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Modeling the Risk of the Salt for Polluting Groundwater Irrigation with Recycled Water and Ground Water Using HYDRUS-1 D

机译:使用HYDRUS-1 D模拟盐分对循环水和地下水污染地下水灌溉的风险

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摘要

Long-term irrigation with recycled water (RW) that contains high salt may pollute groundwater. The HYDRUS-1D model was texted against soil water content and electrical conductivity (ECe) observed in a summer maize and winter wheat rotational field irrigated with ground water (GW) and RW; then, the risk for polluting groundwater in two regions of Beijing was evaluated. The comparisons indicated that the simulated soil water content and ECe values were generally in agreement with the field observations, indicating the reliability of HYDRUS-1D in soils irrigated with GW and RW, The regional prediction results of the proposed simulation model indicated that the average soil ECe at the bottom of vadose zones ranged from 0.400 to 0.896 dS m(-1), and the values in the Tongzhou and Daxing Districts irrigated with RW were 1.40 and 1.09 times, respectively, higher than that irrigated with GW over the next 50 years. Five risk indicators represent salt transporting rime and values were used. The results of the proposed evaluation model showed that the risk scores ranged from 3.04 to 9.32. In the Tongzhou and Daxing Districts, the risk scores of RW irrigation for polluting groundwater were 1.06 and 1.08 times, respectively, higher than that GW irrigation. The risk scores of GW or RW irrigation for polluting groundwater in the Tongzhou District were 1.75 or 1.72 times, respectively, higher than that in the Daxing District. Considering the small risk difference between GW and RW irrigations, RW can he used in both regions. Due to the different vadose zone structures, the Daxing District is more suitable for RW irrigation. The long-term use of RW for irrigation should consider the salt content of RW and vadose zone structure.
机译:使用含高盐的循环水(RW)进行长期灌溉可能会污染地下水。将HYDRUS-1D模型针对在以地下水(GW)和RW灌溉的夏玉米和冬小麦旋转田中观察到的土壤含水量和电导率(ECe)进行了建模;然后,评估了北京两个地区的地下水污染风险。比较表明,模拟土壤含水量和ECe值与实地观测结果基本吻合,表明HYDRUS-1D在GW和RW灌溉土壤中的可靠性,所提出的模拟模型的区域预测结果表明,平均土壤渗流区底部的ECe范围为0.400至0.896 dS m(-1),通水灌溉的通州区和大兴区的ECe分别为未来50年的GW的1.40和1.09倍。 。五个风险指标代表盐运输的雾e和使用的值。所提出的评估模型的结果表明,风险评分范围为3.04至9.32。在通州和大兴区,RW灌溉污染地下水的风险得分分别是GW灌溉的1.06倍和1.08倍。通州地区GW或RW灌溉污染地下水的风险得分分别是大兴区的1.75倍或1.72倍。考虑到GW和RW灌溉之间的风险差异很小,可以在两个地区使用RW。由于渗流带结构的不同,大兴区更适合RW灌溉。 RW长期用于灌溉应考虑RW的盐含量和渗流带结构。

著录项

  • 来源
    《Water, Air, and Soil Pollution》 |2016年第6期|189.1-189.22|共22页
  • 作者单位

    China Agr Univ, Coll Water Resources & Civil Engn, 17 Qinghua East Rd, Beijing 100083, Peoples R China;

    China Agr Univ, Coll Water Resources & Civil Engn, 17 Qinghua East Rd, Beijing 100083, Peoples R China;

    China Agr Univ, Coll Water Resources & Civil Engn, 17 Qinghua East Rd, Beijing 100083, Peoples R China;

    Univ New Hampshire, Inst Study Earth Oceans & Space, 8 Coll Rd, Durham, NH 03824 USA;

    Minist Agr, Natl Agrotech Extens & Serv Ctr, 20 Maizidian St, Beijing 100026, Peoples R China;

    China Agr Univ, Coll Water Resources & Civil Engn, 17 Qinghua East Rd, Beijing 100083, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Groundwater; HYDRUS-1D; Polluting groundwater; Recycled water; Risk; Soil salt;

    机译:地下水;HYDRUS-1D;污染地下水;循环水;风险;土壤盐分;
  • 入库时间 2022-08-17 13:38:22

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