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Linkage between land use patterns and sediment phosphorus sorption behaviors along shoreline of a Chinese large shallow lake (Lake Chaohu)

机译:沿着中国大浅湖(巢湖湖)的土地利用模式和沉积物磷吸附行为之间的联系

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摘要

To test the relationship between phosphorus buffering capacity in sediments of littoral zone and land use, seasonal samples were taken from the soils representing different patterns of land use, together with the littoral zone sediments, along shoreline in Lake Chaohu. There existed significantly positive relationships between equilibrium phosphorus concentration (EPC0) and degree of phosphorus saturation (DPS) defined as ratios of Olsen-P, algae available phosphorus (AAP) and inorganic phosphorus (IP) to maximum sorption capacity (Qmax). So, some easily accessible P parameters especially DPS were indicative of EPC0 in the sediments. Furthermore, the contents of IP, total phosphorus (TP) and organic matter (OM) in the sediments were significantly related to those in the soils. Therefore, the soils could provide the littoral zone with IP either directly or indirectly through TP input; it also provided the Olsen-P through the OM input, as evidenced by the relationship between Olsen-P and OM. It meant that the enhanced OM would enlarge the DPS. On the other hand, the increase in OM paralleled with the increases in Qmax, which lower the DPS simultaneously. Thus, the OM modified sediment phosphorus sorption behaviors in complicated manners. Finally, the soil covered by Fleabane was coupled with the sediment whose EPC0 values were lower and further decreased with strong diffusion from the soils after heavy rains. Hence, shoreline soil may input TP including IP and OM into the lake and alter the DPS together with EPC0 thereby regulating the sediment functions to act as sink or source of phosphorus.
机译:为了测试在沿岸区和土地使用的沉积物的磷缓冲能力之间的关系,季节性样品在巢湖从表示土地利用的不同图案的土壤采取与沿岸带沉积物一起沿着海岸线。存在着平衡磷浓度(EPC0)和定义为最大吸附能力(Q最大)奥尔森-P,藻类可利用磷(AAP)和无机磷(IP)的比率磷饱和度(DPS)的程度之间显著正关系。因此,一些方便p参数特别是DPS都说明在沉积EPC0的。此外,IP,总磷(TP)和有机物(OM)的沉积物中的内容物显著涉及那些在土壤。因此,土壤可能直接或间接地提供具有IP沿岸区通过TP输入;它也通过OM输入提供奥尔森-P,由奥尔森-P和OM之间的关系所证明的。这意味着,增强OM将扩大的DPS。在另一方面,在OM的增加平行与最大尿流率的增加,这同时降低了DPS。因此,OM改性在复杂的方式沉淀磷吸附行为。最后,通过灯盏细辛覆盖的土壤加上其EPC0值均较低,并进一步用强扩散降低从土壤大雨之后的沉淀物。因此,海岸线土壤可以输入TP包括IP和OM入湖和与EPC0从而调节沉积物功能充当信宿或磷的源改变DPS在一起。

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