CN111753247B - Method for acquiring horizontal layered soil grounding parameters by using segmented sampling - Google Patents
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Abstract
Description
技术领域technical field
本发明属于电力系统领域,特别涉及一种用分段采样获取水平分层土壤接地参数的方法。The invention belongs to the field of power systems, and in particular relates to a method for obtaining grounding parameters of horizontally layered soil by subsection sampling.
背景技术Background technique
接地装置是电力系统和电力设备安全稳定运行的前提。准确的接地参数计算为接地装置的设计及运维奠定了理论基础。接地装置埋设于土壤中,土壤介质的分层现象大幅度增加了接地参数的计算难度。因此,水平分层土壤介质中的接地参数计算一直是电力接地领域的一个焦点问题。The grounding device is the prerequisite for the safe and stable operation of the power system and power equipment. Accurate calculation of grounding parameters lays a theoretical foundation for the design, operation and maintenance of grounding devices. The grounding device is buried in the soil, and the stratification of the soil medium greatly increases the difficulty of calculating the grounding parameters. Therefore, the calculation of grounding parameters in horizontally stratified soil media has always been a focal issue in the field of electrical grounding.
目前,国内外相继开展许多研究主要仍是基于全局采样下的复镜像法对接地参数计算方法进行改进,并未从根本上解决全局采样导致的计算问题。全局采样通常并不能准确反演层数多、厚度大的复杂分层土壤格林函数的积分核函数,容易导致计算结果不准确或者完全不收敛等情况。此外,复镜像法个数为土壤层数2倍,存在计算量随着土壤层数线性增加的缺点。如以一个10层土壤为例,该土壤第1层值第10层的土壤电阻率为100,233,42.9,185.7,11.1,185.7,900,150,42.9,17.6,第1层到第9层的土壤厚度为2m,6m,33m,120m,188m,270m,301m,332m,368m,通过全局采样的方法完全无法拟合出积分核函数。At present, many researches at home and abroad are still mainly based on the complex image method under global sampling to improve the calculation method of grounding parameters, which has not fundamentally solved the calculation problem caused by global sampling. Global sampling usually cannot accurately invert the integral kernel function of the Green's function in complex stratified soil with many layers and large thickness, which may easily lead to inaccurate calculation results or no convergence at all. In addition, the number of complex mirror methods is twice the number of soil layers, and there is a disadvantage that the amount of calculation increases linearly with the number of soil layers. For example, taking a 10-layer soil as an example, the soil resistivity of the 10th layer of the soil is 100, 233, 42.9, 185.7, 11.1, 185.7, 900, 150, 42.9, 17.6, from the 1st layer to the 9th layer The soil thickness is 2m, 6m, 33m, 120m, 188m, 270m, 301m, 332m, 368m, and the integral kernel function cannot be fitted by the global sampling method at all.
发明内容Contents of the invention
现有分层土壤中接地参数的计算方法主要基于全局采样下的复镜像法。一方面,对于层数多、厚度大的复杂土壤模型,全局采样可能引起计算结果误差较大或不收敛等问题;另一方面,复镜像个数通常为土壤层数2倍,存在计算量总是随着土壤层数线性增加的问题。鉴于此,本发明提出一种水平分层土壤中接地参数的获取方法。通过分析水平分层土壤中格林函数的分段采样计算方法,研究了分层土壤中接地装置的接地参数计算。The existing calculation methods of grounding parameters in layered soils are mainly based on the complex image method under global sampling. On the one hand, for a complex soil model with many layers and large thickness, global sampling may cause problems such as large errors in calculation results or non-convergence; is a problem that increases linearly with the number of soil layers. In view of this, the present invention proposes a method for obtaining grounding parameters in horizontally layered soil. By analyzing the segmental sampling calculation method of Green's function in horizontal layered soil, the grounding parameters calculation of the grounding device in layered soil is studied.
