首页> 外文会议>Materials Research Society symposium on scientific basis for nuclear waste management"" >Investigation of rock samples using x-ray-microscomputer-tomography before and after mercuryintrusion porosimetry
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Investigation of rock samples using x-ray-microscomputer-tomography before and after mercuryintrusion porosimetry

机译:压汞法之前和之后使用X射线微机断层扫描对岩石样品进行调查

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A new method for the physical characterization of rock matrices for use in site investigations of nuclear waste repositories has been developed. The method can provide information beeded in the assessment of the performance of the geosphere working as a natural barrier retarding the migration of radionuclides by diffusion into the rock matrix. Most conventional methods for the physical characterization of rocks giveonly bulk information. The combination of mercury porosimetry and computer tomography can give 3-D data on mineral-specific porosity distributions with additional pore size information. Additionally, limits for mineral-specific internal surface areas can be estimated, which is essential for the assessment of water-rock interaction and reactive interaction with radionuclides (sorption). Results of measuremdents on granitic rock (granodiorite) from the Baltic shield are discussed and integrated with results by complementary methods.
机译:已经开发出一种新的岩石基质物理表征方法,用于核废料库的现场调查。该方法可为评估地球圈作为天然屏障而发挥的作用提供信息,而天然屏障可通过扩散到岩石基质中来阻止放射性核素的迁移。大多数常规的岩石物理表征方法只能提供大量信息。汞孔隙率法和计算机断层扫描的结合可以提供有关矿物特定孔隙率分布的3-D数据,并提供额外的孔径信息。另外,可以估算矿物比表面积的限值,这对于评估水-岩相互作用和与放射性核素的反应性相互作用(吸附)至关重要。讨论了来自波罗的海盾构的花岗岩(granodiorite)上的测量结果,并通过补充方法将其与结果结合在一起。

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