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  2. Goldich dissolution series - Wikipedia

    en.wikipedia.org/wiki/Goldich_dissolution_series

    S. S. Goldich derived this series in 1938 after studying soil profiles and their parent rocks. [1] Based on sample analysis from a series of weathered localities, Goldich determined that the weathering rate of minerals is controlled at least in part by the order in which they crystallize from a melt.

  3. Water retention curve - Wikipedia

    en.wikipedia.org/wiki/Water_retention_curve

    Due to the hysteretic effect of water filling and draining the pores, different wetting and drying curves may be distinguished. The general features of a water retention curve can be seen in the figure, in which the volume water content, θ, is plotted against the matric potential, . At potentials close to zero, a soil is close to saturation ...

  4. Shrink–swell capacity - Wikipedia

    en.wikipedia.org/wiki/Shrink–swell_capacity

    Expansive soils are the most problematic in regions with very defined wet and dry periods, as opposed to areas that maintain a certain level of moisture throughout the year, as this annual cycle causes the soils to expand and swell every year. [3] Water can also be introduced into the soil through people, or their infrastructure.

  5. Petrophysics - Wikipedia

    en.wikipedia.org/wiki/Petrophysics

    Components of a petrophysical model of a water-wet reservoir rock. Due to the complex microstructure, for a water-wet rock, the following terms comprised a clastic reservoir formation: V ma = volume of matrix grains. V dcl = volme of dry clay. V cbw = volume of clay bound water. V cl = volume of wet clay (V dcl +V cbw). V cap = volume of ...

  6. Carbonate–silicate cycle - Wikipedia

    en.wikipedia.org/wiki/Carbonate–silicate_cycle

    The inorganic cycle begins with the production of carbonic acid (H 2 CO 3) from rainwater and gaseous carbon dioxide. [6] Due to this process, normal rain has a pH of around 5.6. [7] Carbonic acid is a weak acid, but over long timescales, it can dissolve silicate rocks

  7. Cyclic sediments - Wikipedia

    en.wikipedia.org/wiki/Cyclic_sediments

    Cyclic sediments (also called rhythmic sediments [1]) are sequences of sedimentary rocks that are characterised by repetitive patterns of different rock types or facies within the sequence. Processes that generate sedimentary cyclicity can be either autocyclic or allocyclic, and can result in piles of sedimentary cycles hundreds or even ...

  8. Aeolis quadrangle - Wikipedia

    en.wikipedia.org/wiki/Aeolis_quadrangle

    So far, the materials Curiosity has analyzed are consistent with the initial ideas of deposits in Gale Crater recording a transition through time from a wet to dry environment. [ 67 ] On December 3, 2012, NASA reported that Curiosity performed its first extensive soil analysis , revealing the presence of water molecules, sulfur and chlorine in ...

  9. Rock analogs for structural geology - Wikipedia

    en.wikipedia.org/wiki/Rock_analogs_for...

    Silicone oils/polymers can have varying viscosities, which can be changed by adding fillers (dry granular materials) or aolic acid. In combination with brittle model materials, silicone oils/polymers can investigate many processes in salt tectonics, including the deformation of sediments adjacent and above a salt body.