摘要
在超声波频率下,利用脉冲透射法,探讨了实验室条件下流体饱和岩石的频散和衰减机制,对不同围限压力下的干燥和不同粘度流体饱和砂岩样品的衰减特征进行了系统的研究。给出了岩石样品衰减的测量方法,分别对干燥样品和流体饱和样品进行了频谱分析,对衰减机制进行了讨论。利用Biot流模型和BISQ模型分析了流体饱和岩石中与流体流动作用有关的衰减。定量分析了各种衰减机制对弹性波总衰减的相对贡献。讨论了将实验结果引入地震勘探时,与流体流动相关的各种衰减机制的适用性。
By using ultrasonic frequency,pulse transmission technique was used to probe the dispersion and attenuation mechanism of flu- id-saturated rock in laboratory.The attenuation characteristics of dry and different fluid-saturated sandstone samples under different confining pressure were studied.The method of measuring the at- tenuation of rock samples was introduced.Spectrum was analyzed on dry samples and fluid-saturated samples,and the attenuation mechanism discussed.Blot-flow model and BISQ model were sed to analyze the attenuation related to the fluid flowing in fluid-saturat- ed rock.The relative contribution of the attenuation mechanisms to the overall attenuation of elastic wave was quantitatively analyzed. The applicability of the attenuation mechanisms related to fluid flowing was discussed under the condition of introducing experi- mental results into practical seismic exploration.
出处
《石油物探》
EI
CSCD
2008年第4期346-351,17-18,共6页
Geophysical Prospecting For Petroleum
基金
国家重点基础研究计划(973)项目(2007CB209600)资助
作者简介
邓继新（1974-），男，博士，研究方向为岩石物理学。
