Soil moisture sensors can help to reduce the amount of water needed for irrigation. In this paper we describe the PlantCare soil moisture sensor as a new type of heat dissipation sensor, its calibration and the correction for temperature changes. With the PlantCare sensor it is possible to measure the matric potential indirectly to monitor or control irrigation. This sensor is based on thermal properties of a synthetic felt. After a defined heating phase the cooling time to a threshold temperature is a function of the water content in the synthetic felt. The water content in this porous matrix is controlled by the matric potential in the surrounding soil. Calibration measurements have shown that the sensor is most sensitive to ?400 hPa and allows lower sensitivity measurements to ?800 hPa. The disturbing effect of the temperature change during the measurement on the cooling time can be corrected by a linear function and the differences among sensors are minimized by a two point calibration.
References
[1]
Crops and Drops: Making the Best Use of Water for Agriculture; FAO: Rome, Italy, 2002.
[2]
Pardossi, A.; Incrocci, L.; Incrocci, G.; Malorgio, F.; Battista, P.; Bacci, L.; Rapi, B.; Marzialetti, P.; Hemming, J.; Balendonck, J. Root zone sensors for irrigation management in intensive agriculture. Sensors 2009, 9, 2809–2835.
[3]
Young, M.H.; Sisson, J.B. Tensiometry. In Methods of Soil Analysis: Physical Methods; Dane, J.H., Topp, G.C., Eds.; Soil Science Society of America: Madison, WI, USA, 2002; pp. 575–608.
[4]
Scanlon, B.R.; Andraski, B.J. Miscellaneous methods for measuring matric or water potential. In Methods of Soil Analysis: Physical Methods; Dane, J.H., Topp, G.C., Eds.; Soil Science Society of America: Madison, WI, USA, 2002; pp. 643–670.
[5]
Durner, W.; Or, D. Soil Water Potential Measurement. In Encyclopedia of Hydrological Sciences; John Wiley & Sons: Chichester, UK, 2006.
[6]
Phene, C.J.; Hoffman, G.J.; Rawlins, S.L. Measuring soil matric potential in situ by sensing heat dissipation within a porous body. 1. Theory and sensor construction. Soil Sci. Soc. Am. J. 1971, 35, 27–33.
[7]
Reece, C.F. Evaluation of a line heat dissipation sensor for measuring soil matric potential. Soil Sci. Soc. Am. J. 1996, 60, 1022–1028.
[8]
Flint, A.L.; Campbell, G.S.; Ellett, K.M.; Calissendorff, C. Calibration and temperature correction of heat dissipation matric potential sensors. Soil Sci. Soc. Am. J. 2002, 66, 1439–1445.
[9]
Abu-Hamdeh, N.H.; Reeder, R.C. Soil thermal conductivity: Effects of density, moisture, salt concentration, and organic matter. Soil Sci. Soc. Am. J. 2000, 64, 1285–1290.
van Genuchten, M.T. A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Sci. Soc. Am. J. 1980, 44, 892–898.
[12]
Malazian, A.; Hartsough, P.; Kamai, T.; Campbell, G.S.; Cobos, D.R.; Hopmans, J.W. Evaluation of MPS-1 soil water potential sensor. J. Hydrol. 2011, 402, 126–134.
[13]
Hopmans, J.W.; Dane, J.H. Temperature-dependence of soil hydraulic-properties. Soil Sci. Soc. Am. J. 1986, 50, 4–9.
[14]
Feng, M.; Fredlund, D.G.; Shuai, F.S. A laboratory study of the hysteresis of a thermal conductivity soil suction sensor. Geotech. Tes. J. 2002, 25, 303–314.