Mukherjee A, Nair V D, Clark M W, Reddy K R
Geological Sci. Dep., 241 Williamson Hall, P.O. Box 112120, College of Liberal Arts and Sciences, Gainesville, FL 32611-2120, USA.
J Environ Qual. 2009 Mar 25;38(3):878-86. doi: 10.2134/jeq2008.0230. Print 2009 May-Jun.
The U.S. Environmental Protection Agency created the Clean Water Action Plan to develop nutrient criteria for four water body types: lakes and reservoirs, rivers and streams, estuaries, and wetlands. Significant progress has been made in open water systems. However, only areas in and around the Florida Everglades have had numeric nutrient criteria set, due to the complexity, heterogeneity, and limited information available for wetlands. Our objective was to evaluate various soil tests to predict significant P release potential of soil in wetlands. A total of 630 surface soil samples (0-10 cm) were collected for this study from four southeastern states: Florida, Alabama, Georgia, and South Carolina. Soil samples were collected from the center of wetlands, the edge of the wetlands, and from adjacent uplands. The phosphorus saturation ratios (PSR), calculated using P, Fe, and Al molar concentrations from Mehlich 1 (M1-PSR), Mehlich 3 (M3-PSR), and oxalate (Ox-PSR) extractions and the amount of P extracted by different extractants were used to predict P loss potential from a soil. Total phosphorus (TP) concentration in wetland soils, estimated as the 75th percentile of the distribution of least impacted wetland soils as an example, was approximately 550 mg kg(-1). Based on this reference background condition, procedures for obtaining threshold values for P release to the surrounding water bodies were developed and threshold values calculated: M1-P = 24 mg kg(-1), M3-P = 44 mg kg(-1), Ox-PSR = 0.079, M1-PSR = 0.101, and M3-PSR = 0.067.
美国环境保护局制定了《清洁水行动计划》,以制定四种水体类型的营养物标准:湖泊和水库、河流和溪流、河口以及湿地。在开放水域系统方面已取得重大进展。然而,由于湿地的复杂性、异质性以及可用信息有限,只有佛罗里达大沼泽地及其周边地区设定了数值营养物标准。我们的目标是评估各种土壤测试方法,以预测湿地土壤中磷的显著释放潜力。本研究从东南部四个州(佛罗里达州、阿拉巴马州、佐治亚州和南卡罗来纳州)共采集了630个表层土壤样本(0 - 10厘米)。土壤样本分别从湿地中心、湿地边缘以及相邻的高地采集。利用通过Mehlich 1(M1 - PSR)、Mehlich 3(M3 - PSR)和草酸盐(Ox - PSR)提取法得到的磷、铁和铝的摩尔浓度计算出的磷饱和度比率(PSR),以及不同提取剂提取的磷量,来预测土壤中磷的流失潜力。以受影响最小的湿地土壤分布的第75百分位数估算的湿地土壤总磷(TP)浓度约为55毫克/千克。基于此参考背景条件,制定了获取向周边水体释放磷的阈值的程序,并计算出阈值:M1 - P = 24毫克/千克,M3 - P = 44毫克/千克,Ox - PSR = 0.079,M1 - PSR = 0.101,M3 - PSR = 0.067。