Occurrence of total dissolved phosphorus in unconsolidated aquifers and aquitards in Iowa

被引:30
作者
Burkart, MR
Simpkins, WW
Morrow, AJ
Gannon, JM
机构
[1] USDA ARS, Natl Soil Tilth Lab, Ames, IA 50011 USA
[2] Iowa State Univ, Dept Geol & Atmospher Sci, Ames, IA 50011 USA
[3] Iowa Geol Survey, Iowa City, IA 52241 USA
来源
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION | 2004年 / 40卷 / 03期
关键词
ground water hydrology; nonpoint source pollution; water quality; phosphorus; agriculture; till; loess; alluvium;
D O I
10.1111/j.1752-1688.2004.tb04461.x
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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 mug/l 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 mug/l. Water from fractured till in three areas produced the smallest range of concentrations with a median of 40 mug/l. The mean value of TDP in all sample sets exceeded 50 mug/l, 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 mug/l 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.
引用
收藏
页码:827 / 834
页数:8
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