Dunne E J, Culleton N, O'Donovan G, Harrington R, Daly K
Soil and Water Science Department, University of Florida/IFAS, 106 Newell Hall, P.O. Box 110510, Gainesville, FL 32611, USA.
Water Res. 2005 Nov;39(18):4355-62. doi: 10.1016/j.watres.2005.09.007. Epub 2005 Oct 10.
It may be necessary to use constructed wetlands as a land use practice to mitigate phosphorus (P) loss from agriculture in Ireland. The objectives of this study were to determine the ability of two constructed wetland site soils to retain and sorb P. Intact soil/water column studies were used to determine P release/retention rates during a 30-day incubation period. Soil columns flooded with distilled water released P during the first 2 days; however, soluble reactive P (SRP) concentrations in overlying floodwaters decreased thereafter. Soils with overlying floodwaters spiked at 5 and 15 mg SRP L(-1) retained highest amounts of P (p < 0.05) with retention at these concentrations controlled by SRP in overlying waters. Retention rates by soils ranged between 0.3 and 60.9 mg Pm(-2) d(-1). Maximum P sorption capacity (Smax) was higher for wetland soils at Dunhill, Waterford (1464 mg P kg(-1)) in comparison to soils at Johnstown Castle, Wexford (618 mg P kg(-1)). Equilibrium P concentrations (EPC0) were low (in the microg SRP L(-1) range), indicating a high capacity of these soils to sorb P. Phosphorus sorption parameters were significantly related to ammonium oxalate extractable aluminium (Al) and iron (Fe) content of soils.
在爱尔兰,可能有必要将人工湿地作为一种土地利用方式,以减轻农业磷(P)流失。本研究的目的是确定两个人工湿地土壤保留和吸附磷的能力。采用完整土壤/水柱研究来确定30天培养期内的磷释放/保留率。用蒸馏水淹没的土壤柱在最初2天释放磷;然而,此后上覆洪水中的可溶性活性磷(SRP)浓度降低。上覆洪水中SRP浓度分别为5和15 mg L(-1)时,土壤保留的磷量最高(p < 0.05),这些浓度下的保留情况受上覆水中SRP控制。土壤的保留率在0.3至60.9 mg Pm(-2) d(-1)之间。与韦克斯福德约翰斯敦城堡的土壤(618 mg P kg(-1))相比,沃特福德邓希尔湿地土壤的最大磷吸附容量(Smax)更高(1464 mg P kg(-1))。平衡磷浓度(EPC0)较低(在微克SRP L(-1)范围内),表明这些土壤吸附磷的能力很强。磷吸附参数与土壤草酸铵可提取铝(Al)和铁(Fe)含量显著相关。