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Forward Modeling of the Relationship Between Reflection Coefficient and Incident Angle of the P Wave in a Coal Seam

机译:煤层P波反射系数与入射角关系的正演模拟。

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Although the Zoeppritz equation is suitable for a single interface in a thick deposit, it has some limitations for composite reflection waves from both the floor and the roof of coal seams. Based on the ray model, the relationship of the overall reflection coefficient of composite reflection P waves, from coal seam versus incidence angle (AVO), is discussed. The result shows that: 1) the overall reflection coefficient of composite reflection waves from coal seams is a negative value and is determined mainly by the lithology of roof and floor, which is different from the reflection coefficient of a single interface; 2) if the incidence angle ranges from 0° to 6°, the reflection coefficient of composite waves of a coal seam does not change with the incidence angle and 3) if the incidence angle ranges from 6-60° , the reflection coefficient increases monotonically.
机译:尽管Zoeppritz方程适用于厚沉积物中的单个界面,但是它对于来自煤层底部和顶部的复合反射波都有一些限制。基于射线模型,讨论了来自煤层的复合反射P波的全反射系数与入射角(AVO)的关系。结果表明:1)煤层复合反射波的总反射系数为负值,主要由顶板和底板的岩性决定,不同于单一界面的反射系数。 2)入射角在0°至6°范围内,煤层复合波的反射系数不会随入射角而变化; 3)入射角在6-60°范围内时,反射系数会单调增加。

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