[1]杨克兵,张 磊,吴晓宁,等.一种使用岩电资料确定束缚水饱和度及其他参数的方法[J].复杂油气藏,2021,14(02):47-51.[doi:10.16181/j.cnki.fzyqc.2021.02.009]
 YANG Kebing,ZHANG Lei,WU Xiaoning,et al.A method for determining irreducible water saturation and other parameters using core electricity data[J].Complex Hydrocarbon Reservoirs,2021,14(02):47-51.[doi:10.16181/j.cnki.fzyqc.2021.02.009]
点击复制

一种使用岩电资料确定束缚水饱和度及其他参数的方法
分享到:

《复杂油气藏》[ISSN:1674-4667/CN:31-2019/TQ]

卷:
14卷
期数:
2021年02期
页码:
47-51
栏目:
油气开发
出版日期:
2021-06-25

文章信息/Info

Title:
A method for determining irreducible water saturation and other parameters using core electricity data
作者:
杨克兵张 磊吴晓宁苑国辉王慧婧郭西波
中国石油华北油田分公司,河北 任丘 062552
Author(s):
YANG KebingZHANG LeiWU XiaoningYUAN GuohuiWANG HuijingGUO Xibo
PetroChina Huabei Oilfield Company,Renqiu 062552,China
关键词:
岩电实验数据分析幂函数束缚水饱和度可动油饱和度残余油饱和度
Keywords:
core electricity experimentdata analysispower functionirreducible water saturationmovable oil saturationresidual oil saturation
分类号:
TE321
DOI:
10.16181/j.cnki.fzyqc.2021.02.009
文献标志码:
A
摘要:
通过对单块岩电实验资料分析,岩心实验测量的电阻率与含水饱和度数据为幂函数关系。由于测量过程中使用高压气体对孔隙可动水进行驱替,这些测量数据能够反映岩石的孔隙水导电特征。进一步研究表明,当幂函数的电阻率曲线呈平缓变化趋势时,是可动水孔隙的变化影响电阻率曲线;当电阻率曲线呈剧烈变化趋势时,是束缚水孔隙导电起主导作用。因此可从曲线的形态变化确定束缚水饱和度、可动油饱和度、残余油饱和度等参数,就如同确定岩石孔隙度下限一样。与压汞等资料得出的束缚水饱和度资料对比,采用幂函数曲线的斜率截止法可确定岩心的束缚水饱和度,采用曲率最大值法可确定可动油饱和度,二者之间为残余油。初步应用表明,所确定的束缚水饱和度等参数绝对误差在5%以内,能够在实际中推广使用。
Abstract:
Based on the analysis of rock electricity data,the electrical resistivity and water saturation data measured by core experiments have a power function relationship. During the measurement process,high-pressure gas was used to displace the movable water in the pores. Thus,these measurement data can reflect the conductivity characteristics of water in rock pores.Further research showed that when the resistivity curve of the power function shows a gentle change trend,the change of the movable water pores affects the resistivity curve;when the resistivity curve shows a drastic change trend,the conductivity of the irreducible water pores plays a leading role. Therefore,parameters such as irreducible water saturation,movable oil saturation,residual oil saturation,etc. can be determined from the shape change of the curve,just like determining the lower limit of rock porosity.Compared with the irreducible water saturation data obtained by mercury injection data,the slope cut-off method of the power function curve can be used to determine the irreducible water saturation of the core,and the curvature maximum method can be used to determine the movable oil saturation,with residual oil saturation in between. The preliminary application showed that the absolute error of determining irreducible water saturation and other parameters is within 5%,which can be used in practice.

参考文献/References:

