Submerged macrophyte Ceratophyllum demersum affects phosphorus exchange at the sediment-water interface

被引:6
|
作者
Dai, Yanran [1 ]
Cheng, Shuiping [1 ]
Liang, Wei [2 ]
Wu, Zhenbin [2 ]
机构
[1] Tongji Univ, Minist Educ, Key Lab Yangtze River Water Environm, Shanghai 200092, Peoples R China
[2] Chinese Acad Sci, Inst Hydrobiol, State Key Lab Freshwater Ecol & Biotechnol, Wuhan 430072, Peoples R China
基金
中国国家自然科学基金;
关键词
Ceratophyllum demersum L; eutrophic water body; phosphorus release; phosphate sorption; sediment; PHOSPHATE SORPTION; ORGANIC-MATTER; LAKE-SEDIMENTS; BED SEDIMENTS; LAND-USE; RESTORATION; ADSORPTION; RETENTION; RELEASE; BAY;
D O I
10.2166/wst.2015.050
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Substantial research efforts were made to assess the effects of submerged macrophytes on water quality improvement, but information on the mechanism of submerged macrophytes relative to the exchange of phosphorus (P) at the sediment-water interface is very limited. To help fill the void, a popular species, Ceratophyllum demersum L. was chosen to address the effects and mechanisms of submerged macrophyte growth on the processes of P exchange across the sediment-water interface. In treatment mesocosms (planted), equilibrium phosphorus concentration (EPC0) value falls from 68.4 to 36.0 mu g/L, with a mean value of 52.5 mu g/L. Conversely, the distribution coefficient (Kd) value has a predominantly increasing trend. But they are both significantly higher than an unplanted control (p < 0.05). Also, in the planted mesocosm, maximum phosphate sorption capacity (Q(max)) was significantly reduced (4,721-3,845 mg/kg), and most of the linear correlations between different forms of phosphorus and sediment P adsorption parameters were affected (p < 0.05). The EPC0 Percentage Saturation percentages (EPCsat) in planted groups were 325% higher than that in control (p < 0.05). We conclude that C. demersum could promote the release of P from sediments, and soluble reactive phosphorus concentration in overlying water is probably the driving force for P exchange at the sediment-water interface.
引用
收藏
页码:913 / 921
页数:9
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