA-ARS, Alternate Crops and Systems Lab., Bldg. 007, Rm. 116, BARC-West, 10300 Baltimore Ave., Beltsville, MD, 20705
b USDA-ARS Hydrology and Remote Sensing Lab., Bldg. 007, Rm. 106, BARC-W, 10300 Baltimore Ave., Beltsville, MD 20705
c College of Agricultural Sciences, P.O. Box 21360, Rio Piedras, PR 00928
d Dept. of Soil, Crop, and Atmospheric Sciences, Bradfield Hall, Cornell Univ., Ithaca, NY 14853



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Fig. 1. Relationship between available water and the relative transpiration ratio.

 


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Fig. 2. Cumulative rainfall and Class A pan evaporation at Aurora, NY (1983 to 1985).

 


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Fig. 3. Mean water potential data for the 1985 nonirrigated plots from tensiometers and gypsum blocks; (a) water potentials for plots where soil rooting depth >0.50 m and (b) water potentials for plots with soil rooting depth <0.50 m. The symbols T and S indicate timing of 50% tasseling and silking respectively. The calibrated range of the gypsum blocks did not extend to matric potentials more negative than -1500 kPa.

 


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Fig. 4. Comparison of irrigated and nonirrigated corn grain yields as a function of soil depth at Aurora. The same shape symbols are shown for the paired irrigated and nonirrigated plots. Filled symbols denote irrigated plots and hollow symbols nonirrigated.

 


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Fig. 5. Response to irrigation vs. soil depth.

 


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Fig. 6. Corn grain yield vs. soil depth at Aurora, 1983–1985.

 


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Fig. 7. Grain yield vs. calculated stress index for Aurora, 1983–1985.

 


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Fig. 8. Relative yield vs. calculated stress index for Canton, 1983 and 1985 Aurora data.

 


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Fig. 9. Measured relative grain yields and relative yield predicted by Eq. [8] vs. soil depth for the 1985 data.

 





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