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The Release of Endogenous Nitrogen and Phosphorus in the Danjiangkou Reservoir: A Double-Membrane Diffusion Model Analysis

机译:丹江口水库内源性氮和磷的释放:双膜扩散模型分析

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Endogenous contamination from the newly submerged sediment may have an impact on the water quality of the Danjiangkou Reservoir, the water source of the middle route of the South-to-North Water Diversion Project. In this study, in situ sediment samples were collected at different locations (Guojiashan (DJK1), Kongqueyuan (DJK2), Shijiagou (DJK3), Shiqiao Wharf (DJK4), and Songgang Wharf (DJK5) from the north to the south) of the Danjiangkou Reservoir and the upstream tributary using a columnar sediment sampler and statically cultured in laboratory, and the distribution and release of endogenous N and P from the sediment were investigated based on a double-membrane diffusion model. The results showed that the P contents in the main reservoir and the upstream tributary followed the order of . IP accounted for the largest proportion (47.10-59.70%) of total phosphorus (TP), while LP accounted for only a small proportion (0.10-0.90%) of TP. There is a significant difference in the spatial distribution of P at different sampling points, especially for the OP content (226.90?mg·kg -1 ) with a coefficient of variation of 26.90%. The contents of different forms of P and NH 4 + -N decreased from the upstream tributary to the main reservoir, which was mainly attributed to the land use type. In the vertical distribution, the contents of different forms of P in DJK4 and DJK5 decreased with the increase of sediment depth. The contents of NH 4 + -N and PO 4 3- -P in the sediment interstitial water of DJK4 and DJK5 were higher than those in the overlying water. In addition, the contents of NH 4 + -N and PO 4 3- -P were higher in DJK5 than that in DJK4. The static culture experiments showed that N and P were mainly released from the sediment-overlying water interface to the overlying water. The release rate of NH 4 + -N and PO 4 3- -P ranged from 13.08?mg·(m 2 ·d) -1 to 21.39?mg·(m 2 ·d) -1 and from 3.06?mg·(m 2 ·d) -1 to 6.02?mg·(m 2 ·d) -1 , and the release amount calculated based on the double-membrane diffusion model was ?t·a -1 and ?t·a -1 , respectively. Thus, endogenous contamination from the newly submerged land is an important factor affecting the water quality of the Danjiangkou Reservoir.
机译:来自新淹没沉积物的内源性污染可能对丹江口水库的水质产生影响,南水北调项目中间路线的水源。在这项研究中,原位沉积物样本被收集在不同地点(GuojiaShan(DJK1),孔雀园(DJK2),Shiijiagou(DJK3),Shiqiao Wharf(DJK4)和南北到南部的Songgang Wharf(DJK5))丹江口水库和使用柱状沉积物取样器的上游支流和实验室静态培养,以及基于双膜扩散模型研究了来自沉积物的内源性N和P的分布和释放。结果表明,主水库中的P内容和上游支流遵循的顺序。 IP占总磷(TP)的最大比例(47.10-59.70%),而LP仅占TP的小比例(0.10-0.90%)。 P在不同采样点处的P的空间分布存在显着差异,特别是对于OP含量(226.90×mg·kg -1),变异系数为26.90%。不同形式的P和NH 4 + -N的内容从上游支流到主储层的上游支流减少,主要归因于土地使用类型。在垂直分布中,DJK4和DJK5中不同形式的P的内容随着沉积物深度的增加而降低。 DJK4和DJK5的沉积物间质水中NH 4 +--N和PO 4 3--P的含量高于上覆水中的含量。此外,DJK5中NH 4 + -N和PO 4 3--P的内容越高,而不是DJK4。静态培养实验表明,N和P主要从沉积物覆盖水界面释放到上覆水。 NH 4 + -N和PO 4 3--P的释放速率范围为13.08Ωmg·(m 2·d)-1至21.39×mg·(m 2·d)-1和3.06?mg·( m 2·d)-1至6.02?mg·(m 2·d)-1,以及基于双膜扩散模型计算的释放量分别为a-1和a-1 -1 。因此,新淹没的土地的内源性污染是影响丹江口水库水质的重要因素。

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