Modelling the relative permittivity of soils using soil hygroscopic water content
Robinson, D.A.; Cooper, J.D.; Gardner, C.M.K.. 2002 Modelling the relative permittivity of soils using soil hygroscopic water content. Journal of Hydrology, 255 (1-4). 39-49. 10.1016/S0022-1694(01)00508-XFull text not available from this repository.
A model describing the increase in the relative permittivity of water with distance from the soil mineral surface is presented. The model assumes an exponential increase in the value of permittivity with increasing distance from the mineral surface; arguments are presented supporting this approach. The volume of bound water (within the bandwidth of time domain reflectometry, (TDR) 0.01–1 GHz) is considered to be equivalent to the soil hygroscopic water content. The refractive index mixing equation is used as a geometric base into which the model is incorporated. The new equation is tested using measurements of permittivity collected from two drying undisturbed soil cores that contained 10% hygroscopic water. The RMSE of predicted permittivity as a function of water content was found to decrease from 3.5 to less than 1. The model was further tested on data previously presented in the literature and found to correspond reasonably well.
|Programmes:||CEH Programmes pre-2009 publications > Other|
|CEH Sections:||_ Process Hydrology|
|Additional Keywords:||bound water, hygroscopic water, soil relative permittivity, time domain reflectometry TDR, dielectric constant|
|NORA Subject Terms:||Agriculture and Soil Science
|Date made live:||01 May 2012 11:24|
Actions (login required)