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Effects of pH, Temperature, Dissolved Oxygen, and Flow Rate on Phosphorus Release Processes at the Sediment and Water Interface in Storm Sewer

机译:pH,温度,溶解氧和流速对雨水管道沉积物和水界面磷释放过程的影响

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摘要

The effects of pH, temperature, dissolved oxygen (DO), and flow rate on the phosphorus (P) release processes at the sediment and water interface in rainwater pipes were investigated.The sampling was conducted in a residential storm sewer of North Li Shi Road in Xi Cheng District of Beijing on August 3, 2011. The release rate of P increased with the increase of pH from 8 to 10. High temperature is favorable for the release of P. The concentration of total phosphorus (TP) in the overlying water increased as the concentration of DO decreased.With the increase of flow rate from 0.7ms~(?1) to 1.1ms~(?1), the concentration of TP in the overlying water increased and then tends to be stable. Among all the factors examined in the present study, the flow rate is the primary influence factor on P release.The cumulative amount of P release increased with the process of pipeline runoff in the rainfall events with high intensities and shorter durations. Feasible measures such as best management practices and low-impact development can be conducted to control the P release on urban sediments by slowing down the flow rate.
机译:研究了pH,温度,溶解氧(DO)和流速对雨水管中沉积物和水界面处磷(P)释放过程的影响。于2011年8月3日在北京西城区发生。磷的释放速率随pH值从8升高到10而增加。高温有利于磷的释放。上覆水中总磷的浓度随着DO浓度的降低而增加。随着流速从0.7ms〜(?1)增加到1.1ms〜(?1),上覆水中的TP浓度增加,然后趋于稳定。在本研究中考察的所有因素中,流速是影响P释放的主要因素。在高强度,持续时间较短的降雨事件中,P释放的累积量随管道径流的过程而增加。可以采取可行的措施,例如最佳管理实践和低影响的发展,以通过减缓流速来控制城市沉积物中磷的释放。

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