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  2. Fill dirt - Wikipedia

    en.wikipedia.org/wiki/Fill_dirt

    Fill dirt is usually subsoil (soil from beneath topsoil) and underlying soil parent material which has little soil organic matter or biological activity. Fill dirt is taken from a location where soil is being removed as a part of leveling an area for construction; it may also contain sand, rocks, and stones, as well as earth.

  3. Topsoil - Wikipedia

    en.wikipedia.org/wiki/Topsoil

    Topsoil products typically are not as suitable for potting plants or growing fruit and veg as potting soil or compost. Using it for this purpose can also work out prohibitively expensive compared to other alternatives. Topsoil is also used for proper surface grading near residential buildings.

  4. Humus - Wikipedia

    en.wikipedia.org/wiki/Humus

    Humus allows soil organisms to feed and reproduce and is often described as the "life-force" of the soil. [53] [54] The process that converts soil organic matter into humus feeds the population of microorganisms and other creatures in the soil, and thus maintains high and healthy levels of soil life. [53] [54]

  5. Chernozem - Wikipedia

    en.wikipedia.org/wiki/Chernozem

    Chernozem (/ ˈ tʃ ɜːr n ə z ɛ m / CHUR-nə-zem), [a] also called black soil, regur soil or black cotton soil, is a black-colored soil containing a high percentage of humus [3] (4% to 16%) and high percentages of phosphorus and ammonia compounds. [4] Chernozem is very fertile soil and can produce high agricultural yields with its high ...

  6. Filling station - Wikipedia

    en.wikipedia.org/wiki/Filling_station

    People who work in filling stations, live near them, or attend school close to them are exposed to fumes and are at increased lifetime risk of cancer, with risk increased if there are multiple stations nearby. [13] There is some evidence that living near a filling station is a risk for childhood leukemia.

  7. Soil in the United States - Wikipedia

    en.wikipedia.org/wiki/Soil_in_the_United_States

    Soils are the product of climate, organisms and topography, acting on parent (geologic) material over time. Thus the great diversity of geologic materials, geomorphic processes, climatic conditions, biotic assemblages and land surface ages in the United States is responsible for the presence of an enormous variety of mineral and organic soils.