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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Subsurface hydrochemical precision treatment of a coastal acid sulfate soil
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Subsurface hydrochemical precision treatment of a coastal acid sulfate soil

机译:沿海酸性硫酸盐土壤地下液体精密处理

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Some of the most economically valued soils for agricultural use are naturally occurring sulfide rich sediments. However, formation of acid sulfate soils with sulfuric materials (pH = 4) can occur when sulfidic materials are exposed to air, which can then result in mobilisation of large amounts of acid and metals into nearby water bodies. In this study, controlled drainage, subsurface irrigation and hydrochemical precision treatments are combined to reduce acidic discharges on a novel project field in western Finland. The PRECIKEM project field consists of nine identical hydrologically isolated 1 ha subfields. Each field had a drainage system consisting of three subsurface drainage pipes (c. 1.3m deep), a collector pipe, and a control well enabling manual ground-water table management. Utilising such drainage installations already common on farmlands, suspensions of fine-grained (d(50) = 2.5 mu m) calcium carbonate and/or calcium hydroxide were pumped in to control wells in order to be distributed in to subsoils with sulfuric materials via drainage networks with the aim to: (1) neutralise acidity, (2) inhibit microbially mediated sulfide oxidation and (3) immobilise metals. The discharge waters from the fields were monitored during the project period 2012-2016. As is typical for acid sulfate soils with sulfuric materials, the discharge waters from the reference fields (n = 3) that had been treated with water only, had very low pH values (= 4) and the acidity and concentrations of several metals were up to two magnitudes higher than the average in Finnish stream waters. Excavation of selected treated fields revealed the calcium carbonate to have formed a neutralising coating on the surfaces of hydrologically active macropores in the soil matrix near the subsurface drainage pipes. This effectively resulted in a long-term (1-4 years) situation of raised pH, lower acidity and lower concentrations of several acid sensitive metals, most prominently a significant de
机译:一些农业使用的一些最经济价值的土壤是天然存在的硫化物丰富的沉积物。然而,当亚硫酸盐暴露于空气时,可以形成硫酸硫酸盐(pH& = 4)的酸性硫酸盐土壤的形成,然后可以将大量的酸和金属流入附近的水体中。在该研究中,组合控制的排水,地下灌溉和水化精密治疗,以减少芬兰西部新型项目领域的酸性排放。 Precikem项目字段由九个相同的水文隔离1个HA子场组成。每个领域都有一个排水系统,由三个地下排水管(C.1.3M深),收集管和控制良好的手动地面水位管理组成。利用在农田上已经常见的这种排水装置,施加细细颗粒(D(50)=2.5μm)碳酸钙和/或氢氧化钙的悬浮液,以通过引流分配给硫材料的亚底分布旨在:(1)中和酸度,(2)抑制微生物介导的硫化物氧化和(3)固定金属。在2012 - 2016年项目期间监测来自领域的排放水域。与硫酸磺酸盐含有硫酸的典型典型的酸性硫酸盐,从仅用水处理的参考领域(n = 3)的排出水具有非常低的pH值(& = 4)和几种金属的酸度和浓度高于芬兰流水域的平均值高出两个大小。所选处理领域的挖掘显示碳酸钙在地下排水管附近的土壤基质中的水文活性大麦孔的表面上形成了中和涂层。这有效地导致了长期(1-4岁)的升高的pH,较低且较低浓度的几种酸敏感金属的情况,最突出的缺点

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