CN114460654B - Semi-aviation transient electromagnetic data inversion method and device based on L1L2 mixed norm - Google Patents
Semi-aviation transient electromagnetic data inversion method and device based on L1L2 mixed norm Download PDFInfo
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Abstract
Description
技术领域technical field
本发明涉及地球物理航空电磁勘探技术领域,尤其是基于L1L2混合范数的半航空瞬变电磁数据反演方法及装置。The invention relates to the technical field of geophysical aviation electromagnetic exploration, in particular to a semi-aerial transient electromagnetic data inversion method and device based on L1L2 mixed norm.
背景技术Background technique
目前,现有技术中的地球物理电磁勘探多采用航空电磁法,其采用直升机或固定翼飞机搭载发射和观测系统,其无法运用在城市地下空间探测、地面地质调查等场景。另外,现有技术中的航空电磁法采用一维单点反演算法,其在横向上没有约束,数据噪声较强时剖面电阻率连续性较差;在纵向对电阻率约束上通常采用正则化约束,这种正则化约束主要缺点在于使得模型过于光滑,不能有效刻画电性突变界面信息。At present, the geophysical electromagnetic exploration in the prior art mostly adopts the aerial electromagnetic method, which uses a helicopter or fixed-wing aircraft to carry a launch and observation system, which cannot be used in urban underground space exploration, ground geological survey and other scenarios. In addition, the airborne electromagnetic method in the prior art adopts a one-dimensional single-point inversion algorithm, which has no constraints in the lateral direction, and the continuity of the profile resistivity is poor when the data noise is strong; regularization is usually used in the longitudinal constraints on the resistivity. The main disadvantage of this regularization constraint is that it makes the model too smooth and cannot effectively describe the electrical mutation interface information.
例如专利申请号为“202110820825.8”、名称为“一种半航空瞬变电磁电导率-深度成像方法及设备”的中国发明专利,其根据实际情况预先模拟出符合实际情况的电磁响应查询数据库,再将探测到的电磁响应数据在“库”中进行搜索,无需像反演一样进行多次迭代计算,使得半航空瞬变电磁法可以进行快速成像,并快速获得初步成像结果及反演初始模型。For example, the patent application number is "202110820825.8" and the Chinese invention patent titled "A Semi-Aeronautical Transient Electromagnetic Conductivity-Depth Imaging Method and Equipment", which pre-simulates the electromagnetic response according to the actual situation to query the database, and then The detected electromagnetic response data is searched in the "library", and there is no need to perform multiple iterative calculations like inversion, so that the semi-aviation transient electromagnetic method can perform fast imaging, and quickly obtain preliminary imaging results and inversion initial models.
再如专利申请号为“202010751396.9”、名称为“一种无人机半航空时间域电磁探测数据分析解释方法”的中国发明专利,其包括以下步骤:a、对测线数据进行预处理,消除运动噪声;b、对二次场数据进行频谱分析和数字滤波处理;c、形成待成像或反演解释的数据;d、对叠加和抽道后的二次场数据进行一维快速反演,建立地下电性结构剖面,结合地质资料对反演成像结果进行地质解释,形成综合解释结果。Another example is the Chinese invention patent with the patent application number of "202010751396.9" and the title of "A Method for Analysis and Interpretation of UAV Semi-Aeronautical Time Domain Electromagnetic Detection Data", which includes the following steps: a. Preprocessing the survey line data, eliminating Motion noise; b. Perform spectrum analysis and digital filtering on the secondary field data; c. Form data to be imaged or interpreted by inversion; d. Perform one-dimensional fast inversion of the secondary field data after stacking and extraction, Establish a subsurface electrical structural profile, and perform geological interpretation of the inversion imaging results in combination with geological data to form a comprehensive interpretation result.
上述技术存在以下问题:上述技术均存在快速成像结果较为粗糙,不能准确反映地层电阻率值及层分界面信息;对含噪声数据,由于单点反演没有考虑测点的邻近点地层信息的影响,反演结果横向不连续,呈现出条带状。The above techniques have the following problems: the quick imaging results of the above techniques are relatively rough, and cannot accurately reflect the formation resistivity value and layer interface information; for the noisy data, the single-point inversion does not consider the influence of the formation information of the adjacent points of the measurement point. , the inversion results are horizontally discontinuous and appear striped.
