Webn. [Geology] A type of secondary porosity created through the dissolution of a preexisting constituent of a rock, such as a shell, rock fragment or grain. The pore space preserves the shape, or mold, of the dissolved material. See: pore , porosity , secondary porosity Photomicrograph of moldic pore. Web13 Sep 2024 · The magnitude of secondary compression is expressed by the secondary compression index, C α = Δe/Δlog t, in which e = void ratio and t = time. Analysis of test data pertaining to soils of widely varying plasticity characteristics and geological origin indicates that there is an excellent correlation between the initial porosity, no and secondary …
secondary porosity Energy Glossary - Schlumberger
Web22 Jul 2024 · To provide an understanding of The concepts of rock matrix and porosity The difference between original (primary) and induced (secondary) porosity The difference between Total and Effective... WebSecondary porosity is porosity that has developed after the rock has formed. It can include fracture porosity — space within fractures in any kind of rock. Some volcanic rock has a special type of porosity related to … grand canyon south rim shuttle schedule
14.1 Groundwater and Aquifers – Physical Geology
WebFracture porosity is the ratio between the volume of open fractures and the rock's bulk volume. The fracture porosity, if present, is one of the contributions to the rock's porosity. The other porosity contributions are other sources of secondary porosity like vugs or vugular porosity, effective matrix porosity, and non effective matrix porosity like clay … Web3 Oct 2013 · Porosity is calculated as the pore volume of the rock divided by its bulk volume.Two types of porosities can exist in a rock. These are termed primary porosity and secondary porosity. Primary porosity is described as the porosity of the rock that formed at the time of its deposition. Secondary porosity develops after deposition of the rock ... Web8 Apr 2024 · The porosity–permeability characteristics of this kind of igneous rocks were equivalent to state that was intermediate between the 1 st and 3 rd subtypes. With increase in porosity, the exponential growth rate of permeability was lower than that of the 1 st subtype but higher than that of the 3 rd subtype (Table 4 ). grand canyon south rim hummer tour