, Volume 6, Issue 2, pp 0185–0196

Association between Plant Canopies and the Spatial Patterns of Infiltration in Shrubland and Grassland of the Chihuahuan Desert, New Mexico

  • Eric W. Bhark
  • Eric E. Small

DOI: 10.1007/s10021-002-0210-9

Cite this article as:
Bhark, E. & Small, E. Ecosystems (2003) 6: 0185. doi:10.1007/s10021-002-0210-9


Shrubs have invaded extensive areas of grassland in the southwestern United States. The zones of nutrient-rich soil found beneath plant canopies, referred to as “islands of fertility,” are more intense and spaced farther apart in shrubland than in grassland. This difference in the spatial pattern of soil nutrients may reinforce shrub invasion. Changes in water availability in the soil could also influence shrub invasion. Here we compare the spatial patterns of infiltration, defined as the total equivalent water depth entering the soil following individual rainfall events or summed over many events, at adjacent grass- and shrub-dominated sites in the Sevilleta National Wildlife Refuge. We use two infiltration data sets. First, following four rainfall events, we measured soil moisture and wetting front depth at 10-cm intervals along 24-m transects. We estimate infiltration from these data. Second, we use vertical arrays of soil moisture probes to compare infiltration between adjacent canopies and interspaces following 31 storms. In both the grassland and shrubland, infiltration is typically greater beneath plant canopies than beneath interspaces. Canopies are oases where soil moisture is higher than in the surrounding areas. However, infiltration is not greater beneath canopies when surface runoff is limited. In the shrubland, the canopy–interspace infiltration ratio increases as storm size, and therefore runoff, increases. This relationship also exists in the grassland, but it is not as strong or clear. The magnitude of spatial variability of infiltration is similar in shrubland and grassland. In addition, the distance over which infiltration is correlated is approximately 50 cm in both environments. Most of the spatial variability exists between the stem and canopy margin in the shrubland and straddling the canopy margin in the grassland. The most notable difference is that subcanopy oases are spread farther apart in the shrubland because canopies are separated by larger interspaces in this environment.

Key words: plant canopies; infiltration; shrubland; grassland; desertification; semiarid ecosystems; rainfall interception; water availability; soil moisture dynamics; Chihuahan Desert. 

Copyright information

© Springer-Verlag New York Inc. 2003

Authors and Affiliations

  • Eric W. Bhark
    • 1
  • Eric E. Small
    • 1
  1. 1.Department of Geological Sciences, University of Colorado at Boulder, Boulder, Colorado 80309, USAUS

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