state of knowledge of the geothermal provinces of … j... · reservoir: dalha basalts (9 - 4 my),...
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STATE OF KNOWLEDGE OF THEGEOTHERMAL PROVINCES OFREPUBLIC OF DJIBOUTI
ARGEO-C1 ConferenceAddis-Ababa, Ethiopia, 24-29 November 2006
JALLUDIN MohamedDjibouti, CERD
CERD
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FIRST PHASEPreliminary field studiesAsal rift geophysical studiesFirst geothermal drillings in Asal Rift geothermal areaNord-Goubhet geophysical studies
SECOND PHASEHanlé-Gaggadé exploration (field studies and gradient wells)Hanlé geothermal drillingsAsal rift new drillings and geophysicsScaling and corrosion study of Asal rift deep reservoir
ARGEO PROJECT PHASE
GEOTHERMAL EXPLORATIONS IN DJIBOUTI
CERD
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CERD
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GEOLOGY AND SURFACE MANIFESTATIONSCERD
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HANLE 1HANLE 2
HANLE GEOTHERMALEXPLORATION AREARepublic of Djibouti
Hanle plain
Lake Abhe
Lake Asal
CERD
Gaggade plain
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CERDHANLE-GAGGADE GEOCHEMICAL STUDIES (AQUATER-CERD 1983)
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CERDELECTRICAL SURVEY OF HANLE PLAIN (AQUATER-CERD 1983)
"
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Yoboki
Legend
Altitude of the T group (resistant)
Disconinuity
3 0 31.5 Kilometers
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CERDHANLE GRADIENT WELLS
452 m
Coarse alluvium
Fine sand
Mud and silt
Rhyolite
Basalts
TEWEO1 GARABAYIS2
Teweo11.3°/100m43.7°C
Garabayis23°/100m80.8°C
Garabayis12°/100m121.7°C
500m
130°C30°C 100°C
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Dept
h m
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Temperature °C
Dept
h m
Alluviums
Rhyolites
Trachytes
Basalts
HANLE 1 HANLE 2
CERDHANLE DRILLINGS
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Hanlé 1 (1623 m), 72 °C at 1420 m
Hanlé 2 (2038 m), 124 °C at 2020 m
PermeabilityHanlé 1: rhyolites, contact rhyolites-basalts, scoriae, dry below 800 mHanlé 2: basalts, scoriae, dry below 450 m
Bottom hole core of Hanlé 2: 18.8 My
Thick crust with 24 °C/km to 36 °C/km
HANLE EXPLORATION OUTCOMES
CERD
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Asal Geothermal areaRepublic of Djibouti
CERD
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CERDSURFACE MANIFESTATIONS ANDGRADIENT WELLS. ASAL RIFT (BRGM-CERD 1973)
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CERDGRAVIMETRIC SURVEY. BOUGUER ANOMALY (BRGM 1993)
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CERDAMT SURVEY OF THE ASAL RIFT (BRGM 1993)
Altitude -100m
Altitude -300m
Altitude -200m
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CERD
Altitude -100m
Altitude -300m
Altitude -200m
EM SURVEY OF THE ASAL RIFT (BRGM 1993; ORKUSTOFNUN 1988)
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CERD
Cl (M)
Br (mM)
1
4
3
2
1
4
8
2
Lake Asal
Sea water
Deep reservoir
Shallow reservoir
Korili spring
Other springs
Br VERSUS Cl IN ASAL RIFT ZONE
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CERD
Lake Asal
Sea water
Deep reservoir
Shallow reservoir
Korili spring
Other springs
Ca/Cl.10
Li/Cl.104
1.5
0.5
1
1.5 7.5
Na/Cl.10
Li/Cl.104
7.552.5
5
6
7
8
Mg/Cl.10
Li/Cl.104
7.552.5
0.5
1
MAJOR ELEMENTS VERSUS Li (San Juan et al. 1990)
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δD=8δ1
8 O+10
Hot springsCold springsLake Asal 1974Lake Asal 1979Sea water
Sakalol
Korili
-5
+15
-25
+4
δ18O
δD
δ18O VERSUS δD IN ASAL RIFT AREA
CERD
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0
500
1000
1500
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0 100 200 300 400Température °C
Pro
fond
eur m
ASAL3ASAL4ASAL5
Temperature profiles – Asal geothermal area
CERD
Well Depth(m)
Temp. Max (°C)
Temp. Gradient(°C/100m)
A1 1145 261 18
A2 1554 235 14.3
A3 1316 280 15.51
A4 2013 345 15.2
A5 2105 360 15.2
A6 1761 280 12.75
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1316 m
2013 m
2105 m
ASAL 5ASAL4ASAL 3
Asal series
Stratoid series
Dalha basalts
Alluviums
Clays
Hyaloclastites
Rhyolites
Basalts
Trachytes500 m
Interpretative cross section ofAsal rift Geothermal area
CERD
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11/8/87 20/9/87 30/10/87 9/12/87
Wt (
ton/
h)
Production curves of ASAL 3
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WHP (bar)
Tota
l flo
w ra
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DEC.89
MAR.90
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WHP (bar)To
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low
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Production curve of ASAL 1
CERD
