A study on gravity field downward continuation using the regularized equivalent-layer method

被引:3
作者
Li XiaoJie [1 ,2 ,3 ]
Wang ZhenLi [1 ,3 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resource Res, Beijing 100029, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2018年 / 61卷 / 07期
关键词
Downward continuation; Equivalent layer; Tikhonov regularization; Iterative compensation; POTENTIAL FIELDS; ITERATION METHOD; MAGNETIC-FIELD; SURFACE; REDUCTION; PLANE;
D O I
10.6038/cjg2018L0249
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In recent years, dynamic reservoir monitoring technology using time-lapse microgravity method has been receiving much attention of researchers at home and abroad. As a result of the low signal to noise ratio (SNR) and weak signal in observation data, it is impossible to quantitatively interpret fluid migration in reservoirs using time-lapse microgravity data. In order to suppress observation noise and enhance weak signals, this article presents the regularized equivalent source downward continuation (RESDC) method, and derives the RESDC operator in the wavenumber domain. Besides, the iterative compensation algorithm is proposed to compensate for amplitude attenuation of the downward continuation field. With tests on synthetic data, this work further studies the wavenumber response of the filtering operators and the downward continuation operators of regularized equivalent layers at different depths. Results show that the downward continuation field of the RESDC method is more accurate and stable compared with the field from the Tikhonov downward continuation method. Applying the iterative compensation RESDC method to field data of a time-lapse microgravity survey verifies that the proposed method can effectively enhance weak signals and stably realizes large-depth downward continuation.
引用
收藏
页码:3028 / 3036
页数:9
相关论文
共 24 条
[1]   An optimal model of the equivalent source for reduction-to-plane of potential field on uneven surface and the new method to deduce unit potential field expression of the optimal model [J].
An Yu-Lin ;
Chai Yu-Pu ;
Zhang Ming-Hua ;
Huang Jin-Ming ;
Qiao Ji-Hua .
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2013, 56 (07) :2473-2483
[2]  
Bell JB, 1978, Mathematics of Computation, V32, P1320, DOI DOI 10.2307/2006360
[3]   REDUCTION OF MAGNETIC AND GRAVITY DATA ON AN ARBITRARY SURFACE ACQUIRED IN A REGION OF HIGH TOPOGRAPHIC RELIEF [J].
BHATTACHARYYA, BK ;
CHAN, KC .
GEOPHYSICS, 1977, 42 (07) :1411-1430
[4]   EQUIVALENT SOURCE TECHNIQUE [J].
DAMPNEY, CNG .
GEOPHYSICS, 1969, 34 (01) :39-&
[5]   EQUIVALENT SOURCES USED AS AN ANALYTIC BASE FOR PROCESSING TOTAL MAGNETIC-FIELD PROFILES [J].
EMILIA, DA .
GEOPHYSICS, 1973, 38 (02) :339-348
[6]   A stable downward continuation by using the ISVD method [J].
Fedi, M ;
Florio, G .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2002, 151 (01) :146-156
[7]  
GUAN ZN, 1985, ACTA GEOPHYS SINICA, V28, P419
[8]   ANALYSIS OF DISCRETE ILL-POSED PROBLEMS BY MEANS OF THE L-CURVE [J].
HANSEN, PC .
SIAM REVIEW, 1992, 34 (04) :561-580
[9]   CONTINUATION OF POTENTIAL FIELDS BETWEEN ARBITRARY SURFACES [J].
HANSEN, RO ;
MIYAZAKI, Y .
GEOPHYSICS, 1984, 49 (06) :787-795
[10]  
Hou Z, 1982, GEOPHYS GEOCHEMICAL, V6, P33