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IOSR Journal of Engineering (IOSRJEN) www.iosrjen.org
ISSN (e): 2250-3021, ISSN (p): 2278-8719
Vol. 05, Issue 09 (September. 2015), ||V1|| PP 07-12
International organization of Scientific Research 7 | P a g e
The research of oil-water distribution in the eastern block of Chao202-2 area
Liu Jiyu, Chen Haitao, Jin Xin,Sheng Caiwen
1(College of earth science of Northeast Petroleum University, Daqing, Hei Longjiang,China)
2 (Second oil factory of Daqing oil field, Daqing, Hei Longjiang,China)
3 (Well logging technology service company, Daqing, Hei Longjiang,China)
Abstract: - The eastern block of Chao202-2 area belongs to the channel sand body deposition,where the faults
are well developed and complex combination. The oil, water and gas distribution is relatively complex and
influences the injecting-producing relation, so the study of control factors is needed. According to the
geological characteristics of the eastern block of Chao202-2 area, clear regional geological characteristics,
logging identification technology as the core technology and logging identification technique for identifying oil
and water layer, oil-water layer logging interpretation chart was established. With a combination of the
oil-water layer interpretation results, the test resultsand the existing research results of regional geological
features, the characteristics of the oil and water distribution in the block were induced and analyzed. In the
study area, structural reservoir is the main reservoir type. Oil-water distribution is controlled by structural
factors and space configuration of fault and sand body control the oil-water distribution border. From the fault
analysis of the plane, oil-water distribution was determined.
Keywords:oil-water distribution,fault,structure,channel sand body,logging interpretation
I. REGIONAL GEOLOGICAL BACKGROUND
The eastern block of Chao202-2 Area is located in the territory of Zhaozhou County, Daqing City,
Heilongjiang Province, the alar part of Chaoyanggou oil field. The air permeability of the block is 5.2×10-3
μm2
,
the formation oil viscosity is 14.1mPa·s and the ground crude oil viscosity is bigger, which achieves
42.48mPa·s. The study area belongs to river-lake deposits, where the faults are well developed and complex
combination. The results of structural history research show that the tectonic development of the inner block has
the close relation with the structure of the songliao basin development and the formation of the depression.
Roughly experience four stages: fault-depression stage (The Jurassic sedimentary period), rift-depression stage
(Denglouku formation sedimentary period), downwarp stage( the depositional period of Quantou group and
Nenjiang group) and rising stage (After the deposition of the nenjiang formation). The Major reservoir is
located in Fuyu oil layer which belongs to microfacies of the delta front. The main sand body type
is subaqueous distributary channel, whose distribution is mainly controlled by the southwest direction
sedimentary systems distributed from southwest to northeast direction. There is no obvious characteristics on oil
and gas distribution in the study area. The average production of single oil well has decreased year by year and
the average injection water of single water well has decreased after the production. The
production declines fast and the development effect is poor. Therefore, to improve the development effect
and guide the core area evaluation of the similar blocks, we conduct a related study on the oil and water
distribution characteristics in the block.
II. THE RESEARCH ON OIL AND WATER LAYER IDENTIFICATION
Oil and water layer identification is a key link in the process of reservoir development. Either oil layer
mistaken for water layer or water layer mistaken for oil layer will have adverse effect on calculation of reserves
and oil field development produce. Different regions and horizons have different selected evaluation standards.
The oil and water distribution in the study area is relatively complicated, so accurately determining oil and water
layer identification and classification standard is of great significance[1]
. Based on the characteristics of the oil
reservoir in this area, the study of the "four sex of characters", and the logging theory, optimize deep lateral
The research of oil-water distribution in the eastern block of Chao202-2 area
International organization of Scientific Research 8 | P a g e
resistivity curves which can obviously reflect the liquid property, and sonic time difference curves which can
obviously reflect reservoir permeability as the standard for establishing logging parameters in the study area[2]
.
Combined with core and testing materials, apply the data of 52 layers from 8 coring wells including 10 oil layers
, 21 poor oil layers, 16 dry layers and 5 water layer layers. Then, eliminate abnormal point. Finally, get oil and
water layer interpretation and evaluation chart in the study area chart (figure 2.1).Chart accuracy can reach
87.5%, which meets the requirement of oil-water layers interpretation and evaluation in the study area. At the
same time, the oil-water standards are determined as follows:
Oil layer:
216.37AC0543.0R LLD

,of which
m/s220AC 
;
Poor oil layer :
329.28AC0438.0R216.37AC0543.0 LLD

, of which
m/s220AC 
;
Dry layer
17AC023.0R329.28AC0438.0 LLD

,eliminate abnormal points;
Water layer:
17AC023.0R LLD

;
in the formula: RLLD—deep lateral resistivity, Ω·m.
