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Increased temperature sensitivity of net DOC production from ombrotrophic peat due to water table draw-down

By J. M. Clark, D. Ashley, M. Wagner, P. J. Chapman, S. N. Lane, C. D. Evans and A. L. Heathwaite


The production and release of dissolved organic carbon (DOC) from peat soils is thought\ud to be sensitive to changes in climate, specifically changes in temperature and rainfall.\ud However, little is known about the actual rates of net DOC production in response to\ud temperature and water table draw-down, particularly in comparison to carbon dioxide\ud (CO2) fluxes. To explore these relationships, we carried out a laboratory experiment on\ud intact peat soil cores under controlled temperature and water table conditions to\ud determine the impact and interaction of each of these climatic factors on net DOC\ud production. We found a significant interaction (Po0.001) between temperature, water\ud table draw-down and net DOC production across the whole soil core (0 to 55cm depth).\ud This corresponded to an increase in the Q10 (i.e. rise in the rate of net DOC production\ud over a 10 1C range) from 1.84 under high water tables and anaerobic conditions to 3.53\ud under water table draw-down and aerobic conditions between 10 and 40cm depth.\ud However, increases in net DOC production were only seen after water tables recovered to\ud the surface as secondary changes in soil water chemistry driven by sulphur redox\ud reactions decreased DOC solubility, and therefore DOC concentrations, during periods\ud of water table draw-down. Furthermore, net microbial consumption of DOC was also\ud apparent at 1 cm depth and was an additional cause of declining DOC concentrations\ud during dry periods. Therefore, although increased temperature and decreased rainfall\ud could have a significant effect on net DOC release from peatlands, these climatic effects\ud could be masked by other factors controlling the biological consumption of DOC in\ud addition to soil water chemistry and DOC solubility. These findings highlight both the\ud sensitivity of DOC release from ombrotrophic peat to episodic changes in water table\ud draw-down, and the need to disentangle complex and interacting controls on DOC\ud dynamics to fully understand the impact of environmental change on this system

Topics: Agriculture and Soil Science, Ecology and Environment
Year: 2009
DOI identifier: 10.1111/j.1365-2486.2008.01683.x
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