期刊
ENVIRONMENTAL POLLUTION
卷 157, 期 12, 页码 3433-3439出版社
ELSEVIER SCI LTD
DOI: 10.1016/j.envpol.2009.06.020
关键词
DOM; COD; DOC; Acidic deposition; Water treatment; Reservoir ecosystem
资金
- Czech Science Foundation [526/07/P349]
The concentration of chemical oxygen demand (COD), a common proxy for dissolved organic matter (DOM), was measured at seven drinking-water reservoirs and four streams between 1969 and 2006. Nine of them showed significant DOM increases (median COD change +0.08 mg L-1 yr(-1)). Several potential drivers of these trends were considered, including air temperature, rainfall, land-use and water sulfate concentration. Temperature and precipitation influenced inter-annual variations, but not long-term trends. The long-term DOM increase was significantly associated with declines of acidic deposition, especially sulfur deposition. Surface water sulfate concentrations decreased from a median of 62 mg L-1-27 mg L-1 since 1980. The magnitude of DOM increase was positively correlated with average DOM concentration (R-2 = 0.79, p < 0.001). Simultaneously, DOM concentration was positively correlated with the proportion of Histosols within the catchments (R-2 = 0.79, p < 0.001). A focus on the direct removal of DOM by water treatment procedures rather than catchment remediation is needed. (C) 2009 Elsevier Ltd. All rights reserved.
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