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Last modified
7/14/2009 5:02:30 PM
Creation date
6/1/2009 11:57:22 AM
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UCREFRP
UCREFRP Catalog Number
7317
Author
Cowan, M. S., W. R. Cheney and J. C. Addiego.
Title
Executive Summary of the Colorado River Simulation System.
USFW Year
1981.
USFW - Doc Type
Denver, Colorado.
Copyright Material
NO
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1 <br />~` ~~ F-"" <br />by either a minimum release rate, a flood space <br />storage requirement, demands which draw from <br />the reservoir, demands which draw from <br />upstream reservoirs and move water through the <br />reservoir, or the "Laws of the River." The <br />operations of Lakes Powell and Mead are large- <br />ly determined by the criteria and constraints <br />relating to the "Laws of the River." All calcula- <br />tions for reservoir operations aze based on <br />another form of the continuity equation: <br />Change in storage =Inflow -Outflow - <br />Evaporation -Change in bank storage <br />Evaporation, bank storage, and power produc- <br />tion are calculated ea:h time water is moved <br />through a reservoir. Evaporation is determined <br />by a monthly coefficient and the surface area <br />of the lake that month. Change in bank storage <br />is calculates as a percentage of the change in <br />surface storage each month. -This percentage <br />ranges from 6.5 percent in Lake Mead to 15 <br />percent in Lake Powell.. <br />After the entire system is in hydrologic balance, <br />salinities aze computed throughout the system <br />by a mass balance accounting procedure. Initial <br />salinities are read in from the hydrology file. <br />Salt pickup or removal is read in from the de- <br />mand file. The impact of the salt pickup or re- <br />moval is brought into the river by the return <br />flow of an associated diversion. <br />To route salt through a reservoir, complete <br />mixing is assumed. This approach, in a simpli- <br />fied form, was verified by Dr. John Hendrick <br />in his Ph.D. dissertation (1973), Colorado <br />State University, as applicable to Lake Mead <br />on a monthly basis. The concentration of salt <br />in the outflow is assumed equal to a weighted <br />average. of the beginning and ending concentra- <br />tions of the salt in the reservoir. <br />Operational Control Data <br />Operational control data are input to the <br />CRSM and include: reach identification and <br />basin configuration; reach description data <br />(location and identification of diversions, <br />return flows, inflows, and reservoirs); reservoir <br />and powerplant characteristics data; data con- <br />trolling output options- and various run param- <br />eters (i.e., starting and ending dates, etc.); and <br />miscellaneous data which control the opera- <br />tions and conditions specific to the Colorado <br />River Basin. <br />Reservoir operational characteristics data are <br />entered in the form of polynomial equations <br />for the following: <br />1. Reservoir elevation-area-capacity <br />relationships <br />2. Turbine horsepower output at full <br />gate versus head <br />3. Discharge versus head <br />4. Tailwater elevation versus flow <br />Polynomials for the reservoir elevation-azea- <br />capacity curves are selected to reproduce the <br />tables used in the operations of the reservoirs. <br />Manufacturer's rating curves are used for the <br />power output of the powerplants. Other reser- <br />voir operation data contained in the control file <br />are listed below: <br />1. Tazget capacities for each month - <br />rule curves <br />2. Bank storage coefficients <br />9 <br />
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