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Title: ECOHYDROLOGICAL IMPACTS OF WOODY PLANT ENCROACHMENT WITHIN A SEMIARID RIPARIAN ENVIRONMENT 1840

Author
item Scott, Russell - Russ
item HUXMAN, T. - UNIVERSITY OF ARIZONA
item WILLIAMS, D. - UNIVERSITY OF WYOMING

Submitted to: Meeting Abstract
Publication Type: Abstract Only
Publication Acceptance Date: 3/1/2006
Publication Date: 5/22/2006
Citation: Scott, R.L., Huxman, T.E., Williams, D.G. 2006. Ecohydrological impacts of woody plant encroachment within a semiarid riparian environment [abstract]. 27th Conf. on Agricultural & Forest Meteor. 22-25 May, 2006, San Diego, CA. 2006 CDROM.

Interpretive Summary: Across many dryland regions, historically grass-dominated ecosystems have been encroached upon by woody plant species. We compare ecosystem water and carbon dioxide fluxes over a grassland, a grassland-shrubland mosaic, and a fully developed woodland to evaluate potential consequences of woody plant encroachment on important ecosystem processes. All three sites were located in the riparian corridor of a river in the southwest U.S. As such, plants in these ecosystems may have access to moisture at the capillary fringe of the near-surface water table. Using fluxes measured by eddy covariance in 2003 we found that ecosystem evapotranspiration (ET) and net ecosystem exchange of carbon dioxide (NEE) increased with increasing woody plant dominance. Growing season ET totals were in excess of precipitation at all sites. This excess was derived from groundwater, especially during the extremely dry pre-rainy season period when this was the only source of moisture available to plants. Access to groundwater by the deep-rooted woody plants apparently decouples ecosystem ET from gross ecosystem production (GEP) with respect to precipitation. Compared to grasses, the woody plants were better able to use the stable groundwater source and had an increased net carbon dioxide gain during the dry periods. This enhanced plant activity resulted in substantial accumulation of leaf litter on the soil surface that, during rainy periods, may lead to high microbial respiration rates that offset these photosynthetic fluxes. There was a greater disparity between ecosystem water use and the strength of the carbon dioxide sink as woody plants increased across the encroachment gradient. Despite a higher density of woody plants and a greater plant productivity in the woodland than in the shrubland, the woodland produced a larger respiration response to rainfall that largely offset its higher photosynthetic potential. These data suggest that the capacity for woody plants to exploit water resources in riparian areas results in enhanced carbon sequestration at the expense of increased groundwater use under current climate conditions, but the potential does not scale specifically as a function of woody plant abundance.

Technical Abstract: Across many dryland regions, historically grass-dominated ecosystems have been encroached upon by woody plant species. We compare ecosystem water and carbon dioxide fluxes over a grassland, a grassland-shrubland mosaic, and a fully developed woodland to evaluate potential consequences of woody plant encroachment on important ecosystem processes. All three sites were located in the riparian corridor of a river in the southwest U.S. As such, plants in these ecosystems may have access to moisture at the capillary fringe of the near-surface water table. Using fluxes measured by eddy covariance in 2003 we found that ecosystem evapotranspiration (ET) and net ecosystem exchange of carbon dioxide (NEE) increased with increasing woody plant dominance. Growing season ET totals were in excess of precipitation at all sites. This excess was derived from groundwater, especially during the extremely dry pre-rainy season period when this was the only source of moisture available to plants. Access to groundwater by the deep-rooted woody plants apparently decouples ecosystem ET from gross ecosystem production (GEP) with respect to precipitation. Compared to grasses, the woody plants were better able to use the stable groundwater source and had an increased net carbon dioxide gain during the dry periods. This enhanced plant activity resulted in substantial accumulation of leaf litter on the soil surface that, during rainy periods, may lead to high microbial respiration rates that offset these photosynthetic fluxes. There was a greater disparity between ecosystem water use and the strength of the carbon dioxide sink as woody plants increased across the encroachment gradient. Despite a higher density of woody plants and a greater plant productivity in the woodland than in the shrubland, the woodland produced a larger respiration response to rainfall that largely offset its higher photosynthetic potential. These data suggest that the capacity for woody plants to exploit water resources in riparian areas results in enhanced carbon sequestration at the expense of increased groundwater use under current climate conditions, but the potential does not scale specifically as a function of woody plant abundance.