TY  - JOUR
A1  - Lozano-Parra, Javier
A1  - van Schaik, N. Loes M. B.
A1  - Schnabel, Susanne
A1  - Gomez-Gutierrez, Alvaro
T1  - Soil moisture dynamics at high temporal resolution in a semiarid Mediterranean watershed with scattered tree cover
JF  - Hydrological processes
N2  - Subsurface water flows play a key role in the distribution of water and solutes and thereby in the water availability for plants. However, the characterization of different flow processes (i.e.matrix and preferential flow), the frequency and factors that cause them, is relatively rare. This characterization enables a better understanding of spatio-temporal variability of water resources and allows for the design of models to be improved. Using a method based on the time derivative of soil moisture variation known as maximum wetting slope, types of soil wetting processes were classified and quantified. For this, capacitance sensors, which registered the volumetric water content at high temporal resolution (30min) for more than two hydrological years, were installed at different depths and placed in soil moisture stations with different vegetation covers, lithology and topographic position. Results indicated that there is a general behaviour or pattern of soil moisture dynamics in the catchment with a dominant occurrence of slower soil wetting processes (>50%), caused by matrix flows, and a low occurrence of those faster processes (<30%), originated by preferential flows. Nevertheless, when the total volume of water is considered, preferential flow becomes the dominant process, so that the ecological role of both flow types becomes prominent in water-limited environments. Statistical multivariate analyses based on data-mining techniques proved that although both flow types depend on variables associated with precipitation and antecedent soil moisture conditions, faster soil wetting processes are mainly related to variables such as rainfall intensity and topography, while slower soil wetting processes are related to flow velocity, soils or vegetation. Copyright (c) 2015 John Wiley & Sons, Ltd.
KW  - soil moisture dynamics
KW  - high temporal resolution
KW  - capacitive sensors
KW  - water-limited environment
KW  - MARS
Y1  - 2016
U6  - https://doi.org/10.1002/hyp.10694
SN  - 0885-6087
SN  - 1099-1085
VL  - 30
SP  - 1155
EP  - 1170
PB  - Wiley-Blackwell
CY  - Hoboken
ER  -