毛细管向上传质作为集中区生长的过程

A. Mikhailov, I. Vashlaev, M. Y. Kharitonova, M. L. Sviridova
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摘要

地面和大气水分通过从地表蒸发和从大气到地表降水的自然循环过程导致表层土壤的定植。土壤中盐的主要来源是地下水。地下水到达表层土壤并蒸发,其组成盐在土壤中积累。表面盐的浓度可达100%(地壳)。这个过程很普遍。大片的solonetzes分布在亚洲、澳大利亚、南美洲、北非和美国西部的沙漠和半沙漠中。这种自然过程可以应用于从肠道中提取自然资源的领域。盐化土壤表面的过程是缓慢而渐进的,需要研究是否可能用于提取矿物的技术解决方案。在本章中,作者打算说明土壤表层盐渍化现象的有利优势。水溶性盐由于其高流动性,允许沿土壤毛细管系统的定向传质和在通气区的沉积。然而,这种效用并不属于植物生物群。这种现象可以有效和安全地用于近地表集中区的创建。盐溶液从地块深处向上过滤到地表的自然过程将有目的地进行有价值成分的转移,并在蒸发屏障区域沉积。从技术上讲,上升毛细传质过程的速度较低,但相当适合作为工业废物储存和掩埋地点以及小型不合格天然矿藏高度集中地区形成的准备操作。本章介绍了有色金属浓缩生产废料中有用组分传质提升的实验研究结果。
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Upward Capillary Mass Transfer as a Process for Growing Concentration Zones
The natural process of circulation of ground and atmospheric water through evaporation from the surface and precipitation from the atmosphere to the surface leads to colonization of the surface soil layer. The main source of salts in the soil is groundwater. Groundwater reaches the surface soil layer and evaporates, and its constituent salts accumulate in the soil. The concentration of salts on the surface can reach to 100% (crust). This process is widespread. Vast areas of solonetzes are located in deserts and semideserts of Asia, Australia, South America, northern Africa, and the western United States. This natural process can be applied in the field of extraction of natural resources from the bowels. The process of salting the soil surface is low and gradual and is subject to study for possible use in technological solutions for the extraction of minerals. In this chapter, the authors intend to show the beneficial advantages of the phenomenon of surface salinization of the soil layer. Water-soluble salts due to their high mobility allow directional mass transfer along the capillary system of the soil and deposition in the aeration zone. However, the utility does not belong to plant biota. This phenomenon can be effective and safely used in the creation of near-surface concentration zones. The natural process of the filtration upward of salt solutions from the depths of the massif to the surface will purposefully carry out the transfer of valuable components with deposition in the area of the evaporation barrier. The speed of the process of ascending capillary mass transfer is technologically low but rather suitable as a preparatory operation at the place of storage of industrial wastes and burials and in the formation of zones of high concentration of small substandard natural mineral deposits. The chapter presents the results of experimental studies of ascending mass transfer of useful components from the waste material of the concentrating production of nonferrous metals.
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