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Vplyv kry?talizácie síranu sodného na intergranulárnu de?trukciu thassoského mramoru

机译:硫酸钠结晶对Thasso大理石晶间破坏的影响

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The paper deals with sodium sulphate crystallization in pore spaces of Thassos marble and presents the 3D visualization of intergranular fractures causing a?deterioration of the specimen by the salt crystallization. Cylindrical marble specimen with diameter 20?mm and length 50?mm has been submitted to 15?cycles of the dipping in 14?% solution of mirabilite (Na2SO4·10?H2O) according to the STN?EN?12370 standard methodical test. Using electron methods (polarization microscopy, SEM – Scanning electron microscopy, XRD – X-ray diffraction, EMPA – Electron-microprobe analysis) and by monitoring of selected physical parameters (changes in weight and changes in P-waves velocities), in first the mineral composition and microstructure of the marble have been characterized and consequently the effects induced by cyclic activity of sodium sulphate with the marble have been analysed. Mercury intrusion porosimetry (MIP) method has been used for specification of the porosity and detail pore structure. After realised 15 cycles of dipping in salt solution the presence of sodium sulphate in EDS spectrum of the marble has been documented. The sample weight has been reduced about 1.3 % and as well the speed of P-waves propagation has been reduced about 20 %. Before and after salt crystallization test the marble has been characterized using a computed microtomography (CMT), allowing to doing the image about intensity and localization of the created micro-fractures in 3D. It was identified that cyclic salt crystallization caused the decay of the marble predominantly along the dominant dolomite crystal boundaries. The hydration and dehydration reactions of the sodium sulphate and its phase transitions with cyclic changes of humidity and temperature are also discussed in the paper.
机译:本文研究了Thassos大理石孔隙空间中的硫酸钠结晶,并提出了3D可视化的晶间裂缝,该裂缝导致盐结晶使样品劣化。根据STN?EN?12370标准方法测试,将直径20?mm,长度50?mm的圆柱大理石样品浸入14 %%的芒硝(Na2SO4·10?H2O)溶液中的15个循环。首先,使用电子方法(极化显微镜,SEM –扫描电子显微镜,XRD – X射线衍射,EMPA –电子显微探针分析)并监视选定的物理参数(重量变化和P波速度变化)。表征了大理石的矿物成分和微观结构,因此,分析了硫酸钠与大理石的循环活性所引起的影响。汞侵入孔隙率法(MIP)已用于指定孔隙率和细孔结构。在完成15次浸入盐溶液的循环后,已记录了大理石在EDS光谱中存在硫酸钠。样品重量减少了约1.3%,P波传播的速度也降低了约20%。在盐结晶测试之前和之后,已使用计算机显微断层照相术(CMT)对大理石进行了表征,从而可以在3D模式下对所产生的微裂缝的强度和定位进行图像处理。可以确定,环状盐的结晶主要沿主要的白云石晶体边界引起大理石的腐烂。本文还讨论了硫酸钠的水合和脱水反应及其随湿度和温度循环变化的相变。

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