Dissolved organic carbon production and runoff quality following peatland extraction and restoration

被引:22
作者
Strack, M. [1 ]
Toth, K. [2 ]
Bourbonniere, R. [3 ]
Waddington, J. M. [2 ]
机构
[1] Univ Calgary, Dept Geog, Calgary, AB T2N 1N4, Canada
[2] McMaster Univ, McMaster Ctr Climate Change, Hamilton, ON L8S 4K1, Canada
[3] Environm Canada, Natl Water Res Inst, Burlington, ON L7R 4A6, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Decomposition; Dissolved organic carbon; Dissolved organic matter; Peatland; Peat extraction; Restoration; Wetland; FOREST FLOOR; CUTOVER PEATLANDS; MATTER FRACTIONS; ATMOSPHERIC CO2; NATURAL-WATERS; HUMIC-ACID; SOIL; EXPORT; REVEGETATION; REGENERATION;
D O I
10.1016/j.ecoleng.2011.08.015
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
We examined dissolved organic carbon (DOC) production and quality in a cutover (extracted) and restored peatland in eastern Quebec through a combined laboratory DOC production study and an accompanying field DOC runoff quality study. Both temperature and substrate were significant for explaining variability in net DOC production rate in both short (5 days) and longer term (25 day) laboratory incubations. Moss (Sphagnum spp. and Polytricum spp.) produced the least amount of DOC, with initial release rates of 0.02-0.35 mg DOC g(-1) d(-1). Shrubs, and to a lesser extent herbaceous vegetation, showed an initial high release of DOC followed by a decrease. Peat from the restored site had significantly higher longer-term DOC production rates than the cutover site. Humic acid (HA) was more likely to be produced by shrub and herbaceous plant material than by peat, mosses and straw. The hydrophilic (HPI) fraction of the DOC increased at higher temperatures. Despite differences in the surface cover of available substrate (e.g. vascular vegetation, moss, and straw), there was no difference in the quality of DOC exported from the cutover and restored sites. However, hydrological and biogeochemical controls were apparent in temporal variability of DOC quality in discharge. DOC exported during snowmelt and most storm events was high in HPI with little contribution from HA. Since contact time between water and soil is limited during these high flow periods, larger more hydrophobic HA molecules are less likely to be mobilized. Higher export of HA in summer compared to spring and autumn suggests that polycondensation and increased vascular plant productivity are important for controlling seasonal patterns of DOC export quality. As various substrates produced different amounts and quality of DOC, it is likely that the DOC quality exported from the restored site will continue to change as the new vegetation community develops. DOC production rates and DOC quality should be considered when developing a plan to control DOC runoff/export from managed peatlands. (C) 2011 Elsevier BM. All rights reserved.
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页码:1998 / 2008
页数:11
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