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Department of Rangeland Ecology & Management

Texas A&M University

 
Research
The focus of my work is on understanding hydrologic processes on shrublands and in particular understand how and at what scales shrubs modify the water cycle. I am investigating this question using a variety of strategies including large plot rainfall simulation and monitoring of small catchments.

Large Scale Rainfall Simulation
A large plot rainfall simulator has been constructed that is capable of simulating a rainstorm over the tree canopy on a size of about 3 x 12 meters. During the simulated rainstorm we monitor surface runoff, interflow, interception and soil water. Simulation studies have been completed at the Sonora Experiment Station in Sonora, TX and at Honey Creek State Natural Area in Spring Branch, TX. We are currently operating at Camp Bullis in San Antonio, monitoring natural and simulated rainfall over two caves to investigate interactions between brush and recharge processes.

 
Small Catchment Work

Honey Creek, Texas

The Honey Creek Project is a collaborative effort involving several State, Federal and Municipal organizations, where the purpose is to examine how shrub control affects streamflow and water yield. The San Antonio Water System (SAWS) is providing support for us to examine water flow pathways on the Honey Creek site

 

Pajarito Plateau, New Mexico

On the Pajarito Plateau, we monitoring runoff and erosion from a highly degraded piñon-juniper watershed. Runoff and erosion data have been collected at this site since 1993. Support is being provided by the Los Alamos National Laboratory.

 
Runoff and Recharge Processes
Runoff and recharge on the Edwards Plateau are inextricably linked. Runoff generated from the "contributing zone" of the plateau is largely responsible for recharging the Edwards aquifer. Streamflow originates in the higher portions of the Plateau and recharge the aquifer once they cross the highly fractured and porous "recharge zone". This process is extremely important but poorly understood. In particular there is a need to better understand how runoff is generated from the Plateau and its role in recharging the aquifer.
 
 

Frio River, Edwards Plateau

Recharge through Seco Sink Hole
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