地球物理学进展
地毬物理學進展
지구물이학진전
PROGRESS IN GEOPHYSICS
2009年
6期
2202-2207
,共6页
赵军%胡洪%刘应华%蒋智格%陈伟中
趙軍%鬍洪%劉應華%蔣智格%陳偉中
조군%호홍%류응화%장지격%진위중
高矿化度%电阻率校正%图版法%岩心%饱和度
高礦化度%電阻率校正%圖版法%巖心%飽和度
고광화도%전조솔교정%도판법%암심%포화도
high salinity%resistively corretion%chart method%core%saturation
为了克服克拉地区膏盐地层垮塌及地层压力对钻井的影响,在钻井过程中往往采用高矿化度、大密度的钻井液.这使得渗透性地层中观测得到电阻率与实际的电阻率存在较大的偏差,给测井解释带来极大的困难.本文针对克拉地区的实际情况,时高矿化度泥浆影响下的电阻率校正方法进行了探索性研究,提出了基于岩心资料的电阻率校正方法及基于泥浆动态侵入的图版校正电阻率方法,最后通过毛管分析饱和度与校正后电阻率计算饱和度对比验证校正电阻率的可信性.结果表明,校正后电阻率更能真实的反映地层电性特征,进一步提高了测井解释符合率.
為瞭剋服剋拉地區膏鹽地層垮塌及地層壓力對鑽井的影響,在鑽井過程中往往採用高礦化度、大密度的鑽井液.這使得滲透性地層中觀測得到電阻率與實際的電阻率存在較大的偏差,給測井解釋帶來極大的睏難.本文針對剋拉地區的實際情況,時高礦化度泥漿影響下的電阻率校正方法進行瞭探索性研究,提齣瞭基于巖心資料的電阻率校正方法及基于泥漿動態侵入的圖版校正電阻率方法,最後通過毛管分析飽和度與校正後電阻率計算飽和度對比驗證校正電阻率的可信性.結果錶明,校正後電阻率更能真實的反映地層電性特徵,進一步提高瞭測井解釋符閤率.
위료극복극랍지구고염지층과탑급지층압력대찬정적영향,재찬정과정중왕왕채용고광화도、대밀도적찬정액.저사득삼투성지층중관측득도전조솔여실제적전조솔존재교대적편차,급측정해석대래겁대적곤난.본문침대극랍지구적실제정황,시고광화도니장영향하적전조솔교정방법진행료탐색성연구,제출료기우암심자료적전조솔교정방법급기우니장동태침입적도판교정전조솔방법,최후통과모관분석포화도여교정후전조솔계산포화도대비험증교정전조솔적가신성.결과표명,교정후전조솔경능진실적반영지층전성특정,진일보제고료측정해석부합솔.
In order to overcome the influence of collapsed gypsum-sah formation and formation pressure on drilling in the Kela,Kuehe area,people oftern use a fluid of high mineralization and big density during production.This makes the measured resistivity in the permeable strata differ much from the realistic values,and brings great difficulties to log interpretation.Based on the actual case of the Kela area,this work attempts to study the resistivity correction method to the influence of high-mineralization mud.We propose that the obserred resistivity can be corrected based on care data and patterns of dynamic mud intrusion.Then we compare the saturation from hair analysis and that calculated after the correction;and verify the rebiability of the resistivity correction.The result shows that the corrected resistivity can reflect better the real eletric feature of strata and further enhance the accuracy of logging interpretation.