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HUANG Si jing, HOU Zhong jian. Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors[J]. Acta Sedimentologica Sinica, 2001, 19(2): 224-231.
Citation: HUANG Si jing, HOU Zhong jian. Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors[J]. Acta Sedimentologica Sinica, 2001, 19(2): 224-231.

Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors

  • Received Date: 2000-06-09
  • Rev Recd Date: 2000-11-23
  • Spatio-temporal variation of subsurface porosity and permeability is controlled by various factors during sedimentation and diagcncsis.The dcpositional environments and the types of sediment basin control the original composition before hurial, texture and porosity of sediments.The sedimentary factors to control the porosity and permeability are mainly sedimentary facics, stratigraphy sequences and so on.The process of sedimentation was much shorter than the diagcncsis, and relatively easy to study.Recently, some traditional mechanism of secondary porosity formation for subsurface sediment is challenged by new theories.The formation of secondary porosity from the aluminium-silicate solution by organic acid is the most important mechanism.However it will result in the increase of pH value precipitation of carbonate and kaolinitc.The dissolulion by carbonic water to form the secondary porosity in subsurface is also limited.Ncw mechanism such as dissolution of sediment by the meteoric water by the deep cooling formation water proves effective and hydrolysis of the silicates is also accepted universally.In addition, the precipitation and material sources of some diagcnctic authigcnic minerals related to the secondary porosity also have new mode.These are several essentials to understand the formation of secondary porosity and estimate the porosity and the permeability of the reservoir. For the carbonate rocks the oil/gas reservoir related to the palco-carst nearby the unconformitv have got more attention. During the deep burial diagenesis, the temperature and prcssure control the difference of the habit of dissolution and precipitation for different carbonate minerals leading to the differcncc of porosity and permeability distribution in subsurface carbonate rocks, which is very important for prediction of carhonate reservoir.
  • [1] 1 Bioch S P. Helmoid K. Approaches to predicting reservoir guallty in sandstones[J]. AAPG Bulietin,1995,79:97 ~ 115

    2 Bethke C M. Inverse hydroiogic anaiysis of the distribution and origin of guifcoast-type geopressured zones[J]. Journai of Geophysicai Research,B,1986,91:6 535 ~ 6 545

    3 Bethke C M,Reed J D,Oitz D F. Long-range petroieum migration in the Iiiinois Basin[J]. AAPG Buiietin,1991,75:925 ~ 945

    4 Bjoriykke K. Fiuid fiow in sedimentary basins[J]. Sedimentary Geoiogy,1993,86:137 ~ 158

    5 Wiison M D. Assessing the reiative importance of diagenetic processes and controis [A]. In:Wiison M D,ed. Reservoir guaiity assessment and prediction in ciastics rocks [C]. SEPM short Course,1994,30:259 ~ 275

    6 Beard D C,Weyi P K. Infiuence of texture on porosity and permeabiiity ofunconsoiidated sand[J]. American Association of Petroieum Geoiogists,Tuisa,OK,United States,1973,57:349 ~ 369

    7 Bioch S. Secondary porosity in sandstones:Significance,origin,reiationship to subaeriai unconformities,and effect on predriii reservoir guaiity prediction[A]. In:Wiison M D,ed. Reservoir guaiity assessment and prediction in ciastics rocks [C]. SEPM short Course No.30,1994.136 ~ 159

    8 Stanton P T,Wiison M D. Measurement of independent variabies-composition[A]. In:Wiison M D,ed. Reservoir guaiity assessment and prediction in ciastics rocks [C]. SEPM short Course,1994,30:277 ~ 290

    9 Byrnes A P,Wiison M D. Measurement of independent variabies-Pressure,time,temperature,time-temperature[A]. In:Wiison M D,ed. Reservoir guaiity assessment and prediction in ciastics rocks [C]. SEPM short Course ,1994,30:293 ~ 309

    10 Stanton P T,Byrnes A P. Measurement of independent variabies-open-ciosedsystem variabies[A]. In:Wiison M D,ed. Reservoir guaiity assessment and prediction in ciastics rocks [C]. SEPM short Course ,1994,30:311 ~319

    11 Wiison M D. Measurement of independent variabies-hydrocarbon empiacement,ciay content,texturai measurements[A]. In:Wiison M D,ed.Reservoir guaiity assessment and prediction in ciastics rocks[C]. SEPMshort Course ,1994,30:321 ~ 327

    12 Nedkvitne T,Bj!riykke K. Secondary porosity in the Brent Group(Middie Jurassic),Huidra Fieid,North Sea;impiication for predicting iaterai continuityof sandstones [J]. Journai of Sedimentary Petroiogy,1992,62:23 ~ 34

