%0 Journal Article
%T Acoustic wave propagation in a borehole penetrating an inclined layered formation<br>倾斜地层中的井孔声场研究
%A LIN Wei-Jun
%A WANG Xiu-Ming
%A ZHANG Hai-Lan
%A <br>林伟军
%A 王秀明
%A 张海澜
%J 地球物理学报
%D 2006
%I 
%X Understanding acoustic wave propagation in an inclined fluid-filled borehole embedded in 3-D media is essential for acoustic wave logging data processing and interpretation. A 3-D staggered finite-difference (FD) method is used to simulate borehole sonic waves in isotropic inclined layered formations. First, the FD results are compared with those obtained by a Real Axis Integration method for a monopole source in an open borehole vertically imbedded in homogeneous formation. A good agreement has been made for the two methods. Consequently, the FD solutions are confirmed by the analytical solutions. Then, the waveforms for a borehole with various deviations between the borehole axis and the formation interface are calculated. Those for dipole sources are also simulated at a low source centre frequency. The numerical results show that, when the source is under the inclined interface, equivalently going up in a fast (downward) formation, and also as the interface inclined angle increases, the determined slowness curves decreases from the slowness approximately correspondent to that of the slow (upward) formation, to the one in downward formation, and never reaches the real compressional slowness in the upward formation. The corresponding slowness curve, with respect to record points, and above the formation interface, becomes flatter for a long spacing; while the short spacing detection makes the curve sharper. For all spacing with receivers in the upward formation, and the source under the interface in the downward formation, the apparent slowness becomes smaller than the real wave slowness in the upward formation. The larger the inclined angle, the flatter the curves away from the interface range for the large spacing. The shear wave slowness appears the similar features but more sensitive to the inclined angle than the compressional slowness. Also, this effect is controlled by the velocity contrast between the upward and downward formations. The above phenomenon is shown clearly in both snapshot visualization and in slowness calculations with synthetic waveforms, and is well explained with the ray acoustics.
%K Inclined layer
%K Borehole acoustic field
%K Finite difference
%K Acoustic wave logging<br>倾斜地层
%K 井孔声场
%K 有限差分
%K 声波测井
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=1E44AE713D8A6DE0&jid=14DC41C59CBF6770055A7D610D53AE46&aid=6F88D5E98D83FA94&yid=37904DC365DD7266&vid=2A3781E88AB1776F&iid=CA4FD0336C81A37A&sid=03E56C113B4E5A88&eid=E39A3F4E3A67639B&journal_id=0001-5733&journal_name=地球物理学报&referenced_num=5&reference_num=21