Simultaneous Measurement of Soil Water Content and Salinity Using a Frequency-Response Method
N. Zhanga,*,
G. Fana,
K. H. Leea,
G. J. Kluitenbergb and
T. M. Loughinc
a Dep. of Biological and Agricultural Engineering, Kansas State Univ., Manhattan, KS 66502
b Dep. of Agronomy, Kansas State Univ., Manhattan, KS 66502
c Dep. of Statistics, Kansas State Univ., Manhattan, KS 66502

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Fig. 2. Control of soil sample density.
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Fig. 3. The sensor used in the experiment.
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Fig. 4. Functional diagram of the experimental system.
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Fig. 5. Frequency responses of the sensor at four volumetric water contents, 0.11 cmol kg1 salinity, and the 40-mm penetration depth.
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Fig. 6. Frequency responses of the sensor at four salinities, 0.19 m3 m3 volumetric water content, and the 40-mm penetration depth.
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Fig. 7. Frequency responses of the sensor at four penetration depths, 0.29 m3 m3 volumetric water content, and 1.752 cmol kg1 salinity.
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Fig. 8. Actual and predicted volumetric water contents at the 30-mm penetration depth.
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Fig. 9. Actual and predicted salinities at the 30-mm penetration depth.
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Fig. 10. Actual and predicted salinities with two replicate frequency-response data collected at the highest salinity (1.752 cmol kg1) and the lowest water content (0.12 m3 m3) removed.
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Fig. 11. Performances of calibration models established for predicting salinity at four fixed volumetric water levels and a fixed penetration depth (30 mm).
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Fig. 12. Performances of calibration models established for predicting volumetric water content at four fixed salinity levels and a fixed penetration depth (30 mm).
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Copyright © 2004 by the Soil Science Society of America.