因此,急需要提出一种逻辑简单、准确可靠的基于L1L2混合范数的半航空瞬变电磁数据反演方法。Therefore, it is urgent to propose a simple, accurate and reliable semi-aerial transient electromagnetic data inversion method based on L1L2 mixed norm.
发明内容SUMMARY OF THE INVENTION
针对上述问题,本发明的目的在于提供基于L1L2混合范数的半航空瞬变电磁数据反演方法,本发明采用的技术方案如下:In view of the above problems, the purpose of the present invention is to provide a semi-aviation transient electromagnetic data inversion method based on L1L2 mixed norm, and the technical scheme adopted in the present invention is as follows:
第一部分,本发明提供了基于L1L2混合范数的半航空瞬变电磁数据反演方法,采用地面发射瞬变电磁信号,并利用无人机搭载接收装置获取电磁响应数据,其包括以下步骤:In the first part, the present invention provides a semi-aviation transient electromagnetic data inversion method based on L1L2 hybrid norm, which adopts ground-transmitting transient electromagnetic signals, and utilizes a UAV-mounted receiving device to obtain electromagnetic response data, which includes the following steps:
利用接收装置采集待测区域的电磁响应数据;Use the receiving device to collect the electromagnetic response data of the area to be measured;
构建待检测区域的地层模型,并预设迭代终止条件;Build the stratigraphic model of the area to be detected, and preset the iteration termination conditions;
求得电磁响应数据的L2范数约束项对应的横向约束加权矩阵;Obtain the transverse constraint weighting matrix corresponding to the L2 norm constraint term of the electromagnetic response data;
求得或更新电磁响应数据的L1范数约束项对应的纵向约束矩阵;Obtain or update the longitudinal constraint matrix corresponding to the L1 norm constraint term of the electromagnetic response data;
将数据拟合梯度项、L1范数约束项、L2范数约束项构成目标函数,并求得对地层模型的增量求导等于零后的展开公式;The data fitting gradient term, the L1 norm constraint term, and the L2 norm constraint term constitute the objective function, and the expansion formula after the incremental derivation of the formation model is equal to zero is obtained;
利用展开公式反演计算求得地层模型增量并修正地层模型,达到迭代终止条件后获得反演成像图像。The formation model increment is obtained by inversion calculation using the expansion formula, and the formation model is corrected, and the inversion imaging image is obtained after the iteration termination condition is reached.
第二部分,本发明提供了一种半航空瞬变电磁数据反演装置,其包括:The second part, the present invention provides a semi-aviation transient electromagnetic data inversion device, which includes:
电磁信号激发模块,安装在待测的地质区域,并激发发射瞬变电磁信号;The electromagnetic signal excitation module is installed in the geological area to be measured, and stimulates and emits transient electromagnetic signals;
电磁信号接收装置,与电磁信号激发模块耦合,搭载在无人机上,并采集电磁响应数据;The electromagnetic signal receiving device is coupled with the electromagnetic signal excitation module, mounted on the drone, and collects electromagnetic response data;
地层模型构建模块,获取地层信息并构建地层模型;Stratigraphic model building module, obtain stratigraphic information and build stratigraphic model;
地层模型修正模块,与地层模型构建模块连接,并采用数据拟合梯度项、L1范数约束项、L2范数约束项进行修正,利用修正后的地层模型进行反演。The stratigraphic model correction module is connected to the stratigraphic model building module, and uses the data fitting gradient term, the L1 norm constraint term, and the L2 norm constraint term for correction, and uses the corrected stratigraphic model for inversion.
第三部分,本发明提供了一种计算机可读存储介质,其存储有计算机程序,所述计算机程序被处理器执行时,实现基于L1L2混合范数的半航空瞬变电磁数据反演方法的步骤。The third part, the present invention provides a computer-readable storage medium, which stores a computer program, and when the computer program is executed by a processor, realizes the steps of a semi-aviation transient electromagnetic data inversion method based on L1L2 hybrid norm .
与现有技术相比,本发明具有以下有益效果:Compared with the prior art, the present invention has the following beneficial effects:
(1)本发明采用地面发射瞬变电磁信号,并利用无人机搭载接收装置获取电磁响应数据,其具有精度更高、实施方便、成本更低、安全性好的优点;还具有勘探速度快,可以跨越障碍勘探的优点。本发明在城市地下空间探测、地面地质调查、矿产资源勘查、环境监测领域具有广阔的应用前景。(1) The present invention adopts the ground-transmitting transient electromagnetic signal, and uses the UAV to carry the receiving device to obtain the electromagnetic response data, which has the advantages of higher precision, convenient implementation, lower cost, and good safety; it also has the advantages of fast exploration speed , the advantages of exploration that can overcome obstacles. The invention has broad application prospects in the fields of urban underground space detection, ground geological survey, mineral resource exploration and environmental monitoring.