AC—interval transit time,μs/m.
Figure2.1 Oil-water interpretation and evaluation chart in the eastern block of Chao202-2 area
Applying oil-water interpretation and evaluation chart has explained 120 wells in the study area, which were
divided into 152 oil layers, 289 poor oil layers, 220 dry layers, 78 water layers.
III. OIL AND WATER DISTRIBUTION CHARACTERISTICS
3.1 The whole region of oil and water distribution
The interpretation results projected to the scattered point, it can be seen that the whole region has no uniform
oil-water interface (Figure 3.1).
The research of oil-water distribution in the eastern block of Chao202-2 area
International organization of Scientific Research 9 | P a g e
Figure 3.1 oil-water distribution map of the whole region
Seen from the reservoir section of it, structure becomes low and sand body development gradually
becomes poor from west to east (figure 3.2). Different fault blocks have different oil-water distribution
characteristics, roughly divided into “up oil, bottom water”, “up water, bottom oil” and “water in oil”. Seen
from the Figure 3.3, structure becomes low from north to south and the oil-water distribution characteristics of
different fault blocks are very complex [3-4]
, which is the same as east-west profile.
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
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F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
RL3S
RL3D
10C90-80
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-82 GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-84
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-86
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
LLS
LLD
10C97-91
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F352
F353
F354
F355
RL3S
RL3D
10C98-92
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
RL3S
RL3D
10C100-94
横向比例尺0 50 100 150米
Water layer Dry layerOil layer
west
east
M
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
RL3S
RL3D
10C90-80
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-82 GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-84
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-86
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
LLS
LLD
10C97-91
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F352
F353
F354
F355
RL3S
RL3D
10C98-92
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
RL3S
RL3D
10C100-94
横向比例尺0 50 100 150米
Water layer Dry layerOil layer Water layer Dry layerOil layer
west
east
M
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
RL3S
RL3D
10C90-80
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-82 GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-84
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-86
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
LLS
LLD
10C97-91
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F352
F353
F354
F355
RL3S
RL3D
10C98-92
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
RL3S
RL3D
10C100-94
横向比例尺0 50 100 150米
Water layer Dry layerOil layer
west
east
M
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
RL3S
RL3D
10C90-80
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-82 GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-84
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C90-86
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
LLS
LLD
10C97-91
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F352
F353
F354
F355
RL3S
RL3D
10C98-92
GR
SP
深度 地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
RL3S
RL3D
10C100-94
横向比例尺0 50 100 150米
Water layer Dry layerOil layer Water layer Dry layerOil layer
west
east
M
Figure 3.2 East-west reservoir profile map in the eastern block of Chao202-2 area
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
GR
SP
深
度
86587087588088589089590090591091592092593093594094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C94-84
GR
SP
深
度
89590090591091592092593093594094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
RL3S
RL3D
10C98-82
GR
SP
深
度
94094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110111511201125113011351140114511501155116011651170117511801185
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F352
LLS
LLD
10C103-81
GR
SP
深
度
945950955960965970975980985990995100010051010101510201025103010351040104510501055106010651070107510801085109010951100110511101115112011251130113511401145115011551160116511701175
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
LLS
LLD
10C111-80
GR
SP
深
度
98098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110111511201125113011351140114511501155116011651170117511801185
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
RL3S
RL3D
10C114-76
GR
SP
深
度
980985990995100010051010101510201025103010351040104510501055106010651070107510801085109010951100110511101115112011251130113511401145115011551160116511701175118011851190119512001205
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
RL3S
RL3D
10C120-76
north
south
Water layer Dry layerOil layer
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
GR
SP
深
度
86587087588088589089590090591091592092593093594094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
RL3S
RL3D
10C94-84
GR
SP
深
度
89590090591091592092593093594094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
RL3S
RL3D
10C98-82
GR
SP
深
度
94094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110111511201125113011351140114511501155116011651170117511801185
