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Sorption and mobility of arsenic in desert soils when applied with municipal wastewater effluent.

机译:与市政废水一起使用时,砷在沙漠土壤中的吸附和迁移率。

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摘要

Disposal of arsenic (As) concentrates that result from drinking water treatment procedures is a problem that must be considered when developing such procedures. A simple and low cost solution is to land apply the Arsenic concentrates with the municipal wastewater effluent. To examine the extent of arsenic wells across the continental United States that exceed the 10 parts per billion (ppb) maximum contaminant level (MCL), and to select a study site, a geographic information system (GIS) study was performed. Kinetic batch experiments were carried out on three diverse soils collected from a land application facility in New Mexico. Arsenate [As(V)] solutions, in buffer or wastewater effluent, ranging from 5 mg L-1 to 100 mg L-1 , were equilibrated with the soils for 12 to 504 h. Finally, As(V) column breakthrough curve (BTC) experiments were performed on the same three soils in the presence and absence of wastewater effluent, at pore-water velocities of 0.7 and 1.4 cm h-1. One-site and two-site kinetic models were fit to each BTC to determine As(V) sorption over time, and to obtain solute transport parameters including dispersion coefficient (D), retardation factor (R), and partition coefficient (Kd). The GIS study found that 60% of the continental U.S. "high arsenic" wells (> 10 mug L -1 As) were located on farmland, and that these high arsenic wells were located in all regions of the country. The presence of wastewater effluent decreased the sorption of arsenic (decreae of Freundlich Kf values) for As(V) on all soils at all reaction times. Furthermore, wastewater effluent caused the % As(V) sorbed over time to remain low, for all three soils, regardless of the initial As(V) concentration. The presence of wastewater effluent decreased sorption (R) of As(V) for each soil column and pore-water velocity (PWV). Furthermore, wastewater effluent caused the mass recovery of As(V) from all columns to exceed 100%, and may be responsible for desorbing preexisting arsenic from the soils. Thus, it appears that while soil is typically an effective sorbent for As(V) in dimple aqueous solutions, when the contaminant is added with wastewater effluent, its sorption is decreased, and its mobility through soil is increased.
机译:饮用水处理程序产生的砷浓缩物的处置是制定此类程序时必须考虑的问题。一种简单且低成本的解决方案是将砷浓缩物与市政废水一起土地施用。为了检查整个美国大陆上超过10亿分之十(ppb)最大污染物水平(MCL)的砷井的范围,并选择一个研究地点,进行了地理信息系统(GIS)研究。在新墨西哥州的土地施用设施中收集的三种不同土壤上进行了动力学批量实验。缓冲液或废水中砷浓度为5 mg L-1至100 mg L-1的[As(V)]溶液与土壤平衡12至504 h。最后,在存在和不存在废水的情况下,在相同的三种土壤上,以0.7和1.4 cm h-1的孔隙水速度对As(V)柱穿透曲线(BTC)进行了实验。将一个站点和两个站点的动力学模型拟合到每个BTC,以确定随时间的As(V)吸附,并获得包括弥散系数(D),延迟因子(R)和分配系数(Kd)的溶质传输参数。 GIS研究发现,美国大陆有60%的“高砷”井(> 10杯L -1 As)位于农田上,而这些高砷井则分布在美国所有地区。废水流出物的存在降低了所有反应时间所有土壤上砷(V)的砷吸附(Freundlich Kf值降低)。此外,对于三种土壤,无论初始As(V)浓度如何,废水流出物都会导致随时间推移吸附的As(V)的百分比保持较低。废水的存在降低了每个土壤柱的As(V)的吸附(R)和孔隙水速度(PWV)。此外,废水流出物导致所有色谱柱中As(V)的质量回收率超过100%,并且可能负责从土壤中解吸预先存在的砷。因此,似乎在污点水溶液中土壤通常是有效的As(V)吸附剂,但是当污染物与废水一起添加时,其吸附力降低,并且在土壤中的迁移率增加。

著录项

  • 作者

    Nemmers, Sylvia Jean.;

  • 作者单位

    New Mexico State University.;

  • 授予单位 New Mexico State University.;
  • 学科 Agriculture Soil Science.;Geochemistry.;Environmental Sciences.;Water Resource Management.
  • 学位 Ph.D.
  • 年度 2010
  • 页码 88 p.
  • 总页数 88
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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