Evaluation of in situ capping with clean soils to control phosphate release from sediments.
Evaluation of in situ capping with clean soils to control phosphate release from sediments.
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DOI:
10.1016/j.scitotenv.2012.08.053
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发表时间:
2012-11
期刊:
影响因子:
--
通讯作者:
Di Xu;S. Ding;Qin Sun;Ji-cheng Zhong;Wei Wu;Fei Jia
中科院分区:
文献类型:
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作者:
Di Xu;S. Ding;Qin Sun;Ji-cheng Zhong;Wei Wu;Fei Jia
Evaluation of in situ capping with clean soils to control phosphate release from the sediments of a eutrophic bay in Lake Taihu was performed after 18months of capping. The concentrations of dissolved reactive phosphate (DRP) in pore waters and DRP resupply from native sediments and capped sediments were determined using high-resolution dialysis (HR-Peeper) and a Zr-oxide diffusive gradients in thin films (Zr-oxide DGT) technique. The adsorption isotherm of these sediments was further investigated using a modified Langmuir model. The results showed low concentrations of DRP in pore waters with a low resupply from the sediments for sustaining pore water DRP concentration after capping. The calculated flux to the overlying water following the capping treatment was approximately half of that for the native sediments, implying that the capping reduced the release of phosphate from the sediments. The low resupply of the sediments after capping was further demonstrated by larger partitioning coefficient (Kp) values and greater adsorption capacity (Qmax) values, while zero equilibrium concentrations (EPC0s) were similar to those in native sediments. The larger Kpand Qmaxwere attributed to higher active Fe and Al introduced by the capping, indicating that the binding of phosphate onto the active Fe and Al played a critical role in reducing the internal loading of phosphorous.