Record Details

page 134

Digital Collections at BYU

Field Value
Title page 134 Central Utah Project, Bonneville Unit : Diamond Fork Power System : final Environmental Impact Statement, page 134
Coverage Electronic reproduction;
Format 134 text/PDF
Rights Brigham Young University; http://lib.byu.edu/about/copyright/generic.php Public Domain Public
Language English; eng; en
Relation Central Utah Project; Western Waters Digital Library; CHAPTER IV AFFECTED environment AND environmental consequences table 28 diamond fork power system water quality data summary alternativereservoir Alternative reservoir present conditions sixth water flow through syar reservoir sixth water reservoir monks hollow reservoir fifth water pumped storage fifth water reservoir monks hollow reservoir sixth water pumped storage syar reservoir sixth water reservoir monks hollow reservoir 1964 DPR syar reservoir sixth water reservoir hayes reservoir reservoir size maximum capacity acre feet maximum surface area acres maximum depth feet reservoir condition mean depth feet average content acre feet detention time days maximum reservoir temperature C condition al condition b2 ba stream condition diamond fork below monks hollow maximum stream temperature C condition ai A 1 condition b2 ba dissolved oxygen egl mgl condition A al 1 condition b2 ba 17 21 17 21 711 7 11 711 910 31 64 22 590 1 2 7 10 16 19 560 19 85 30 540 1 2 8 11 16 19 31400 343 230 82 23800 2040 20 40 915 9 15 17 20 9 15 17 20 48 4 8 6 610 gio glo 10 49700 530 277 88 41500 70 90 12 16 17 19 31400 313400 343 232 82 23900 35 55 13 17 17 19 13 17 17 19 14 34 8 6 610 gio glo 10 4400 70 116 68 2450 21450 2 7 7 11 16 19 620 20 82 31 560 1 8 11 16 19 31400 343 232 82 23900 35 55 9 15 1720 17 20 9 15 17 20 48 4 8 6 610 gio 10 930 30 65 22 600 1 7 10 16 19 1020 28 105 32 770 1 811 8 11 16 19 9 11 16 19 A fl 108 48 4 8 6 610 gio 10 51500 680 180 130 60 29800 20 80 915 9 15 17 1719 19 I 1 1 condition A is for those years when water is released from below the thermocline in 2 condition B is for those years when water is released from above the thermocline in strawberry reservoir 3 presently the dissolved oxygen levels in strawberry reservoir range from 0 to 3 mgl egl below the thermocline and from 6 to 10 egl mgl above the thermocline the low range values shown in this table are expected only locally in association with the low values of the inflows from strawberry reservoir the potential 2 to 5 mgl egl values will not occur over the entire water column and are not expected to impact the fisheries the dissolved oxygen levels in fifth water and monks hollow reservoirs are not expected to be any lower than those currently found in strawberry reservoir 4 below sixth water reservoir 134
Identifier http://cdm15999.contentdm.oclc.org/cdm/ref/collection/WesternWatersProject/id/3986

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