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    SO4−Na·Ca型矿井水难沉降颗粒物在不同离子条件下的分散稳定性特征

    Dispersion stability characteristics of SO4−Na·Ca type mine water-resistant settling particle under different ion conditions

    • 摘要: 煤矿矿井水中颗粒物由黏土、煤粉及少量非黏土矿物组成,具有细小的粒径分布和明显的煤岩表面特性,在矿井水中表现出较高的分散稳定性,成为矿井水处理的重点。选取山西省西山矿区典型SO4−Na·Ca型矿井水,通过沉降实验分离出难沉降颗粒物并对其物理及组分特征进行解析。通过设计单因素变量实验分析难沉降颗粒物在该水型典型阳离子(Ca2+、Mg2+、Na+)及阴离子(Cl、\mathrmSO_4^2- )变化下表现出的分散稳定性差异,基于颗粒物表面Zeta电位分布和DLVO理论计算从微观层面对水化学性质对颗粒间作用行为的影响机制进行探究。研究结果表明:随着阳离子 Ca2+、Mg2+、Na+浓度的增加,矿井水难沉颗粒物分散稳定性逐步降低,颗粒物表面Zeta 电位绝对值和颗粒间排斥势能逐渐减小,减小程度为Ca2+>Mg2+>Na+,其中Ca2+在20 mmol/L时颗粒间排斥势能的能垒由4.77 \times 10−18 J降低至1.05 \times 10−18 J,Zeta电位绝对值由53.7 mV降低至6.2 mV。阴离子变量条件下,20 mmol/L MgSO4的颗粒物Zeta电位绝对值相较于20 mmol/L MgCl2增加了7 mV,颗粒间排斥势能能垒由2.06 \times 10−18 J升高至3.66 \times 10−18 J,表明\mathrmSO_4^2- 相较于C1增加了难沉降颗粒物分散稳定性与颗粒间排斥势能。这一发现有助于根据水化学类型优化混凝处理,对矿井水的再生利用具有重要意义。

       

      Abstract: Particulate matter in mine water is composed of clay, pulverized coal and a small amount of non-clay minerals, which has fine particle size distribution and obvious coal-rock surface characteristics, and shows high dispersion stability in mine water, which has become the focus of mine water treatment. The typical SO4−Na·Ca type mine water in Xishan mining area of Shanxi Province is selected, and the particles which are difficult to settle are separated by sedimentation experiment, and their physical and component characteristics are analyzed. Single-factor variable experiments were designed to analyze the differences in dispersion stability of difficult settling particles under the changes of typical cations (Ca2+, Mg2+, Na+) and anions (C1, \mathrmSO_4^2- ) of the water type. Based on the Zeta potential distribution on the surface of particles and the DLVO theoretical calculation, the mechanism of the influence of water chemical properties on the interaction behavior of particles was investigated from the microscopic level. The results show that with the increase of cationic Ca2+, Mg2+ and Na+ concentrations, the dispersion stability of refractory particles in mine water gradually decreases, and the absolute Zeta potential on the surface of particles and the repulsion potential energy between particles gradually decrease, and the reduction degree is Ca2+>Mg2+>Na+. When Ca2+ is at 20 mmol/L, the energy barrier of intergranular repulsion potential energy decreases from 4.77×10−18 J to 1.05×10−18 J, and the absolute value of Zeta potential decreases from 53.7 mV to 6.2 mV. Under the condition of anionic variable, the absolute Zeta potential of 20 mmol/L MgSO4 particles increased by 7 mV compared with 20 mmol/L MgCl2, and the potential energy barrier of interparticle repulsion increased from 2.06×10−18 J to 3.66×10−18 J. It is shown that \mathrmSO_4^2- compared with C1 increases the stability and interparticle repulsion potential energy of the dispersion system. This discovery is helpful to optimize coagulation treatment according to the type of water chemistry, and has important significance for the recycling of mine water.

       

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