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How do Plants Control Soil Moisture?

Transpiration, root water uptake and hydraulic redistribution

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Last Update: June 2008 by Maite Guardiola-Claramonte

Moisture stored in the soil controls the partitioning of energy and water fluxes through the land surface. Understanding and quantifying this partitioning is key for the performance of hydrological models. Biosphere 2 offers unique environmental controls to study the partitioning of transpiration and evaporation for different ecosystems.

Experimental Approach:

Dry-down experiment in piñion pines at B2: nine piñon pines and three soil pots are located at three different temperature and humidity regimes: ambient temperature, +4°C and +4°C with +7% higher humidity. The weight of each pot (Lysimeter) and soil moisture at 5 different depths (Figure 2) is monitored continuously together with measurements of energy fluxes above the canopy (Figure 1). Simultaneously, needles and soil samples have been taken for isotope analysis.

Figure 1. Piñon pines' experimental setting at three different temperatures
Figure 2. Soil moisture probes are located at five different depths within the root bulb, or within the pot, in case of bare soil.
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Peter A. Troch
Department of Hydrology and Water Resources
John W. Harshbarger Building
1133 E James E. Rogers Way Tucson, AZ 85721
Tel: (520) 626-1277 Fax: (520) 621-1422
patroch@hwr.arizona.edu

 
Website created by Steve Lyon and Patrick Broxton. Last updated 09/2011 .