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 … 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 …
Secondary Porosity System - an overview ScienceDirect …
WebPrimary porosity and permeability are dependent on the size, shape, and grading and packing of the sediment grains and also on the manner of their initial consolidation. … WebSecondary porosity can develop before the burial, after the burial, or as a result of other tectonic activity. Shrinkage of certain minerals creates fractures, and porosity increases. … how to delete rss folder in outlook
Secondary Porosity - an overview ScienceDirect Topics
Websecondary porosity. 1. n. [Geology] The porosity created through alteration of rock, commonly by processes such as dolomitization, dissolution and fracturing. See: … WebDissolution of either grains or cements in a sandstone leads to the development of secondary porosity. In the 1970s and 1980s, many publications suggested that mineral dissolution was a key process whereby significant porosity could be created at depth. Such porosity could then be occupied by petroleum. 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 ). the most fastest zodiac sign