. . "822167624"^^ . "Perturbation (geology)"@en . . . . . . . . . "3301776"^^ . . . . "Perturbaci\u00F3n (geolog\u00EDa)"@es . "2252"^^ . . . "Perturbation (from Latin: perturbare \"to confuse, disorder, disturb\", from per- \"through\" + turbare \"disturb, confuse,\" from turba \"turmoil, crowd\") is a set of pedology (soil study) and sedimentary geology processes relating to changes in the nature of water-borne alluvial sediments and in situ soil deposits over time."@en . . . . "La perturbaci\u00F3n es un t\u00E9rmino asociado a cambios en la naturaleza de los dep\u00F3sitos aluviales en el tiempo. La edafoperturbaci\u00F3n se refiere a la perturbaci\u00F3n que no es causada por iluviaci\u00F3n. En suelo arcilloso, los cambios en humedad causa procesos de expansiones y de contracciones que deforman severamente las acumulaciones aluviales. En otras ocasiones, es la neoformaci\u00F3n de compuestos ed\u00E1ficos, como en el caso de precipitaci\u00F3n de carbonato, causando fragmentaci\u00F3n y desorganizaci\u00F3n de las cubiertas arcillosas. La actividad bi\u00F3tica es tambi\u00E9n una importante causa de perturbaci\u00F3n. La crioclastia puede afectar la conservaci\u00F3n de las acumulaciones iluviales en climas fr\u00EDos. \n* Datos: Q5658542"@es . . . . . "La perturbaci\u00F3n es un t\u00E9rmino asociado a cambios en la naturaleza de los dep\u00F3sitos aluviales en el tiempo. La edafoperturbaci\u00F3n se refiere a la perturbaci\u00F3n que no es causada por iluviaci\u00F3n. En suelo arcilloso, los cambios en humedad causa procesos de expansiones y de contracciones que deforman severamente las acumulaciones aluviales. En otras ocasiones, es la neoformaci\u00F3n de compuestos ed\u00E1ficos, como en el caso de precipitaci\u00F3n de carbonato, causando fragmentaci\u00F3n y desorganizaci\u00F3n de las cubiertas arcillosas. La actividad bi\u00F3tica es tambi\u00E9n una importante causa de perturbaci\u00F3n. La crioclastia puede afectar la conservaci\u00F3n de las acumulaciones iluviales en climas fr\u00EDos."@es . . . . . . "Perturbation (from Latin: perturbare \"to confuse, disorder, disturb\", from per- \"through\" + turbare \"disturb, confuse,\" from turba \"turmoil, crowd\") is a set of pedology (soil study) and sedimentary geology processes relating to changes in the nature of water-borne alluvial sediments and in situ soil deposits over time. \n* Pedoturbation (from Greek: \u03C0\u03AD\u03B4\u03BF\u03BD (p\u00E9don), \"soil\") involves mixing between soil horizons, and is an important factor in soil formation. Pedoturbation includes churning clays, cryoturbation, and bioturbation. Types of bioturbation include faunal pedoturbation (animal burrowing), and floral pedoturbation (root growth, tree-uprootings). Pedoturbation transforms soils through destratification, mixing, and sorting, as well as creating preferential flow paths for soil gas and infiltrating water. The zone of active bioturbation is termed the soil biomantle. \n* Soil perturbation that is not pedoturbation. Precipitation of surface salts also causes localized disruption of soils. Because it does not result in mixing between soil horizons, it is not considered pedoturbation. \n* In geology, bioturbation is the displacement and mixing of sediment particles (i.e. sediment reworking) and solutes (i.e. biologically-mediated irrigation) by benthic zone (bottom water) fauna (animals) or flora (plants). Activity of bacteria is yet another important cause of perturbation in the geological record. Field termites are especially important in tropical climate regions within 15\u00B0 of the equator."@en . . . . . . . . . .