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  2. Bulk density - Wikipedia

    en.wikipedia.org/wiki/Bulk_density

    Bulk density. In materials science, bulk density, also called apparent density, is a material property defined as the mass of the many particles of the material divided by the bulk volume. Bulk volume is defined as the total volume the particles occupy, including particle's own volume, inter-particle void volume, and the particles' internal ...

  3. 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 fraction of volume often given in percent. The amount of porosity in a soil depends on the minerals that make up the soil and on the amount of sorting occurring within the soil structure. For example, a sandy soil will have a larger porosity than a silty sand ...

  4. Gassmann's equation - Wikipedia

    en.wikipedia.org/wiki/Gassmann's_equation

    Gassmann's equation. Gassmann's equations are a set of two equations describing the isotropic elastic constants of an ensemble consisting of an isotropic, homogeneous porous medium with a fully connected pore space, saturated by a compressible fluid at pressure equilibrium. First published in German [1] by Fritz Gassmann, the original work was ...

  5. Pore structure - Wikipedia

    en.wikipedia.org/wiki/Pore_structure

    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. [1][2] Pores are the openings in the surfaces impermeable porous matrix which gases, liquids, or even foreign microscopic ...

  6. Physical properties of soil - Wikipedia

    en.wikipedia.org/wiki/Physical_properties_of_soil

    Physical properties of soil. The physical properties of soil, in order of decreasing importance for ecosystem services such as crop production, are texture, structure, bulk density, porosity, consistency, temperature, colour and resistivity. [1] Soil texture is determined by the relative proportion of the three kinds of soil mineral particles ...

  7. Porosity - Wikipedia

    en.wikipedia.org/wiki/Porosity

    Porosity. Ratio of void volume and total volume of a porous material. Porosity or void fraction is a measure of the void (i.e. "empty") spaces in a material, and is a fraction of the volume of voids over the total volume, between 0 and 1, or as a percentage between 0% and 100%. Strictly speaking, some tests measure the "accessible void", the ...

  8. Void ratio - Wikipedia

    en.wikipedia.org/wiki/Void_ratio

    Void ratio. The void ratio ( ) of a mixture of solids and fluids (gases and liquids), or of a porous composite material such as concrete, is the ratio of the volume of the voids ( ) filled by the fluids to the volume of all the solids ( ). It is a dimensionless quantity in materials science and in soil science, and is closely related to the ...

  9. Density logging - Wikipedia

    en.wikipedia.org/wiki/Density_logging

    Density logging is a well logging tool that can provide a continuous record of a formation's bulk density along the length of a borehole. In geology, bulk density is a function of the density of the minerals forming a rock (i.e. matrix) and the fluid enclosed in the pore spaces. This is one of three well logging tools that are commonly used to ...