Stomatal regulation of transpiration constrains leaf water potential (Psi(L)) within species-specific ranges that presumably avoid excessive tension and embolism in the stem xylem upstream. However, the hydraulic resistance of leaves can be highly variable over short time scales, uncoupling tension in the xylem of leaves from that in the stems to which they are attached. We evaluated a suite of leaf and stem functional traits governing water relations in individuals of 11 lowland tropical forest tree species to determine the manner in which the traits were coordinated with stem xylem vulnerability to embolism. Stomatal regulation of Psi(L) was associated with minimum values of water potential in branches (Psi(br)) whose functional significance was similar across species. Minimum values of Psi(br) coincided with the bulk sapwood tissue osmotic potential at zero turgor derived from pressure-volume curves and with the transition from a linear to exponential increase in xylem embolism with increasing sapwood water deficits. Branch xylem pressure corresponding to 50% loss of hydraulic conductivity (P (50)) declined linearly with daily minimum Psi(br) in a manner that caused the difference between Psi(br) and P (50) to increase from 0.4 MPa in the species with the least negative Psi(br) to 1.2 MPa in the species with the most negative Psi(br). Both branch P (50) and minimum Psi(br) increased linearly with sapwood capacitance (C) such that the difference between Psi(br) and P (50), an estimate of the safety margin for avoiding runaway embolism, decreased with increasing sapwood C. The results implied a trade-off between maximizing water transport and minimizing the risk of xylem embolism, suggesting a prominent role for the buffering effect of C in preserving the integrity of xylem water transport. At the whole-tree level, discharge and recharge of internal C appeared to generate variations in apparent leaf-specific conductance to which stomata respond dynamically.
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http://dx.doi.org/10.1007/s00442-008-0974-5 | DOI Listing |
Integr Environ Assess Manag
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Federal University of the Agreste of Pernambuco, Garanhuns, Brazil.
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Ningbo Key Lab of Polymer Materials, Ningbo Institute of Materials Technology and Engineering, Chinese Academy of Sciences, 315211 Ningbo, P. R. China.
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January 2025
Department of Chemical Engineering, Indian Institute of Science, Bengaluru, Karnataka 560012, India.
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Geothermal Energy and Geofluids Group, Institute of Geophysics, Department of Earth and Planetary Sciences, ETH Zurich, Zurich 8092, Switzerland.
Carbon capture and storage (CCS) and CO-based geothermal energy are promising technologies for reducing CO emissions and mitigating climate change. Safe implementation of these technologies requires an understanding of how CO interacts with fluids and rocks at depth, particularly under elevated pressure and temperature. While CO-bearing aqueous solutions in geological reservoirs have been extensively studied, the chemical behavior of water-bearing supercritical CO remains largely overlooked by academics and practitioners alike.
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January 2025
Technology R&D Center, Huaneng Lancang River Hydropower Inc., Kunming 650000, China.
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