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Phosphorus enrichment in floodplain subsoils as a potential source of freshwater eutrophication

机译:洪泛区磷富集作为淡水富营养化的潜在来源

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Despite decades of management efforts, freshwater eutrophication has not been effectively mitigated in each affected ecosystem. This might be due to insufficient knowledge of the sources of phosphorus (P) inputs into surface waters. We sampled 2 m-deep soil profiles in four floodplain areas under differently managed grassland in Germany under dry and moist conditions regarding soil moisture and precipitation. Four soil P fractions of decreasing solubility were determined. We found systematic enrichment of easily soluble P forms in the floodplain subsoils (average: from 87.5 cm depth). Water-soluble P in these "deep P stocks" was positively correlated with total phosphorus concentrations in the adjacent surface waters. Our data cautiously suggest increased P mobilization from deep P stocks under moist conditions. Drier conditions coincided with increased P retention, resulting in relatively large amounts of easily soluble P which could readily be desorbed and lost at the next stronger precipitation event. We found no effects of grassland management on deep P stock features and dynamics. Deep P stocks might be considered a new source of diffuse P losses from soils. To effectively mitigate freshwater eutrophication, best management practices need to be developed to minimize P transfer from deep P stocks.
机译:尽管数十年的管理努力,但在每个受影响的生态系统中尚未有效减轻淡水富营养化。这可能是由于对表面水域的磷(P)的来源的知识不足。我们在德国不同管理的草原下的四个洪泛区采样了2个M深的土壤曲线,在土壤水分和降水的干燥和潮湿条件下。测定了溶解度降低的四种土壤p部分。我们发现在洪泛区解基质中易溶的P形式(平均值:87.5cm深度),我们发现系统富集。在这些“深层P股”中的水溶性P与相邻表面水中的总磷浓度正相关。我们的数据谨慎提示,在潮湿条件下从深层P库存增加P动员。干燥条件与P保留增加,导致相对大量的易溶性P,可以在下一个更强大的降水事件下容易地解吸并丢失。我们发现草地管理对深层P股功能和动态的影响。深层P股票可能被认为是土壤中漫射P损失的新来源。为了有效减轻淡水富营养化,需要开发最佳管理实践,以最大限度地减少深层P股票的P转移。

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