Campbell Scientific 253 253-L and 257-L (Watermark 200) Soil Matric Potential - Page 24
TABLE 7-3., Comparison of, Estimated Soil Water Potential, and R, at 21°C, kPa Non, Linear, Equation
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253-L and 257-L Soil Matric Potential Sensors 7.2.3.2 Non-Linear Relationship For more precise work, calibration and temperature compensation in the range of 10 to 100 kPa has been refined by Thompson and Armstrong (1987), as defined in the non-linear equation, SWP = Rs 0.01306[1.062(34.21 − Ts + 0.01060Ts 2 ) − Rs ] where SWP is soil water potential in kPa TABLE 7-3. Comparison of Estimated Soil Water Potential and Rs at 21°C kPa (NonLinear Equation) -9 -14 -20 -27 -35 -45 -56 -69 -85 -105 kPa (Linear Equation) -3.7 -11 -18 -26 -33 -41 -48 -56 -63 -70 -78 -85 -92 -99 -107 -115 -122 -129 -144 -159 -174 -188 -199 (Rs) kOhms 1.00 2.00 3.00 4.00 5.00 6.00 7.00 8.00 9.00 10.00 11.00 12.00 13.00 14.00 15.00 16.00 17.00 18.00 20.00 22.00 24.00 26.00 27.50 18