This title appears in the Scientific Report :
2014
Please use the identifier:
http://dx.doi.org/10.1016/j.jhydrol.2014.01.069 in citations.
Effect of soil hydraulic properties on the relationship between the spatial mean and variability of soil moisture
Effect of soil hydraulic properties on the relationship between the spatial mean and variability of soil moisture
Knowledge of spatial mean soil moisture and its variability over time is needed in many environmental applications. We analyzed dependencies of soil moisture variability on average soil moisture contents in soils with and without root water uptake using ensembles of non-stationary water flow simulat...
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Personal Name(s): | Martínez García, Gonzalo (Corresponding Author) |
---|---|
Pachepsky, Yakov A. / Vereecken, Harry | |
Contributing Institute: |
Agrosphäre; IBG-3 |
Published in: | Journal of hydrology, 516 (2014) S. 154 - 160 |
Imprint: |
Amsterdam [u.a.]
Elsevier
2014
|
DOI: |
10.1016/j.jhydrol.2014.01.069 |
Document Type: |
Journal Article |
Research Program: |
Terrestrial Systems: From Observation to Prediction Modelling and Monitoring Terrestrial Systems: Methods and Technologies |
Publikationsportal JuSER |
Knowledge of spatial mean soil moisture and its variability over time is needed in many environmental applications. We analyzed dependencies of soil moisture variability on average soil moisture contents in soils with and without root water uptake using ensembles of non-stationary water flow simulations by varying soil hydraulic properties under different climatic conditions. We focused on the dry end of the soil moisture range and found that the magnitude of soil moisture variability was controlled by the interplay of soil hydraulic properties and climate. The average moisture at which the maximum variability occurred depended on soil hydraulic properties and vegetation. A positive linear relationship was observed between mean soil moisture and its standard deviation and was controlled by the parameter defining the shape of soil water retention curves and the spatial variability of saturated hydraulic conductivity. The influence of other controls, such as variable weather patterns, topography or lateral flow processes needs to be studied further to see if such relationship persists and could be used for the inference of soil hydraulic properties from the spatiotemporal variation in soil moisture. |