石油钻探技术
石油鑽探技術
석유찬탐기술
PETROLEUM DRILLING TECHNIQUES
2014年
2期
102-106
,共5页
许昊东%黄根炉%张然%韦红术%程锋瑞
許昊東%黃根爐%張然%韋紅術%程鋒瑞
허호동%황근로%장연%위홍술%정봉서
径向磁干扰%钻柱磁化%轴向磁干扰%方位角
徑嚮磁榦擾%鑽柱磁化%軸嚮磁榦擾%方位角
경향자간우%찬주자화%축향자간우%방위각
radial magnetic interference%drillstring magnetization%axial magnetic interference%azimuth angle
为提高磁力随钻测量的井眼轨迹精度,研究了随钻测量磁干扰校正方法。利用随钻测量参数,计算井斜角、工具面角和方位角;采取360°旋转钻柱记录、分析径向磁力计读数的方法,纠正磁热点引起的径向磁干扰;采用循环迭代的方法,纠正钻柱磁化引起的轴向磁干扰。通过仿真测量参数、磁干扰数据和地磁参数,应用磁干扰校正方法计算得到校正方位角,并与实测方位角、真实方位角进行了对比,结果发现,在其他井眼参数保持不变的条件下,井斜角接近90°或方位角接近90°、270°时,实测方位角误差变大;井斜角接近0°或方位角接近0°、180°时,实测方位角误差变小;真实方位角为0°~180°时,实测方位角比真实方位角小,真实方位角为180°~360°时,实测方位角比真实方位角大;井眼轨迹接近水平东或水平西方向时,轴向磁干扰的校正效果最差。磁干扰校正方法能够提高方位角测量精度,减少无磁钻铤长度。
為提高磁力隨鑽測量的井眼軌跡精度,研究瞭隨鑽測量磁榦擾校正方法。利用隨鑽測量參數,計算井斜角、工具麵角和方位角;採取360°鏇轉鑽柱記錄、分析徑嚮磁力計讀數的方法,糾正磁熱點引起的徑嚮磁榦擾;採用循環迭代的方法,糾正鑽柱磁化引起的軸嚮磁榦擾。通過倣真測量參數、磁榦擾數據和地磁參數,應用磁榦擾校正方法計算得到校正方位角,併與實測方位角、真實方位角進行瞭對比,結果髮現,在其他井眼參數保持不變的條件下,井斜角接近90°或方位角接近90°、270°時,實測方位角誤差變大;井斜角接近0°或方位角接近0°、180°時,實測方位角誤差變小;真實方位角為0°~180°時,實測方位角比真實方位角小,真實方位角為180°~360°時,實測方位角比真實方位角大;井眼軌跡接近水平東或水平西方嚮時,軸嚮磁榦擾的校正效果最差。磁榦擾校正方法能夠提高方位角測量精度,減少無磁鑽鋌長度。
위제고자력수찬측량적정안궤적정도,연구료수찬측량자간우교정방법。이용수찬측량삼수,계산정사각、공구면각화방위각;채취360°선전찬주기록、분석경향자력계독수적방법,규정자열점인기적경향자간우;채용순배질대적방법,규정찬주자화인기적축향자간우。통과방진측량삼수、자간우수거화지자삼수,응용자간우교정방법계산득도교정방위각,병여실측방위각、진실방위각진행료대비,결과발현,재기타정안삼수보지불변적조건하,정사각접근90°혹방위각접근90°、270°시,실측방위각오차변대;정사각접근0°혹방위각접근0°、180°시,실측방위각오차변소;진실방위각위0°~180°시,실측방위각비진실방위각소,진실방위각위180°~360°시,실측방위각비진실방위각대;정안궤적접근수평동혹수평서방향시,축향자간우적교정효과최차。자간우교정방법능구제고방위각측량정도,감소무자찬정장도。
In order to improve accuracy of well trajectory measured by MWD ,magnetic interference correction was studied .Inclination angle ,tool-face and azimuth angle were worked out when surveying with magnetic MWD .Cross-axial magnetic interference originating from magnetic hot spots in the NMDC was corrected by rotating drillstring 360° and analyzing cross-axial magnetometer data .Axial magnetic interfer-ence originates from the magnetization of ferromagnetic portions of the drill string was corrected by loop it-eration method .A series of conclusions were reached by a group of simulation data including survey data , magnetic interference data and geomagnetic parameters :the error of measured azimuth was larger when in-clination approaches 90° or azimuth approaches 90° ,270°;the error of measured azimuth was smaller when inclination approaches 0° or azimuth approaches 0° ,180°;the measured azimuth was smaller than true azi-muth when true azimuth was between 0° and 180°;the measured azimuth was larger than true azimuth when true azimuth was between 180° and 360°;the effect of correcting axial magnetic interference was poo-rer when trajectory approaches horizontal west or east and the correcting algorithm was stable .