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Dielectric Relaxation of Bound Water versus Soil Matric Pressure

^a IMAG-DLO, P.O. Box 43, NL-6700 AA, Wageningen, the Netherlands
^b Dep. of Water Resources, Wageningen Agricultural Univ., Wageningen, the Netherlands
^c DLO, P.O. Box 59, NL-6700 AB Wageningen, the Netherlands

View larger version (24K): [in a new window]   Fig. 1. An overview of the relationship between the different energy states of bound water in soil. The relaxation frequency, fr, and the soil matric pressure, pm, are plotted as a function of activation enthalpy, H*. The bar on top of the graph is an indication of the number of water layers bound to a soil particle. White represents no water and black a large amount of water layers. The bar at the bottom refers to the numbers of the list in the text