本发明采用的技术方案,如下:The technical scheme that the present invention adopts is as follows:
一种用分段采样获取水平分层土壤接地参数的方法,包括以下步骤:A method for obtaining grounding parameters of horizontal layered soils by subsection sampling, comprising the following steps:
建立柱坐标系下的水平分层土壤计算模型,将土壤水平分为n层;Establish a horizontal layered soil calculation model under the cylindrical coordinate system, and divide the soil into n layers horizontally;
构建包含土壤分层结构参数的积分核函数,进一步构建第二积分核函数并根据第二积分核函数的极值点进行分段采样,在不同分段上进行3阶拟合,再通过积分变量替换,根据Bessel函数的积分性质并结合分部积分法求解上述积分,求得源点在第一层的土壤格林函数;Construct the integral kernel function including soil layer structure parameters, further construct the second integral kernel function and perform segmental sampling according to the extreme points of the second integral kernel function, perform third-order fitting on different segments, and then pass the integral variable Replacement, according to the integral nature of the Bessel function and combined with the integration by parts method to solve the above integral, obtain the soil Green's function whose source point is in the first layer;
将接地装置分为若干小段,在接地装置上定义两类节点:第一类节点为e类导体节点,认为外部注入电流是通过e类节点,第二类节点为m类对地节点,该节点上仅存在泄漏电流;Divide the grounding device into several small sections, and define two types of nodes on the grounding device: the first type of node is the e-type conductor node, and it is considered that the external injection current passes through the e-type node, and the second type of node is the m-type grounding node. There is only leakage current on the
采用节点电压法,建立含e类节点和m类节点的节点电压方程和仅对m类节点的电压方程;Using the node voltage method, establish the node voltage equation including e-type nodes and m-type nodes and the voltage equation only for m-type nodes;
根据以上两组节点电压方程,求解出接地网上任意节点的电位,进一步求得每个m类节点的泄露电流Imi;According to the above two sets of node voltage equations, the potential of any node on the grounding grid is solved, and the leakage current I mi of each m-type node is further obtained;
将每段的泄露电流Imi视作点源,结合第一层的土壤格林函数,采用叠加原理则求得接地装置的接地电阻和地表电位分布。The leakage current I mi of each section is regarded as a point source, combined with the soil Green's function of the first layer, and the superposition principle is used to obtain the grounding resistance and surface potential distribution of the grounding device.
本发明还计算了典型接地装置在3种典型分层土壤中的接地参数,并对比CDEGS的计算结果,验证了本发明工作的有效性和准确性。The present invention also calculates the grounding parameters of typical grounding devices in three typical layered soils, and compares the calculation results of CDEGS to verify the effectiveness and accuracy of the work of the present invention.
本发明提出的水平分层土壤中接地参数的分段采样数值计算方法,根据积分核函数极值点进行分段采样,避免了传统复镜像法中计算量是随土壤层数线性增加的不足,具有更高的计算效率。如在计算土壤电阻率具有单调性的接地电阻时,无论土壤层数有多少,只要积分核函数F(λ)没有出现极值点,仅需要固定数量的采样点,计算量不会增加。The segmental sampling numerical calculation method of the grounding parameters in the horizontal layered soil proposed by the present invention performs segmental sampling according to the extremum point of the integral kernel function, avoiding the deficiency that the amount of calculation increases linearly with the number of soil layers in the traditional complex image method, It has higher computational efficiency. For example, when calculating the grounding resistance with monotonic soil resistivity, no matter how many soil layers there are, as long as the integral kernel function F(λ) does not have an extreme point, only a fixed number of sampling points are needed, and the calculation amount will not increase.
全局采样方法并不适用与土壤分层厚度较厚的情况,当土壤分层厚度过厚容易导致采样步长过小,从而引起计算结果发散。此外,实际土壤分层复杂多变,采用全局采样的方式无法避免漏掉积分核函数的关键特征。分段采样后可更准确地计算任意复杂水平分层土壤中的接地参数,具有更强的适应性。The global sampling method is not suitable for thicker soil layers. When the soil layer thickness is too thick, the sampling step size is too small, which will cause the calculation results to diverge. In addition, the actual soil stratification is complex and changeable, and the global sampling method cannot avoid missing the key features of the integral kernel function. After subsection sampling, the grounding parameters in any complex horizontal layered soil can be calculated more accurately, and it has stronger adaptability.