(2)本发明考虑测点电阻率分布的纵向空间约束(正则项)采用L1范数,而在横向空间约束采用L2范数的反演方法。它的目标函数中,包含了L1范数和L2范数两种约束项,分别考虑了地层垂直方向各层之间的参数相互约束即纵向约束和相临测点之间各地层的横向约束两个方面的问题,反演结果相较于一般方法的结果在地层横向上更连续,而在纵向上对地层的识别更准确。(2) The present invention adopts the L1 norm for the vertical space constraint (regular term) of the resistivity distribution of the measuring point, and the inversion method of the L2 norm for the lateral space constraint. Its objective function includes two constraints, the L1 norm and the L2 norm, which respectively consider the parameter mutual constraints between the layers in the vertical direction of the stratum, that is, the vertical constraints and the lateral constraints between the adjacent measurement points. Compared with the results of the general method, the inversion results are more continuous in the horizontal direction of the formation, and the identification of the formation in the vertical direction is more accurate.
(3)本发明采用自适应的正则化因子来调节约束项的权重,使得反演的拟合精度更高,迭代更加稳定。(3) The present invention adopts an adaptive regularization factor to adjust the weight of the constraint term, so that the inversion has higher fitting precision and more stable iteration.
(4)本发明对含约束躁数据反演迭代稳定,能够清晰分辨地层电性界面,弥补当今半航空时间域电磁探测数据反演解释系统的缺陷。(4) The invention is iteratively stable for the inversion of constrained data, can clearly distinguish the electrical interface of the formation, and makes up for the defects of the current semi-aviation time domain electromagnetic detection data inversion and interpretation system.
综上所述,本发明具有逻辑简单、准确可靠、探测高效等优点,在地球物理航空电磁勘探技术领域具有很高的实用价值和推广价值。To sum up, the present invention has the advantages of simple logic, accuracy and reliability, high detection efficiency, etc., and has high practical value and promotion value in the technical field of geophysical aviation electromagnetic exploration.
附图说明Description of drawings
为了更清楚地说明本发明实施例的技术方案,下面将对实施例中所需使用的附图作简单介绍,应当理解,以下附图仅示出了本发明的某些实施例,因此不应被看作是对保护范围的限定,对于本领域技术人员来说,在不付出创造性劳动的前提下,还可以根据这些附图获得其他相关的附图。In order to illustrate the technical solutions of the embodiments of the present invention more clearly, the following briefly introduces the accompanying drawings used in the embodiments. It should be understood that the following drawings only show some embodiments of the present invention, and therefore should not be It is regarded as a limitation on the protection scope, and for those skilled in the art, other related drawings can also be obtained according to these drawings without any creative effort.
图1为本发明的逻辑流程图。FIG. 1 is a logic flow diagram of the present invention.
图2为本发明中某地区的地下水低阻异常反演结果。Figure 2 shows the inversion results of groundwater low-resistance anomalies in a certain area in the present invention.
图3为本发明中某地区的理论模型与反演结果对比图。FIG. 3 is a comparison diagram of the theoretical model and inversion results of a certain region in the present invention.
图4为本发明中某地区实测数据反演成像图。FIG. 4 is an inversion imaging diagram of measured data in a certain area in the present invention.
具体实施方式Detailed ways
为使本申请的目的、技术方案和优点更为清楚,下面结合附图和实施例对本发明作进一步说明,本发明的实施方式包括但不限于下列实施例。基于本申请中的实施例,本领域普通技术人员在没有做出创造性劳动的前提下所获得的所有其他实施例,都属于本申请保护的范围。In order to make the purpose, technical solutions and advantages of the present application clearer, the present invention will be further described below with reference to the accompanying drawings and examples. The embodiments of the present invention include but are not limited to the following examples. Based on the embodiments in the present application, all other embodiments obtained by those of ordinary skill in the art without creative work shall fall within the protection scope of the present application.