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
F342
F343
F351
F352
LLS
LLD
10C103-81
GR
SP
深
度
945950955960965970975980985990995100010051010101510201025103010351040104510501055106010651070107510801085109010951100110511101115112011251130113511401145115011551160116511701175
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
F341
LLS
LLD
10C111-80
GR
SP
深
度
98098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110111511201125113011351140114511501155116011651170117511801185
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
RL3S
RL3D
10C114-76
GR
SP
深
度
980985990995100010051010101510201025103010351040104510501055106010651070107510801085109010951100110511101115112011251130113511401145115011551160116511701175118011851190119512001205
地层
F111
F112
F113
F114
F115
F121
F122
F123
F131
F132
F133
F14
F151
F152
F153
F161
F162
F163
F171
F172
F173
F211
F212
F221
F222
F23
F241
F242
F251
F252
F253
F311
F312
F321
F322
F331
F332
F333
RL3S
RL3D
10C120-76
north
south
Water layer Dry layerOil layer Water layer Dry layerOil layer
Figure 3.3 South-north reservoir profile map in the eastern block of Chao202-2 area
The research of oil-water distribution in the eastern block of Chao202-2 area
International organization of Scientific Research 10 | P a g e
3.2The controlling factors of oil-water distribution
According to above analysis, the oil-water distribution is mainly controlled by two factors in the research
blocks.
1. The fault structure has some influence on oil-water distribution. The faults are developed well in the
study area. By the study of chemical and physical properties of oil, gas and water in the reservoir near both sides
of faults, it shows that the oil, water and gas property has many differences near both sides of faults, which
indicates that the fault in the study area has a certain sealing ability and can form a mutual non-nterference
reservoir. Therefore, the fault block may have a complex oil-water distribution from vertical (horizontal)
direction in both side of the fault [5-6]
.
2. The sedimentary lithology has some influence on oil-water distribution. The sand body in the reservoir
of the study area is preexisting sand body relative to the structure while the structure of the sand body is late
structure relative to the sand body. The research area mainly develops channel sand body and point bar sand
body. The river channel sand body is in dendritic distribution. The air permeability of the main channel is
6.1×10-3
μm2
, the air permeability of the non main channel is 4.8×10-3
μm2
, and the reservoir permeability is
lower. There is a large amount of argillaceous filling between river and river and the connectivity between sand
body is poor, which ensures the independence of sand body between oil and water distribution characteristics
[7-8]
.
3.3 The characteristics of the oil-water distribution controlled by different blocks
Based on the analysis of the above, the spatial configuration of fault and sand body controls the boundary
of oil-water distribution. On the basis of controlling factors, the district can be divided into 10 blocks (figure
3.4). According to the characteristics of oil and water distribution, it is divided into three types.
Figure 3.4 oil-water distribution map of the whole region of blocks
1、The oil layer and water layer are developed at the same time within the same fault block. The characteristics
of the oil-water distribution is “up oil, bottom water”. In fault block 4, for example, the structure of the fault
block becomes low from north to south. Although the water well 135-46 is in the higher position than the oil
wells in the south, due to the combination of fault and structure, the water well 135-46 located In different
blocks compares with the well in the south. The characteristics of the oil-water distribution in the block is that
the oil reservoir is in the north and the water reservoir is in the south. The regularities of distribution accord with
oil-water distribution characteristics of structural reservoir (figure 3.5).
The research of oil-water distribution in the eastern block of Chao202-2 area
International organization of Scientific Research 11 | P a g e
Figure 3.5 oil-water distribution map of the F131
2、The oil layer and water layer are developed at the same time within the same fault block. The characteristics
of the oil-water distribution is “up water, bottom oil”. In block 10, for example, with relatively higher position,
the well 131-24 inside the fault belongs to the water layer, while other wells with relatively lower position
belongs to oil layer. The main reason for forming this type is that sedimentary facies belts of the well 131-24 are
different from the other three wells. Mudstone segment in the middle causes the different distribution of oil and
water (figure 3.6).
Figure 3.6 oil-water distribution map of the F171
3. Within the same fault block, just the oil layer or water layer is developed. In block 8, for example, the well
133-65 inside the block belongs to the water layer and the same layer in adjacent block is oil layer. Although the
characteristic of “ high water, low oil” can be seen in the oil and water distribution scatter plot, the water well
and the oil well are divided by the fault which has a certain closed feature to make them form independent fault
blocks. In the same oil layer, the wells of different fault blocks don’t disturb each other (figure 3.7).
