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Last modified
1/26/2010 12:34:25 PM
Creation date
10/11/2006 10:54:45 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8271.200
Description
Colorado River Basin Salinity Control Program - Development and History - UCRB 13a Assessment
Basin
Colorado Mainstem
Water Division
5
Date
9/21/1980
Title
SPE 9314 - The Availability of Water for Oil Shale Development in the Upper Colorado River Basin
Water Supply Pro - Doc Type
Report/Study
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<br />of' 9314 <br /> <br />J. WILLIAM McDONALD <br /> <br />3 <br /> <br />l'I'" <br />00 <br />C,Jl <br />C,.n <br /> <br />from more than 30,000 milligrams per liter (mg/l) to <br />8S low as 1.000 mg/I. Water of such quality, Which <br />will probably have high fluoride and boron concentra- <br />tions also, would have to be treated before being <br />applied to any industrial use (or before being dis- <br />charged to surface screams 1n the case of excess mine <br />drainage) . <br /> <br />Since the shale resource 1s a geologic member of <br />the Piceance Creek structural basin, it 1s likely <br />that ground water will be an important consideration <br />1n the development of an oil shale industry, whether <br />used as a source of 6upply or not. For example, <br />dewatering of mines and underground retorts could <br />produce amounts of water significantly in excess of <br />a plant's consumptive use requirements. Finally~ the <br />quality of the ground water has cost implication for <br />its use and disposal. <br /> <br />Uinta Basin, Utah. The Uinta Basin is a large <br />artesian basin in northeastern Utah which extends from <br />the Colorado border to the edge of the Great Basin <br />near Salt Lake City. The aquifer is presently in a <br />steady-state condition~ with discharge equaling re- <br />charge. Estimates of total water storage have not <br />been made. <br /> <br />With respect to water quality. total dissolved <br />solids concentrations range from a high of 4,030 oog/l <br />in the northeast portion of 011 shale tracts U-a and <br />U-b to a low of 1,760 rog/l in the southwest portion. <br />Hardness also varies northeast to southwest from <br />1,000 rog/l to 69 rog/l. The water is a sodluoo-su1fate- <br />bicarbonate type. The high levels of sulfate and <br />hardness would require treatment for any industrial <br />application. <br /> <br />Impacts of Developin~ Water Supplies <br /> <br />Developing water supplies for an oil shale in- <br />dustry may be expected to have a variety of economic, <br />social, and ecological impacts. Furthermore. the <br />impacts ~111 vary from one means of supply to the <br />next (e.g., surface water and ground water dev~lop- <br />ment may be expected to lead to different sets of im- <br />pacts) . <br /> <br />Impacts of Developing Surface Water Supplies. <br />As noted earlier, surface water supplies will be <br />available only if reservoir and pipeline facilities <br />are constructed. A very small work force is all that <br />would be required to operate and maintain Buch facil- <br />ities (on the order of 1 to 10 people for the ~ater <br />supply system of each unit-sized oil shale plant). <br />In contrast, the operational work force of a unit- <br />sized plant itself ~ould probably number around 1,000 <br />people. Thus, the economic and social impacts of <br />surface water developments would be insignificant in <br />contrast to the substantial impacts which would be <br />caused by the population growth that ~ill be asso- <br />ciated with the development of an oil shale industry. <br /> <br />The major impacts of developing surface water <br />supplies would stem from the depletion and re-'regula- <br />tion of stream flows. Fiehery habitat conditions and <br />recreational opportunities (e.g.~ rafting and kay- <br />aking) would be affected. Such effects could either <br />increase or decrease habitat availability and recrea- <br />tional opportunities depending upon the circumstances <br />at hand. <br /> <br />While it is difficult to generalize about in- <br />stream impacts, it is probable, given the likely 10- <br /> <br />cation of concentrated oil shale developments, that <br />the White River in Colorado and Utah would be more <br />adversely affected than any other river in the Upper <br />Basin. The second most impacted river would likely <br />be the Colorado Main Stem River from about Rifle to <br />Cameo, Colorado. <br /> <br />Both of these rivers are inhabited by federally <br />designated rare and endangered species (e.g., the <br />Colorado River squawfish and the humpbak chub). Thus, <br />the availability of surface water for oil shale devel- <br />opment in these two basins is a matter ~hich will <br />have to be considered not only in the context of state <br />water laws, but also 1n the context of the laws and <br />programs pertaining to the preservation and enhance- <br />ment of such species. <br /> <br />Impacts of Transferrin~ Water from lrri~ated <br />A~riculture. While it is not anticipated that there <br />need be transfers of significant amounts of water <br />from irrigaced agriculture to the oil shale industry, <br />such transfers are nonetheless possible under each <br />Upper Basin State's water rights system, as noted <br />earlier. The impacts that would be associated with <br />such transfers are discussed below. <br /> <br />With respect to economic imp8cts~ an acre-foot <br />of water transferred to the oil shale industry from <br />irrigated agriculture would, all other things being <br />equal, result in a regional loss in personal income <br />due to reductions in the size of agricultural sector. <br />However, there would be a regional income gain due to <br />the increased size of the industrial sector. Gener- <br />ally speaking, the gain would be from 10 to 100 times <br />greater than the loss. Any such transfers would also <br />result in a redistribution of income and economic <br />weal th. <br /> <br />Transfers of water from irrigated agriculture <br />would likely reduce the number of farm units in a <br />region and, in turn, the number of families deriving <br />their means from such enterprises. Thus, one might <br />be tempted to infer that significant changes in the <br />rural nature of the Upper Basin would accompany such <br />cransfers. However, the Upper Basin (or certain <br />counties therein) will bear scant resemblance to the <br />rural area it is today if a 1.5 million bbl/day <br />industry does come to pass. Thus. one must conclude <br />that such transfers would play a minor. role in shaping <br />social and economic conditions in the Upper Basin <br />relative to the larger economic and demographic force <br />that would be' brought to bear by oil shale develop- <br />ment in general. <br /> <br />It should also be noted that declines in irri- <br />gated agriculture may result from circumstances other <br />than transfers of water. For example, migration of <br />workers out of the agricultural labor market into <br />the more lucrative energy industries could reduce <br />agricultural activities. Other factors that could <br />cause declines in irrigated agriculture, regardless <br />of questions of water transfers, include urban land <br />conversion pressures in energy impacted communities <br />and the general cost-price squeeze that agricultural <br />enterprises face. In short, agricultural activities <br />and the social conditions associated with them will <br />probably change even if the oil shale industry does <br />not purchase water from irrigated agriculture. <br /> <br />Impacts of Develo?in~ Ground Water. As with the <br />economic and social impacts of reservoir construction <br />and operation, the impacts of ~ell drilling and <br />maintenance would pale in contrast to the economic <br />
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