实施例1Example 1
如图1所示,本实施例提供了基于L1L2混合范数的半航空瞬变电磁数据反演方法及装置,具体来说,本实施例的装置包括:电磁信号激发模块、电磁信号接收装置、地层模型构建模块和地层模型修正模块;其中,电磁信号激发模块安装在待测的地质区域,并激发发射瞬变电磁信号。另外,电磁信号接收装置,与电磁信号激发模块耦合,搭载在无人机上,并采集电磁响应数据;地层模型构建模块,获取地层信息并构建地层模型;地层模型修正模块,与地层模型构建模块连接,并采用数据拟合梯度项、L1范数约束项、L2范数约束项进行修正,利用修正后的地层模型进行反演。As shown in FIG. 1 , this embodiment provides a method and device for inversion of semi-aviation transient electromagnetic data based on L1L2 hybrid norm. Specifically, the device in this embodiment includes: an electromagnetic signal excitation module, an electromagnetic signal receiving device, A stratigraphic model building module and a stratigraphic model correction module; wherein, the electromagnetic signal excitation module is installed in the geological region to be measured, and stimulates and emits transient electromagnetic signals. In addition, the electromagnetic signal receiving device, coupled with the electromagnetic signal excitation module, is mounted on the UAV and collects electromagnetic response data; the formation model building module obtains formation information and constructs the formation model; the formation model correction module is connected with the formation model building module , and use the data fitting gradient term, L1 norm constraint term, L2 norm constraint term for correction, and use the corrected stratigraphic model for inversion.
在本实施例中,该半航空瞬变电磁数据反演方法包括以下步骤:In this embodiment, the semi-aviation transient electromagnetic data inversion method includes the following steps:
第一步,利用接收装置采集待测区域的电磁响应数据,其中,还包括以下基础信息:接收线圈面积、线源长度、单条测线的测点数、总测线数、电流峰值、抽道时间数、抽道时间;依次获取参与运算的的所有测点的x、y坐标、高程、各时间道对应的响应值。The first step is to use the receiving device to collect the electromagnetic response data of the area to be measured, which also includes the following basic information: the area of the receiving coil, the length of the line source, the number of measurement points of a single measurement line, the total number of measurement lines, the current peak value, and the extraction time. number and channel extraction time; sequentially obtain the x, y coordinates, elevations, and corresponding response values of each time channel of all measuring points involved in the operation.
第二步,根据实际工作场所构建待检测区域的地层模型,并预设迭代终止条件。其中,地层模型的参数包括总地层数、总地层厚度、起始地层厚度、任一层的电阻率。另外,迭代终止条件包括最大迭代次数和最小拟合误差。In the second step, the stratigraphic model of the area to be detected is constructed according to the actual workplace, and the iteration termination conditions are preset. The parameters of the formation model include the total number of formations, the total formation thickness, the initial formation thickness, and the resistivity of any layer. In addition, the iteration termination conditions include the maximum number of iterations and the minimum fitting error.
第三步,求得电磁响应数据的L2范数约束项对应的横向约束加权矩阵;求得或更新电磁响应数据的L1范数约束项对应的纵向约束矩阵;将数据拟合梯度项、L1范数约束项、L2范数约束项构成目标函数并对模型增量求导等于零后展开公式,利用展开公式反演计算求得模型增量并修正模型,达到迭代终止条件后获得反演成像图像The third step is to obtain the transverse constraint weighting matrix corresponding to the L2 norm constraint term of the electromagnetic response data; obtain or update the longitudinal constraint matrix corresponding to the L1 norm constraint term of the electromagnetic response data; fit the data to the gradient term, L1 norm term The number constraint term and the L2 norm constraint term constitute the objective function, and after the model increment is derived to be equal to zero, the formula is expanded, and the model increment is obtained by inversion calculation using the expansion formula and the model is corrected. After reaching the iteration termination condition, the inversion imaging image is obtained.