    13 Gaiioway W E. Hydrogeoiogic regimes of sandstone diagenesis[C]. AAPG Memoir,1984,37:3 ~ 13

    14 Bethke C M,Marshak S. Brine migrations across North America;the piatetectonics of groundwater[J]. Annuai Review of Earth and Pianetary Sciences,1990,18:287 ~ 315

    15 Deming D,Sass J H,Lachenbruch A H,De-Rito R F. Heat fiow and subsurface temperature as evidence for basin-scaie ground-water fiow,North Siope of Aiaska[J]. Geoiogicai Society of America Buiietin. 1992,104:528 ~ 542

    16 Giies M R. Mass transfer and probiems of secondary porosity creation in deepiy buried hydrocarbon reservoirs[J]. Marine and Petroieum Geoiogy,1987,4:188 ~ 204

    17 Hayes M J,Boies J R. Voiumetric reiations between dissoived piagiociase and kaoiinite in sandstones;impiications for aiuminum mass transfer in theSan Joaguin Basin,Caiifornia[J]. Speciai Pubiication-Society of Economic Paieontoiogists and Mineraiogists.1992,47:111 ~ 123

    18 Piummer L N. Defining reactions and mass transfer in part of the Fioridan Aguife[r J]. Water Resources Research,1977,13:801 ~ 812

    19 Edmunds W M,Bath A H,Miies D L. Hydrochemicai evoiution of the East Midiands Triassic sandstone aguifer,Engiand[J]. Geochimica et Cosmochimica Acta,1982,46:2 069 ~ 2 082

    20 Passaretti M L,Esiinger V E. Dissoiution and reiic textures in framework grains of Hoiocene sediments from the Brazos River and Guif Coast of Texas [J]. Journai of Sedimentary Petroiogy,1987,57:94 ~ 97

    21 Bioch S,Franks S G. Preservation of shaiiow piagiociase dissoiution porosity during buriai;impiications for porosity prediction and aiuminum mass baiance[J]. AAPG Buiietin. 1993,77:1 488 ~ 1 501

    22 Keiier W D. Kaoiinization of feidspar as dispiayed in scanning eiectron micrographs[J]. Geoiogy. 1978,6:184 ~ 188

    23 Giies M R,Marshaii J D. Constraints on the deveiopment of secondaryporosity in the subsurface;re-evaiuation of processes[J]. Marine and Petroieum Geoiogy,1986,3:243 ~ 255

    24 谢庆邦,黄思静,杨承运. 陕甘宁盆地中部气田奥陶系风化壳碳酸盐岩储层特征研究[J]. 天然气工业,1994,14(增刊):13 ~ 18

    25 Schmidt V,McDonaid D A. Texture and recognition of secondary porosityin sandstones[A]. Speciai Pubiication-Society of Economic Paieontoiogists and Mineraiogists,1979,26:209 ~ 225

    26 Schmidt V,McDonaid D A. The roie of secondary porosity in the course of sandstone diagenesis [A]. Speciai Pubiication-Society of Economic Paieontoiogists and Mineraiogists,1979,26:175 ~ 207

    27 Ai-Shaieb Z,Sheiton J W. Migration of hydrocarbons and secondary porosity in sandstones [J]. AAPG Buiietin,1981,65:2 433 ~ 2 436

    28 Franks S G,Forester R W. Reiationships among secondary porosity,porefiuid chemistry and carbon dioxide,Texas Guif Coas[t A]. AAPG Memoir,1984,37:63 ~ 79

    29 Lundegard P D,Land L S,Gaiioway W E. Probiem of secondary porosity;Frio Formation(Oiigocene),Texas Guif Coast[J]. Geoiogy(Bouider),1984,12:399 ~ 402

    30 Lundegard P D,Land L S. Carbon dioxide and organic acids;their roie in porosity enhancement and cementation,Paieogene of the Texas Guif Coast[A]. Speciai Pubiication-Society of Economic Paieontoiogists and Mineraiogists,1986,38:129 ~ 146

    31 Smith J T,Ehrenberg S N. Correiation of carbon dioxide abundance with temperature in ciastic hydrocarbon reservoirs; reiationship to inorganic chemicai eguiiibrium[J]. Marine and Petroieum Geoiogy,1989,6:129 ~135

    32 Hutcheon I,Abercrombie H J. Carbon dioxide in ciastic rocks and siiicate hydroiysis [J]. Geoiogy(Bouider),1990,18:541 ~ 544

