Articles | Volume 15, issue 2
Hydrol. Earth Syst. Sci., 15, 561–567, 2011
https://doi.org/10.5194/hess-15-561-2011

Special issue: Observing and modeling the catchment-scale water cycle

Hydrol. Earth Syst. Sci., 15, 561–567, 2011
https://doi.org/10.5194/hess-15-561-2011

  11 Feb 2011

11 Feb 2011

Desert shrub stemflow and its significance in soil moisture replenishment

X.-P. Wang1,2, Z.-N. Wang1, R. Berndtsson2, Y.-F. Zhang1, and Y.-X. Pan1 X.-P. Wang et al.
  • 1Shapotou Desert Research and Experiment Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
  • 2Department of Water Resources Engineering, Lund University, 22100 Lund, Sweden

Abstract. Stemflow of xerophytic shrubs represents a significant component of water replenishment to the soil-root system influencing water utilization of plant roots at the stand scale, especially in water scarce desert ecosystems. In this study, stemflow of Caragana korshinskii was quantified by an aluminum foil collar collection method on re-vegetated sand dunes of the Shapotou restored desert ecosystem in northwestern China. Time domain reflectometry probes were inserted horizontally at 20 different soil profile depths under the C. korshinskii shrub to monitor soil moisture variation at hourly intervals. Results indicated that 2.2 mm precipitation was necessary for the generation of stemflow for C. korshinskii. Stemflow averaged 8% of the gross precipitation and the average funnelling ratio was as high as 90. The soil moisture in the uppermost soil profile was strongly correlated with individual rainfall and the stemflow strengthened this relationship. Therefore, it is favourable for the infiltrated water redistribution in the deeper soil profile of the root zone. Consequently, stemflow contributes significantly to a positive soil moisture balance in the root zone and the replenishment of soil moisture at deeper soil layers. This plays an important role in plant survival and the general ecology of arid desert environments.