{"title":"Experimental Design for Surface-to-Borehole Hydrocarbon Applications","authors":"B. Kriegshäuser, A. Tripp, L. Tabarovsky","doi":"10.5636/JGG.49.1659","DOIUrl":null,"url":null,"abstract":"We discuss in a simplified surface-to-borehole example the resolution of the coefficient of anisotropy λ for an anisotropic layer sandwiched in an isotropic half-space as a function of transmitter-receiver configuration and magnetic field components. Our analysis supposes that the horizontal resistivity of the anisotropic bed has been established by previous logging, and that only horizontal magnetic fields will be used to determine the vertical resistivity. The resolution analysis shows that for the model studied the coefficient of anisotropy λ can be resolved within 10% for a broad range of transmitter-receiver configurations if ∂B x /∂t and ∂B y /∂t are used jointly in the interpretation. Using only ∂B x /∂t or ∂B y /∂t individually, λ can only be resolved for a limited range of transmitter-receiver configurations. A joint interpretation of both horizontal magnetic field components facilitates a better resolution of the coefficient of anisotropy compared to a single interpretation.","PeriodicalId":156587,"journal":{"name":"Journal of geomagnetism and geoelectricity","volume":"17 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1997-11-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of geomagnetism and geoelectricity","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5636/JGG.49.1659","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
We discuss in a simplified surface-to-borehole example the resolution of the coefficient of anisotropy λ for an anisotropic layer sandwiched in an isotropic half-space as a function of transmitter-receiver configuration and magnetic field components. Our analysis supposes that the horizontal resistivity of the anisotropic bed has been established by previous logging, and that only horizontal magnetic fields will be used to determine the vertical resistivity. The resolution analysis shows that for the model studied the coefficient of anisotropy λ can be resolved within 10% for a broad range of transmitter-receiver configurations if ∂B x /∂t and ∂B y /∂t are used jointly in the interpretation. Using only ∂B x /∂t or ∂B y /∂t individually, λ can only be resolved for a limited range of transmitter-receiver configurations. A joint interpretation of both horizontal magnetic field components facilitates a better resolution of the coefficient of anisotropy compared to a single interpretation.
在一个简化的地对井的例子中,我们讨论了夹在各向同性半空间中的各向异性层的各向异性系数λ的分辨率作为收发器结构和磁场分量的函数。我们的分析假设各向异性地层的水平电阻率已经通过之前的测井得到,并且只使用水平磁场来确定垂直电阻率。解析分析表明,对于所研究的模型,如果同时使用∂B x /∂t和∂B y /∂t进行解释,则各向异性系数λ在广泛的收发配置下可以在10%以内被解析。仅单独使用∂B x /∂t或∂B y /∂t, λ只能在有限范围的发送-接收配置中解析。与单一解释相比,两种水平磁场分量的联合解释有助于更好地确定各向异性系数。