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 stream condition reservoir size reservoir operating condition diamond fork below monks hollow maximum capacity alternativereservoir Alternative reservoir acre feet present conditions sixth water flow through syar reservoir 910 sixth water reservoir 560 monks hollow reservoir 31400 fifth water pumped storage fifth water reservoir 49700 monks hollow reservoir 31400 sixth water pumped storage syar reservoir 4400 sixth water reservoir 620 monks hollow reservoir 31400 1964 DPR syar reservoir 930 sixth water reservoir 1020 hayes reservoir 51500 maximum surface area acres 31 19 343 530 343 70 20 343 30 28 680 maximum depth feet 64 85 230 277 232 116 82 232 65 105 180 mean depth feet 22 30 82 88 82 68 31 82 22 32 60 average content acre feet 590 540 23800 41500 23900 2450 560 23900 600 770 29800 detention time days 1 2 1 2 2040 20 40 7090 70 90 35 55 2 7 1 35 55 1 1 20 80 maximum reservoir maximum stream dissolved oxygen temperature C temperature C range egl mgl condition condition condition condition condition condition A al 1 b2 ba A al 1 b2 ba A ai 1 bl bl2 bla 7 10 8 11 915 9 15 12 16 13 17 7 11 8 11 915 9 15 710 7 10 811 8 11 9 15 1619 16 19 16 19 17 20 17 19 17 19 16 19 16 19 17 20 16 19 1619 16 19 17 19 17 21 9 15 13 17 9 15 9 11 17 21 17 20 17 19 17 20 16 19 711 7 11 48 4 8 248 148 14 24 8 48 4 8 44 4 8 7 11 6 10 6 10 6 10 6 10 I 1 1 condition A is for those years when water is released from below the thermocline in strawberry reservoir T 2 condition B is for those years when water is released from above the thermocline therraocline in strawberry reservoir T 3 presently the dissolved oxygen levels in strawberry reservoir range from 0 to 3 mgl egl below the thermocline and from 6 to 10 mgl egl 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/3135

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