4.7 Article

How do rubber (Hevea brasiliensis) plantations behave under seasonal water stress in northeastern Thailand and central Cambodia?

Journal

AGRICULTURAL AND FOREST METEOROLOGY
Volume 213, Issue -, Pages 10-22

Publisher

ELSEVIER
DOI: 10.1016/j.agrformet.2015.06.011

Keywords

Tropical deciduous trees; Stomatal control; Transpiration; Water vapor flux; Eddy covariance; Soil moisture

Funding

  1. Global COE (Centers of Excellence) Program (GCOE) of the Japan Society for the Promotion of Science (JSPS)
  2. National Aeronautics and Space Administration (NASA) [NNG04GH59G, NNX08AL90G]
  3. grant from Kyushu University
  4. project Estimation and simulation of carbon stock change of tropical forest in Asia - Ministry of Agriculture, Forestry and Fisheries, Japan
  5. Ministry of Education, Science and Culture, Japan [23405028]
  6. granted project Program for risk information on climate change from the Ministry of Education, Science and Culture, Japan
  7. Office of Science of the U.S. Department of Energy (DOE) through the Earth System Modeling program
  8. Battelle Memorial Institute [DE-AC05-76RLO1830]
  9. NASA Earth System Science grant [NNG04GH59G, NX08AL90G]
  10. Geo-Informatics and Space Technology Development Agency of Thailand
  11. National University of Singapore (NUS) [R-109-000-092-133]
  12. Asia-Pacific Network for Global Change Research (APN) grant [ARCP2008-01CMY]
  13. Grants-in-Aid for Scientific Research [23405028] Funding Source: KAKEN

Ask authors/readers for more resources

Delineating the characteristics of biosphere-atmosphere exchange in rubber (Hevea brasiliensis Mull. Arg.) plantations, which are rapidly expanding throughout mainland Southeast Asia, is important to understanding the impacts of the land-use change on environmental processes. In attempt to shed new light on the impacts of conversion to rubber, we have conducted eddy flux measurements over a 3-year period in two rubber plantation sites: (1) Som Sanuk, located in northeastern Thailand; and (2) Cambodian Rubber Research Institute (CRRI), located in central Cambodia. Both sites have a distinct dry season. We used a combination of actual evapotranspiration (E-T) flux measurements and an inverted version of a simple 2-layer E-T model for estimating the mean canopy stomatal conductance (g(s)). The potential water balance (precipitation (P) - potential evaporation (ET-POT)) for each season (i.e., December-February: DJF, March-May: MAM, June-August: JJA, and September-November: SON) revealed when and how the water use is controlled. In the seasons when actual water balance (P - E-T) was negative (DJF and MAM), the deficit was compensated with soil water from the previous season at depths of 0-2 m (Thailand site) and 0-3 m (Cambodia site). At both sites, the reference value of g(s) (g(sref)) and the sensitivity of g(s) to atmospheric demand (m) appeared to be less in DJF and MAM than each in the other two 3-month periods (seasons). On average, in a whole year, m/g(sref) was less in Thailand (-0.6) than in Cambodia (near 0.6 for part of the year), suggesting that there was less sufficient stomatal regulation at the Thailand site, where there might be little risk of water stress-induced hydraulic failure because of its higher annual rainfall amount. In comparison, at CRRI where annual P - ET-POT was negative, there was stricter stomatal regulation, preventing excessive xylem cavitation. (C) 2015 Elsevier B.V. All rights reserved.

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