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Repulsive hydration forces between calcite surfaces and their effect on the brittle strength of calcite-bearing rocks

机译:方解石表面之间的排斥水合作用力及其对含方解石岩石脆性强度的影响

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摘要

The long-term mechanical strength of calcite-bearing rocks is highly dependent on the presence and nature of pore fluids, and it has been suggested that the observed effects are due to changes in nanometer-scale surface forces near fracture tips and grain contacts. In this letter, we present measurements of forces between two calcite surfaces in air and water-glycol mixtures using the atomic force microscope. We show a time- and load-dependent adhesion at low water concentrations and a strong repulsion in the presence of water, which is most likely due to hydration of the strongly hydrophilic calcite surfaces. We argue that this hydration repulsion can explain the commonly observed water-induced decrease in strength in calcitic rocks and single calcite crystals. Furthermore, this relatively simple experimental setup may serve as a useful tool for analyzing surface forces in other mineral-fluid combinations.This research has been published in Geophysical Research Letters. © 2015 American Geophysical Union
机译:方解石岩石的长期机械强度高度依赖于孔隙流体的存在和性质,并且已表明观察到的影响是由于裂缝尖端和晶粒接触附近纳米尺度表面力的变化所致。在这封信中,我们介绍了使用原子力显微镜测量空气和水-乙二醇混合物中两个方解石表面之间的力的方法。我们在低水浓度下表现出时间依赖性和负荷依赖性,在水的存在下会产生强烈的排斥力,这很可能是由于强亲水性方解石表面的水合作用所致。我们认为这种水合排斥作用可以解释水在钙质岩和方解石晶体中普遍观察到的强度下降。此外,这种相对简单的实验装置可以作为分析其他矿物流体组合中表面力的有用工具。这项研究已发表在《地球物理研究快报》上。 ©2015美国地球物理联盟

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