具体来说:Specifically:
(1)正演响应计算(1) Forward Response Calculation
半航空瞬变电磁勘探中,接收线圈主要接收的是磁场Hz分量,本实施例中正演响应基于分析水平层状垂直分量Hz:In the semi-aviation transient electromagnetic survey, the receiving coil mainly receives the magnetic field Hz component. In this embodiment, the forward response is based on analyzing the horizontal layered vertical component Hz :
进行频时转换,得到磁场强度关于时间的变化率:Perform frequency-time conversion to get the rate of change of the magnetic field strength with respect to time:
求得感应电动势,其表达式为:To obtain the induced electromotive force, its expression is:
式子中,Hz(w)表示垂直分量的频率域磁场响应(A/m);w表示采样角频率(rad/s);I表示电流强度(A);设定导线源的中心位于坐标原点,沿x轴向两侧延伸至L和-L;R表示偏移距;rTE表示TE模式下的反射系数;k0表示空气介质波数;z表示线圈接收高度(m);J1表示一阶Bessel函数与前面雅可比矩阵不一样;λ表示积分变量;In the formula, H z (w) represents the frequency domain magnetic field response of the vertical component (A/m); w represents the sampling angular frequency (rad/s); I represents the current intensity (A); the center of the wire source is set at the coordinate The origin, extending to L and -L on both sides of the x-axis; R represents the offset distance; r TE represents the reflection coefficient in TE mode; k 0 represents the air medium wave number; z represents the coil receiving height (m); J 1 represents The first-order Bessel function is different from the previous Jacobian matrix; λ represents the integral variable;
式中,ReHz(wj)表示取Hz(wj)的实部;N表示线圈匝数;S表示线圈的有效面积(m2);μ0表示真空下的磁导率(4π×10-7H/m)。In the formula, ReHz(w j ) represents the real part of Hz(w j ); N represents the number of turns of the coil; S represents the effective area of the coil (m 2 ); μ 0 represents the magnetic permeability under vacuum (4π×10 − 7 H/m).
采用余弦变换将频率域响应Hz(w)变换成时间域响应Vz(t)。The frequency domain response H z (w) is transformed into the time domain response V z (t) using a cosine transform.
(2)反演成像方法(2) Inversion imaging method
基于混合范数的半航空瞬变电磁数据反演方法是基于拟合观测数据,同时获得最理想的约束模型的一种最优化反演算法,其基本思路是把地下介质分成多层层状结构,把每层厚度加入模型约束函数,即粗糙度矩阵,通过计算得到每层电阻率,从而构建地下地电结构。其总目标函数可归结为:The semi-airborne transient electromagnetic data inversion method based on hybrid norm is an optimal inversion algorithm based on fitting observation data and obtaining the most ideal constraint model. The basic idea is to divide the underground medium into multi-layered layered structures. , the thickness of each layer is added to the model constraint function, that is, the roughness matrix, and the resistivity of each layer is obtained through calculation, thereby constructing the underground geoelectric structure. Its overall objective function can be summed up as:
展开为expands to
式中:φ(m)表示总目标函数;λ表示正则化因子;φm(m)表示模型约束目标函数;φd(m)表示观测数据目标函数;M表示模型向量可表示为公式(3);σ表示电阻率。In the formula : φ( m ) represents the total objective function; λ represents the regularization factor; φm(m) represents the model constraint objective function; φd(m) represents the observation data objective function; M represents the model vector, which can be expressed as formula (3 ); σ represents resistivity.
M=[σ11,σ12…σ1p…σi1,σi2,…σip…σn1,σn2…σnp]T (6)M=[σ 11 ,σ 12 …σ 1p …σ i1 ,σ i2 ,…σ ip …σ n1 ,σ n2 …σ np ] T (6)
公式(5)右边其中第一项数据拟合项,F(M)表示模型向量M的正演响应,Wd一般为主对角矩阵,其元素为观测数据噪声的倒数;第二项为模型垂向约束项也称正则惩罚项,Wm为模型垂向约束矩阵,本实施例采用模型约束项为:The first item on the right side of formula (5) is the data fitting item, F(M) represents the forward response of the model vector M, W d is generally a main diagonal matrix, and its elements are the reciprocal of the observed data noise; the second item is the model The vertical constraint term is also called the regular penalty term, W m is the model vertical constraint matrix, and the model constraint term used in this embodiment is:
即单位一阶差分算子;第三项为模型横向约束项,本文考虑测点前后左右四个相邻测点约束项,Wh,i为横向约束矩阵,q表示约束项个数,同样采用一阶差分算子表示为:That is, the unit first-order difference operator; the third item is the lateral constraint item of the model. In this paper, four adjacent measurement point constraint items are considered, W h, i are the transverse constraint matrix, q represents the number of constraint items, and the same The first-order difference operator is expressed as:
由于L1范数存在不可导情况,会使迭代不稳定,正则项最速下降方向无法得到。可取一个小值ξ,将公式(5)改写如下:Since the L1 norm is non-derivable, the iteration will be unstable, and the direction of the fastest descent of the regular term cannot be obtained. A small value ξ can be taken, and formula (5) can be rewritten as follows:
采用迭代重加权最小二乘法(IRLS),可将L1正则项改写:Using iterative reweighted least squares (IRLS), the L1 regular term can be rewritten:
本实施例对这种算法做出改进,将L1正则项表示为:This embodiment improves this algorithm, and expresses the L1 regular term as:
其中,V为对角加权矩阵,主对角线上元素为:Among them, V is the diagonal weighting matrix, and the elements on the main diagonal are:
其中,V表示对角加权矩阵,xi表示加权模型向量元素ξ表示一个小值;XT表示加权模型向量矩阵的转置;X表示加权模型向量;表示纵向约束项粗糙度矩阵转置;Wm表示纵向约束粗糙度矩阵。Among them, V represents the diagonal weighting matrix, xi represents the weighted model vector element ξ represents a small value; X T represents the transpose of the weighted model vector matrix; X represents the weighted model vector; represents the transposition of the longitudinal constraint item roughness matrix; W m represents the longitudinal constraint roughness matrix.
