首页> 外文期刊>Transactions of the ASABE >DISSOLVED PHOSPHORUS TRANSPORT DURING STORM AND BASE FLOW CONDITIONS FROM AN AGRICULTURALLY INTENSIVE SOUTHEASTERN COASTAL PLAIN WATERSHED
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DISSOLVED PHOSPHORUS TRANSPORT DURING STORM AND BASE FLOW CONDITIONS FROM AN AGRICULTURALLY INTENSIVE SOUTHEASTERN COASTAL PLAIN WATERSHED

机译:农业密集型东南沿海平原流域暴雨和基流条件下的溶解态磷运移

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摘要

The high density of animal production in southeastern Coastal Plain watersheds has caused some soils to contain excess amounts of plant-available soil phosphorus (P). Runoff, erosion, and leaching can transport P to surface water systems and out of these watersheds. High P concentrations in downstream aquatic ecosystems can increase the risk of eutrophication. Our objectives were to determine stream dissolved phosphorus (DP) mass loads transported under storm and base flow conditions and to examine relationships between precipitation, stream flow, and DP concentrations and export loads from an agriculturally intensive Coastal Plain watershed. This watershed was separated into four subwatersheds, and stream flows at their outlets were separated into base and storm flow conditions. Over the 2-year study period, stream base flow accounted for the majority of total stream flow at all outlets (58% to 73%). Average stream total DP mass loads at the watershed outlet in 1994 and 1995 were 234 and 477 mg DP ha -1 d -1 , and higher DP mass loads (57% to 71% of the cumulative total) were exported during base flow conditions. In 1995, a series of intense storm events over two months caused a large DP pulse (approximately 63% of the stream’s yearly annual DP mass load) to exit the watershed. Regression analysis showed a linear relationship (P 0.001) between log 10 instantaneous stream flow and log 10 DP export. Our results showed that more DP was exported during stream base flow conditions. However, intensive summer storms can greatly accelerate stream DP export from this agriculturally intensive Coastal Plain watershed
机译:东南沿海平原流域的高动物生产密度导致一些土壤中含有过量的植物可利用的土壤磷(P)。径流,侵蚀和淋滤可将P运到地表水系统,并从这些流域中运出。下游水生生态系统中的高P浓度会增加富营养化的风险。我们的目标是确定在风暴和基础流量条件下运输的河流溶解磷(DP)质量负荷,并检查降水量,河流流量和DP浓度与农业密集型沿海平原流域的出口负荷之间的关系。该流域分成四个子流域,其出口处的水流分为基础流和暴雨流条件。在为期2年的研究期内,河流基本流量占所有出口总流量的大部分(58%至73%)。 1994年和1995年,流域出口处的平均河道总DP负荷为234和477 mg DP ha -1 d -1 ,且DP负荷较高(57%在基本流量条件下,出口了总计的71%)。 1995年,历时两个月的一系列强烈风暴事件导致了大的DP脉动(约占河流年度DP年度负荷的63%)离开分水岭。回归分析显示log 10 瞬时流与log 10 DP出口之间的线性关系(P <0.001)。我们的结果表明,在流基流条件下,更多的DP被出口。但是,夏季强烈的暴风雨可以大大加速该农业密集型沿海平原流域的流DP出口

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