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  2. Weathering - Wikipedia

    en.wikipedia.org/wiki/Weathering

    The materials left after the rock breaks down combine with organic material to create soil. Many of Earth's landforms and landscapes are the result of weathering, erosion and redeposition. Weathering is a crucial part of the rock cycle; sedimentary rock, the product of weathered rock, covers 66% of the Earth's continents and much of the ocean ...

  3. Alternate wetting and drying - Wikipedia

    en.wikipedia.org/wiki/Alternate_wetting_and_drying

    Alternate wetting and drying (AWD) is a water management technique, practiced to cultivate irrigated lowland rice with much less water than the usual system of maintaining continuous standing water in the crop field. It is a method of controlled and intermittent irrigation.

  4. Honeycomb weathering - Wikipedia

    en.wikipedia.org/wiki/Honeycomb_weathering

    Most commonly, researchers have advocated salt weathering as the primary explanation for the formation of honeycomb weathering. Currently, it is considered to be polygenetic in origin; being the result of complex interaction of physical and chemical weathering processes, which include salt weathering and cyclic wetting and drying.

  5. Crustose lichen - Wikipedia

    en.wikipedia.org/wiki/Crustose_lichen

    Saxicolous crustose lichens play an important role in the weathering of rocks. Repeated contraction and expansion of thalli occurs in response to alternate periods of wetting and drying, resulting in the breakdown of rock fragments and removal of mineral grains from the rock surfaces. [18]

  6. Canal lining - Wikipedia

    en.wikipedia.org/wiki/Canal_lining

    A common method to reduce future swelling in expansive soils is to subject the soil to wetting and drying cycles prior to construction of the lining. [6] Lab testing has shown that subjecting a clayey soil to wetting and drying cycles leads to a hysteresis of shrinkage in the soil, significantly reducing its free swelling potential. [7]

  7. Fluorine cycle - Wikipedia

    en.wikipedia.org/wiki/Fluorine_cycle

    The fluorine cycle is the series of biogeochemical processes through which fluorine moves through the lithosphere, hydrosphere, atmosphere, and biosphere. Fluorine originates from the Earth’s crust, and its cycling between various sources and sinks is modulated by a variety of natural and anthropogenic processes.

  8. Boron cycle - Wikipedia

    en.wikipedia.org/wiki/Boron_cycle

    The boron cycle is the biogeochemical cycle of boron through the ... boron cycles through the biosphere by rock weathering, and wet and dry deposition from the ...

  9. Rock (geology) - Wikipedia

    en.wikipedia.org/wiki/Rock_(geology)

    The use of rock has had a huge impact on the cultural and technological development of the human race. Rock has been used by humans and other hominids for at least 2.5 million years. [22] Lithic technology marks some of the oldest and continuously used technologies. The mining of rock for its metal content has been one of the most important ...