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  2. Capillary flow porometry - Wikipedia

    en.wikipedia.org/wiki/Capillary_flow_porometry

    In order to measure the pore size by capillary flow porometry it is necessary to impregnate the samples with a wetting liquid. An inert gas flow is used to displace the liquid that is in the pores and the pressure required to empty the most constricted part of the pore is measured. [3]

  3. Porosimetry - Wikipedia

    en.wikipedia.org/wiki/Porosimetry

    Porosimetry is an analytical technique used to determine various quantifiable aspects of a material's porous structure, such as pore diameter, total pore volume, surface area, and bulk and absolute densities. The technique involves the intrusion of a non-wetting liquid (often mercury) at high pressure into a material through the use of a ...

  4. Pore structure - Wikipedia

    en.wikipedia.org/wiki/Pore_structure

    Micro CT of porous medium: Pores of the porous medium shown as purple color and impermeable porous matrix shown as green-yellow color. Pore structure is a common term employed to characterize the porosity, pore size, pore size distribution, and pore morphology (such as pore shape, surface roughness, and tortuosity of pore channels) of a porous medium.

  5. Porosity - Wikipedia

    en.wikipedia.org/wiki/Porosity

    Porosity is the ratio of pore volume to its total volume. Porosity is controlled by: rock type, pore distribution, cementation, diagenetic history and composition. Porosity is not controlled by grain size, as the volume of between-grain space is related only to the method of grain packing.

  6. Thermoporometry and cryoporometry - Wikipedia

    en.wikipedia.org/wiki/Thermoporometry_and...

    A currently exciting application for NMR Cryoporometry is the measurement of porosity and pore-size distributions, in the study of carbon, charcoal and biochar. Biochar is regarded as an important soil enhancer (used since pre-history), and offers great possibilities for carbon dioxide removal from the biosphere .

  7. Pore space in soil - Wikipedia

    en.wikipedia.org/wiki/Pore_space_in_soil

    The porosity is a measure of the total pore space in the soil. This is defined as a ... A widely used classification of pore size is that of Brewer (1964): [1] [2] [3]

  8. Nuclear magnetic resonance in porous media - Wikipedia

    en.wikipedia.org/wiki/Nuclear_magnetic_resonance...

    It makes use of the Gibbs-Thomson effect : small crystals of a liquid in the pores melt at a lower temperature than the bulk liquid : The melting point depression is inversely proportional to the pore size. The technique is closely related to that of the use of gas adsorption to measure pore sizes (Kelvin equation).

  9. Liquid entry pressure - Wikipedia

    en.wikipedia.org/wiki/Liquid_entry_pressure

    where is a pore geometry coefficient (= 1 for cylindrical pores and 0 < < 1 for non-cylindrical pores), [3] is the liquid surface tension, is the contact angle measured on the liquid side, where the liquid-vapor interface meets the membrane surface, and is the maximum pore size of the membrane.