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Published online 23 January 2008
Published in Vadose Zone J 7:31-38 (2008)
DOI: 10.2136/vzj2007.0025
© 2008 Soil Science Society of America
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Parameter Estimation of a Root Water Uptake Model under Salinity Stress

Haruyuki Fujimakia,*, Yoshitake Andoa, Yibin Cuib and Mitsuhiro Inouec

a Univ. of Tsukuba, 1-1-1 Tennodai, Tsukuba, Ibaraki 305-8572, Japan
b School of the Environment, Nanjing Univ., Nanjing 210093, China
c Arid Land Research Center, Tottori Univ., 1390 Hamasaka, Tottori 680-8550, Japan


Figure 1
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FIG. 1. Schematic of the experimental setup.

 

Figure 2
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FIG. 2. Relationship between dielectric permittivity and water content for Tottori sand.

 

Figure 3
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FIG. 3. Dependence of bulk electrical conductivity on water content for Tottori sand. Electrical conductivity of the soil solution was 5.4 dS m–1.

 

Figure 4
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FIG. 4. Measured and fitted soil water retention curve (drying).

 

Figure 5
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FIG. 5. Time evolution of air temperature, relative humidity, and solar radiation in the greenhouse.

 

Figure 6
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FIG. 6. Time evolution of water content.

 

Figure 7
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FIG. 7. Time evolution of electrical conductivity of soil solution. Arrows indicate when irrigations were performed.

 

Figure 8
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FIG. 8. Distribution of normalized root density for each column.

 

Figure 9
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FIG. 9. Time evolution of daily transpiration.

 

Figure 10
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FIG. 10. Salinity stress response function for the soybean.

 

Figure 11
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FIG. 11. Comparison of measured and calculated ratio of actual to potential daily transpiration.

 

Figure 12
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FIG. 12. Examples of the profiles of osmotic head, normalized root density, and {alpha}sβ (column C) at 12:00 p.m. on August 2 and August 11.

 





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