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<br />Comments to SWSI, November 3, 2003J by John Wiener <br /> <br />29 <br /> <br />2. ditch to gated pipe <br />3. pipe to gated pipe <br />4. pipe to surge valve <br />5. furrow to sprinkler <br />6 ~ furrow to drip <br />7. furrow to subsurface drip <br />8. sprinkler to better sprjnkJer (e.g. low pressure or drag hose) <br />9.. sprinkler to drip <br />10. sprinkler to subsurface drip <br />11. better sprinkler to drip <br />12~ better sprinkrer to subsurface drip <br />13. drip to subsurface drip <br /> <br />Structural changes to land: <br /> <br />14. terracing, contouring <br />15. leveJin 9 <br />16. aJtered tiUage or conservation tiUage. <br /> <br />Information management <br />17. 'rrigation scheduling to meet needs by soH moisture <br />18. deficit irrigation (strategic deficits; timing shortages) <br />19. fertilizer timing <br /> <br />Crop changes <br />20. change crops J cr,op m ix, or rotation <br /> <br />Although the permutations of these factors would be intractable, farming does not apply all of <br />them, and the scope of practical inquiry is considerably smaUer. <br /> <br />What to do? An approach to the problem of estimating irrigation efficiency and <br />return flow obligations: <br /> <br />A. To the extent possible, a first step would be to narrow the range of crops and thus agronomic <br />faotors which may be relevant. Perhaps only a few need be considered, such as fodder cornt <br />table or sweet corn, alfalfa, a hay crop, a small grain (oats?), and a representative vegetable. <br /> <br />B. Secondt the set of 20 changes noted could be narrowed as well, using expert opinion and <br />experience to select the most likely or most common changes for a given basin or agricultural <br />reg ion. <br /> <br />c. Third, the 5oi' and sub-soil properties cQurd be consjderedt and representative types could be <br />identified if there is sufficient representativeness in a given region. The Arkansas Val fey t for <br />example, has underlying georogic and geomorphic uniformity, but ditches have different areas of <br />soil types and soil processes which may be important variables (e~g4 the different salinity <br />conditions mapped by Gates at al., as well as different soils). <br /> <br />D. The integration of the first three steps would be identification of the range of cases which can <br />be reasonably expected to cover a usefuJ portion of current water use and potentia' transfers. <br />Although daunting in prospect, the extent of Jocal knowredge from agricultural extension and <br />USDA and other experts, as wen as the private sector, will quickly provide much of this. <br /> <br />E. Taking the selected set of representative cases~ the final question may be asked: can the <br />re'evant irrigation and return flow conditions be adequately estimatedJ given the current state of <br />knowledge? <br />