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Effect of water table drawdown on peatland dissolved organic carbon export and dynamics

地下水位 泥炭 溶解有机碳 环境科学 水文学(农业) 水位下降(水文) 缺氧水域 碳循环 地表水 排水 生态系统呼吸 水位 生态系统 地下水 地质学 含水层 涡度相关法 环境化学 生态学 化学 环境工程 生物 岩土工程 地图学 地理
作者
Maria Strack,J. M. Waddington,Richard A. Bourbonniere,E. L. Buckton,K. Shaw,Pete Whittington,Jonathan S. Price
出处
期刊:Hydrological Processes [Wiley]
卷期号:22 (17): 3373-3385 被引量:180
标识
DOI:10.1002/hyp.6931
摘要

Abstract Peatlands play an important role in the global carbon cycle, and loss of dissolved organic carbon (DOC) has been shown to be important for peatland carbon budgets. The objective of this study was to determine how net production and export of DOC from a northern peatland may be affected by disturbance such as drainage and climate change. The study was conducted at a poor fen containing several pool–ridge complexes: (1) control site–no water table manipulation; (2) experimental site–monitored for one season in a natural state and then subjected to a water table drawdown for 3 years; (3) drained site–subjected to a water table drawdown 9 years prior to monitoring. The DOC concentration was measured in pore water along a microtopographic gradient at each site (hummock, lawn and hollow), in standing water in pools, and in discharge from the experimental and drained sites. The initial water table drawdown released ∼3 g of carbon per square metre in the form of DOC, providing a large pulse of DOC to downstream ecosystems. This value, however, represents only 1–9% of ecosystem respiration at this site. Seasonal losses of DOC following drainage were 8–11 g of carbon per square metre, representing ∼17% of the total carbon exchange at the experimental study site. Immediately following water table drawdown, DOC concentrations were elevated in pore water and open water pools. In subsequent seasons, DOC concentration in the pool declined, but remained higher than the control site even 11 years after water‐table drawdown. This suggests continued elevated net DOC production under lower water table conditions likely related to an increase in vegetation biomass and larger water table fluctuations at the experimental and drained sites. However, the increase in concentration was limited to initially wet microforms (lawns and hollows) reflecting differences in vegetation community changes, water table and soil subsidence along the microtopographic gradient. Copyright © 2008 John Wiley & Sons, Ltd and Her Majesty the Queen in right of Canada.
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