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  2. Drainage equation - Wikipedia

    en.wikipedia.org/wiki/Drainage_equation

    the soil's hydraulic conductivity (Ka and Kb) by measurements; the depth of the bottom of the aquifer (Di) the design drain spacing (L) can be found from the equation in dependence of the drain depth (Dd) and drain radius (r). Drainage criteria

  3. Double digging - Wikipedia

    en.wikipedia.org/wiki/Double_digging

    Double digging is a gardening technique used to increase soil drainage and aeration. It involves the loosening of two layers of soil , and the addition of organic matter. Double digging is typically done when cultivating soil in a new garden, or when deep topsoil is required.

  4. Sheet mulching - Wikipedia

    en.wikipedia.org/wiki/Sheet_mulching

    The soil is analyzed and its pH is adjusted (if needed). The soil is moisturized (if needed) to facilitate the activity of decomposers. The soil is then covered with a thin layer of slowly decomposing material (known as the weed barrier), typically cardboard. This suppresses the weeds by blocking sunlight, adds nutrients to the soil as weed ...

  5. Garden waste dumping - Wikipedia

    en.wikipedia.org/wiki/Garden_waste_dumping

    Garden waste, or green waste dumping is the act of discarding or depositing garden waste somewhere it does not belong.. Garden waste is the accumulated plant matter from gardening activities which involve cutting or removing vegetation, i.e. cutting the lawn, weed removal, hedge trimming or pruning consisting of lawn clippings. leaf matter, wood and soil.

  6. Raised-bed gardening - Wikipedia

    en.wikipedia.org/wiki/Raised-bed_gardening

    Raised bed gardening. Raised-bed gardening is a form of gardening in which the soil is raised above ground level and usually enclosed in some way. Raised bed structures can be made of wood, rock, concrete or other materials, and can be of any size or shape. [1] The soil is usually enriched with compost. [2]

  7. Topsoil - Wikipedia

    en.wikipedia.org/wiki/Topsoil

    Topsoil is composed of mineral particles and organic matter and usually extends to a depth of 5-10 inches (13–25 cm). Together these make a substrate capable of holding water and air which encourages biological activity.

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