The research of oil-water distribution in the eastern block of Chao202-2 area
International organization of Scientific Research 12 | P a g e
Figure 3.7 oil-water distribution map of the F171
IV. CONCLUSION
1. In the study area, the main reservoir type is structural reservoir. Oil-water distribution is controlled by
structural factors and the space configuration of fault and sand body controlled oil-water distribution border.
2. From the analysis of the plane, the oil-water distribution can be divided into three types:
(1) Within the same block, oil and water layer are developed at the same time. Oil-water distribution is “up oil,
bottom water”.
(2) Within the same block, oil and water layer are developed at the same time. Oil-water distribution is “up
water, bottom oil”.
(3) Within the same fault block, the oil or water layer is only developed one.
REFERENCES
[1] Shi Shangming,Guan Shuai,Han Jianbin ect. The research of oil-water layer identification and evaluation
of fuyang formation in gaotaizi oilfield [J]. Science Technology and Engineering, 2011,13:2897-2901.
[2] Liu Weilin,Liu Jiang,Zhang Junlong ect. The study on the interpretation chart for oil and water zone
classification in Puxi area[J]. Petroleum geology & oilfield development in Daqing, 2003,01:57-59.
[3] LV Guiyou.Research on high-resolution sequence stratigraphy and oil & water distribution rules of
Heidimiao layer in Yingtai area[D].Northeast Petroleum University,2013.
[4] QIU Cuiying. Oil water distribution and control factor of Taibei development zone of daqing
oilfield[D].Northeast Petroleum University,2013.
[5] WANG Kui,YANG Jing,HOU Guangzong ect. Present status and development tendency of research on
fault closure property[J].Fault-block oil & gas field,2008,03:43-45.
[6] FU Xiaofei,LI Wenlong,LV Yanfang ect. Quantitative estimation of lateral fault seal and application in
hydrocarbon exploration[J]. Geological review, 2011,03:387-397.
[7] GUAN Yu. Research of water and oil distribution of the complex structure lithology reservoir in Gao20
oil area[D].Jilin University,2012.
[8] XU Guangbo. Oil-water distribution and the main controlling factors on fuyu oil layer in Toutai oilfield
[D].Northeast Petroleum University,2013.

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B05910712

  • 1. IOSR Journal of Engineering (IOSRJEN) www.iosrjen.org ISSN (e): 2250-3021, ISSN (p): 2278-8719 Vol. 05, Issue 09 (September. 2015), ||V1|| PP 07-12 International organization of Scientific Research 7 | P a g e The research of oil-water distribution in the eastern block of Chao202-2 area Liu Jiyu, Chen Haitao, Jin Xin,Sheng Caiwen 1(College of earth science of Northeast Petroleum University, Daqing, Hei Longjiang,China) 2 (Second oil factory of Daqing oil field, Daqing, Hei Longjiang,China) 3 (Well logging technology service company, Daqing, Hei Longjiang,China) Abstract: - The eastern block of Chao202-2 area belongs to the channel sand body deposition,where the faults are well developed and complex combination. The oil, water and gas distribution is relatively complex and influences the injecting-producing relation, so the study of control factors is needed. According to the geological characteristics of the eastern block of Chao202-2 area, clear regional geological characteristics, logging identification technology as the core technology and logging identification technique for identifying oil and water layer, oil-water layer logging interpretation chart was established. With a combination of the oil-water layer interpretation results, the test resultsand the existing research results of regional geological features, the characteristics of the oil and water distribution in the block were induced and analyzed. In the study area, structural reservoir is the main reservoir type. Oil-water distribution is controlled by structural factors and space configuration of fault and sand body control the oil-water distribution border. From the fault analysis of the plane, oil-water distribution was determined. Keywords:oil-water distribution,fault,structure,channel sand body,logging interpretation I. REGIONAL GEOLOGICAL BACKGROUND The eastern block of