L - Alaska Energy Data Inventory

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SECTION BPROJECT DESCRIPTION AND COST ESTIMATESTABLE OF CONTENTSItemSUMMARY OF CHANGESGeneral~JatanaDevil CanyonWATANADamSpillwayOutlet WorksDiversion Features and OperationPenstocks and WaterwaysDEVIL CANYONMa i n DamSpillwayDiversion StructurePowerplantPenstocks and WaterwaysCONSTRUCTION SCHEDULEGeneralDiversion PlansMa in DamsPower-on-LineTransmission LineCOST ESTIMATESDetailed Cost EstimatesCont -j ngenc i esWatanaDevil CanyonPageB-1B-1B-18-2B-3B-3B-3B-48-4B-4B-5B-5B-5B-5B-6B-6B-7B-7B-7B-7B-7B-8B-9B-9B-10B-10B-llLIST OF TABLESNumber Title PageB-1 Detailed Cost Estimate - Watana (First added) B-13B-2 Detailed Cost Estimate Devil Canyon Concrete Gravity(Second added) B-23i
Page 1 and 2: Southcentral Railbelt Area, AlaskaU
Page 3: SECTION AHYDROLOGYThe 1976 Interim
Page 7 and 8: SUMMARY OF CHANGESGENERALField surv
Page 9 and 10: WATANADAMThe crest length of the da
Page 12: POWERPLANTThe access tun~el to the
Page 15 and 16: COST ESTIMATESDETAILED COST ESTIMAT
Page 17 and 18: The construction facility requireme
Page 19 and 20: TABLE B-1--DETAILED COST ESTIMATEWA
Page 21 and 22: CostAccountNumber0404.2"II\I\L[ L;-
Page 23 and 24: 1/\1 ~ LI_ 1\- 1- -IJU /\ l LI_IJ e
Page 25 and 26: 1/\ I \ II ! \ - I - -Il L"I/\I L I
Page 27 and 28: I/\[ILL 11-1--l)LII\JUjJ COSIISIJr~
Page 29 and 30: TABLE B-2--DETAILED COST ESTIMATtDE
Page 31 and 32: T/\I~LEIJI:VIL CMYOI~Il-2--DUAILED
Page 33 and 34: TA3LE 8-2--DETAILED COST LST1MATE--
Page 35 and 36: TABLE B-2--UETAILED COST LSTIMATE--
Page 39 and 40: 2:18!l14~ODEVIL CANYONDilioncit rtf
Page 41 and 42: ,.------rr I.35' 5' 8' 12' 3' 7'II
Page 43 and 44: STOPLOG SLOT_N0!i~~OLMAXIMUM SURCHA
Page 45 and 46: \"ABA~DO!, ED,---j"AIRSTAIP(\ SWITC
Page 47 and 48: SECTION CPOWER STUDIES AND ECONOMIC
Page 49 and 50: TABLE OF CONTENTS (cont)ItemPlan Ju
Page 51 and 52: SUMMARY OF CHANGESThis section upda
Page 53 and 54: TABLE C-lSTUDY AREA POPULATION AS P
Page 55 and 56:
in 1959 to $4,644 in 1970 while the
Page 57 and 58:
nI'-JTABLE C-4ALASKA ECONOMIC INDIC
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PRESENT AND HISTORICAL POWER REQUIR
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SUMMARY OF CHANGESFUTURE POWER NEED
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and Economic Research and from the
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Fisheries: The fisheries sector pri
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in employment required to process t
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The level of construction employmen
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Government expenditures other than
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SECTORSAgri cultureEmploymentHIGHTA
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SECTORSHIGHLumber 1. Annual cut by
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TABLE C- 8 (cont)nIN"-.JSECTORSMini
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TABLE C-8 (cont)n ,N1.0SECTORSTotal
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of employment in these industries w
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growth rate for Anchorage (1973-197
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TABLE C-11SELF-SUPPLIED INDUSTRY SE
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Peak PowerTABLE C-13ANCHORAGE-COOK
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CREDIT FOR ENERGY AND CAPACITYThe a
Page 91 and 92:
ut before Devil Canyon power would
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Fi gure C-3ANNUAL HEAD DURATION CUR
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TABLE C-15USABLE CAPACITY AND ENERG
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14Fi gure C- 512SOUTHCENTRAL RAILBE
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percent of average. The 10 month pe
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2,185-_-_--~ MAXIMUM WATER SURFACE-
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50 20I I10 8 5 4 3I I I I IRECURREN
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TABLE C-18ANNUAL COST COMPUTATIONS(
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Natural Gas AlternativeIn not provi
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essentially doubling gas use by tha
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NOTES TO TABLE C-19:11 Based on "Oi
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TABLE C-211976 ALASKA GAS USE JjUse
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To gain an exemption based on an in
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capita 1 rel ocati on wi 11 affect
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The thermal alternatives are proced
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TABLE C-23INTERTIE CAPACITY BENEFIT
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These figures indicate that, given
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Variations in the Load Forecast and
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during construction assume that flu
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For this analysis, inflation is ass
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downward pressure on prices. To off
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Three sample cases are analysed. Fi
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Figure C-II350SENSITIVITY TO INFLAT
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CORPS OF ENGINEERSU S. ARMY2:::z:::
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.. :;UFF IllE. T PLA •• T S 1"
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a,,[~: ".C"O"".. EA .C"",,,A;.~ C~S
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.. 01[.: .. I.C"O" .... E'~CHU~ ..
