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The effect of water table fluctuation on soil respiration in a lower coastal plain forested wetland in the southeastern U.S.
Author(s) -
Miao Guofang,
Noormets Asko,
Domec JeanChristophe,
Trettin Carl C.,
McNulty Steve G.,
Sun Ge,
King John S.
Publication year - 2013
Publication title -
journal of geophysical research: biogeosciences
Language(s) - English
Resource type - Journals
eISSN - 2169-8961
pISSN - 2169-8953
DOI - 10.1002/2013jg002354
Subject(s) - wetland , environmental science , diel vertical migration , water table , hydrology (agriculture) , soil respiration , soil carbon , marsh , carbon cycle , ecosystem , atmospheric sciences , soil water , soil science , ecology , groundwater , geology , oceanography , geotechnical engineering , biology
Anthropogenic and environmental pressures on wetland hydrology may trigger changes in carbon (C) cycling, potentially exposing vast amounts of soil C to rapid decomposition. We measured soil CO 2 efflux ( R s ) continuously from 2009 to 2010 in a lower coastal plain forested wetland in North Carolina, U.S., to characterize its main environmental drivers. To understand and quantify the spatial variation due to microtopography and associated differences in hydrology, measurements were conducted at three microsites along a microtopographic gradient. The seasonal hysteresis in R s differed by microtopographic location and was caused by the transitions between flooded and nonflooded conditions. Because flooded R s was small, we reported R s dynamics mainly during nonflooded periods. A nested model, modified from conventional Q 10 (temperature sensitivity) model with dynamic parameters, provided a significantly better simulation on the observed variation of R s . The model performed better with daily data, indicating that soil temperature ( T s ) and water table depth (WTD) were the primary drivers for seasonal variation. The diel variation of R s was high and independent of T s and WTD, which both had small diel variations, suggesting the likely association with plant activity. Overall, the site‐average soil CO 2 efflux was approximately 960–1103 g C m −2 yr −1 in 2010, of which 93% was released during nonflooded periods. Our study indicates that R s is highly linked to hydroperiod and microtopography in forested wetlands and droughts in wetlands will accelerate soil C loss.