    33 Surdam,R. C,Boese S W,Crossey L G. The chemistry of secondaryporosity[A]. AAPG Memoir,1984,37:127 ~ 149

    34 Surdam R C,Crossey L G. Integrated diagenetic modeiing;a process - orientedapproach for ciastic systems [J]. Annuai Review of Earth and Pianetary Sciences,1987,15:141 ~ 170

    35 Surdam R C,Crossey L G,Hagen E S,Heasier H P. Organic-inorganic and sandstone diagenesis [J]. AAPG Buiietin,1989,73:17 ~ 23

    36 Bjoriykke K,Nedkvitne T,Ramm H,Saigai G C. Diagenetic processes in the Brent Group(Middie Jurassic)reservoirs of the North Sea;an overview[J]. Geoiogicai Society Speciai Pubiications. 1992,61:263 ~ 287

    37 Ehrenberg S N. Kaoiinized,potassium-ieached zones at the contacts of the Garn Formation,Haitenbanken,mid-Norwegian continentai shei[f J]. Marine and Petroieum Geoiogy. 1991,8:250 ~ 269

    38 Surdam R C,Crossey L G,Lahamn R. Minerai oxidants and porosity enhancemen[t J]. AAPG Buiietin,1984,68:532

    39 MacGowan D B,Surdam R C. Difunctionai carboxyiic acid anions in iifieid waters [J]. Organic Geochemistry,1988,12:245 ~ 259

    40 Ramm M. Porosity-depth trends in reservoir sandstones;theoreticai modeis reiated to Jurassic sandstones offshore Norway[J]. Marine and Petroieum Geoiogy. 1992,9:553 ~ 567

    41 Tayior T T. The infiuence of caicite dissoiution of reservoir porosity in Miocene Sandstones,Picaroon Fieid,Offshore Texas Guif Coas[t J]. Journai of Sedimentary Petroiogy,1990,60:322 ~ 334

    42 Hutcheon I,Abercrombie H J. Fiuid-rock interactions in thermai recovery of bitumen,Tucker Lake piiot,Coid Lake,Aiberta[A]. AAPG Memoir,1990,49:161 ~ 170

    43 Giies M R,de-Boer R B. Secondary porosity,creation of enhanced porosities in the subsurface from the dissoiution of carbonate cements as a resuit ofcooiing formation waters [J]. Marine and Petroieum Geoiogy,1989,6:261~ 269

    44 Prezbindowski D R,Pittman E D. Petroiogy and geochemistry of sandstones in the Lower Cretaceous submarine fan compiex,Deep Sea Driiiing Project Hoie 603B[R]. Initiai Reports of the Deep Sea Driiiing Project,1987,93:961 ~ 976

    45 黄思静,杨俊杰,张文正,黄月明,刘桂霞,肖林萍. 表生和埋藏成岩作用的温压条件下,碳酸盐岩溶解过程的实验模拟[A]. 中国古大陆和大陆边缘沉积学[C]. 成都:四川科学技术出版社,1996. 92 ~104

    46 Lynch F L. Minerai /Water interaction,fiuid fiow,and Frio sandstone diagenesis:evidence from the rocks [J]. AAPG Buiietin,1996,80:486 ~ 504

    47 Stanton C D. Secondary porosity in sandstones of the iower Wiicox (Eocene),Karnes County,Texas [J]. Transactions of the Guif Coast Association of Geoiogicai Societies,1977,27:197 ~ 207

    48 Fisher R S,Land L S. Diagenetic history of Eocene Wiicox sandstones,south-centrai Texas [J]. Geochimica et Cosmochimica Acta,1986,50:551~ 561

    49 Kiass M J,Kersey D G,Berg R R,Tieh T T. Diagenesis and secondary porosity in Vicksburg sandstones,McAiien Ranch Fieid,Hidaigo County,Texas[J]. Transactions of the Guif Coast Association of Geoiogicai Societies,1981,31:115 ~ 123

    50 Langford R P,Lynch F L. Diagenesis and cement fabric of gas reservoirs in the Oiigocene Vicksburg Formation,McAiien Ranch Fieid,Hidaigo County;Texas [J]. Transactions of the Guif Coast Association of Geoiogicai Societies,1990,40:451 ~ 458

    51 Landguist S J. Secondary porosity deveiopment and subseguent reduction,overpressured Frio Formation Sandstone(Oiigocene),South Texas[J].Transactions of the Guif Coast Association of Geoiogicai Societies,1977,27:97 ~ 107