L2范数约束项中加权矩阵D展开为:The weight matrix D in the L2 norm constraint is expanded as:
其中,r表示横向约束项加权矩阵对角元素;n表示第n个测点;p表示测点n的第p个临点。Among them, r represents the diagonal element of the transverse constraint weighting matrix; n represents the nth measurement point; p represents the pth adjacent point of the measurement point n.
可根据实际情况考虑不同对角线加权元素,采用距离加权时这里x和y是所计算的测点到参与计算的相临点之间的相对坐标,这里计算的两点之间的距离取倒数。若不考虑加权,ri取对角元素为1。最后计算项并加入目标函数。Different diagonal weighting elements can be considered according to the actual situation, when distance weighting is used Here x and y are the relative coordinates between the calculated measuring point and the adjacent points involved in the calculation, and the distance between the two points calculated here is the reciprocal. If weighting is not considered, ri takes the diagonal element as 1. final calculation term and add the objective function.
关于模型修正量Δmk求导,并令求导后的式子等于0,得到模型修正量的求解公式:Take the derivation of the model correction amount Δm k , and set the derived formula equal to 0 to obtain the solution formula of the model correction amount:
其中,右边第一项为数据拟合梯度项,第二项为L1范数垂向空间约束项,第三项为L2范数横向空间约束项(正则化梯度项)。另外,表示雅可比矩阵转置;表示数据拟合项粗糙度矩阵转置;Wd表示数据拟合项粗糙度矩阵;dobs表示实测响应数据;F(Mk)表示模型向量正演计算项;λ1表示第一正则化因子;表示纵向约束项粗糙度矩阵转置;Vk表示纵向约束项加权矩阵;Wm表示纵向约束项粗糙度矩阵;Mk表示模型向量;λ2表示第二正则化因子;表示横向约束粗糙度矩阵转置;Di表示横向约束加权矩阵;Wh,i表示横向约束粗糙度矩阵。Among them, the first term on the right is the data fitting gradient term, the second term is the L1 norm vertical space constraint term, and the third term is the L2 norm lateral space constraint term (regularized gradient term). in addition, represents the transpose of the Jacobian matrix; represents the transposition of the data fitting item roughness matrix; W d represents the data fitting item roughness matrix; d obs represents the measured response data; F(M k ) represents the model vector forward calculation term; λ 1 represents the first regularization factor ; represents the longitudinal constraint term roughness matrix transposition; V k represents the longitudinal constraint term weighting matrix; W m represents the longitudinal constraint term roughness matrix; M k represents the model vector; λ 2 represents the second regularization factor; represents the transposition of the transverse constraint roughness matrix; D i represents the transverse constraint weight matrix; W h,i represents the transverse constraint roughness matrix.
第四步,采用自适应正则化因子调节L1范数约束项和L2范数约束项在反演过程中的权重;并利用修正后的地层模型进行反演,并获得反演成像图像。In the fourth step, the adaptive regularization factor is used to adjust the weight of the L1 norm constraint term and the L2 norm constraint term in the inversion process; and the modified stratigraphic model is used for inversion, and the inversion imaging image is obtained.
