Impact of wastewater irrigation on the dynamics of metal concentration in the vadose zone: simulation with NETPATH--part II.

Abstract

Understanding and quantification of geochemical processes in vadose zone of sewage-effluent-irrigated soils are helpful in predicting the transference of metals and other ions to food chain and groundwater. Hence, an attempt has been made to simulate various geochemical processes occurring in the flow path of infiltrating sewage water down the vadose zone with the help of Net Geochemical Reaction Along the Flow Path (NETPATH). This study area was located in Western Delhi, India, where sewage effluents originating from Keshopur Sewage Treatment plant have been used for irrigation since 1979. Agricultural lands receiving irrigation through sewage and tube well water were selected for this study. The results indicated that groundwater of 20- and 10-year sewage-irrigated lands was slightly oversaturated in respect of calcite and dolomite, and undersaturated in respect of gypsum. The shallow groundwater of 5-year sewage-irrigated field was undersaturated in case of calcite, dolomite, and gypsum. Among the metals, major focus was given on Fe and Mn as these two metals are redox prone and relatively more mobile than other metals under saturated conditions. There was reduction in concentration of Fe and Mn in groundwater samples of 20-year sewage-irrigated field as compared to that in sewage effluent. Such reduction in concentration of Fe and Mn could be ascribed to the formation of goethite and manganite in vadose zone, respectively, as revealed by simulation with NETPATH. Similarly, in case of 10- and 5-year sewage-irrigated fields, increase in Fe and Mn concentrations in groundwater was due to dissolution of siderite and pyrulusite, respectively. NETPATH software could explain the variation in diethylene triamine pentaacetic acid (DTPA)-extractable Fe and Mn content in vadose zone to the extent of 94 and 65%, respectively.