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  2. Bhatsa Dam - Wikipedia

    en.wikipedia.org/wiki/Bhatsa_Dam

    The height of the dam above lowest foundation is 88.5 m (290 ft) while the length is 959 m (3,146 ft). The volume content is 18.25 km 3 (4.38 cu mi) and gross storage capacity is .97615 km 3 (0.23419 cu mi). [1] Bhatsa Dam with open gates due to overflow of water

  3. Parshall flume - Wikipedia

    en.wikipedia.org/wiki/Parshall_flume

    The derived equations above will always underestimate actual flow since both the derived C and n values are lower than their respective chart values. For the Parshall flume equation used to calculate the flow rate, both empirical values C and n are known constants (with various values for each Parshall flume size) leaving Ha (depth upstream) as ...

  4. Irrigation scheduling - Wikipedia

    en.wikipedia.org/wiki/Irrigation_scheduling

    Irrigation scheduling is the process used by irrigation system managers to determine the correct frequency and duration of watering. The following factors may be taken into consideration: Precipitation rate of the irrigation equipment – how quickly the water is applied, often expressed in inches or mm per hour.

  5. Irrigation - Wikipedia

    en.wikipedia.org/wiki/Irrigation

    Micro-irrigation, sometimes called localized irrigation, low volume irrigation, or trickle irrigation is a system where water is distributed under low pressure through a piped network, in a pre-determined pattern, and applied as a small discharge to each plant or adjacent to it. Traditional drip irrigation use individual emitters, subsurface ...

  6. Field capacity - Wikipedia

    en.wikipedia.org/wiki/Field_capacity

    This usually occurs two to three days after rain or irrigation in pervious soils of uniform structure and texture. The nominal definition of field capacity (expressed symbolically as θ fc) is the bulk water content retained in soil at −33 kPa (or −0.33 bar) of hydraulic head or suction pressure.

  7. Drainage equation - Wikipedia

    en.wikipedia.org/wiki/Drainage_equation

    A drainage equation is an equation describing the relation between depth and spacing of parallel subsurface drains, depth of the watertable, depth and hydraulic conductivity of the soils.