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<br />000Y.14. <br /> <br />3 <br /> <br />necessitate similar analyses there.. Releases from the Narrows Reservoir and <br />from the proposed Two Forks Reservoir will require such studies on the South <br />Platte River. Major releases to industrial users such as Eastman Kodak on the <br />Cache la poudre River will bring pressure there for better estimates. <br /> <br />-, <br /> <br />The methodology and techniques for these determinations are not well es- <br />tablished because of Colorado's utilization of long river reaches for trans- <br />portation of water and Colorado's Appropriation Doctrine are somewhat unique <br />in the world. It is well, however, to pay tribute to Mr. Hinderlider and his <br />early studies at this time hecause his pioneering work serves as a fine ex- <br />ample for modern day hydrologists. <br /> <br />OBJECT I VES <br /> <br />I ' <br /> <br />This assignment was undertaken In Water Division No.2 to determine the <br />travel time and transit losses of the Frylngpan-Arkansas Project water diver- <br />sions introduced into the Arkansas River because the Southeastern Colorado <br />Water Conservancy District must repay the Federal Government over a SOJyear <br />period for the cost of the project, and it is realized that accurate travel <br />time and an accurate charge for transit losses are required so that the re- <br />payment contract is not jeopardized. The Division of Water Resources, the <br />Southeastern Water Conservancy District, and the U. S. Geological Survey are <br />presently cooperating in an effort to determine travel time and transit losses <br />of transmountain diversions of the Fryingpan-Arkansas Project down the Arkansas <br />River, and it has been determined that It will be necessary to Interpret the <br />results of the hydrologic data developed by the U.S.G.S. so that it can be <br />used for administrative purpo~s by the State Engineer in a practical and <br />everyday manner. It was further determined that to be able to Interpret the <br />basic hydrologic, data to the best possible extent, the engineer would need an <br />intimate knowleqge of the Arkansas River from its headwaters to the points of <br />diversion downstream. This, coupled with the desire to experiment with addi- <br />tional ideas and techniques for determining travel times and transit losses, <br />led to the present study to evaluate many techniques in the analysis of travel <br />time and transit loss. <br /> <br />PROCEDURES <br /> <br />These technlquQs, utilizing temperature recordings at critical points, <br />the use of fluorescein dye, the use of floating objects which could be <br />physically observed, and the measuring of dissolved solids In the river at <br />critical points and critical times, were chosen. In addition, the engineer <br />examined the river channel for much of its length to observe localized hydro- <br />logic and hydraulic conditions. For instance, the general relationship be- <br />tween riffles and pools, areas of ground water inflow, reaches of rocky canyon <br />which are essentially impervious, the character of Irrigation diversion head- <br />works along the river, the location of tributaries, and the general exposure <br />of the water surface as related to evaporation potential, were considered to <br />be matters requiring personal field knowledge. Numerous photographs were <br />taken for record purposes and for subsequent study In the office. These in- <br />cluded black and white, color, and Infra-red, both from on the ground and <br />from the ai r. <br />