物探与化探
物探與化探
물탐여화탐
GEOPHYSICAL AND GEOCHEMICAL EXPLORATION
2014年
1期
90-95
,共6页
王赛昕%刘天佑%欧洋%高文利%邱礼泉%冯杰
王賽昕%劉天祐%歐洋%高文利%邱禮泉%馮傑
왕새흔%류천우%구양%고문리%구례천%풍걸
井中磁测%弱信号识别%倾斜角%解析信号振幅%均值归一
井中磁測%弱信號識彆%傾斜角%解析信號振幅%均值歸一
정중자측%약신호식별%경사각%해석신호진폭%균치귀일
borehole magnetic survey%weak signal detection%tilt-angle%analytical signal amplitude%normalizing with a mean value
井中磁测仪器距离场源近,磁测资料受到钻孔打穿磁性体产生的内磁场影响,往往存在强干扰压制有用信号,因此研究井中磁测资料预处理与弱信号识别方法具有重要意义。笔者将地面重磁资料边界识别中倾斜角总水平导数和解析信号振幅方法改进后应用于井中磁测资料预处理中,提出倾斜角垂向导数和均值归一解析信号振幅方法。通过模型分析证明了两种方法都可识别强弱不同的井旁磁性体位置,反映边界信息,且给出了计算均值归一解析信号振幅过程中窗口选择的依据。将两种方法应用于江苏某工区ZK002孔磁测资料预处理中,得出倾斜角垂向导数方法应用于实测资料中会放大干扰,而均值归一解析信号振幅方法增强了该钻孔弱异常信息,且压制了干扰信号,处理结果与磁化率测井和钻孔资料相对应。
井中磁測儀器距離場源近,磁測資料受到鑽孔打穿磁性體產生的內磁場影響,往往存在彊榦擾壓製有用信號,因此研究井中磁測資料預處理與弱信號識彆方法具有重要意義。筆者將地麵重磁資料邊界識彆中傾斜角總水平導數和解析信號振幅方法改進後應用于井中磁測資料預處理中,提齣傾斜角垂嚮導數和均值歸一解析信號振幅方法。通過模型分析證明瞭兩種方法都可識彆彊弱不同的井徬磁性體位置,反映邊界信息,且給齣瞭計算均值歸一解析信號振幅過程中窗口選擇的依據。將兩種方法應用于江囌某工區ZK002孔磁測資料預處理中,得齣傾斜角垂嚮導數方法應用于實測資料中會放大榦擾,而均值歸一解析信號振幅方法增彊瞭該鑽孔弱異常信息,且壓製瞭榦擾信號,處理結果與磁化率測井和鑽孔資料相對應。
정중자측의기거리장원근,자측자료수도찬공타천자성체산생적내자장영향,왕왕존재강간우압제유용신호,인차연구정중자측자료예처리여약신호식별방법구유중요의의。필자장지면중자자료변계식별중경사각총수평도수화해석신호진폭방법개진후응용우정중자측자료예처리중,제출경사각수향도수화균치귀일해석신호진폭방법。통과모형분석증명료량충방법도가식별강약불동적정방자성체위치,반영변계신식,차급출료계산균치귀일해석신호진폭과정중창구선택적의거。장량충방법응용우강소모공구ZK002공자측자료예처리중,득출경사각수향도수방법응용우실측자료중회방대간우,이균치귀일해석신호진폭방법증강료해찬공약이상신식,차압제료간우신호,처리결과여자화솔측정화찬공자료상대응。
As the logging instrument is placed near the field source, the borehole magnetic data are likely to be affected by the internal magnetic field when the drill hole penetrates the magnetic body. As a result, the useful signal is often suppressed by strong jamming and not easy to identify. Therefore, it is important to find a method which can identify the weak signal through data preprocessing. In this paper, the methods for ground survey, called total horizontal derivate of tilt-angle and analytical Signal Amplitude, were used in bore-hole magnetic survey. The authors proposed vertical derivative of tilt-angle through coordinate transformation and a new method called Equalized Analytical Signal Amplitude. Through data processing of the model, the authors point out that the two kinds of methods can both identify the magnetic body and give the boundary information. The authors also give a standard to choose a suitable window to cal-culate the Equalized Analytical Signal Amplitude. The two kinds of methods were applied to Jiangsu ZK002 borehole magnetic data pre-processing. The vertical derivative of tilt-angle enlarged the interference of data, wheres the Equalized Analytical Signal Amplitude uses normalized method to identify the weak signal and suppress the interference. The Equalized Analytical Signal Amplitude is also well consistent with the results of magnetic susceptibility logging and the borehole data in ZK002.