[1]SHANGBZ,HAMMANJG,CHENHL,etal.Amodeltocorrelatepermeabilitywithefficientporosityandirreduciblewatersaturation[C].Denver:SPEAnnualTechnicalConferenceandExhibition,2003:SPE-84303-MS
[2]WANGYD,BANDALMS,MORENOJE,etal.Asystematicapproachtoincorporatecapillarypressure-saturationdataintoreservoirsimulation[C].Adelaide:SPEAsiaPacificOil&GasConferenceandExhibition,2006:SPE-101013-MS.
[3]BASBUGB,KARPYNZT.Estimationofpermeabilityfromporosity,specificsurfacearea,andirreduciblewatersaturationusinganartificialneuralnetwork[C].BuenosAires:LatinAmerican&CaribbeanPetroleumEn-gineeringConference,2007:SPE-107909-MS.
[4]YANGYH,BIRMINGHAMTJ.Irreduciblewatersatur-ationhasbeendeterminedasthekeyfactorgoverninghydrocarbonproductionfromlowpermeabilitycarbonateatthewattenbergfieldintheDenverJulesburgBasin[C].Denver:SPEAnnualTechnicalConferenceandExhibition,2008:SPE-115210-MS.
[5]CASSOUG,POIRIER-COUTANSAISX,RAMAMOO-RTHYR.Movableoilsaturationevaluationinanultra-maturecarbonateenvironment[C].AbuDhabi:SPWLAMiddleEastRegionalSymposium,2007:SPWLA-MERS-2007-U.
[6]BUSTOSUD,BARREROGS,ALDANAI,etal.Understandingthemovableoilandfree-waterdis-tributioninheavy-oilsands,LlanosBasin,Colombia[C].Medellín:SPEHeavyandExtraHeavyOilConference,2014:SPE-171142-MS.
[7]FERREIRAFC,BOOTHR,OLIVEIRAR,etal.Mo-dellingirreduciblewatersaturationinheterogeneousrocksfrompore-sizedistribution[C].AbuDhabi:AbuDhabiInternationalPetroleumExhibition&Conference,2016:SPE-183446-MS.
[8]GOETZD,KNIGHTR,TERCIERP.Alaboratorypro-cedureforestimatingirreduciblewatersaturationfromcuttings[J].TheLogAnalyst,1996,37(4):SPWLA-1996-v37n4a1.
[9]DENNISD.Irreduciblewatersaturationfrommagnetic-resonance-imaginglogs[J].JournalofPetroleumTechnology,1997,49(11):1247-1249.
[10]ORABYE,EUBANKSDL.Determinationofirreduciblewatersaturationusingmagneticresonanceimaginglogs(MRIL):acasestudyfromEastTexas,USAM[C].Bahrain:MiddleEastOilShowandConference,1997:SPE-37772-MS.
[11]SOLATPOURR,BRYANJL,KANTZASA.Onest-imatingirreduciblewatersaturationintightformationsusingnuclearmagneticresonancerelaxometry[C].Calgary:SPECanadaUnconventionalResourcesConference,2018:SPE-189803-MS.
[12]王晓畅,范宜仁,邓少贵,等.基于离心试验数据确定束缚水饱和度[J].中国石油大学学报(自然科学版),2009,33(3):76-79,94.
[13]王翼君,唐洪明,郑马嘉,等.核磁共振法表征碳酸盐岩孔隙结构及束缚水饱和度的局限性:基于实验分析[J].海相油气地质,2018,23(3):89-96.
[14]谢然红,肖立志,刘家军.核磁共振测井时域分析法数值模拟及影响因素分析[J].地球物理学报,2011,54(8):2184-2192.
[15]朱林奇,张冲,石文睿,等.结合压汞实验与核磁共振测井预测束缚水饱和度方法研究[J].科学技术与工程,2016,16(15):22-29.
[16]GODAHM,MAIERH,BEHRENBRUCHP.UseofartificialIntelligencetechniquesforpredictingirre-duciblewatersaturation-Australianhydrocarbonbasins[C].Jakarta:AsiaPacificOilandGasConferenceandExhibition,2007:SPE-109886-MS.
[17]UGURUC,UDOFIAA,OLADIRANO.Estimatingirre-duciblewatersaturationandrelativepermeabilityfromlogs[C].Tinapa-Calabar:NigeriaAnnualInternationalConferenceandExhibition,2010:SPE-140623-MS.
[18]LIT,ZHOUX,CUIYJ,etal.Derivationofcontinuousirreduciblewatersaturationandporethroataperturedistributionfromwelllogsinanoffshorebrownfield[C].Houston:OffshoreTechnologyConference,2018:OTC-28788-MS.
[19]ARCHIEGE.Theelectricalresistivitylogasanaidindeterminingsomereservoircharacteristics[J].TransactionsoftheAIME,1942,146(1):54-62.
[20]卢艳,杨清山,刘传平.水驱油岩石物理响应特征实验研究[J].测井技术,2018,42(4):371-376.
[21]杨克兵,王竞飞,马凤芹,等.阿尔奇公式的适用条件分析及对策[J].天然气与石油,2018,36(2):58-63.

备注/Memo

备注/Memo:
收稿日期:2020-09-14 ;改回日期:2020-10-15 。
第一作者简介: 杨克兵(1967—),高级工程师,从事测井及地质综合研究。E-mail:ykbyzm123@sina.com。
更新日期/Last Update: 2021-06-30