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<br />000172 <br /> <br />SECTION I <br /> <br />INTRODUCTION <br /> <br />" <br /> <br />The matter of canal and stream losses in Colorado has long been a sub- <br />ject of great interest to irrigators, to state water administrators, municipal <br />officials, and others, and has been the objective of numerous field and office <br />studies since the early days of the development of the State. Seepage runs <br />have been made on many of the major irrigation ditches in the State at one <br />time or another, and most irrigation companies have ditch loss estimates which <br />the ditch rider uses in distributing water to the users. Ditch officials <br />real ize that the percentage of ditch loss varies greatly, depending upon the <br />amount of water being carried in the ditch, though they often apply a flat per- <br />centage for the sake of convenience and because of somewhat I imited basic data. <br />Generally when the amount of water being carried in the ditch drops to low <br />levels, the ditch loss percentage rises to a high value. With lower amounts of <br />water in the ditch, the technique of sectional ization of the ditch for admini- <br />stration purposes is used. <br /> <br />From the early beginning of irrigation in Colorado when reservoirs were <br />first constructed, rivers and streams have been used to transport water from <br />the reservoir to ditch headgates many miles below the reservoir. More re- <br />cently the wide use of exchanges from One ditch to another has meant more use <br />of natural streams and rivers for transportation of decreed water. Historically, <br />stream losses have been estimated and appropriate charges n~de to those trans. <br />porting the water, and while it was known that these losses were only generally <br />rough estimates, it was realized that there was nothing better to use. <br /> <br />f:. <br /> <br />On some of the streams of the State of Colorado, substantial effort has <br />been made to help define stream losses and travel times, and the most notable <br />of this work has been on the Arkansas River and the Cache la Poudre. Mean- <br />while, however, other rivers, such as the Colorado, have had almost no work <br />done, and only rough guesses exist relative to travel times and transit losses. <br /> <br />. <br /> <br />Following the drouth of the mid-1950's, unit costs of water have been rising <br />steadily throughout the State with the most notable increases occurring on the <br />eastern slope of Colorado where most of the State's urban development has <br />occurred and where the most intense farm land irrigation takes place. The ccn- <br />struction of large transmountain diversion projects and the construction of <br />large reservoirs in the stream headwaters has created more dependence on <br />natural streams and rivers for transportation purposes. This increase in the <br />amount of water transported in natural waterways, coupled with the higher unit <br />prices for water, has brought to bear more pressure for more accurate and <br />dependable estimates of travel time and transit loss. It is clear, even to <br />the layman, that the transportation downstream of 50,000 acre-feet of water <br />using a transit loss estimate which is only two percent off can result in an <br />overcharge or an undercharge of 1,000 acre-feet of water. With water being <br />worth perhaps $10 an acre-foot, this could represent a $10,000 error. This can <br />affect repayment capabil ities for particular projects. Perhaps more important <br />than the monetary aspect, however, is the potential adverse effect upon owners <br />of vested water rights where an under estimation of two percent would mean that <br />1,000 acre-feet was being taken from the natural waters available for distri- <br />bution to them for use by those transporting water. <br />