An approach for quick estimation of maximum height of capillary rise ...
2014年12月1日 · Capillary fringe is the saturated zone from the water table to the air entry head, r is the equivalent pore radius in micrometers. This equation indicates that the difference between the maximum height of capillary rise and the height …
capillary head - Glossary of Meteorology
(Also called capillary pressure head.) The potential, expressed in units of water head, due to the capillarity of a porous medium in the presence of a wetted liquid.
CAPILLARY中文(简体)翻译：剑桥词典 - Cambridge Dictionary
The created plasma is confined by the capillary wall, electrode material and flow in a specified chamber through a hollow electrode.
Capillary pressure - Wikipedia
Capillary pressure can serve as both an opposing or driving force for fluid transport and is a significant property for research and industrial purposes (namely microfluidic design and oil extraction from porous rock). It is also observed in natural phenomena.
Capillary Pressure - SpringerLink
2016年1月1日 · For convenience, soil scientists continue to refer to ψ as the “capillary head.”
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A general form of capillary rise equation in micro-grooves
2020年11月12日 · Micro-grooves utilize capillary action to deliver a liquid, with no need for an extra pumping device, which makes them unique and desirable for numerous systems.
CNS capillary telangiectasia | Radiology Reference Article ...
2024年1月15日 · Most capillary telangiectasias occur in the pons, cerebellum and spinal cord. Capillary telangiectasias are mostly located in the brainstem, especially the pons. They are usually solitary, but can sometimes be multiple.
The relative permeability-saturation-capillary head (kr-S-hc) relationships of soils are the soil properties which control air and water flow during in-situ air sparging. An
Numerical Solution of Richards' Equation: A Review of …
2017年10月19日 · Rather, the capillary head (ψ) is continuous, and it is better to write the Richards' equation with capillary head as the dependent variable and evaluate the moisture content in terms of ψ, θ = θ(ψ). This can be done in either a mixed form:
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