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Sediment phosphorus dynamics in tile-fed drainage ditches

机译:瓷砖喂水沟槽中的沉积磷动力学

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Stream sediments may regulate aqueous phase phosphorus (P) concentrations The objectives of this work were to study the equilibrium P concentrations between the aqueous phase and sediments in tile-fed drainage ditches Sediments from three ditches in Indiana, USA, were sampled and evaluated as P sources or sinks. Sediments that potentially release P to aqueous solutions could be chemically amended to sequester labile P. Sediment deposition from episodic storm events could increase the P buffering capacity of drainage ditches In fluvarium studies (initial concentration of 0.55 mM P), aqueous P concentrations after 120 h were 0.075 mM and 0.111 mM for pre-dredged and dredged sediments, respectively. Phosphorus release from sediments to the aqueous solution was greater from the dredged sediments. These studies are expanding our understanding of the dynamic nature of P in agricultural ditches, and aiding in the development of ditch management practices to reduce downstream P transport.
机译:流沉积物可以调节水相磷(P)浓度这项工作的目的是研究从印第安纳印第安纳州印第安纳州的三个沟渠中的瓷砖灌注沟之间的平衡P浓度与美国的三个沟渠进行取样和评估来源或汇。沉积物,潜在地释放到水溶液中的沉积物可以化学修正,以进行化学修正,以螯合稳定性沉积物沉积物沉积物沉积物沉积物沉积物沉积物沉积物沉积物沉积物沉积物可以增加排水沟的P缓冲能力在血液研究中(初始浓度为0.55mm P),120小时后P浓度水溶液浓度预疏浚和疏浚沉积物分别为0.075毫米和0.111毫米。从疏浚沉积物沉积物沉积物中磷释放较大。这些研究正在扩大我们对农业沟渠中P的动态性质的理解,并帮助发展沟渠管理实践,以减少下游P运输。

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