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The effects of red soil in removing phosphorus from water column and reducing phosphorus release from sediment in Lake Taihu

机译:红壤对太湖水柱除磷及减少底泥中磷释放的影响

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摘要

A natural red soil and a lanthanum-modified soil (LMS) were tested to compare their phosphorus (P) adsorption capacities and their effectiveness in removing P from the water column and reducing P release from sediment. The equilibrium of P adsorption demonstrated that the maximum P adsorption for the soil was 1.29 and 2.22 mg g~(-1) at pH 8.5 and 5.5, respectively, and for the LMS these were increased by 45.6 and 77.6% at pH 8.5 and 5.5, respectively, indicating that the soil was effective in P adsorption and the doping of lanthanum could substantially increase P adsorption. The sediment-water column incubation showed that, due to the P adsorption of the soil and LMS, the total P in the water column decreased by 58.5, 60.6, 68.2 and 77.2% for 180 g m~(-2) soil, 900 g m~(-2) soil, 180 g m~(-2) LMS and 900 g m~(-2) LMS treated systems, respectively, in a short time (6 h), and the capping layer substantially reduced the P release from sediment during column incubation, indicating that the soils were effective in reducing internal P load. However, considering the cost of LMS, the natural soil was suggested to be a cost-effective material to control internal P load.
机译:测试了天然的红色土壤和镧改性的土壤(LMS),以比较它们对磷(P)的吸附能力以及它们从水柱中去除磷和减少磷从沉积物中释放的有效性。磷的吸附平衡表明,在pH 8.5和5.5下,土壤对P的最大吸附量分别为1.29和2.22 mg g〜(-1);对于LMS,在pH 8.5和5.5下,土壤的最大P吸附量分别增加了45.6和77.6%。分别表明土壤对磷的吸附有效,而镧的掺杂可大大提高磷的吸附。沉积物-水柱的温育表明,由于土壤和LMS对P的吸附,对于180 gm〜(-2),900 gm〜的土壤,水柱中的P总量分别降低了58.5、60.6、68.2和77.2%。 (-2)在短时间内(6 h)分别处理了180 gm〜(-2)LMS和900 gm〜(-2)LMS处理过的系统,并且封盖层显着减少了色谱柱期间沉积物中的P释放温育表明土壤有效减少了内部磷负荷。但是,考虑到LMS的成本,建议将天然土壤作为控制内部P负荷的经济有效材料。

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