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首页> 外文期刊>Journal of the American Water Resources Association >OCCURRENCE OF TOTAL DISSOLVED PHOSPHORUS IN UNCONSOLIDATED AQUIFERS AND AQUITARDS IN IOWA
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OCCURRENCE OF TOTAL DISSOLVED PHOSPHORUS IN UNCONSOLIDATED AQUIFERS AND AQUITARDS IN IOWA

机译:IOWA中未溶解的含水层和含水层中总溶解磷的发生率

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Seven sets of ground water samples from 103 observation wells were analyzed for total dissolved phosphorus (TDP) in four areas and five materials including loess and loess derived alluvium in the Deep Loess Hills of western Iowa, outwash and fractured till adjacent to Clear Lake in north central Iowa, fractured till in central Iowa, and a sand and gravel aquifer in northwest Iowa. Land use in ground water recharge zones in all four areas is dominated by crop or animal production or both. Concentrations of TDP exceeding the minimum laboratory detection limit of 20 μg/1 as P were found in all areas and in all materials sampled. Samples from the outwash deposits associated with Clear Lake contained significantly larger concentrations than all other areas and materials with a median of 160 μg/1. Water from fractured till in three areas produced the smallest range of concentrations with a median of 40 μg/1. The mean value of TDP in all sample sets exceeded 50 μg/1, an important ecological threshold that causes increased productivity in lakes and perennial streams and one being considered as a surface water nutrient standard by regulatory agencies. These results clearly show that ground water in essentially all near-surface aquifers and aquitards discharging to Iowa's streams and lakes is capable of sustaining P concentrations of 50 to 100 μg/1 in streams, lakes, and reservoirs. Consequently, even if point discharges and sediment sources of P are substantially reduced, ground-water discharge to surface water may exceed critical thresholds under most conditions.
机译:分析了爱荷华州西部深黄土丘陵地区的黄土和黄土冲积层中的四个区域和五种物质的总溶解磷(TDP),分析了来自103个观测井的七套地下水的总溶解磷(TDP),经过冲刷和压裂直至与北部的Clear Lake相邻爱荷华州中部,直到爱荷华州中部都破裂,爱荷华州西北部有砂砾石含水层。在这四个地区中,地下水补给区的土地利用主要是作物或动物生产或两者兼而有之。在所有区域和所有采样材料中都发现TDP的浓度超过最低实验室检测极限P的20μg/ 1。来自Clear Lake的外溢沉积物样品的浓度明显高于所有其他区域和物质,中位数为160μg/ 1。从裂缝直到三个区域的水产生的最小浓度范围为40μg/ 1。所有样品中TDP的平均值均超过50μg/ 1,这是一个重要的生态阈值,导致湖泊和多年生河流生产力提高,监管机构将其视为地表水养分标准。这些结果清楚地表明,排放到爱荷华州河流和湖泊的几乎所有近地表含水层和水塘中的地下水都能在河流,湖泊和水库中维持50至100μg/ 1的P浓度。因此,即使P的点排放和沉积物来源大大减少,在大多数情况下地下水向地表水的排放也可能超过临界阈值。

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