本实施例提供了正则化因子采用自适应调节方法,数据梯度项作为分子,五个模型约束梯度项作为分母。采用一个参数a分别调节λ1和λ2在目标函数中的权重,用于调节纵向约束项和横向约束项在迭代过程中的权重问题,其具体公式如下:This embodiment provides that the regularization factor adopts an adaptive adjustment method, the data gradient term is used as the numerator, and the five model constraint gradient terms are used as the denominator. A parameter a is used to adjust the weights of λ 1 and λ 2 in the objective function respectively, which are used to adjust the weights of the vertical and horizontal constraints in the iterative process. The specific formula is as follows:
其中,a表示权重比例参数;表示拟合数据梯度项;表示纵向约束梯度项;表示横向约束梯度项。Among them, a represents the weight ratio parameter; represents the fitted data gradient term; represents the longitudinal constraint gradient term; represents the laterally constrained gradient term.
实施例2Example 2
本实施例提供了一种计算机可读存储介质,其存储有计算机程序,所述计算机程序被处理器执行时,实现实施例1中的半航空瞬变电磁数据反演方法的步骤。This embodiment provides a computer-readable storage medium, which stores a computer program, and when the computer program is executed by a processor, implements the steps of the semi-aviation transient electromagnetic data inversion method in
实施例3Example 3
如图2至图3所示,本实施例以含噪声5%地下低阻模型数据反演为例:As shown in Figure 2 to Figure 3, this embodiment takes the data inversion of an underground low-resistance model with a noise of 5% as an example:
将无人机半航空瞬变电磁技术运用于模拟寻找地下水中,在背景电阻率为100Ω·m的高阻层(厚度240米)中设置10Ω·m的地下水低阻层(厚度60米),反演中以1.05为指数增长因子设置各层厚度,反演的初始模型为50Ω·m的均匀半空间。反演结果如图2所示。从图中可以看出总体来说该反演结果分成“高-低-高”三层,其中高阻分布于100Ω·m-110Ω·m之间,反演出的电阻率为10Ω·m左右,非常接近真实模型,无人机半航空瞬变电磁反演方法能有效的反演出低阻异常,对含噪声数据反演稳定,对电性界面刻画清晰。这说明半航空瞬变电磁对于低阻异常体反应敏感。The semi-aviation transient electromagnetic technology of unmanned aerial vehicle is used to simulate the search for groundwater, and a groundwater low-resistance layer (thickness 60m) of 10Ω·m is set in a high-resistance layer (thickness 240m) with a background resistivity of 100Ω·m. In the inversion, the thickness of each layer is set with an exponential growth factor of 1.05, and the initial model of the inversion is a uniform half-space of 50Ω·m. The inversion results are shown in Figure 2. It can be seen from the figure that the inversion result is generally divided into three layers of "high-low-high", in which the high resistance is distributed between 100Ω·m-110Ω·m, and the inversion resistivity is about 10Ω·m. Very close to the real model, the UAV semi-aviation transient electromagnetic inversion method can effectively invert low-resistance anomalies, inversion of noisy data is stable, and the electrical interface is clearly depicted. This shows that the semi-aviation transient electromagnetic is sensitive to low-resistance anomalies.
实施例4Example 4
如图4所示,本实施例以某地实测数据进行分析,将飞行探测数据进行简单处理后,采用均匀半空间作为初始模型,同时对多条测线进行反演结果如图所示。整体电阻率表现为低-高-低分布趋势,整体反演效果较好,该种方法反演速度较一维单点反演更快,从图中可以看出反演结果的连续性也较好,对电性界面的刻画非常清晰,并且对含噪声数据的反演迭代过程更加稳定。As shown in Figure 4, in this embodiment, the measured data of a certain place is used for analysis, and after simple processing of the flight detection data, the uniform half-space is used as the initial model, and the results of inversion of multiple survey lines are shown in the figure. The overall resistivity shows a low-high-low distribution trend, and the overall inversion effect is better. The inversion speed of this method is faster than that of the one-dimensional single-point inversion. It can be seen from the figure that the continuity of the inversion results is also better. Well, the characterization of the electrical interface is very clear, and the inversion iteration process for noisy data is more stable.
上述实施例仅为本发明的优选实施例,并非对本发明保护范围的限制,但凡采用本发明的设计原理,以及在此基础上进行非创造性劳动而作出的变化,均应属于本发明的保护范围之内。The above-mentioned embodiments are only the preferred embodiments of the present invention, and are not intended to limit the protection scope of the present invention. Any changes made by adopting the design principles of the present invention and non-creative work on this basis shall belong to the protection scope of the present invention. within.
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