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  2. Soil water (retention) - Wikipedia

    en.wikipedia.org/wiki/Soil_water_(retention)

    Pores (the spaces that exist between soil particles) provide for the passage and/or retention of gasses and moisture within the soil profile.The soil's ability to retain water is strongly related to particle size; water molecules hold more tightly to the fine particles of a clay soil than to coarser particles of a sandy soil, so clays generally retain more water. [2]

  3. Hydroponics - Wikipedia

    en.wikipedia.org/wiki/Hydroponics

    The hydroponic method of plant production by means of suspending the plant roots in a solution of nutrient-rich, oxygenated water. Traditional methods favor the use of plastic buckets and large containers with the plant contained in a net pot suspended from the centre of the lid and the roots suspended in the nutrient solution.

  4. Soil moisture - Wikipedia

    en.wikipedia.org/wiki/Soil_moisture

    By convention it is defined at 0.33 bar suction. [20] [21] Available water and unavailable water The water that plants may draw from the soil is called the available water. [20] [22] Once the available water is used up the remaining moisture is called unavailable water as the plant cannot produce sufficient suction to draw that water in ...

  5. Plant nutrients in soil - Wikipedia

    en.wikipedia.org/wiki/Plant_nutrients_in_soil

    Nutrients in the soil are taken up by the plant through its roots, and in particular its root hairs.To be taken up by a plant, a nutrient element must be located near the root surface; however, the supply of nutrients in contact with the root is rapidly depleted within a distance of ca. 2 mm. [14] There are three basic mechanisms whereby nutrient ions dissolved in the soil solution are brought ...

  6. Field capacity - Wikipedia

    en.wikipedia.org/wiki/Field_capacity

    Veihmeyer and Hendrickson [3] realized the limitation in this measurement and commented that it is affected by so many factors that, precisely, it is not a constant (for a particular soil), yet it does serve as a practical measure of soil water-holding capacity. Field capacity improves on the concept of moisture equivalent by Lyman Briggs.

  7. Home composting - Wikipedia

    en.wikipedia.org/wiki/Home_composting

    Apply a 3-6 inch layer to the bed and rake. [18] Amend Soil: Mix 1–2 inches of the compost into the top 3–5 inches of the soil. [18] This can also be done before adding plants or seeds to aerate the soil and add nutrients. [19] Fertilizer: Add 1-2 inches of compost to grass or plant pots and rake or mix. [19] Compost Tea (liquid fertilizer)