Clark, J. M.; Ashley, D.; Wagner, M.; Chapman, P. J.; Lane, S. N.; Evans, C. D.
ORCID: https://orcid.org/0000-0002-7052-354X; Heathwaite, A. L..
2009
Increased temperature sensitivity of net DOC production from ombrotrophic peat due to water table draw-down.
Global Change Biology, 15 (4).
794-807.
10.1111/j.1365-2486.2008.01683.x
Abstract
The production and release of dissolved organic carbon (DOC) from peat soils is thought
to be sensitive to changes in climate, specifically changes in temperature and rainfall.
However, little is known about the actual rates of net DOC production in response to
temperature and water table draw-down, particularly in comparison to carbon dioxide
(CO2) fluxes. To explore these relationships, we carried out a laboratory experiment on
intact peat soil cores under controlled temperature and water table conditions to
determine the impact and interaction of each of these climatic factors on net DOC
production. We found a significant interaction (Po0.001) between temperature, water
table draw-down and net DOC production across the whole soil core (0 to 55cm depth).
This corresponded to an increase in the Q10 (i.e. rise in the rate of net DOC production
over a 10 1C range) from 1.84 under high water tables and anaerobic conditions to 3.53
under water table draw-down and aerobic conditions between 10 and 40cm depth.
However, increases in net DOC production were only seen after water tables recovered to
the surface as secondary changes in soil water chemistry driven by sulphur redox
reactions decreased DOC solubility, and therefore DOC concentrations, during periods
of water table draw-down. Furthermore, net microbial consumption of DOC was also
apparent at 1 cm depth and was an additional cause of declining DOC concentrations
during dry periods. Therefore, although increased temperature and decreased rainfall
could have a significant effect on net DOC release from peatlands, these climatic effects
could be masked by other factors controlling the biological consumption of DOC in
addition to soil water chemistry and DOC solubility. These findings highlight both the
sensitivity of DOC release from ombrotrophic peat to episodic changes in water table
draw-down, and the need to disentangle complex and interacting controls on DOC
dynamics to fully understand the impact of environmental change on this system.
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