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Evaluation of the impact of pyrite oxidation on rock characteristics and environment by laboratory tests

机译:通过实验室测试评估黄铁矿氧化对岩石特性和环境的影响

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Pyrite is a common and abundant sulfidic mineral subject to oxidation. The weathering characteristics of rock-bearing pyrite sometimes impose serious influences on the surrounding environment as the oxidation of pyrite (FeS_2) generates acid drainage that results in the acceleration of rock weathering and the discharge of heavy metals into the environment. Such an accelerated weathering of rocks can reduce its mechanical properties and therefore menace the stability of rock structures, such as excavated slopes and tunnels. The evolution of physical properties of rocks and the chemical composition of drainage were evaluated in this study by a weathering test using a double Soxhlet extractor for 1 month in a laboratory setting. Three groups of biotite gneiss classified according to their pyrite content were used for the Soxhlet extraction experiment (group A with less than 0.1 wt% of pyrite; group B with about 3.3 wt% of disseminated pyrite; group C with about 5.65 wt% of vein type pyrite). The massive groups A and B had limited weathering on the surface; however, group C with the pyrite vein experienced weathering on the surface as well as along the pyrite vein. The weathering type regulated by the occurrence of pyrite apparently controlled the mechanical properties of the rock samples and the chemistry of the drainage. Groups A and B showed no significant quick absorption ratio after the 1-month experiment; however, group C had about 10 % increase in value. The uniaxial compressive strength of the three groups decreased about 20, 10 and 45 % for groups A, B and C, respectively. The mechanical properties of the samples and the chemical compositions of the drainage indicate that the oxidation of pyrite contained in the samples accelerated weathering, resulting in deterioration of mechanical properties of the rocks, and could result in the discharge of heavy metals and acid into the environment with the drainage.
机译:黄铁矿是一种易氧化的常见且丰富的硫化矿物。含铁黄铁矿的风化特性有时会对周围环境造成严重影响,因为黄铁矿(FeS_2)的氧化会产生酸排泄,从而导致岩石风化的加速和重金属向环境的排放。岩石的这种加速风化会降低其机械性能,因此会威胁岩石结构(例如开挖的边坡和隧道)的稳定性。在这项研究中,通过使用双索氏提取器在实验室环境中进行了1个月的耐候性测试,评估了岩石的物理性能演变和排水的化学成分。索氏提取实验使用了三组按其黄铁矿含量分类的黑云母片麻岩(A组的黄铁矿含量少于0.1 wt%; B组的弥散性黄铁矿含量约为3.3 wt%; C组的静脉含量约为5.65 wt%黄铁矿类型)。大量的甲,乙族在表面的风化作用有限;然而,具有黄铁矿脉的C组在表面以及沿黄铁矿脉都经历了风化。由黄铁矿的发生所调节的风化类型显然控制了岩石样品的机械性能和排水化学。在经过1个月的实验后,A组和B组没有明显的快速吸收率。但是,C组的价值增加了​​约10%。对于A,B和C组,三组的单轴抗压强度分别降低了约20%,10%和45%。样品的机械性能和排水的化学成分表明,样品中所含的黄铁矿的氧化加速了风化作用,导致岩石的机械性能下降,并可能导致重金属和酸排放到环境中。随着排水。

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