What Do Plants Leave after Summer on the Ground?

The Effect of Afforested Plants in Arid Environments

Journal Article (2019)
Author(s)

César Jimenez Rodriguez (TU Delft - Water Resources, Instituto Tecnologico de Costa Rica)

AMJ Gerrits (TU Delft - Water Resources)

Stefan Uhlenbrook (UNESCO World Water Assessment Program)

J. Wenninger (IHE Delft Institute for Water Education)

Research Group
Water Resources
Copyright
© 2019 C.D. JIMENEZ RODRIGUEZ, Miriam Coenders-Gerrits, S. Uhlenbrook, J.W. Wenninger
DOI related publication
https://doi.org/10.3390/w11122559
More Info
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Publication Year
2019
Language
English
Copyright
© 2019 C.D. JIMENEZ RODRIGUEZ, Miriam Coenders-Gerrits, S. Uhlenbrook, J.W. Wenninger
Research Group
Water Resources
Issue number
12
Volume number
11
Pages (from-to)
1-19
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Abstract

The implementation of afforestation programs in arid environments in northern China had modified the natural vegetation patterns. This increases the evaporation flux; however, the influence of these new covers on the soil water conditions is poorly understood. This work aims to describe the effect of Willow bushes (Salix psammophila C. Wang and Chang Y. Yang) and Willow trees (Salix matsudana Koidz.) on the soil water conditions after the summer. Two experimental plots located in the Hailiutu catchment (Shaanxi province, northwest China), and covered with plants of each species, were monitored during Autumn in 2010. The monitoring included the soil moisture, fine root distribution and transpiration fluxes that provided information about water availability, access and use by the plants. Meanwhile, the monitoring of stable water isotopes collected from precipitation, soil water, groundwater and xylem water linked the water paths. The presence of Willow trees andWillow bushes reduce the effect of soil evaporation after summer, increasing the soil moisture respect to bare soil conditions. Also, the presence of soil water with stable water isotope signatures close to groundwater reflect the hydraulic lift process. This is an indication of soil water redistribution carried out by both plant species.