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AwEA:,,·.C-;[O~A.,E~ .en". tl·E C
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"f".ll"l"·;t.---------------1.•
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• .. E,u ."'CI'I"" ... tA~C~~~A'E
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4~EU .:-'(';(I"A",£."C"IHAiof C'SI
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A'E": ... ' .. v ..... E... C",· .
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aRE.: .... CHOkAioEA .CHn~AmE C.St:
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- .. fA: ...·.(H(\.." .. £A.C"U~A
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A .. E .. : .... (.,0 .... £l.r ..
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1."'(£4 .\ .. C"vII\A·~€.'.C" "
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EXHIBIT C-2LOAD RESOURCE ANALYSES (
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Figure C-2-24000SOUTH CENT RAL RAIL
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50004000SOUTI1CENTRAL RAILBELTLOADS
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Year1994199519961997199819992000200
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TABLE C-4-lCOAL-FIRED, FERC VALUESB
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TABLE C-4-3COAL - FI RED, FEDERAL F
Page 175 and 176:
TABLE C-4-5OIL-FIRED, FERC VALUES(M
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('"')I.+:00TABLE C-4-7OIL-FIRED, FE
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EXHI BIT C-5POWER BENEFIT CALCULATI
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00.. -'-Innl>~E5E~'TP::;;ESf"'TIOA;
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---_._-_ ... _------- _._---_._----
Page 185 and 186:
---.----.... ----~.('")I(J1I0'1..O'
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~ ,P~ESE 'IT:: -'ESt. 'IT""~ T- -4i
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c--'oPC!!£~E"TP~!St~T ~4C!.ET1~LE
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":)~1U"1I......N"PI( SE~T"~T" "":';
Page 193 and 194:
-~, -~.---P,! Sf'lT c·: ;f', ,,\ ~
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.. ---~.-.P'lO: SEt. T PRE:iEIIT MA
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PRESE~r PRESENT MAR~ETAeLE PRESE~T
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~~ .. --~----.-.-,---,.,JIl " : R!:
Page 201 and 202:
----------------------------------
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__ ~ ____ , ___ M_" ___ T ___._-_.-
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.,. PRESE'. T - ·PREstsT \4ARI3.74
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-~- ... "------------_._-----"";;ES
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.~~----CJIU1w •0PRESENT PRESENT ~
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TABLE C-6-1INVESTMENT COST WITH 2 Y
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WatanaTABLE C-6-3INVESTMENT COST WI
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EXHIBIT C-7CORRESPONDENCE
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-2-in the Beluga area to serve a re
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TABLE IAnnual Fixed Charge RatesAnc
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TABLE IIIHydroelectric Plant Power
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TABLE IVHydroelectric Plant Power V
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TABLE VHydroelectric Plant Power Va
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TABLE VIHydroe1ectric Plant Power V
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Department of Ener~yAlaska Power Ad
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Colonel George RobertsonPage TwoNov
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SECTION DFOUNDATION AND MATERIALSTA
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Number0-180-190-200-210-220-230-240
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NumberEXHIBITSTitle0-1 location Map
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4. The 1976 report recognized that
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REGIONAL GEOLOGYPHYSIOGRAPHYThe are
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gradients, became incised within gl
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The upper reaches of the reservoir
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SEISMIC REFRACTION SURVEYDEVIL CANY
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SCOPE OF INVESTIGATIONSField Reconn
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TABLE D-lSurface TipLocation Elevat
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TABLE 0-3Date High of Low of Date H
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The lower ri ver valley fl oor rang
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consists of 6 feet of silty clay ov
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At least two deposits of lake sedim
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few hours and then handled in the n
Page 263 and 264:
In general terms, the geology in th
Page 265 and 266:
This central section is supported,
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e designed so that there is a minim
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Quarry sites were located on the le
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to moisture contents higher than op
Page 273 and 274:
granitic rock with the remainder co
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-1I~u.s. Sf.MC)AID SII\I! ~ .. ICIB
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oI..j:::.oI ; . ~ ~.~.ST~,wt~i.~ .'
