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IRRIGATION SCHEDULING
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Information requirements for Water-Budget Irrigation Scheduling The actual water budget equation is simple, a starting soil moisture depletion and five numbers to add or subtract to determine the ending soil moisture depletion. The problems, and the costs, of water budget scheduling come with identifying those numbers. Accurate water budget irrigation scheduling requires knowledge of the following . . .
Most people doing water budget scheduling will also take (or they should be taking) regular measurements of soil and/or plant moisture. This will make sure that the estimates of the numbers are accurate. This looks like a lot of information and it is. But there are many sources available to you. Also, scheduling consultants will develop the required numbers as part of their service. Looking at the help available to you in finding the information needed (by category): SOILS - the Reference section of this handbook describes important properties of most important soils in the District. The UC Extension specialists also will have information, including Extension pamphlet #21463, "Holding Capacities of California Soils". Knowledge of the soil will provide estimates of field capacities and permanent wilting points as well as any restrictions to root zone development and salt levels. A very fine point of irrigation scheduling concerns the estimate of available water holding capacity, AWHC. We've said that AWHC is equal to the field capacity minus the permanent wilting point. And we've also said that it does no good to soak water into a soil already at field capacity as it will just drain through the root zone. However, depending on the soil and the depth of the root zone, it may take 2 or more days for this excess water to soak through. In this time the crop can be using some of the excess. In real terms, the AWHC may be somewhat more than the accepted value of field capacity minus permanent wilting point. The effect of this slow drainage in increasing the practical soil moisture reservoir vary with the soil. The effect will be greater on finer soils and deeper root zones than on coarse soils and shallower root zones. ROOT ZONES - it can be very difficult to set effective root zones and may take a couple of years of experience, especially with annual crops. Your UC Cooperative Extension specialist or consulting agronomist will have information for you. Make sure you consider any restrictions on the root zones due to hard pans or high water tables. The root zone of an annual is going to change constantly up to plant maturity. But the effective root zone does not have to be the full depth of the rooting system. For example, in cotton it is common to choose an effective root zone of 4 feet. This is done even though the full system might go to 6 foot or more. Remember, the effective root zone is where you want to control soil moisture. ALLOWABLE DEPLETIONS - AD's are a measure of how much stress is to be applied to a crop. AD's may change with the season. With cotton it was common (although not recommended with newer varieties) to put heavy water stress on early and then go to a more regular routine once the plant was fruiting. Be aware of the different growth stages of your crops and how they should be manipulated during these stages. Also, if you have fields with high salinity, the AD is likely to be lower than normal (keeping more moisture in the root zone). The Crop Data Sheets in the Reference chapter contain recommended water stress levels for the different growth stages of most important District crops. Many times, allowable depletions are "backed-in to" when first starting irrigation scheduling. The Grower is checking a field and finally decides to irrigate. The irrigation scheduling system is checked for the soil moisture depletion at the time of the irrigation. This is then converted to an allowable depletion for future use. |
For example, the maximum soil moisture reservoir (SMRmax ) of a field is calculated to be 5 inches. The Grower has decided that the crop is ready for irrigation. The irrigation schedule calculates that 2 inches of water have been used by the crop since the last irrigation (with no rainfall occurring). Thus the soil moisture depletion is at 2 inches at the time of irrigation. Now . . . AD% = 100 *
(SMD / SMRmax ) The Grower is letting the crop use 40 percent of the soil moisture reservoir between irrigations and this 40 percent allowable depletion will be used to schedule the next irrigation. EVAPOTRANSPIRATION, ETc - the District publishes the printed Irrigation Guide on a weekly basis, daily on the web site,with three editions for the North, Central, and South regions. All the major crops in the District, with several planting dates for many,are covered in the Guide. It includes a summation of the past 7 and 14 days and seasonal water use plus a predicted water use in the next 7 and 10 days. The Irrigation Guide provides information making it easier to schedule irrigations. It can also help in using the WWD Irrigation Scheduling Chart . The Scheduling Chart is used to calculate the next irrigation date. The District's Irrigation Guide is easy to use and contains direct estimates of crop water use. However, some consultants will develop their own estimates using a reference ET and crop coefficients. Although more time-consuming and subject to the same errors as the District's Guide, it does allow a field/crop specific approach to scheduling. An explanation of using reference ET and crop coefficients is contained in the Appendix. RAIN - rainfalls are reported by radio, TV, and newspapers. Many times they get their information from weather stations at airports. Actual rainfall in your field can vary widely from reported. Rain gauges are cheap. Place one near your fields to get an accurate measure of the actual rainfall. Note also that the total rainfall may not have soaked into the ground. Depending on the storm's intensity and duration, along with pre-existing field surface and moisture conditions, there might be significant runoff. It is your experience that judges how much rainfall is EFFECTIVE rainfall, rainfall that actually soaked into your field. Also, remember that soil at field capacity will still take in water. Rain may soak into the ground, but if the rain occurs just after a good irrigation, it may just be more deep percolation. IRRIGATION - there are many different methods used to estimate the actual net irrigation. Some people will take a soil moisture measurement a day or two after an irrigation to see what went on. (Remember that the "feel" method is the cheapest, fastest, most flexible method available.) Some will assume that the irrigation is excessive (especially with surface irrigations) and that soil moisture depletions are taken to zero during an irrigation. If using a sprinkle or trickle system, you should know what the application rate of the system is (refer to the System Management chapter of this handbook). Then, it is a simple matter of multiplying the application rate times the set time to estimate the irrigation. In most irrigation scheduling systems, a gross irrigation is reported so that the total amount of water delivered to the field can be tracked. The net irrigation, used in the water budget equation, is determined by applying an efficiency factor. That is . . . NET IRR = GROSS IRR x EFF The efficiency of an irrigation system can be estimated (See System Management and the Appendix). Many irrigation specialists offer this service. It is a good idea to have your system evaluated for distribution uniformity and irrigation efficiency. A detailed example of water budget irrigation scheduling is contained in the Appendix. There are also two UC publications that contain detailed examples and in-depth discussions of all of the above. They are numbers 21419, "The Water Budget Method - Irrigation Scheduling for Southern San Joaquin Valley Deciduous Orchards" and 21454 "Irrigation Scheduling - A Guide for Efficient On-Farm Water Management" Previous Page Next Page Top of Page |
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Last updated September 2000 |
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