Response of soil CO2 efflux to water manipulation in a tallgrass prairie ecosystem

• Published in: Plant and soil 2002-03, Vol.240 (2), p.213-223
• Main Authors: Liu, Xiaozhong, Wan, Shiqiang, Su, Bo, Hui, Dafeng, Luo, Yiqi
• Format: Article
• Language: English
• Subjects: Agricultural and forest climatology and meteorology. Irrigation. Drainage; Agricultural and forest meteorology; Agronomy. Soil science and plant productions; Animal and plant ecology; Animal, plant and microbial ecology; Biological and medical sciences; Biosphere; Carbon dioxide; Chemical, physicochemical, biochemical and biological properties; Climatology, meteorology; Drought; Ecosystems; Fundamental and applied biological sciences. Psychology; General agronomy. Plant production; Generalities. Techniques. Climatology. Meteorology. Climatic models of plant production; Moisture content; Organic matter; Physics, chemistry, biochemistry and biology of agricultural and forest soils; Prairies; Soil columns; Soil moisture; Soil science; Soils; Synecology; Terrestrial ecosystems; Water levels; Water treatment
• ISSN: 0032-079X; 1573-5036
• DOI: 10.1023/a:1015744126533

Although CO^sub 2^ efflux plays a critical role in carbon exchange between the biosphere and atmosphere, our understanding of its regulation by soil moisture is rather limited. This study was designed to examine the relationship between soil CO^sub 2^ efflux and soil moisture in a natural ecosystem by taking advantage of the historically long drought period from 29 July to 21 September 2000 in the southern Central Great Plain, USA. At the end of August when soil moisture content at the top 50 mm was reduced to less than 50 g kg^sup -1^ gravimetrically, we applied 8 levels of water treatments (simulated to rainfall of 0, 10, 25, 50, 100, 150, 200, and 300 mm) with three replicates to 24 plots in a Tallgrass Prairie ecosystem in Central Oklahoma, USA. In order to quantify root-free soil CO^sub 2^ efflux, we applied the same 8 levels of water treatments to 24 500-mm soil columns using soil from field adjacent to the experimental plots. We characterized dynamic patterns of soil moisture and soil CO^sub 2^ efflux over the experimental period of 21 days. Both soil moisture content and CO^sub 2^ efflux showed dramatic increases immediately after the water addition, followed by a gradual decline. The time courses in response to water treatments are well described by Y=Y^sub 0^+ate^sup -bt^, where Y is either soil moisture or CO^sub 2^ efflux, t is time, Y^sub 0^, a, and b are coefficients. Among the 8 water treatments, the maximal soil CO^sub 2^ efflux rate occurred at the 50 mm water level in the field and 100 mm in the root-free soil 1 day after the treatment. The maximal soil CO^sub 2^ efflux gradually shifted to higher water levels as the experiment continued. We found the relationship between soil CO^sub 2^ efflux and soil moisture using the data from the 21-day experiment was highly scattered, suggesting complex mechanisms determining soil CO^sub 2^ efflux by soil moisture.[PUBLICATION ABSTRACT]