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-•jI20,c:;I~l- :r!260~1lDIl5so zG
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NPDEN-GS-L(79-S-404)14 NOV 1978WATA
Page 283 and 284:
.:..:;;)u"' ....,;>-'...;:;;z~';>-'
Page 285 and 286:
"t.-ax. ~H (l: ritJ/-O l:U:U~+.t:"~
Page 287 and 288:
~----------------------------------
Page 289 and 290:
______ +-S_Bmp---"-_1_e_N_o_-C_o_m_
Page 291 and 292:
Coefficient of Permeapility, ~O' 10
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TIME IN MINUTESos 2 S 10 20 so 100
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SHEET NO. 1TIME IN MINUTES2.05\I)~T
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O,j'/_6 /Coefficient of Permeapllit
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SHEET No. 2~0.1 0.2__ I. fl~ + - t'
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2.0 0 .1~O l--0.2j-TIME IN MINUTESt
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0'C-oS'-ZvCONCRETE AGGREGATE SOURCE
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U. S. ARMY..6,000-\'\., J t\/ __"J"
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CORPS OF ENGINEERSU~ S~ ARMYooooo0I
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CORPS OF ENGINEERSU, S. ARMYLEGENDS
Page 311 and 312:
- 2200- 2100- 2000~~v~, ~-,~IN.!M\I
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QTP-I2.• v BORROW.TP-IOTP-19~'"'-
Page 315 and 316:
CORPS OF ENGINEERSU. S, ARMYTOP Of
Page 317 and 318:
CORPS OF ENGINEERSU. $. ARMYTOP OF
Page 319 and 320:
CORPS OF ENGINEERSVALUE ENGINEERING
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DEPARTMENT OF THE ARMY ~~;~~5"'''''
Page 323 and 324:
DEPARTMENT OF THE ARMY~ORTH PACifiC
Page 325 and 326:
PfP¥M/CII~pp_~"1:U:I\IO __- ___=="
Page 327 and 328:
II~J1 01 SOUTHCENTRAL RAILBELT AREA
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SOUTHCENTRAL RAILBELT AREA. ALASKAS
Page 331 and 332:
i '7OATES- S,TAIft:7 APRv. _4START
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Dt.'I OAtLt,. DATES' $TART ~AY 1978
Page 335 and 336:
HOL£ . DEPTH OF CWERlURDENROCK DRI
Page 337 and 338:
RF. v.1978 CQMP. 3 Atr,OIAM. OF HOL
Page 339 and 340:
"OL!.OwS NEA":SHEAR ZONE,pc.ATE ll
Page 341 and 342:
I' [+r0017 3Z'l3'10.8SIB11'7. ~132
Page 343 and 344:
', J' II cH-llSOUTNCUT'''IL .... II
Page 345 and 346:
[)I
Page 347 and 348:
UR-249 BOXES'"ATAiiA OA:"SITE.. ) J
Page 349 and 350:
Page 351 and 352:
CORPS OF ENGINEERSNOTE ~O LOCAL CON
Page 353 and 354:
Page 355 and 356:
~~~R __________________CORPS OF ENG
Page 357 and 358:
Page 359 and 360:
Page 361 and 362:
RECONNAISSANCE OF THE RECENT GEOLOG
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IllustrationsFigu~1. Overlay showin
Page 365 and 366:
ice-rich which increases the probab
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Krinitzsky, Corps of Engineers, by
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GEOLOGIC BACKGROUNDThe geology of t
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table 1.Inferred faulta in the gene
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list of the kinds of scarps and lan
Page 375 and 376:
Ground and aerial observations alon
Page 377 and 378:
Wefound no evidence of active fault
Page 379 and 380:
are present. The fresh scarps obser
Page 381 and 382:
fault. Csejtey and others (1978) do
Page 383 and 384:
Visual observations during helicopt
Page 385 and 386:
Table 3.Location of selected exampl
Page 387 and 388:
elieved to be due to the combined e
Page 389 and 390:
lock. Two such slides were observed
Page 391 and 392:
Table 6.Locations where patterned g
Page 393 and 394:
Both tills and Tertiary fluviatile
Page 395 and 396:
Table 7.First-Order leveling from t
Page 397 and 398:
sand dikes that developed during se
Page 399 and 400:
earthquakes, according to presently
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SUMMARYOur geologic reconnaissance
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REFERENCES CITEDAnon., 1962, Engine
Page 405:
Turner, D. L. and Smith, T. E., 197
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EARTHQUAKE ASSESSMENT AT THESUSITNA
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PART I: INTRODUCTION1. The followin
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overflights, low sun angle photogra
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VII. ~yerybody runs outdoors. Damag
Page 416 and 417:
differences in fault mechanism and
Page 418 and 419:
not from lesser motions but simply
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PART III: EARTHQUAKE EVALUATION39.