Chao202-2 Area is located in the territory of Zhaozhou County, Daqing City, Heilongjiang Province, the alar part of Chaoyanggou oil field. The air permeability of the block is 5.2×10-3 μm2 , the formation oil viscosity is 14.1mPa·s and the ground crude oil viscosity is bigger, which achieves 42.48mPa·s. The study area belongs to river-lake deposits, where the faults are well developed and complex combination. The results of structural history research show that the tectonic development of the inner block has the close relation with the structure of the songliao basin development and the formation of the depression. Roughly experience four stages: fault-depression stage (The Jurassic sedimentary period), rift-depression stage (Denglouku formation sedimentary period), downwarp stage( the depositional period of Quantou group and Nenjiang group) and rising stage (After the deposition of the nenjiang formation). The Major reservoir is located in Fuyu oil layer which belongs to microfacies of the delta front. The main sand body type is subaqueous distributary channel, whose distribution is mainly controlled by the southwest direction sedimentary systems distributed from southwest to northeast direction. There is no obvious characteristics on oil and gas distribution in the study area. The average production of single oil well has decreased year by year and the average injection water of single water well has decreased after the production. The production declines fast and the development effect is poor. Therefore, to improve the development effect and guide the core area evaluation of the similar blocks, we conduct a related study on the oil and water distribution characteristics in the block. II. THE RESEARCH ON OIL AND WATER LAYER IDENTIFICATION Oil and water layer identification is a key link in the process of reservoir development. Either oil layer mistaken for water layer or water layer mistaken for oil layer will have adverse effect on calculation of reserves and oil field development produce. Different regions and horizons have different selected evaluation standards. The oil and water distribution in the study area is relatively complicated, so accurately determining oil and water layer identification and classification standard is of great significance[1] . Based on the characteristics of the oil reservoir in this area, the study of the "four sex of characters", and the logging theory, optimize deep lateral
  • 2. The research of oil-water distribution in the eastern block of Chao202-2 area International organization of Scientific Research 8 | P a g e resistivity curves which can obviously reflect the liquid property, and sonic time difference curves which can obviously reflect reservoir permeability as the standard for establishing logging parameters in the study area[2] . Combined with core and testing materials, apply the data of 52 layers from 8 coring wells including 10 oil layers , 21 poor oil layers, 16 dry layers and 5 water layer layers. Then, eliminate abnormal point. Finally, get oil and water layer interpretation and evaluation chart in the study area chart (figure 2.1).Chart accuracy can reach 87.5%, which meets the requirement of oil-water layers interpretation and evaluation in the study area. At the same time, the oil-water standards are determined as follows: Oil layer: 216.37AC0543.0R LLD  ,of which m/s220AC  ; Poor oil layer : 329.28AC0438.0R216.37AC0543.0 LLD  , of which m/s220AC  ; Dry layer 17AC023.0R329.28AC0438.0 LLD  ,eliminate abnormal points; Water layer: 17AC023.0R LLD  ; in the formula: RLLD—deep lateral resistivity, Ω·m. AC—interval transit time,μs/m. Figure2.1 Oil-water interpretation and evaluation chart in the eastern block of Chao202-2 area Applying oil-water interpretation and evaluation chart has explained 120 wells in the study area, which were divided into 152 oil layers, 289 poor oil layers, 220 dry layers, 78 water layers. III. OIL AND WATER DISTRIBUTION CHARACTERISTICS 3.1 The whole region of oil and water distribution The interpretation results projected to the scattered point, it can be seen that the whole region has no uniform oil-water interface (Figure 3.1).
