M the evolution of soil water storage for either water resource management or fl ood risk prevention requires knowledge of the soil water content profi les during infi ltration and evaporation.Forests are present in many sensitive areas such as most mountain areas of Europe. Forest fl oor soils are generally covered by forest litter layers of variable thickness. Th e role of forest litter should therefore be accounted for in forest hydrologic models, as indicated by Ogée and Brunet (2001), who reported the lack of moisture measurements as a limitation for validating modeling approaches.Th e relevance of forest litter water content in the hydrologic behavior of forest land becomes even more crucial when taking into account its eff ect on the water repellency of litter material. In fact, recent studies have shown a relationship between wetting properties and the water content of forest litter, suggesting water content threshold values below which the organic material becomes hydrophobic (e.g., Greiff enhagen et al., 2005).Time domain refl ectometry is a much used method for the measurement of water content, as it is noninvasive and does not require sample collection for time-consuming laboratory measurements; however, the TDR technique has shown limitations for its use in loose material such as forest litter. In these materials, it is diffi cult to establish and maintain good contact between the probe and the surrounding material.Th e aim of this work was to develop a TDR probe that can be used for loose materials while ensuring optimum working conditions in terms of ease of insertion into the porous medium, contact with the surrounding porous medium, and homogeneity and confi nement of electrical energy storage.
Theory
Probe DesignTh e design of TDR probes has been described in the literature by several researchers (e.g., Chudobiak et al., 1979;Dalton and van Genuchten, 1986;Heimovaara, 1993;Ferré et al., 1998). Th e diff erent concepts vary in terms of dimensions, spacing, shape, and diameter of the probe wires (plates or rods). As a result, they diff er with respect to their infl uence on bulk soil electrical conductivity (EC) interference, sampling volume, and the spatial distribution of the electrical energy. Th e aim of probe design is usually to fi nd a good compromise between mitigation of the EC eff ect (i.e., short rods) that causes attenuation of the TDR waveform, and the length and spacing of the probe wires to A : EC, electrical conductivity; MAE, mean absolute error; TDR, time domain refl ectometry.O R Knowledge of water content is important for water resources management and risk preven on. For areas covered with forest, the presence of decomposed or undecomposed forest li er poses a real problem for the monitoring of volumetric water content. Tradi onal methods such as me domain refl ectometry (TDR) are diffi cult to apply, as the inconsistence of the porous material o en leads to density modifi ca ons close to the probe wires. The aim of this work was to develop a TDR probe that can be used for loo...