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  2. Permanent wilting point - Wikipedia

    en.wikipedia.org/wiki/Permanent_wilting_point

    Permanent wilting point (PWP) or wilting point (WP) is defined as the minimum amount of water in the soil that the plant requires not to wilt. If the soil water content decreases to this or any lower point a plant wilts and can no longer recover its turgidity when placed in a saturated atmosphere for 12 hours.

  3. Soil moisture - Wikipedia

    en.wikipedia.org/wiki/Soil_moisture

    A flooded field will drain the gravitational water under the influence of gravity until water's adhesive and cohesive forces resist further drainage at which point it is said to have reached field capacity. [20] At that point, plants must apply suction to draw water from a soil. By convention it is defined at 0.33 bar suction.

  4. Available water capacity - Wikipedia

    en.wikipedia.org/wiki/Available_water_capacity

    The concept, put forward by Frank Veihmeyer and Arthur Hendrickson, [3] assumed that the water readily available to plants is the difference between the soil water content at field capacity (θ fc) and permanent wilting point (θ pwp): θ a ≡ θ fc − θ pwp

  5. Soil - Wikipedia

    en.wikipedia.org/wiki/Soil

    Soil moisture levels, in order of decreasing water content, are saturation, field capacity, wilting point, air dry, and oven dry. Field capacity describes a drained wet soil at the point water content reaches equilibrium with gravity. Irrigating soil above field capacity risks percolation losses. Wilting point describes the dry limit for ...

  6. Water content - Wikipedia

    en.wikipedia.org/wiki/Water_content

    Below the wilting point plants are no longer able to extract water. At this point they wilt and cease transpiring altogether. At this point they wilt and cease transpiring altogether. Conditions where soil is too dry to maintain reliable plant growth is referred to as agricultural drought , and is a particular focus of irrigation management.

  7. Water retention curve - Wikipedia

    en.wikipedia.org/wiki/Water_retention_curve

    In 1907, Edgar Buckingham created the first water retention curve. [2] It was measured and made for six soils varying in texture from sand to clay. The data came from experiments made on soil columns 48 inch tall, where a constant water level maintained about 2 inches above the bottom through periodic addition of water from a side tube.

  8. Transpiration - Wikipedia

    en.wikipedia.org/wiki/Transpiration

    If not effectively taken care of, cavitation can cause a plant to reach its permanent wilting point, and die. Therefore, the plant must have a method by which to remove this cavitation blockage, or it must create a new connection of vascular tissue throughout the plant. [ 17 ]

  9. Wilting - Wikipedia

    en.wikipedia.org/wiki/Wilting

    Wilting is the loss of rigidity of non-woody parts of plants. This occurs when the turgor pressure in non- lignified plant cells falls towards zero, as a result of diminished water in the cells . Wilting also serves to reduce water loss, as it makes the leaves expose less surface area. [ 1 ]