  • 3. The research of oil-water distribution in the eastern block of Chao202-2 area International organization of Scientific Research 9 | P a g e Figure 3.1 oil-water distribution map of the whole region Seen from the reservoir section of it, structure becomes low and sand body development gradually becomes poor from west to east (figure 3.2). Different fault blocks have different oil-water distribution characteristics, roughly divided into “up oil, bottom water”, “up water, bottom oil” and “water in oil”. Seen from the Figure 3.3, structure becomes low from north to south and the oil-water distribution characteristics of different fault blocks are very complex [3-4] , which is the same as east-west profile. F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 RL3S RL3D 10C90-80 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-82 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-84 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-86 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 LLS LLD 10C97-91 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F352 F353 F354 F355 RL3S RL3D 10C98-92 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 RL3S RL3D 10C100-94 横向比例尺0 50 100 150米 Water layer Dry layerOil layer west east M F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 RL3S RL3D 10C90-80 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-82 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-84 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-86 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 LLS LLD 10C97-91 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F352 F353 F354 F355 RL3S RL3D 10C98-92 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 RL3S RL3D 10C100-94 横向比例尺0 50 100 150米 Water layer Dry layerOil layer Water layer Dry layerOil layer west east M F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 RL3S RL3D 10C90-80 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-82 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-84 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-86 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 LLS LLD 10C97-91 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F352 F353 F354 F355 RL3S RL3D 10C98-92 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 RL3S RL3D 10C100-94 横向比例尺0 50 100 150米 Water layer Dry layerOil layer west east M F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 RL3S RL3D 10C90-80 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-82 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-84 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C90-86 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 LLS LLD 10C97-91 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F352 F353 F354 F355 RL3S RL3D 10C98-92 GR SP 深度 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 RL3S RL3D 10C100-94 横向比例尺0 50 100 150米 Water layer Dry layerOil layer Water layer Dry layerOil layer west east M Figure 3.2 East-west reservoir profile map in the eastern block of Chao202-2 area F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 GR SP 深 度 86587087588088589089590090591091592092593093594094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C94-84 GR SP 深 度 89590090591091592092593093594094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 RL3S RL3D 10C98-82 GR SP 深 度 94094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110111511201125113011351140114511501155116011651170117511801185 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F352 LLS LLD 10C103-81 GR SP 深 度 945950955960965970975980985990995100010051010101510201025103010351040104510501055106010651070107510801085109010951100110511101115112011251130113511401145115011551160116511701175 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 LLS LLD 10C111-80 GR SP 深 度 98098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110111511201125113011351140114511501155116011651170117511801185 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 RL3S RL3D 10C114-76 GR SP 深 度 980985990995100010051010101510201025103010351040104510501055106010651070107510801085109010951100110511101115112011251130113511401145115011551160116511701175118011851190119512001205 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 RL3S RL3D 10C120-76 north south Water layer Dry layerOil layer F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 GR SP 深 度 86587087588088589089590090591091592092593093594094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 RL3S RL3D 10C94-84 GR SP 深 度 89590090591091592092593093594094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 RL3S RL3D 10C98-82 GR SP 深 度 94094595095596096597097598098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110111511201125113011351140114511501155116011651170117511801185 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 F342 F343 F351 F352 LLS LLD 10C103-81 GR SP 深 度 945950955960965970975980985990995100010051010101510201025103010351040104510501055106010651070107510801085109010951100110511101115112011251130113511401145115011551160116511701175 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 F341 LLS LLD 10C111-80 GR SP 深 度 98098599099510001005101010151020102510301035104010451050105510601065107010751080108510901095110011051110111511201125113011351140114511501155116011651170117511801185 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 RL3S RL3D 10C114-76 GR SP 深 度 980985990995100010051010101510201025103010351040104510501055106010651070107510801085109010951100110511101115112011251130113511401145115011551160116511701175118011851190119512001205 地层 F111 F112 F113 F114 F115 F121 F122 F123 F131 F132 F133 F14 F151 F152 F153 F161 F162 F163 F171 F172 F173 F211 F212 F221 F222 F23 F241 F242 F251 F252 F253 F311 F312 F321 F322 F331 F332 F333 RL3S RL3D 10C120-76 north south Water layer Dry layerOil layer Water layer Dry layerOil layer Figure 3.3 South-north reservoir profile map in the eastern block of Chao202-2 area
  • 4. The research of oil-water distribution in the eastern block of Chao202-2 area International organization of Scientific Research 10 | P a g e 3.2The controlling factors of oil-water distribution According to above analysis, the oil-water distribution is mainly controlled by two factors in the research blocks. 1. The fault structure has some influence on oil-water distribution. The faults are developed well in the study area. By the study of chemical and physical properties of oil, gas and water in the reservoir near both sides of faults, it shows that the oil, water and gas property has many differences near both sides of faults, which indicates that the fault in the study area has a certain sealing ability and can form a mutual non-nterference reservoir. Therefore, the fault block may have a complex oil-water distribution from vertical (horizontal) direction in both side of the fault [5-6] . 2. The sedimentary lithology has some influence on oil-water distribution. The sand body in the reservoir of the study area is preexisting sand body relative to the structure while the structure of the sand body is late structure relative to the sand body. The research area mainly develops channel sand body and point bar sand body. The river channel sand body is in dendritic distribution. The air permeability of the main channel is 6.1×10-3 μm2 , the air permeability of the non main channel is 4.8×10-3 μm2 , and the reservoir permeability is lower. There is a large amount of argillaceous filling between river and river and the connectivity between sand body is poor, which ensures the independence of sand body between oil and water distribution characteristics [7-8] . 3.3 The characteristics of the oil-water distribution controlled by different blocks Based on the analysis of the above, the spatial configuration of fault and sand body controls the boundary of oil-water distribution. On the basis of controlling factors, the district can be divided into 10 blocks (figure 3.4). According to the characteristics of oil and water distribution, it is divided into three types. Figure 3.4 oil-water distribution map of the whole region of blocks 1、The oil layer and water layer are developed at the same time within the same fault block. The characteristics of the oil-water distribution is “up oil, bottom water”. In fault block 4, for example, the structure of the fault block becomes low from north to south. Although the water well 135-46 is in the higher position than the oil wells in the south, due to the combination of fault and structure, the water well 135-46 located In different blocks compares with the well in the south. The characteristics of the oil-water distribution in the block is that the oil reservoir is in the north and the water reservoir is in the south. The regularities of distribution accord with oil-water distribution characteristics of structural reservoir (figure 3.5).
