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Electrical Power for Valdez and the Copper River Basin-1981

Electrical Power for Valdez and the Copper River Basin-1981

Electrical Power for Valdez and the Copper River Basin-1981

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As stated previously, two alternative sites have been proposed <strong>for</strong><strong>the</strong> powerhouse. Ei<strong>the</strong>r site would require clearing of approximately1.5 acres <strong>for</strong> construction purposes. Some alteration of <strong>the</strong> streambank<strong>and</strong> streambed will result from installation of <strong>the</strong> tailrace <strong>and</strong>sedimentation could occur. The magnitude of <strong>the</strong>se impacts could bereduced significantly depending on <strong>the</strong> construction techniquesutilized <strong>and</strong> <strong>the</strong> time of work.Impacts which would result from ei<strong>the</strong>r of <strong>the</strong> proposed powerhousealternatives were described above. Those impacts which would vary,depending on <strong>the</strong> site selected, are described below.<strong>Power</strong>house Alternative Itl: The discharge of flow from this alternativeis proposed by·<strong>the</strong> CE directly from <strong>the</strong> tailrace into AllisonCreek. Radical flow changes would result <strong>and</strong> all adverse impactsdescribed previously <strong>for</strong> alteration of flow would occur. In addition,if instream flows were totally dependent on power generation needs,periods of very low flow could result when <strong>the</strong> power plant was shutdown <strong>for</strong> maintenance or o<strong>the</strong>r reasons.The discharge of all project flows into Allison Creek at this sitewould also result in temperature <strong>and</strong> possibly dissolved oxygenimpacts occurring in <strong>the</strong> total reach of Allison Creek utilized byf ish. Flows in <strong>the</strong> creek above this site may not have any appreciablebuffering effect <strong>for</strong> maintenance of natural water qualitysince <strong>the</strong>y would be low in relation to <strong>the</strong> flow through <strong>the</strong> powerhouse.<strong>Power</strong>house Alternative 1t2: Impacts described above <strong>for</strong> site Itl mayalso be applicable to this alternative. This alternative has twotailraces proposed. If <strong>the</strong> tailrace waters were discharged directlyinto Port <strong>Valdez</strong> during <strong>the</strong> summer months, a portion of <strong>the</strong> salmonpopulation could be diverted away from spawning areas in <strong>the</strong> naturalstream by <strong>the</strong> larger quantities of Allison Creek water issuing from<strong>the</strong> tailrace into Port <strong>Valdez</strong>. Diverting water from <strong>the</strong> powerhousethrough <strong>the</strong> tailrace positioned in Allison Creek would alleviatethis impact; however, those impacts discussed above under powerhouse1t1 would occur. Hhen <strong>the</strong> discharge is diverted back through <strong>the</strong>tailrace into Port <strong>Valdez</strong>, some of <strong>the</strong> redds could be dewatered.Also, <strong>the</strong> discharge could prove to be such an attractant to adultsalmon that <strong>the</strong>y would pool up below <strong>the</strong> discharge <strong>and</strong> not utilizeo<strong>the</strong>r portions of <strong>the</strong> stream or intertidal area <strong>for</strong> spawning.Periods of very low flow during powerhouse shut down could alsoresult from this alternative. The proposed 6 inch diversion pipecould be used to add supplemental water to <strong>the</strong> creek. However, <strong>the</strong>use of <strong>the</strong> diversion pipe <strong>for</strong> long periods to supply water to <strong>the</strong>stream or as a substantial supplement to natural flows could alsocause early fry emergence as dicussed earlier.Diversion of flows directly into Port <strong>Valdez</strong> during most of <strong>the</strong> yearwould result in a reduction of water velocity in <strong>the</strong> natural stream~bed which could result in sedimentation of <strong>the</strong> spawning gravel.

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