Laserfiche WebLink
<br />Comments to SWSIJ November 3, 2003t by John Wiener <br /> <br />28 <br /> <br />Does this example define the problem? If not, can it be corrected or repafred? If it doest then <br />the approach which seems most usefu' right now is a meeting of the rjght people, to work on how <br />and under what circumstances the kind of Uclose enough II estimations described can be <br />producedt For example, are there geological limitationst such that Plains alJuvial river valleys <br />could use an approach that wouJd not work well enough in montane environments, or vice versa? <br />Are soil conditions critical, or simply a factor that has to be taken into account? And can NACS <br />maps suffice, or shourd there be some program for competent engineers to make measures <br />which wou'd suffice? And so on... I envision this, if it can be done, to be a sort of very <br />transparent expert system applying the necessary terms and information to make useable <br />estimations to begin experiments with new management techniques. <br /> <br />Additional features of the problem: What are the variables? <br /> <br />FortunatelYt there are a smaU number of changes in technology that may be sufficiently common <br />to warrant consideration~ But~ are there a relatively small number of other important features to <br />make this feasibre? Can the slope, son, depth of horizonst and other factors be treated in simple <br />enough form to make adequate estimations achievable with the needed speed and low cost? Or, <br />are there some conditions in which these estimations can be madet and others in whjch they <br />should not be used? <br /> <br />From a different perspective, there are various conditions identified in materials such as those <br />from the Cooperative Extension Service, on how to identify best management practices (BMPs) <br />for irrigation for a given field (e.g~ Waskom 1994). These variables may be important for the <br />problem at hand. <br /> <br />They include: <br /> <br />Soil and crop properties: <br />1. Water holding capacity of different soil textures (sometimes called fierd capacity; measure <br />usually by inohes of water per foot of soil); additionally, depth to different soil horizons may be <br />important <br /> <br />2. Maximum rooting depths of different crops4 <br /> <br />3. Approximate efficiency of the various irrigation appUcation methods (for BMP considerations, <br />mean percentages of technologies have been described as: <br />· furrow - 40% <br />· surge -. 60% <br />· sprinkler - 75% <br />· drip - 90% <br /> <br />These are means for rough guidance] subject to site and particular technology features. <br /> <br />4. The total seasonal crop water use is also important for selection of irrigation technology, and <br />should be relevant to estimation of the consumptive use from a glven combination of choices and <br />place. <br /> <br />There are also relatively few changes in irrigation technology that make sense and increase water <br />de'ivery effici~ncy (Smith et al 1996; CP'A, various)~ They include: <br /> <br />Structural changes to irrigation technology~ <br />1 4 ditch to pipe <br />1. ditch to Uned pipe (significantJy different from pipe?) <br />