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The Effects of Structural Characteristics of Low Seepage Sandstone Uranium Ore Rock on Permeability

机译:低渗砂岩铀矿石岩石结构特征对渗透性的影响

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It is great important for the development of China's uranium mining to efficiently extract low seepage sandstone uranium ore rock. It is the objective of this paper to present the effects of the structural characteristics of the low seepage sandstone uranium ore rock on permeability. Samples of sandstone from a uranium mine in XinJiang province were used to carry out experimental research on permeability. These tests were carried out on ore rock with particle size and distribution characteristics determined by a homemade permeability test device. The research indicates that the sandstone uranium deposits may be classified as low seepage because the particle size falls within the range 0.1~1.6mm, that the distribution of particle sizes observed conforms to low seepage fractal characteristics, the permeability decreases when the value of the ore particle size distribution of fractal dimensions increases, and the permeability decreases with particle size decreasing, and that the decrease of the permeability is not a linear change, but is an obviously exponentially decreasing functional relationship.
机译:对中国铀矿业的发展有效提取低渗漏砂岩铀矿石是非常重要的。本文的目的是呈现低渗流砂岩铀矿石岩石上的结构特征对渗透性的影响。新疆铀矿的砂岩样品用于对渗透率进行实验研究。这些试验在矿石上进行,粒度和由自制渗透性测试装置确定的分布特性。该研究表明,砂岩铀沉积物可以被分类为低渗出,因为粒度落在0.1〜1.6mm的范围内,所以观察到粒度的分布符合低渗流分形特征,当矿石的值时渗透率降低分形尺寸的粒度分布增加,并且渗透性随粒径减小而降低,并且渗透性的降低不是线性变化,而是一种明显的幂态关系。

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