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  2. Sod - Wikipedia

    en.wikipedia.org/wiki/Sod

    Sod is grown on specialist farms. For 2009, the United States Department of Agriculture reported 1,412 farms had 368,188 acres (149,000.4 ha) of sod in production. [9]It is usually grown locally (within 100 miles of the target market) [10] to minimize both the cost of transport and also the risk of damage to the product.

  3. Tillage - Wikipedia

    en.wikipedia.org/wiki/Tillage

    A Kenyan farmer holding tilled soil. Dries the soil before seeding. [17] Soil loses nutrients, like nitrogen and fertilizer, and its ability to store water. [17] [note 2] Decreases the water infiltration rate of soil. (Results in more runoff and erosion [17] [19] as the soil absorbs water more slowly than before) [note 3]

  4. Broadcast seeding - Wikipedia

    en.wikipedia.org/wiki/Broadcast_seeding

    Broadcasting is used in areas of low rainfall and low soil fertility. It is a seeding method often used in areas that are too heavily sloped or wet to use mechanical seeding methods. Broadcast seeding may be suited for seeding smaller plots that are less than 1 acre (0.4047 hectares) in area.

  5. Lawn - Wikipedia

    en.wikipedia.org/wiki/Lawn

    A lawn (/ l ɔː n /) is an area of soil-covered land planted with grasses and other durable plants such as clover which are maintained at a short height with a lawn mower (or sometimes grazing animals) and used for aesthetic and recreational purposes—it is also commonly referred to as part of a garden.

  6. Runoff curve number - Wikipedia

    en.wikipedia.org/wiki/Runoff_curve_number

    Selection of a hydrologic soil group should be done based on measured infiltration rates, soil survey (such as the NRCS Web Soil Survey), or judgement from a qualified soil science or geotechnical professional. The table below presents curve numbers for antecedent soil moisture condition II (average moisture condition).

  7. Physical properties of soil - Wikipedia

    en.wikipedia.org/wiki/Physical_properties_of_soil

    Soil temperature depends on the ratio of the energy absorbed to that lost. [68] Soil has a mean annual temperature from -10 to 26 °C according to biomes. [69] Soil temperature regulates seed germination, [70] breaking of seed dormancy, [71] [72] plant and root growth [73] and the availability of nutrients. [74]