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Rehabilitation studies on saline land caused by potash mining activity.

机译:钾盐开采活动对盐碱地的修复研究。

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摘要

The salinity at the waste management areas at potash mines is extreme. Saturated brine seeps from the tailings pile and contaminates the surrounding land killing vegetation and affecting soil structure. Conventional saline land reclamation practices cannot be applied directly because of the high salt concentrations and the continued inputs. Some major modifications of saline land reclamation practices are, therefore, required.;The movement of Na upwards in the profile of an area of low salinity was affected by the (Na) in the base of the profile and climate, in the form of evapotranspirational losses. The vegetation cover did not affect the movement of Na. To maintain low (Na) in the soil profiles, the (Na) in the saline base must be kept low and, where possible, the water table kept low.;In the revegetation trials, the movement of Na into the sewage sludge amendments was slower than into the topsoil amendments. This affected the vegetation which became established on the two amendments. The vegetation on the topsoil amendment was all killed after 3 months but the vegetation on the sewage sludge amendment remained for the 3 years of the field trial. Of the five species of grass planted, Agropyron trachycaulum and Elymus junceus proved to be best suited to the saline conditions on the sewage sludge amendment. These species also showed considerable salt tolerance at germination and at the mature stage in the laboratory.;The greenhouse column study also showed that the movement of Na into the topsoil was faster than into the sewage sludge amendment. The surface of the sewage sludge amendment dried out, reducing evaporation from that amendment, indicating that evaporation driving the mass flow of water and Na into the amendment might be the key factor affecting the movement of Na into the two materials.;Some of the factors affecting the movement of NaCl into areas of comparatively low salinity surrounded by extreme salinity were investigated. Methods of rehabilitating extremely saline areas with high NaCl inputs, by applying amendments and using salt tolerant vegetation, were investigated using field plots, a greenhouse column study, laboratory testing of the salinity tolerance of vegetation and the Trasee/Tracon computer model.;The Trasee/Tracon computer model indicated that the surface evaporation from the sewage sludge was less than from the topsoil. The model accurately simulated Na movement in both the field and column studies. Potential revegetation scenarios are also discussed.
机译:钾盐矿废物管理区的盐度极高。饱和盐水从尾矿堆中渗出,污染周围土地,杀死植被并影响土壤结构。由于盐浓度高和投入持续,传统的盐碱土地开垦方法无法直接应用。因此,需要对盐碱地开垦实践进行一些重大修改。在低盐度区域剖面中,Na的向上运动受剖面和气候基础中的(Na)以蒸散作用的形式影响损失。植被覆盖没有影响Na的运动。为了保持土壤剖面中的低(Na),必须将盐碱中的(Na)保持在较低水平,并在可能的情况下将地下水位保持在较低水平。;在植被恢复试验中,将Na运入污水污泥改良剂中的方法是:慢于表土修正案。这影响了在两个修正案中确立的植被。 3个月后,表土改良剂上的植被全部被杀死,但污泥改良剂上的植被在实地试验的3年中仍然保留。在种植的五种草中,Agropyron trachycaulum和Elymus junceus被证明最适合污水污泥改良剂中的盐分条件。这些物种在实验室发芽和成熟阶段也显示出相当高的耐盐性。温室柱研究还显示,Na向表层土壤中的迁移比向污水污泥改良剂中的迁移更快。污水污泥修正物的表面变干,减少了该修正物的蒸发,表明蒸发驱动水和Na的质量流进入修正物,可能是影响Na迁移到两种物质中的关键因素。研究了影响NaCl进入盐度相对较低,被极端盐度包围的区域的运动。通过田间试验,温室大棚研究,植物耐盐度实验室测试和Trasee / Tracon计算机模型,研究了通过应用修正和使用耐盐植被修复高盐分盐度高盐地区的方法。 / Tracon计算机模型表明,污水污泥的表面蒸发少于表层土壤的蒸发。该模型在田间研究和柱研究中都能准确模拟Na的运动。还讨论了潜在的植被恢复方案。

著录项

  • 作者

    Thorpe, Mark Bramley.;

  • 作者单位

    The University of Saskatchewan (Canada).;

  • 授予单位 The University of Saskatchewan (Canada).;
  • 学科 Environmental Sciences.;Engineering Mining.
  • 学位 Ph.D.
  • 年度 1989
  • 页码 182 p.
  • 总页数 182
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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