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Last modified
1/26/2010 2:21:28 PM
Creation date
10/12/2006 1:27:45 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8274.400
Description
Colorado River Basin Salinity Control - General Basinwide Salinity Issues - NPDES
Basin
Colorado Mainstem
Water Division
5
Date
9/1/1995
Author
Applied Hydrology
Title
Salinity Control Study - NPDES Permit No. CO - 0042161 - Prepared for Twentymile Coal Company
Water Supply Pro - Doc Type
Report/Study
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<br /> <br />., <br /> <br />,... <br />,... <br />l\:> <br />CD <br /> <br />~ <br />~,~ <br /> <br />j::; <br /> <br />".:. <br /> <br />'~"~ <br /> <br />" <br /> <br />, NPDES;Permit No. CO-0042161 <br />Salinity Control Study <br /> <br />Twentymile Coal Company <br /> <br />3.0 Options for Reduction or Elimination of Salt Discharge <br /> <br />Discharge occurs at Point 001 (Station 115) to mine dewatering at the Fish Creek Borehole. <br />Average )nonthly flows range fromO to 0.9 cfs~ although instantaneous flow as high as L8cfs <br />has been :measured; flow commonly ceases when pumps are not active. <br /> <br />Treatment or containment options which would eliminate or reduce salt discharge from the <br />mine discharge are developed below. These options include complete salt elimination by deep <br />well inj~ion of all pumped water (Option 1), partial salt removal by reverse osmosis <br />(Option 2), and partial salt reduction by deep well injection (Option 3). The conceptual details <br />for these iopdons are developed further in this Section. <br /> <br />3.1 Option 1: - Deep Well Injection Elimination of Sait Discharge <br /> <br />Deep well injection and eVapOration pond treatment were initially considered for complete salt <br />elimination. It was concluded that an evaporation pond would not be suitable for treatment of <br />this disc~arge because there is no place to locate an evaporation pond large enough to treat this <br />relativel)\ large and nearly continuous flow. Thus the only practical option for complete <br />elimination of salt discharge would be deep well injection. Based on the report <br />"Reconn.issance of Ground-Water Resources in a Part of the Yampa River Basin Between <br />Craig anJI Steamboat Springs, Moffat and Routt Counties, Colorado" (Brogden and Giles, <br />1977), tile shallowest formation which would appear to be suitable for deep well injection is <br />the Dakola Sandstone, at a depth more than 6000 feet below surface. ' , ' <br /> <br />In this conceptual evaluation, it is assumed that two deep injection wells would be required to <br />accomm4date the entire discharge. These injection wells would be installed at two different <br />locations; each approximately 1,000 feet from the existing sedimentation pond. Ideally, each <br />injection, well should be capable of injecting flows up to 500 gpm so that each well cOuld <br />accomm4date most discharges and both wells would have sufficient capacity for the higlJ.est <br />discharg4 measured during the 1990 through 1994 record of 800 gpm. This would permit pne <br />well to treat normal discharge in the event that the other well was out of service for repair or <br />maintenance, It would also provide additional injection capacity in the event that mine ' <br />discharg~ rates were to increase. ' <br /> <br />The existing sedimentation pond would remain to facilitate removal of particulates but would <br />be expanded and upgraded to provide storage and surge capacity in this option. The primary <br />outlet wOuld be closed. The emergency outlet would discharge only under upset or by-pass <br />conditions such as plugging Qt: the injection wells, equipment failure, or extreme storm events. <br /> <br />, <br />1 <br />, <br />';]' <br />>1 <br />" <br />, <br />) <br />.' <br /> <br />, <br />. <br /> <br />AHA Fdc:name: 14S~Nl.DOC <br /> <br />Page 14 <br /> <br />2:52 PM 09129/95 <br /> <br />j <br />
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