3D mapping of water in oolithic limestone at atmospheric and vacuum saturation using X-ray micro-CT differential imagingMA BooneDepartment of Geology and Soil Science-UGCT, Ghent University, Krijgslaan 281 S8,9000 Ghent, BelgiumMmarijn.boone@ugent.beT. De KockDepartment of Geology and Soil Science-UGCT, Ghent University, Krijgslaan 281 S8,9000 Ghent, BelgiumT. BultreysDepartment of Geology and Soil Science-UGCT, Ghent University, Krijgslaan 281 S8,9000 Ghent, Belgium

摘要

Determining the distribution of fluids in porous sedimentary rocks is of great importance in many geological fields. However, this is not straightforward, especially in the case of complex sedimentary rocks like limestone, where a multidisciplinary approach is often needed to capture its broad, multimodal pore size distribution and complex pore geometries. This paper focuses on the porosity and fluid distribution in two varieties of Massangis limestone, a widely used natural building stone from the southeast part of the Paris basin (France).The Massangis limestone shows locally varying post-depositional alterations, resulting in different types of pore networks and very different water distributions within the limestone. Traditional techniques for characterizing the porosity and pore size distribution are compared with state-of-the-art neutron radiography and X-ray computed microtomography to visualize the distribution of water inside the limestone at different imbibition conditions. X-ray computed microtomography images have the great advantage to non-destructively visualize and analyze the pore space inside of a rock, but are often limited to the larger macropores in the rock due to resolution limitations. In this paper, differential imaging is successfully applied to the X-ray computed microtomography images to obtain sub-resolution information about fluid occupancy and to map the fluid distribution in three dimensions inside the scanned limestone samples. The detailed study of the pore space with differential imaging allows understanding the difference in the water uptake behavior of the limestone, a primary factor that affects the weathering of the rock.