makroporach
Makroporach, or macroporosity, refers to the presence and measure of large pore spaces in materials such as soils and rocks. It is a component of total porosity that governs how fluids move and are stored within a substrate. Macroporosity is distinguished from microporosity, which involves much smaller pores that retain water more tenaciously and contribute less to immediate flow.
In soil science, macropores are commonly defined as pores larger than about 0.08 millimeters in diameter, though
Formation and management of macroporosity are influenced by biotic and abiotic processes. Biogenic creation occurs through
In geology and hydrogeology, macroporosity describes large interconnected pore spaces in rocks and carbonate formations that