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Orthoclase surface structure dissolution measured in situ by x-ray reflectivityand atomic force microscopy

机译:通过X射线反射率和原子力显微镜原位测量的正长石表面结构溶解

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Orthoclase (001) surface topography and interface structure were measured duringdissolution by using in situ atomic force microscopy (AFM) and synchrotrons X-ray reflectivity at pH 1.1-12.9 and T = 25-84 C. Terrace roughening at low pH and step motion at high pH were the main phenomena observed, and dissolution rates

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