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Impact of sulfate and chloride on sediment phosphorus release in the Yangtze Estuary Reservoir, China

机译:硫酸盐和氯化物对长江口水库底泥磷释放的影响

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摘要

The impact of sulfate (SO_4 ~(2-) and chloride (Cl~-) on phosphorus (P) release from sediment in the drinking water reservoir of Yangtze River Estuary was studied systematically. A significant correlation between sodium (Na~+), Cl~-, SO_4 ~(2-) and total P was found, suggesting that P was directly or indirectly associated with these ions. SO_4 ~(2-) and Cl - were important factors that had an impact on P release from the sediment. The results showed that both sulfate and chloride enhanced phosphorus release from sediment. In the sulfate treatment, the decrease of organic phosphorus (OP) suggested that the mineralization of OP enhanced P release from sediment. Phosphonate was the main factor affecting the P release under sulfate condition. In chloride treatment, the sediment composition of iron (Fe), aluminum (Al), calcium (Ca) and magnesium (Mg) increased. The P fractions of Fe/Al-P, Ca-P and OP in sediment also increased. However, the increase of P was unstable after chloride treatment and was easy to release under disturbance. In this study, it was observed that sulfate and chloride could increase the risk of eutrophication in the Yangtze River Estuary drinking water reservoir.
机译:系统研究了硫酸盐(SO_4〜(2-)和氯化物(Cl〜-)对长江口饮用水水库沉积物中磷(P)释放的影响,其中钠(Na〜+),发现Cl〜-,SO_4〜(2-)和总磷,表明P与这些离子直接或间接缔合,SO_4〜(2-)和Cl-是影响P从沉积物中释放的重要因素。结果表明,硫酸盐和氯化物均增加了底泥中磷的释放,在硫酸盐处理过程中,有机磷(OP)的减少表明,OP的矿化作用增强了底泥中磷的释放,其中磷酸盐是影响磷释放的主要因素。在氯化物处理中,铁(Fe),铝(Al),钙(Ca)和镁(Mg)的沉积物组成增加,沉积物中Fe / Al-P,Ca-P和OP的P分数也增加氯化物处理后磷的增加不稳定且容易在干扰下释放。在这项研究中,观察到硫酸盐和氯化物会增加长江口饮用水水库富营养化的风险。

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