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Scale deposits in 6 inches production lineAsal 1 geothermal well (BRGM-CERD 1981)
CERD – Republic of Djibouti
CERD
180 µm
Spharelite
Galena
Baryte x3000Silencerdeposits
Sulphidedeposits300 m depth
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Asal 3 well testing dataCERD
0
0.5
1
1.5
2
2.50.01 0.1 1 10 100
Time hour
Dra
wdo
wn
bar
155-225 ton/h300-357 ton/h
79-130 ton/h225-300 ton/h
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60
70
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110
120
130
3 4 5 6 7 8
1/QN ( (Qj-Q(j-1) * log (t-t(j-1) ) )
( Pi -
Pw
f ) /
QN
Drawdowns. ASAL3 Multirate drawdown. ASAL3
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1/QN ( (Qj - Q(j-1) * log (( t - t(j-1))
( Pi -
Pw
f ) /
QN
Injectivity test. ASAL4 Multirate drawdown. ASAL6
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CERDHYDRODYNAMIC PROPERTIES OF THE DEEP RESERVOIR IN ASAL RIFT ZONE
Semilog Bilog
Wtton/h
ΔQton/h
khdm
skin khdm
79 - 130 51 15.6 - 5 15.6Multiple 15.9
155 - 225 70 15.75.7
- 5- 5
166
225 - 300 75 6300 - 357 57 13.4 - 5 13.4
5.88787 - 0
7.3357357 - 0
khdm
ΔQton/h
Wtton/h
BilogSemilog
After injection
Injectivity
0.28
0.70.670
khdm
khdm
Qm3/h
BilogSemilog
3.7106.913.165.2 - 78.3
6.4Multiple
4.11Multiple
khdm
skinkhdm
ΔQton/h
Wtton/h
ASAL3 recovery tests
ASAL3 Drawdown tests ASAL4 injectivity test
ASAL6 Drawdown tests
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CERD
74
75
76
77
78
79
80
81
82
1 10 100 1000 10000 100000
Build-up décembre 1987 Build-up mars 1990
Pres
sion
à 1
100
( ta + tp ) / ta
PRESSURE BUILD-UP MEASUREMENTS. ASAL3
70
72
74
76
78
80
82
84
0 50 100 150 200 250 300
Total flow ton/h
Pre
ssur
e at
110
0 m
dep
th B
ar
Production 1rst period of 1rst phase
Production 2nd period of 1rst phase
Production 2nd phase
Before production 1rst phase
77 days after stop production phase 1
Before production phase 2
Pressure build up after stop fo phase 2 production
Estimated by build-up after phase 2
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Reservoir recognized by ASAL1, ASAL3 and ASAL 6 in the same areaTemperature 260 °C to 280 °CReservoir: Dalha basalts (9 - 4 My), 1050 m to 1300 mASAL 3 production:
Initial characteristics: total mass flow 360 t/h for 12.5 WHPKh: 6.3 dmTDS in the reservoir: 116 000 ppmScaling in the well (6 to 10 mm): sulphides (PbS, ZnS)Scaling in surface equipment: amorphous Si with Fe and MnSevere decrease of the production rateDecrease of the bottom hole pressure: 3.5 bars
DEEP RESERVOIR RESULTS IN ASAL
CERD
Recognized on all Asal geothermal wells but not yet studiedReservoir: Top of Stratoid series and the bottom of Asal seriesLocated between 300 m and 600 mTemperature 130 °C to 190 °CTDS : 50 g/l
ASAL INTERMEDIATE RESERVOIR
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NORD-GOUBHET AND ARTAGEOPHYSICAL SURVEYS (BRGM 1983; GEOTHERMICA 1982)
CERD
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CERD
LAKE ABHE AND OBOCK GEOTHERMAL PROSPECTS
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CERDGROUNDWATER THERMAL ANOMALIESDJIBOUTI AQUIFER
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CERD
HANLE-GAGGADE BASINS ZONEDrilling results not conclusive in Hanle basinExploration by drilling not completedNeed for new geophysical surveys as EM, AMTReevaluate possibility of new drillings
ASAL RIFT ZONEDeep reservoir of high enthalpy demonstrated in ASAL1 areaLateral extension of deep reservoir not yet evidentPermeability and circulations controled by fracturesMajor problem of scaling still to resolveGeophysical surveys describe complex structures of reservoirs Fairly good understanding of fluids origins based on geochemistry and isotopes
Shallow reservoir medium enthalpy preliminary significant resultsShallow reservoir likely to have good extension
CONCLUSIONS
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ASAL RIFT ZONEComplete exploration for the deep reservoir extensionSolutions for the scaling problem of the deep reservoirComplete EM survey of Asal rift zoneStudy faisability of the mineral extraction from the deep reservoir high TDS fluidRealize exploration with drillings in the shallow reservoirDevelop both reservoirs for electricity production
OBOCK ZONERealize geophysical surveys with EM and AMT methodsRealize geochemical and isotopic studies on the hydrothermal manifestationsExploration drillingsFaisability study
LAKE ABHE AND GAGGADE ZONESRealize geophysical surveys with EM and AMT methodsRealize geochemical and isotopic studies on the hydrothermal manifestationsExploration drillingsFaisability study
PERSPECTIVES FOR GEOTHERMAL DEVELOPMENT
CERD
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CERD
Thank you