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PART IV:INTERPRETED PEAK MOTIONS46.
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48. The motions in Table 2 of this
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~;arthquake-inducedlancisli(ies51 1
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()2. Possible induced seismicity fr
Page 430 and 431:
L1. Simpson, David W. (1976), Seism
Page 432 and 433:
mz ....0~a:::I&J...JI&JUU-
Page 434 and 435:
6050ItviEAN+ c:rtvi EANFAR FIELDu 4
Page 436 and 437:
40r-~------~----~------.-----~-----
Page 438 and 439:
30NEAR FIELD20--. ...II)oAI 3U~u 2I
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EXHIBIT 0-4Procedure for Estimating
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IntroductionThe procedure outlined
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equirements.Procedure(1) From the c
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NO. 340-104 DIETZGEN G~APH PAPERMIL
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-W-1oIWa::oenrr:wCL0:::WI 3:glL.M
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EXHIBIT 0-5U.S. Geologicaly Survey
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UNITED STATES DEPARTMENT OF THE INT
Page 454 and 455:
Contact between the dominantly fels
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poorly exposed plutons in the weste
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TKtminor K-feldspar, muscovite, gar
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KarKmSOUTHEASTERN TALKEETNA MOUNTAI
Page 462 and 463:
siltstone, shale, sandstone, and co
Page 464 and 465:
Plutonic and metamorphic rocksKumSE
Page 466 and 467:
These epizonal plutonic rocks, unde
Page 468 and 469:
Jamand K-feldspar. Where altered, t
Page 470 and 471:
JmbJmiThe metamorphic rocks of the
Page 472 and 473:
JpsPELITIC MICA SCHIST (Probably Lo
Page 474 and 475:
similar to their correlative map un
Page 476 and 477:
they form an interlayered heterogen
Page 478 and 479:
Jslate Paleozoic or probable late P
Page 480 and 481:
Most of the cleavage is probably ax
Page 482 and 483:
intercalated in approximately equal
Page 484 and 485:
of the enveloping rocks are of a di
Page 486 and 487:
Dsbto medium grained, locally with
Page 488 and 489:
exposed gabbro occurs in a lens abo
Page 490 and 491:
lRlbpebbles which probably were der
Page 492 and 493:
and are high in titanium (normalize
Page 494 and 495:
StructureThe rocks of the Talkeetna
Page 496 and 497:
dips steeply toward the southeast.
Page 498 and 499:
TectonicsThe Talkeetna Mountains an
Page 500 and 501:
tectonic transport. This is further
Page 502 and 503:
other middle Tertiary and younger f
Page 504 and 505:
Csejtey, 8~la, Jr., Nelson, W. H.,
Page 506 and 507:
Jones, D. L., Silberling, N. J., Cs
Page 508 and 509:
T.~I.I.--rot ••• lua-.c,oo .,
Page 510 and 511:
Table 1.··ContlnuedU'lCOI \l'lIap
Page 512 and 513:
""'I) nUlliberd1 .. 1_~L-un!!field"
Page 514 and 515:
SECTION EENVIRONMENTAL ASSESSMENT
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INTRODUCTIONIn the almost 4 years s
Page 518 and 519:
BIOLOGICAL CHARACTERISTICSMammals -
Page 520 and 521:
ENVIRONMENTAL IMPACTS OF THE DEVIL
Page 522 and 523:
1. The project ;s designed to impou
Page 524 and 525:
In addition to the lands discussed
Page 526:
SECTION FRECREATIONAL ASSESSMENTNon
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