  • 5. The research of oil-water distribution in the eastern block of Chao202-2 area International organization of Scientific Research 11 | P a g e Figure 3.5 oil-water distribution map of the F131 2、The oil layer and water layer are developed at the same time within the same fault block. The characteristics of the oil-water distribution is “up water, bottom oil”. In block 10, for example, with relatively higher position, the well 131-24 inside the fault belongs to the water layer, while other wells with relatively lower position belongs to oil layer. The main reason for forming this type is that sedimentary facies belts of the well 131-24 are different from the other three wells. Mudstone segment in the middle causes the different distribution of oil and water (figure 3.6). Figure 3.6 oil-water distribution map of the F171 3. Within the same fault block, just the oil layer or water layer is developed. In block 8, for example, the well 133-65 inside the block belongs to the water layer and the same layer in adjacent block is oil layer. Although the characteristic of “ high water, low oil” can be seen in the oil and water distribution scatter plot, the water well and the oil well are divided by the fault which has a certain closed feature to make them form independent fault blocks. In the same oil layer, the wells of different fault blocks don’t disturb each other (figure 3.7).
  • 6. The research of oil-water distribution in the eastern block of Chao202-2 area International organization of Scientific Research 12 | P a g e Figure 3.7 oil-water distribution map of the F171 IV. CONCLUSION 1. In the study area, the main reservoir type is structural reservoir. Oil-water distribution is controlled by structural factors and the space configuration of fault and sand body controlled oil-water distribution border. 2. From the analysis of the plane, the oil-water distribution can be divided into three types: (1) Within the same block, oil and water layer are developed at the same time. Oil-water distribution is “up oil, bottom water”. (2) Within the same block, oil and water layer are developed at the same time. Oil-water distribution is “up water, bottom oil”. (3) Within the same fault block, the oil or water layer is only developed one. REFERENCES [1] Shi Shangming,Guan Shuai,Han Jianbin ect. The research of oil-water layer identification and evaluation of fuyang formation in gaotaizi oilfield [J]. Science Technology and Engineering, 2011,13:2897-2901. [2] Liu Weilin,Liu Jiang,Zhang Junlong ect. The study on the interpretation chart for oil and water zone classification in Puxi area[J]. Petroleum geology & oilfield development in Daqing, 2003,01:57-59. [3] LV Guiyou.Research on high-resolution sequence stratigraphy and oil & water distribution rules of Heidimiao layer in Yingtai area[D].Northeast Petroleum University,2013. [4] QIU Cuiying. Oil water distribution and control factor of Taibei development zone of daqing oilfield[D].Northeast Petroleum University,2013. [5] WANG Kui,YANG Jing,HOU Guangzong ect. Present status and development tendency of research on fault closure property[J].Fault-block oil & gas field,2008,03:43-45. [6] FU Xiaofei,LI Wenlong,LV Yanfang ect. Quantitative estimation of lateral fault seal and application in hydrocarbon exploration[J]. Geological review, 2011,03:387-397. [7] GUAN Yu. Research of water and oil distribution of the complex structure lithology reservoir in Gao20 oil area[D].Jilin University,2012. [8] XU Guangbo. Oil-water distribution and the main controlling factors on fuyu oil layer in Toutai oilfield [D].Northeast Petroleum University,2013.