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a Wageningen Univ., Dep. of Environmental Science, Soil Physics, Ecohydrology and Groundwater Management Group, Droevendaalsesteeg 4, 6708 PB, Wageningen, The Netherlands
b ALTERRA, Droevendaalsesteeg 4, 6708 PB, Wageningen, The Netherlands
* Corresponding author (martine.vanderploeg{at}wur.nl).
Received 1 June 2007.
In many regions of the world, plant growth and productivity are limited by water deficits. As a result of more frequent and intense droughts, the area of land characterized as very dry has more than doubled since the 1970s. Consequently, understanding root water uptake under water-stressed conditions is gaining importance. The performance of a recently developed polymer tensiometer (POT) designed to measure matric potentials down to –1.6 MPa was evaluated and compared with volumetric moisture content measurements in dry soil. Three irrigation intensities created severe, intermediate, and no water stress conditions in lysimeters with growing maize (Zea mays L.) plants. By monitoring matric potentials using POTs, levels of local water stress in our experiments were better defined. When the defined stress levels were reached, volumetric moisture measurements for this particular loam soil were below 0.1, thus less informative compared with matric potential measurements. The observed matric potential profiles indicate significant root water uptake between 0.3- and 0.5-m depth in the later growth stages under water-stressed conditions. The temporal pattern of matric potential profiles reflected changing root water uptake behavior under dry conditions. As the total soil water potential is a direct indication of the amount of energy required by plants to take up water, POTs may contribute to quantifying root water uptake in dry soils.
Abbreviations: IS, intermediate stress NS, no stress POT, polymer tensiometer RLD, root length density SS, severe stress TDR, time domain reflectometry
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