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Em4885 irrigation management practices to protect ground water

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27<br />

CHAPTER 4<br />

There are two major families of <strong>irrigation</strong> scheduling techniques. One is generally called<br />

“checkbook” or “<strong>water</strong> budget.” With checkbook scheduling, the <strong>irrigation</strong> manager first<br />

defines the depth or volume of root zone <strong>to</strong> manage. He/she then attempts <strong>to</strong> identify,<br />

measure, and predict all <strong>water</strong> going in<strong>to</strong> and out of this root zone. A common <strong>water</strong><br />

budget equation is:<br />

D 2 = D 1 + ETc + DEEP - IRR - RAIN + UP<br />

where:<br />

D 2 = root zone depletion at the end of a day<br />

D 1 = root zone depletion at the start of a day<br />

ETc = crop evapotranspiration for the day<br />

DEEP = deep percolation out of the root zone for the day<br />

IRR = <strong>irrigation</strong> <strong>water</strong> added <strong>to</strong> the root zone that day<br />

RAIN = effective rainfall for the day (that portion of the gross rainfall that infiltrates)<br />

UP = upwards percolation of <strong>water</strong> in<strong>to</strong> the root zone from a high <strong>water</strong> table<br />

These fac<strong>to</strong>rs are seen in Figure 4-8, a schematic of the crop root zone identifying the<br />

various types of <strong>water</strong> moving in<strong>to</strong> and out of it.<br />

All variables are defined in terms of inches of <strong>water</strong>. An <strong>irrigation</strong> is called for when the<br />

resulting <strong>to</strong>tal soil <strong>water</strong>, or soil <strong>water</strong> depletion, is predicted <strong>to</strong> reach some predetermined<br />

level, the “<strong>management</strong> allowed depletion” (refer <strong>to</strong> the discussion in Chapter 3 regarding<br />

soil-<strong>water</strong>-plant relationships). Checkbook <strong>irrigation</strong> scheduling will result in an estimate of<br />

both the timing and amount of <strong>irrigation</strong>s.<br />

Irrigation - IN<br />

Upward Movement from<br />

a Shallow Aquifer - IN<br />

Evapotranspiration - OUT<br />

Rain/Snow - IN<br />

Surface Runoff - O<br />

Deep Percolation - OUT<br />

FIGURE 4-8. Schematic indicating the different categories of <strong>water</strong> coming in<strong>to</strong> and going out<br />

of the effective crop root zone

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