4.7 Article

The relationship of water-soluble carbon and hot-water-soluble carbon with soil respiration in agricultural fields

Journal

AGRICULTURE ECOSYSTEMS & ENVIRONMENT
Volume 156, Issue -, Pages 116-122

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.agee.2012.05.012

Keywords

Readily available carbon; Substrate availability; Soil respiration; Andosol; Fluvisol

Funding

  1. Bio-oriented Technology Research Advancement Institution, Japan
  2. Japan Society for the Promotion of Science
  3. Japan Science and Technology Agency

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Factors controlling soil respiration (R-S) are of great interest because R-S plays a Critical role in determining global atmospheric carbon dioxide (CO2) concentrations. Substrate availability is one of the most important factors controlling R-S. Soil microorganisms consume various substrates ranging from simple sugars supplied by aboveground photosynthesis to complex humic acids in soil organic matter; however, substrate decomposition rates depend on substrate availability. Thus, R-S is partly determined by the amount and quality of available substrate. However, accurate quantification of the amount of available substrate is difficult because soil microorganisms utilize carbon (C) substrates of varying quality for R-S. Watersoluble C (WSC), hot-water-soluble C (HWSC), and microbial biomass C are known as indicators of the amount of available soil C substrate. We continuously measured R-S in two contrasting soils, Andosol and Fluvisol, during the cultivation of soybean and brassica crops with a 6-month fallow period between them. The total annual R-S in Andosol and Fluvisol were 376 +/- 23 and 408 +/- 49 g CO2-C m(-2), respectively, with no significant difference between them. WSC and HWSC were measured every month during R-S measurement. During the soybean growth period, R-S and WSC were correlated, and soil type did not affect R-S. During the fallow period, R-S, HWSC and microbial biomass C in Fluvisol were higher than those in Andosol, despite the total soil C in Andosol being higher than that in Fluvisol. R-S during brassica crop growth was not correlated with any of the measured substrate indicators. We therefore concluded that the relationships among the measures of available substrates and R-S at the field level could provide vital information on seasonal changes in the interaction between the effects of soil type and plants on R-S, thereby leading to a better understanding of belowground C dynamics. (C) 2012 Elsevier B.V. All rights reserved.

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