Agronomy Journal Journal of Natural Resources and Life Sciences Education
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Xylem Hydraulics and the Soil–Plant–Atmosphere Continuum

Opportunities and Unresolved Issues

John S. Sperry*, Volker Stiller and Uwe G. Hacke

Biol. Dep., Univ. of Utah, 257 S, 1400E, Salt Lake City, UT 84112. Financial support from USAID and NSF (IBN-0112213)



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Fig. 1. Vulnerability curves of crop species, showing how the percentage loss of hydraulic conductivity in the xylem (PLC) increases as xylem pressure becomes more negative. Data from Neufeld et al. (1992), Sperry (2000), Stiller et al. (2003), and Stiller and Sperry (2002).

 


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Fig. 2. Hysteresis in vulnerability curves. During dehydration, the percentage loss of hydraulic conductivity in xylem (PLC) increases because of cavitation. During rehydration, the dashed line shows the expected pattern where embolized xylem conduits are not refilled with water until the xylem pressure rises above the -2T/r limit (see text), which is very close to atmospheric. The left-hand limit is for a conduit filled with water vapor, and the right-hand limit is for an air-filled conduit. The dotted line shows a novel rehydration pattern reported for some species in which refilling occurs despite substantial negative pressures in the transpiration stream. From Hacke and Sperry (2003).

 


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Fig. 3. The cavitation fatigue phenomenon. (A) Water birch (Betula occidentalis Hook.) stems possess the same vulnerability curve between repeated measurements on the same material (first vs. second curves). (B) Sunflower (Helianthus annuus L.) stems show cavitation fatigue, wherein the second curve is much more vulnerable than the first (asterisks denote significant differences at the p < 0.01 level). Cavitation fatigue occurs naturally in intact, droughted plants and appears to be reversible in sunflower. From Hacke et al. (2001b).

 


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Fig. 4. Hypothetical structure–function relationships in intervessel pits. From Carlquist (1989).

 





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