Contrasting strategies of hydraulic control in two codominant temperate tree species

Matheny, Ashley M.; Fiorella, Richard P.; Bohrer, Gil; Poulsen, Christopher J.; Morin, Timothy H.; Wunderlich, Alyssa; Vogel, Christoph S.; Curtis, Peter S.

doi:10.1002/eco.1815

Contrasting strategies of hydraulic control in two codominant temperate tree species

Journal Article · Fri Dec 23 00:00:00 EST 2016 · Ecohydrology

DOI:https://doi.org/10.1002/eco.1815· OSTI ID:1418515

^[1]; ^[2]; Bohrer, Gil ^[3]; Poulsen, Christopher J. ^[4]; Morin, Timothy H. ^[3]; Wunderlich, Alyssa ^[3]; Vogel, Christoph S. ^[5]; Curtis, Peter S. ^[6]

The Ohio State Univ., Columbus, OH (United States). Dept of Civil, Environmental, and Geodetic Engineering; DOE Office of Scientific and Technical Information (OSTI)
Univ. of Michigan, Ann Arbor, MI (United States). Dept. of Earth and Environmental Sciences; Univ. of Utah, Salt Lake City, UT (United States). Dept. of Geology and Geophysics
The Ohio State Univ., Columbus, OH (United States). Dept of Civil, Environmental, and Geodetic Engineering
Univ. of Michigan, Ann Arbor, MI (United States). Dept. of Earth and Environmental Sciences
Univ. of Michigan, Pellston, MI (United States). Biological Station
The Ohio State Univ., Columbus, OH (United States). Dept of Evolution, Ecology, and Organismal Biology

Biophysical controls on plant water status exist at the leaf, stem, and root levels. Therefore, we pose that hydraulic strategy is a combination of traits governing water use at each of these three levels. Here, we studied sap flux, stem water storage, stomatal conductance, photosynthesis, and growth of red oaks (Quercus rubra) and red maples (Acer rubrum). These species differ in stomatal hydraulic strategy and xylem architecture and may root at different depths. Stable isotope analysis of xylem water was used to identify root water uptake depth. Oaks were shown to access a deeper water source than maples. During non-limiting soil moisture conditions, transpiration was greater in maples than in oaks. However, during a soil dry down, transpiration and stem water storage decreased by more than 80% and 28% in maples but only by 31% and 1% in oaks. We suggest that the preferential use of deep water by red oaks allows the species to continue transpiration and growth during soil water limitations. In this case, deeper roots may provide a buffer against drought-induced mortality. Using 14 years of growth data, we show that maple growth correlates with mean annual soil moisture at 30 cm but oak growth does not. The observed responses of oak and maple to drought were not able to be explained by leaf and xylem physiology alone. Finally, we employed the Finite-difference Ecosystem-scale Tree Crown Hydrodynamics model version 2 plant hydrodynamics model to demonstrate the influence of root, stem, and leaf controls on tree-level transpiration. We conclude that all three levels of hydraulic traits are required to define hydraulic strategy.

View Accepted Manuscript (DOE)

Research Organization:: Rutgers Univ., Newark, NJ (United States)

Sponsoring Organization:: National Science Foundation; USDOE; USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23)

Grant/Contract Number:: SC0007041

OSTI ID:: 1418515

Alternate ID(s):: OSTI ID: 1401886

Journal Information:: Ecohydrology, Journal Name: Ecohydrology Journal Issue: 3 Vol. 10; ISSN 1936-0584

Publisher:: WileyCopyright Statement

Country of Publication:: United States

Language:: English

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54 ENVIRONMENTAL SCIENCES
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Acer rubrum
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stable isotope analysis
stem water storage

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