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Nutrient Content at the Sediment-Water Interface of Tile-Fed Agricultural Drainage Ditches

机译:平铺式农业排水沟沉积物-水界面的养分含量

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Extensive network of tile drains present in the Midwest USA accelerate losses of nutrients to receiving ditches, rivers and eventually to the Gulf of Mexico. Nutrient inputs from agricultural watersheds and their role in affecting water quality have received increased attention recently; however, benthic sediment-nutrient interactions in tile-fed drainage ditches is still a matter of active research in consideration to nutrient discharge from tile drains. In this study, phosphorus (P) and nitrogen (N) contents and variability of nutrient retention ability of benthic sediments upstream and downstream from tile drain outlets were evaluated in managed agricultural drainage ditches in Indiana. Sediment samples were collected every three months upstream and downstream from selected tile drains in three ditches in northwest Indiana. Sediment equilibrium P concentrations (EPC0) were measured to examine P adsorption-desorption and equilibrium characteristics of benthic sediments in the ditches. P sorption index (PSI), exchangeable P (ExP), and exchangeable NH4+-N (ExN) were measured to evaluate nutrient retention ability and readily available nutrient content of benthic sediments. Results indicated a dynamic interaction between benthic sediment and overlying water column where sediments were acting as a sink or a source of P. There were no differences in nutrient retention ability between sediments collected upstream and sediments collected downstream from the selected tile drains. While the data, except for ExN, was comparable to reported values by previous studies in Indiana’s drainage ditches, there was no particular seasonal pattern in the content of exchangeable nutrient content in sediments at all three sites. This study also suggested that nutrient uptake by benthic sediments in these drainage ditches is not always efficient; therefore watershed management should focus on minimizing the delivery of nutrients into ditches while maintaining their drainage functionality.
机译:美国中西部地区广泛存在的瓷砖排水管网络加速了养分流失,这些营养流向了沟渠,河流,最终流向了墨西哥湾。最近,来自农业流域的营养投入及其在影响水质中的作用得到了越来越多的关注;然而,考虑到瓷砖排水沟中养分的排放,瓷砖喂养排水沟中底栖沉积物-养分的相互作用仍然是一个积极的研究问题。在这项研究中,在印第安纳州管理的农业排水沟中评估了瓷砖排水口上游和下游的底栖沉积物中磷(P)和氮(N)的含量以及养分保留能力的变化。每三个月从印第安纳州西北部三个沟渠中选定的排水沟上游和下游收集沉积物样本。测量沉积物的平衡磷浓度(EPC 0 ),以检查沟中底栖沉积物对磷的吸附-解吸和平衡特性。测量了P的吸收指数(PSI),可交换的P(ExP)和可交换的NH 4 + -N(ExN),以评估养分保持能力和易获得的养分含量底栖沉积物。结果表明,底栖沉积物与上层水柱之间的动力相互作用,其中沉积物充当磷的汇或源。在选定的排水沟上游收集的沉积物和下游收集的沉积物之间的养分保留能力没有差异。尽管除ExN以外的数据与印第安纳州排水沟的先前研究报告的值相当,但在所有三个地点的沉积物中可交换营养成分的含量并没有特定的季节性模式。这项研究还表明,在这些排水沟中底栖沉积物对养分的吸收并不总是有效的。因此,流域管理应着重于最大程度地减少养分向沟渠中的输送,同时保持其排水功能。

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