Ecosystem-level evapotranspiration and water-use efficiency in the desert biome of Biosphere 2

被引:11
|
作者
Tubiello, FN
Lin, G
Druitt, JW
Marino, BDV
机构
[1] Columbia Univ, NASA, Goddard Inst Space Studies, New York, NY 10025 USA
[2] Biosphere 2 Ctr Res & Educ, Oracle, AZ 85623 USA
[3] Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA
关键词
Biosphere; 2; evapotranspitration; elevated CO2; ecosystems;
D O I
10.1016/S0925-8574(98)00103-7
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
We estimate whole-system water and carbon fluxes for the desert biome of Biosphere 2 under two different daily-mean CO2 concentrations: 450 ppmv and 850 ppmv. The desert mesocosm occupies an area of approximately 1500 m(2), has a total atmospheric Volume of about 25000 m(3) and contains a heterogeneous distribution of plants and soils. Atmospheric water content and CO2 concentrations were measured continuously using a variety of sensors, including a Li-cor 6262 for CO2 deployed within the experimental area. Daily carbon and water budgets were calculated in the desert biome, isolated from the rest of Biosphere 2 by deploying isolation curtains for 24-h periods. Data collected for six closure periods suggest that elevated CO2 concentration increased whole-system carbon uptake, while evapotranspiration remained constant. As a result, whole-system water-use efficiency (WUE, defined as net ecosystem carbon uptake per unit water transpired) in the Biosphere 2 desert increased by more than 40%. Our measurements investigate soil-plant processes at a medium scale, ideally bridging the gap between traditional controlled-environment growth chambers and open-field studies. (C) 1999 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:263 / 271
页数:9
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