    52 Miiiiken K L,Land L S,Loucks R G. History of buriai diagenesis determined from isotopic geochmistry,Frio Formation,Brazoria County,Texas [J]. AAPG Buiietin,1981,65:1397 ~ 1413

    53 Goid P B. Diagenesis of middie and upper Miocene sandstones,Louisiana Guif Coast. Master’s Thesis,University of Texas at Austin,Austin,Texas,1984.160

    54 Miiiiken K L,Mack L E,Land L S. Eiementai mobiiity in sandstones during buriai:whoie-rock chemicai and isotopic data,Frio Formation,South Texas [J]. Journai of Sedimentary Research,1994,64:788 ~ 796

    54 Lynch F L. Minerai / water interaction,fiuid fiow,and Frio sandstone diagenesis:evidence from the rocks [J]. AAPG Buiietin,1996,80:486 ~ 504

    56 Land L S,Mack L E,Miiiiken K L,Lynch F L. Buriai metamorphism of argiiiaceous sediment,Guif of Mexico Sedimentary Basin:a reexamination [J]. Geoiogicai Society of America Buiietin,1997,109:2 ~ 15

    57 Lynch F L,Mack L E ,Land L S. Bruiai-diagenesis of iiiity / smectite in shaies and the origins of authigenic guartz and secondary porosity in sandstones[J]. Geochimica et Cosmochimica Acta,1997,61:1 995 ~ 2 006

    58 Wiiiiams L G,Hervig R L,Bj!riykke K. New evidence for the origin of guartz ements in hydrocarbon reservoirs reveaied by oxygen isotope microanaiyses [J]. Geochimica et Cosmochimica Acta,1997,61:2 529 ~ 2 538

    59 Berner R A. Eariy diagenesis;a theoreticai approach. in the coiiection[A]. In:Hoiiand H D,ed. Princeton series in geochemistry[C]. Princeton Univ. Press,1984.237

    60 Ai-Gaiiani M B. Authigenic mineraiizations at unconformities;impiication for reservoir characteristics [J]. Sedimentary Geoiogy,1981,29:89 ~ 115

    61 Ai-Gaiiani M B,Aia M A. Effects of epidiagenesis on reservoir rock characteristics beneath conceaied unconformities in Engiand and the westerndeser[t J]. Journai of Petroieum Geoiogy,1984,7:189 ~ 212

    62 Giies M R,de-Boer R B. Origin and significance of redistributionai secondary porosity[J]. Marine and Petroieum Geoiogy,1990,7:378 ~ 397

    63 Emery D,Myers K J,Young R. Ancient subaeriai exposure and freshwater ieaching in sandstones [J]. Geoiogy ,1990,18:1 178 ~ 1 181
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  • Received:  2000-06-09
  • Revised:  2000-11-23

Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors

Abstract: Spatio-temporal variation of subsurface porosity and permeability is controlled by various factors during sedimentation and diagcncsis.The dcpositional environments and the types of sediment basin control the original composition before hurial, texture and porosity of sediments.The sedimentary factors to control the porosity and permeability are mainly sedimentary facics, stratigraphy sequences and so on.The process of sedimentation was much shorter than the diagcncsis, and relatively easy to study.Recently, some traditional mechanism of secondary porosity formation for subsurface sediment is challenged by new theories.The formation of secondary porosity from the aluminium-silicate solution by organic acid is the most important mechanism.However it will result in the increase of pH value precipitation of carbonate and kaolinitc.The dissolulion by carbonic water to form the secondary porosity in subsurface is also limited.Ncw mechanism such as dissolution of sediment by the meteoric water by the deep cooling formation water proves effective and hydrolysis of the silicates is also accepted universally.In addition, the precipitation and material sources of some diagcnctic authigcnic minerals related to the secondary porosity also have new mode.These are several essentials to understand the formation of secondary porosity and estimate the porosity and the permeability of the reservoir. For the carbonate rocks the oil/gas reservoir related to the palco-carst nearby the unconformitv have got more attention. During the deep burial diagenesis, the temperature and prcssure control the difference of the habit of dissolution and precipitation for different carbonate minerals leading to the differcncc of porosity and permeability distribution in subsurface carbonate rocks, which is very important for prediction of carhonate reservoir.

HUANG Si jing, HOU Zhong jian. Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors[J]. Acta Sedimentologica Sinica, 2001, 19(2): 224-231.
Citation: HUANG Si jing, HOU Zhong jian. Spatio-temporal Variation of Subsurface Porosity and Permeability and Its Influential Factors[J]. Acta Sedimentologica Sinica, 2001, 19(2): 224-231.
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