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  2. Available water capacity - Wikipedia

    en.wikipedia.org/wiki/Available_water_capacity

    It is also known as available water content (AWC), profile available water (PAW) [2] or total available water (TAW). 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 ...

  3. Soil moisture sensor - Wikipedia

    en.wikipedia.org/wiki/Soil_moisture_sensor

    A simple soil moisture sensor for gardeners. Soil moisture sensors measure the volumetric water content in soil. [1] Since the direct gravimetric measurement of free soil moisture requires removing, drying, and weighing of a sample, soil moisture sensors measure the volumetric water content indirectly by using some other property of the soil, such as electrical resistance, dielectric constant ...

  4. Soil moisture - Wikipedia

    en.wikipedia.org/wiki/Soil_moisture

    [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. Wilting point The wilting point is the minimum amount of water plants need to not wilt and approximates the boundary between available and unavailable water.

  5. Water retention curve - Wikipedia

    en.wikipedia.org/wiki/Water_retention_curve

    Water retention curve is the relationship between the water content, θ, and the soil water potential, ψ. The soil moisture curve is characteristic for different types of soil, and is also called the soil moisture characteristic. It is used to predict the soil water storage, water supply to the plants (field capacity) and soil aggregate stability.

  6. Soil water (retention) - Wikipedia

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

    Available water is that which the plants can utilize from the soil within the range between field capacity and wilting point. Roughly speaking for agriculture (top layer soil), soil is 25% water , 25% air , 45% mineral , 5% other; water varies widely from about 1% to 90% due to several retention and drainage properties of a given soil.

  7. The Worst Time to Water Indoor and Outdoor Plants ... - AOL

    www.aol.com/worst-time-water-indoor-outdoor...

    The timing of when you water plants impacts how effectively they can absorb water. But just as important as knowing when to water plants is knowing when not to water them.

  8. Parshall flume - Wikipedia

    en.wikipedia.org/wiki/Parshall_flume

    Named after its creator, Dr. Ralph L. Parshall of the U.S. Soil Conservation Service, the Parshall flume is a fixed hydraulic structure used in measuring volumetric flow rate in surface water, industrial discharges, municipal sewer lines, and influent/effluent flows in wastewater treatment plants. The Parshall flume accelerates the flow by ...

  9. How Often Should You Water Indoor Plants in Winter to ... - AOL

    www.aol.com/often-water-indoor-plants-winter...

    But if you water your plants from the top down, direct your watering can to the soil to avoid wet leaves and mildew issues. 3. Empty Plant Saucers.