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Last modified
1/26/2010 2:27:20 PM
Creation date
10/12/2006 2:23:14 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8276.851
Description
La Verkin Springs Unit - Colorado River Salinity Control Program
State
UT
Basin
Colorado Mainstem
Date
1/1/1984
Title
La Verkin Springs Unit Utah Preliminary Findings Report
Water Supply Pro - Doc Type
Report/Study
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<br />VII. DESCRIPTION OF ANALYSIS FOR DESALTING PLANT ALTERNATIVE <br /> <br />This section describes, on a step by step basis, the analysis of the La Verkin <br />Springs Unit which considers a desalting plant. This desalting plant is <br />described in the previous report (USSR, February 1979). All the assumptions <br />listed in the main report are valid here. <br /> <br />The desalting plant alternat!ve considered here diverts 10.9 ft3/sec of La <br />Verkin Springs, returns 83ft /sec of product water (284 mg/L) to the Virgin <br />River and utilized 2.9 ft /sec of replacement water (705 mg/L) from Quail Creek <br />Reservoi r. <br /> <br />A. Estimate Concentration of Major Ions in Product Water From Desalting Plant <br /> <br />1. From Appendix C, Plans and Estimates (USBR, Fe~ruary 1979), the <br />product water salinity is 284 mg/L; 6328 AF/~ear, 8.74 ft /sec. The flow of <br />La Verk1n Springs was considered to be 12 ft /sec in the previous design <br />esticlates. The actual recovery rate is 8.74/12 = 73;,. <br /> <br />2. Consider La Verkin SP3ing flow to be 10.9 ft3/sec and an actual <br />recovery rate of 73~ yields 8 ft /sec at a salinity of 284 mg/L. <br /> <br />3. Fru~ Appendix C, plans and estimates, (USBR, February 1979) the feed <br />water for the final 2 stage processing has the ionic distribution and dissolved <br />solids concentration below: <br /> <br />Na <br />Ca <br />Mg <br />K <br />Cl <br />504 <br />Sl <br />F <br />B <br />TDS - <br /> <br />2615 mg/L <br />180 mg/ L <br />119 mg/L <br />184 mg/L <br />3408 mg/L <br />1930 m9/L <br />29 mg/L <br />2.6 mg/L <br />5 mg/L <br />8472.6 <br /> <br />4. Assume the percent ionic distribution does not change. Then the <br />ionic distribution of the product water which is returned to the river can <br />be apprC~lmatEd by multiplying each ion by 284/8473. The result of this <br />esti~~tE is presEnte~ bflow: <br /> <br />Na 88 mg/L <br />Ca 6 mg I L <br />"1g li. T:1g/ L <br />K 6 mg! L <br />Cl 114 mg!L <br />SO 65 mg/L <br />Si4 1 mg!L <br />F <br />B <br />TDS 284 mg!L <br /> <br />1CJ <br /> <br />OC2624 <br />
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