脉冲中子-中子测井影响因素的数值模拟  

Numerical simulation for influence factor of pulsed neutron-neutron logging

作　　者：张锋[1,2] 王新光[1,2] 

机构地区：[1]中国石油大学地球资源与信息学院,山东青岛266555 [2]中国石油大学CNPC测井重点实验室,山东青岛266555

出　　处：《中国石油大学学报（自然科学版）》2009年第6期46-51,共6页Journal of China University of Petroleum(Edition of Natural Science)

基　　金：国家自然科学基金项目(40774058)

摘　　要：利用蒙特卡罗方法建立各种条件下的套管井计算模型,模拟相应的热中子时间谱,进而计算地层宏观吸收截面。模拟结果表明:地层的宏观吸收截面随着孔隙度和含水饱和度的增加而增加,且源距越小、地层水的矿化度和泥质含量越高、套管的尺寸越大、仪器越居中、俘获截面越高的岩性地层条件下,地层的宏观吸收截面值也越大;套管壁厚和水泥环对地层宏观吸收截面没有影响,但套管壁越厚、水泥环厚度越小,热中子总计数越低。利用脉冲中子测井数据确定地层含水饱和度时应对各种影响因素作相应的校正。The calculation models under the condition of different cased well situation were established by Monte Carlo method, and the relevant thermal neutron time spectrum was simulated. The formation macroscopic cross section was also calculated. The results show that the formation macroscopic cross section increases with porosity and water saturation increasing, and the thermal capture capability is powerful under the condition of small spacing, high salinity and shale content, large cased size, centralized tool and high capture lithology formation. The thickness of the casing and the cement do not affect formation macroseopic absorption cross section, but the bigger the casing thickness and the smaller the cement thickness, the lower the total count of the thermal neutron. It must be corrected for different influential factor when the formation water saturation is determined by pulsed neutron logging data.

关 键 词：脉冲中子-中子测井 含水饱和度 地层宏观吸收截面 蒙特卡罗模拟 

分 类 号：P631.817[天文地球—地质矿产勘探]