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Resolving orthoclase dissolution processes with atomic force microscopy and X-ray reflectivity

机译:用原子力显微镜和X射线反射率解决原石酶溶解过程

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Direct measurements of orthoclase (001) were performed using in situ atomic force microscopy (AFM) and synchrotron X-ray reflectivity to reveal the A-scale dissolution process as a function of pH and temperature. Distinct processes were observed, involving mainly terrace roughening at pH = 1.1 and step motion at pH = 12.9. A gel-like surface coating was observed to form at acidic pH under slow fluid flow-rate conditions. No coating was observed either at alkaline pH or at acidic pH under high fluid flow-rate conditions. The corresponding dissolution rates were measured directly at pH = 1.1 12.9 at ~50 ℃ using real-time X-ray reflectivity measurements, and reacted interface structures were derived from crystal truncation rod measurements after reaction at both acidic and alkaline pH. Our observations reveal, under these experimental conditions, that 1) orthoclase dissolution is controlled by at least two separate surface reactions having distinct reactive sites; 2) dissolution is stoichiometric at alkaline pH and only minimally nonstoichiometric (limited to one unit-cell depth) at acidic pH; previously identified nonstoichiometric layer thicknesses derived from macroscopic measurements are associated with the formation of the gel-like coatings; 3) dissolution rates measured at freshly cleaved (001) surfaces are comparable to those derived from steady-state powder dissolution rates for both alkaline and acidic pH; and 4) elevated transient dissolution rates are not observed for freshly cleaved surfaces but are obtained under alkaline conditions after reacting the orthoclase (001) surface at acidic pH. These observations clarify differences in orthoclase dissolution mechanisms as a function of pH, demonstrate the utility of AFM and X-ray scattering methods for measuring A-scale structures and face-specific dissolution rates on single crystals and place new constraints on the understanding of alkali feldspar weathering processes.
机译:使用原位原子力显微镜(AFM)和同步加速器X射线反射率直接测量原石酶(001),以揭示A级溶解过程随pH和温度的变化。观察到不同的过程,主要包括在pH = 1.1时平台粗糙和在pH = 12.9时步进运动。在缓慢的流体流速条件下,在酸性pH下观察到形成了凝胶状表面涂层。在高流体流速条件下,在碱性pH或酸性pH下均未观察到涂层。通过实时X射线反射率测量,在pH = 1.1 12.9〜50℃的条件下,直接测量相应的溶出速率,并在酸性和碱性pH下反应后,通过晶体截断棒的测量得出反应的界面结构。我们的观察结果表明,在这些实验条件下,1)原核酶的溶解受至少两个具有不同反应位点的独立表面反应控制; 2)在碱性pH下的溶解是化学计量的,而在酸性pH下的溶解最少是非化学计量的(限于一个晶胞深度);从宏观测量得出的先前确定的非化学计量层厚度与凝胶状涂层的形成有关。 3)在新鲜劈裂(001)表面测得的溶出速率与从碱性和酸性pH值的稳态粉末溶出速率得出的溶出速率相当; 4)在新近切割的表面上未观察到升高的瞬时溶解速率,但是在碱性条件下使正原酶(001)表面在酸性pH下反应后获得。这些观察结果阐明了原石酶溶解机制随pH的变化的差异,证明了AFM和X射线散射方法可用于测量A晶体的结构和单晶上特定于面的溶解速率,并对碱长石的理解提出了新的限制。风化过程。

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