1. Effects of salinity and wet–dry treatments on C and N dynamics in coastal-forested wetland soils: Implications of sea level rise.
- Author
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Liu, Xijun, Ruecker, Alexander, Song, Bo, Xing, Jing, Conner, William H., and Chow, Alex T.
- Subjects
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SOIL salinity , *SOIL science , *WETLAND soils , *CARBON in soils , *NITROGEN in soils , *SEA level - Abstract
Forested wetlands dominated by baldcypress ( Taxodium distichum) and water tupelo (Nyssa aquatica ) are commonly found in coastal regions of the southeastern United States. Global climate change and in particular sea level rise will alter the frequency and magnitude of wet/dry periods and salinity levels in these ecosystems. Soil microcosm experiments were set up to identify the effects of water level variations (0.4–3.0 g-water g-soil −1 ) and salinity changes (0, 1 and 5 ppt of NaCl) on greenhouse gas emissions (CH 4 , CO 2 , and N 2 O) and dissolved organic carbon (DOC) characteristics from forested wetland soils. Our results indicate that, the effect of water level was much greater than salt intrusion on C and N cycling. Wet–dry treatments significantly decreased DOC production and total CH 4 -C loss, aromatic and humic-like substance compounds in DOC were increased in both flooding and wet–dry treatments after 60-d incubation. The molecular weight (MW) of DOC, as indicated by E2/E3 ratio and spectral slope, after flooding treatments was higher than that in wet–dry treatments. A first order kinetic model showed there was a positive linear correlation (r 2 = 0.73) between CO 2 emission rate and DOC concentration which indicated that CO 2 was mainly generated from DOC. An exponential kinetic model was applied to describe the correlation between CH 4 emission rate and DOC concentration (r 2 = 0.41). This study demonstrates that an increase in salinity, and in particular variations in wet–dry cycles, will lead to changes in the formation of climate-relevant greenhouse gases, such as CH 4 , CO 2 , and N 2 O. [ABSTRACT FROM AUTHOR]
- Published
- 2017
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