发明名称 Method to determine local variations of the earth's magnetic field and location of the source thereof
摘要 A method to determine the earth's magnetic field vector along a sub-surface wellpath having unknown and possibly changing azimuth, in the presence of a magnetic disturbance caused by a magnetic source external to the wellpath includes estimating the three components of the earth field along the three axes of a magnetic sensor package by a polynomial function of measured depth along the wellpath. Upon removal of the earth's magnetic field from the measurements, the resultant magnetic field of the disturbance is determined and can be used to determine the position and orientation of the source of the disturbance.
申请公布号 US9448329(B2) 申请公布日期 2016.09.20
申请号 US201314021602 申请日期 2013.09.09
申请人 SCIENTIFIC DRILLING INTERNATIONAL, INC. 发明人 Hove Jim
分类号 G01V11/00;G01V3/08;E21B47/022;E21B7/04 主分类号 G01V11/00
代理机构 代理人 Locklar Adolph
主权项 1. A process for determining the location of an underground object having a magnetic field comprising: a) supplying a magnetic sensor package adapted to measure three vector components of a magnetic field and at least one accelerometer; b) determining the vector components of a total magnetic field vector at each of a plurality of measured depth locations along a well path, the components at each location comprising a first vector component in the direction of the well path, and a second vector component lying in a plane normal to the well path; c) determining the direction of the gravity vector at each of said plurality of locations along the well path; d) using the determined direction of the gravity vector at each location to resolve the determined total field vector components into resolved horizontal and vertical components of the total field, said resolved components comprising a horizontal component in the direction of the well path, and a horizontal component perpendicular to the well path, and lying in a vertical plane which contains the first vector in the direction of the well path; e) estimating the direction of the well path with respect to the fixed magnetic field component path at each location as a mathematical function of distance of the location along the well path; f) estimating the magnitude of the fixed horizontal magnetic field; g) calculating estimated horizontal magnetic field components from the estimated fixed magnetic field and the mathematical function, at each location; h) adjusting the parameters of the mathematical function and the estimate of fixed horizontal magnetic field to determine the earth magnetic field; i) subtracting the determined earth magnetic field from the measured total magnetic field along the well path to obtain a determined magnetic field of the underground object; j) selecting parametric model parameters; k) creating a best fit list with a pre-determined number of model slots; l) selecting a range for each parameter and an incremental value for each parameter; m) creating a parametric model using the model parameters, wherein the parametric model has a predicted magnetic field of the underground object; n) comparing the predicted field of the underground object with the determined magnetic field of the underground object to obtain a parametric model fit; o) assigning the parametric model to a slot on the best fit list if the model slots do not each have a model assigned or if the parametric model has a lower fit than any other model on the best fit list; p) removing the model corresponding to the highest fit if the number of models on the best fit list exceeds the predetermined number of slots; q) determining if any model on the best fit list has a corresponding fit that is less than or equal to a pre-determined desired fit; r) iterating each parameter by the incremental value for that parameter and repeating operations m) to q) if no model has a corresponding fit that is less than or equal to a pre-determined desired fit s) determining the location of an underground object having a magnetic field using the parametric model.
地址 Houston TX US