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Effects of Effluent Irrigation on Seal Formation, Infiltration, and Soil Loss during Rainfall

机译:降雨过程中污水灌溉对海豹形成,入渗和土壤流失的影响

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摘要

The use of effluent for irrigation could affect the chemical and hydraulic properties of soils due to its high salt and organic matter (OM) content, and, consequently, the rainfall–infiltration–runoff–erosion relationships during the subsequent rainy season. This study investigates the effects of long-term effluent irrigation on soil chemical properties, seal formation, infiltration, and soil loss under rainfall. Simulated rainfall (85 mm) was applied to (i) air-dried or (ii) prewetted clay and sandy soils from plots that had been irrigated with fresh water (FW) or effluent for >10 yr. Effluent irrigation increased the total OM content and the exchangeable sodium percentage (ESP) of the soils. The cumulative infiltration in FW- and effluent-irrigated clay soils was 6.5 and 5.6 mm, respectively, in the initially dry soils, and 52.3 and 51.5 mm, respectively, in the prewetted soils. In the FW- and effluent-irrigated sandy soils, the corresponding values of cumulative infiltration were 79.5 and 44.7 mm, and 85.0 and 56.3 mm, respectively. In the sandy soil, the higher sodium adsorption ratio (SAR) values in the leachate of effluent-irrigated soil led to greater clay dispersion, which enhanced seal formation, reduced infiltration, and increased soil loss. In the clay soil, slaking was the main process involved in seal formation, neglecting the possible deleterious effect of effluent irrigation. When slaking was prevented, the SAR values in the leachate of the effluent-irrigated soil decreased during rainfall and were similar to those of the FW-irrigated soil at the end of the applied rainfall amount. This was probably due to the exchange of adsorbed Na with soluble Ca, which minimized the differences in clay dispersion, infiltration, and soil loss. Therefore, in the clay soil, aggregate slaking might be the main process involved in seal formation and affecting infiltration and erosion. These results show that the effect of effluent irrigation on infiltration, runoff, and soil loss depends on the soil type (amount of clay and CaCO3) and the dominant mechanisms of seal formation. Therefore, to prevent a possible deleterious effect on soil structure, it is necessary to identify sensitive areas and soils before the application of effluents for irrigation.
机译:由于污水中的盐分和有机质(OM)含量高,因此,降雨渗入可能会影响土壤的化学性质和水力性质。随后雨季中的–runoff–erosion 关系。这项研究 研究了长期污水灌溉对降雨条件下 土壤化学性质,密封形成,渗透和 土壤流失的影响。 应用于(i)风干或(ii)用淡水(FW)灌溉的 地盘中预先湿润的粘土和沙土上的模拟降雨(85 mm)或流出物 超过10年。污水灌溉增加了土壤的总OM含量 和土壤交换性钠百分比(ESP)。在最初干燥的土壤中, 和52.3分别在FW和污水灌溉的黏土 中的 累积入渗分别为6.5和5.6 mm。在预湿润的土壤中分别为51.5 mm。 在FW和污水灌溉的沙质土壤中,相应的 累积入渗值分别为79.5和44.7 mm,以及 85.0和56.3毫米。在沙质土壤中,流出物灌溉的土壤中渗出液中较高的钠吸附率(SAR)值导致更大的粘土分散,从而增强了密封的形成, 减少了渗透,增加了土壤流失。在黏土中, 解冻是形成海豹的主要过程,忽略了 污水灌溉的可能有害作用。如果防止 结块,则 灌溉土壤的渗滤液中的SAR值在降雨期间会降低,并且与FW-F相似。施加的 降雨量结束时的灌溉土壤。这可能是由于吸附的 Na与可溶性Ca的交换,这使粘土 的分散,入渗和土壤流失的差异最小化。因此,在黏土 中,团粒的剥落可能是 印章形成并影响渗透和侵蚀的主要过程。这些 结果表明,污水灌溉对土壤入渗, 径流和土壤流失的影响取决于土壤类型(粘土 和CaCO < sub> 3 )和密封形成的主要机制。因此, 为防止可能对土壤结构造成的有害影响, 有必要在 灌溉废水应用之前确定敏感区域和土壤。

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  • 来源
    《Soil Science Society of America Journal》 |2005年第5期|1432-1439|共8页
  • 作者单位

    Institute of Soil, Water and Environmental Sciences, the Volcani Center, Agricultural Research Organization, P.O. Box 6, Bet Dagan, 50250, Israel;

    Institute of Soil, Water and Environmental Sciences, the Volcani Center, Agricultural Research Organization, P.O. Box 6, Bet Dagan, 50250, Israel;

    Institute of Soil, Water and Environmental Sciences, the Volcani Center, Agricultural Research Organization, P.O. Box 6, Bet Dagan, 50250, Israel;

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