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Dissolution of minerals with rough surfaces

机译:用粗糙表面溶解矿物质

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We study dissolution of minerals with initial rough surfaces using kinetic Monte Carlo simulations and a scaling approach. We consider a simple cubic lattice structure, a thermally activated rate of detachment of a molecule (site), and rough surface configurations produced by fractional Brownian motion algorithm. First we revisit the problem of dissolution of initial flat surfaces, in which the dissolution rate r(F) reaches an approximately constant value at short times and is controlled by detachment of step edge sites. For initial rough surfaces, the dissolution rate r at short times is much larger than r(F); after dissolution of some hundreds of molecular layers, r decreases by some orders of magnitude across several time decades. Meanwhile, the surface evolves through configurations of decreasing energy, beginning with dissolution of isolated sites, then formation of terraces with disordered boundaries, their growth, and final smoothing. A crossover time to a smooth configuration is defined when r = 1:5r(F); the surface retreat at the crossover is approximately 3 times the initial roughness and is temperature-independent, while the crossover time is proportional to the initial roughness and is controlled by step-edge site detachment. The initial dissolution process is described by the so-called rough rates, which are measured for fixed ratios between the surface retreat and the initial roughness. The temperature dependence of the rough rates indicates control by kink site detachment; in general, it suggests that rough rates are controlled by the weakest microscopic bonds during the nucleation and formation of the lowest energy configurations of the crystalline surface. Our results are related to recent laboratory studies which show enhanced dissolution in polished calcite surfaces. In the application to calcite dissolution in alkaline environment, the minimal values of recently measured dissolution rate spectra give rF similar to 10(-9) mol/(m(2) s), and the cal
机译:我们使用动力学蒙特卡罗模拟和缩放方法研究矿物质的溶解与初始粗糙表面。我们考虑一个简单的立方格晶格结构,分子(位点)的热激活速率,以及由分数褐色运动算法产生的粗糙表面构造。首先,我们重新审视初始平坦表面的溶解问题,其中溶出速率R(F)在短时间内达到近似恒定的值,并且通过脱位位点的脱离来控制。对于初始粗糙表面,短次溶出速率R远大于R(F);在溶解数百个分子层之后,r在几十年中逐渐减少了一些数量级。同时,表面通过减小能量的配置演变,从分离的位置溶解开始,然后形成具有无序界限的露台,它们的生长和最终平滑。当R = 1:5R(F)时,定义了平滑配置的交叉时间;交叉处的表面撤退约为初始粗糙度的3倍,并且与温度无关,而交叉时间与初始粗糙度成比例,并且由逐步站点脱离控制。初始溶解过程由所谓的粗糙速率描述,该粗糙率针对表面撤退与初始粗糙度之间的固定比率测量。粗糙率的温度依赖性表示通过扭结站点脱离的控制;通常,它表明粗速率由最弱的微观键控制在成核期间和形成结晶表面的最低能量配置。我们的研究结果与最近的实验室研究有关,其在抛光的方解石表面中显示出增强的溶解。在碱性环境中的方解石溶解的施用中,最近测量的溶解速率光谱的最小值使RF类似于10(-9)摩尔/(m(2))和CAL

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