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<br />'"":) <br /> <br />r -~ <br /> <br />~ <br />c8_~ _ _____ ___________ <br />"'- - ':;1 <br />or greater assumed releases from stornge, vnll have the effect of reducing <br />losses of water from the reservoir by evaporation and spill (a result which <br />is evident and admitted), and vrill thereby increase the "amou"'ts of usable <br />water," - a conclusion questioned by Colorado depending on wh~t is meant by <br />"usable water." On the other hand, the ~raphs and other tS:~lUlations Bubmit- <br />ted by Kansas tend to show that greater assumed relee,ses from storaze are <br />also accompanied by smaller average volumas of water in storage, and by per- <br />iods of greater frequency and longer duration when the reservoir 'viII be <br />empty. This means that the assumed greater releases from storage must be <br />made during shorter periods of time, and that any release in exoess of essen- <br />tial irrigation requirerrwnts at the time, even though such excess release <br />be at divertible rates, may in f'aot be wasted and lost t~ough non-use. Ele- <br />ments of time as well as volume are neoessarily involved in such water supply <br />and irrigation requirment considerations, and estimates of losses of water <br />should inolude totals fram both river and reservoir. <br /> <br />-7- <br /> <br />re, <br /> <br />18. As shawn by available streamflow records at the State line and Garden <br />City, relatively large volumes of divertible strearnflows (and of so-called <br />"usable water" as here calculated by Kansas) were wasted and lost through non- <br />use for the reason that, at the intermittent ti~~s of their occurrence, their <br />volumes were in excess of essential irrigation requirements at the time. Plans <br />for operating the irrigation pool in Caddoa Reservoir should not be;based on <br />arbitrarily assumed releases from storage, but should recognize, ,among other <br />things, that water supplies at and below Caddoa are related to each other, <br />are parts of the waters of the intsrstate stream, and are not unlimited in <br />amount; and that reservoir operations, to regulate Caddoa flows heretotore di- <br />verted and used in Colorado and Kansas, and to conserve Caddoa flovm hereto- <br />fore unused and wasted by Garden City, should oontemplate releases from stor- <br />age to supplement the supplies divsrted from unregulated streamflows and re- <br />ceived fram natural precipitation. <br /> <br />'--- <br /> <br />19. From river and reservoir oper~tion studies previously made by Colo- <br />rado it appears tl--8.t "demands on the reservoir" asslJ.'lIed by Kansas in Studies <br />3 and 4 ,were arbitrary and excessive, with the result that the calculated <br />greater' "amounts of usable water," and of so-called "new water" estimated <br />therefrom, are misleading. The reported results of Study 2, after correction <br />for "Caddo a flmvs heretofor's used in Kansas," indicate an avernge annual quan- <br />tity'of so-called "new water" that appears to be consistent with the quantity <br />of so-called "surplus" calculated by Colorado for the same period used by <br />Kansas, when the tvlO results are adjusted to the same basis for ths amcunts <br />of water heretofore used in Water District 67 and in Kansas. <br /> <br />;.- <br /> <br />20. Both the "new water" and "surplus" quantities above mentioned were <br />calculated, and reported as averages, for a study period representing what <br />may be termed the first-half of the useful life of Caddoa Reservoir irrigation <br />pool, during which the effective storage capacity, progressively diminished <br />by siltation, averaged about 300,000 acre feet. Similar studies covering the <br />second-half of the useful life of the irrigation pool, if made, would involve <br />an effective storage oapacity aver.~ing about 100,000 acre feet, or one-third <br />that assumed for the studies under discussion, and probably would disclose <br />oorrespondingly smallsI' quantities of "new" or "surplus" wntsr. \ihen the <br /> <br />'- <br />