在接地参数的计算中,将接地装置分为若干小段且定义了m和e类节。e类节点为每一段的两个端部节点,认为外部注入电流是通过e类节点,m类节点为每一段的中点处,且该节点上仅存在泄漏电流,不与外部电气设备发生连接,无外部电流注入。这样处理使得不同节点之间具有微小的电位差,解决了实际中不同节点是不等电位的问题。In the calculation of the grounding parameters, the grounding device is divided into several small sections and the m and e sections are defined. The e-type nodes are the two end nodes of each section. It is considered that the external injection current passes through the e-type nodes, and the m-type nodes are at the midpoint of each section, and there is only leakage current on this node, and it is not connected to external electrical equipment. , no external current injection. Such processing makes there be a slight potential difference between different nodes, which solves the problem that different nodes are not equipotential in practice.
本发明提出的计算方法为分层土壤介质中接地装置的设计和接地参数准确计算奠定了夯实的理论基础。The calculation method proposed by the invention lays a solid theoretical foundation for the design of the grounding device and the accurate calculation of the grounding parameters in the layered soil medium.
附图说明Description of drawings
图1是分层土壤中的格林函数;Figure 1 is the Green's function in stratified soil;
图2是F(λ)的分布;Figure 2 is the distribution of F(λ);
图3是矩形方框接地网实际模型;Fig. 3 is the actual model of the rectangular frame grounding grid;
图4是矩形方框接地网电路模型;Fig. 4 is a rectangular box ground grid circuit model;
图5是水平接地极的计算模型;Figure 5 is the calculation model of the horizontal ground electrode;
图6是水平接地极泄露电流计算。Figure 6 is the calculation of the leakage current of the horizontal ground electrode.
具体实施方式Detailed ways
下面给出一个非限定性实例,对本发明方法作进一步说明。A non-limiting example is given below to further illustrate the method of the present invention.
下面对本发明的方法进行具体分析:The method of the present invention is concretely analyzed below:
(1)水平分层土壤中格林函数的建立(1) Establishment of Green's function in horizontally stratified soil
根据基本电磁场理论,建立柱坐标系下的水平分层土壤计算模型如图1所示。采用求解空间泊松方程的方法,第i层土壤中任意一点的电位方程:According to the basic electromagnetic field theory, a horizontally layered soil calculation model in the cylindrical coordinate system is established, as shown in Figure 1. Using the method of solving the spatial Poisson equation, the potential equation of any point in the i-th layer of soil:
式(1)中,δ为土壤介质中位于第1层土壤的点电流源,ρ1为点电流源所在的第1层土壤的电阻率。为土壤中任一点的电位,r,z为柱坐标系下r,z方向的坐标。In formula (1), δ is the point current source located in the first layer of soil in the soil medium, and ρ1 is the resistivity of the first layer of soil where the point current source is located. is the potential of any point in the soil, and r and z are the coordinates in the r and z directions in the cylindrical coordinate system.
分层土壤边界条件为:The layered soil boundary conditions are:
为第一层土壤分界面的电位,/>为第i层土壤分界面的电位,h0为源点距地表的垂直距离,hi为第i层土壤下侧分界面在地表下的垂直距离,ρi表示第i层土壤的电阻率,i=1,2,3……n,n为土壤层数。 is the potential at the interface of the first layer of soil, /> is the potential of the i-th layer soil interface, h 0 is the vertical distance from the source point to the surface, h i is the vertical distance of the i-th layer soil lower interface below the surface, ρi represents the resistivity of the i-th layer soil, i=1,2,3...n, n is the number of soil layers.
采用柱坐标下的分离变量法,可将式(1)写成如下通式:Using the method of separating variables in cylindrical coordinates, formula (1) can be written as the following general formula:
其中为源点在第1层土壤中的电位,J0(λr)为第一类贝塞尔函数,Ai(λ,X)和Bi(λ,X)为积分核函数,X为分层土壤的电阻率和厚度,λ为积分常数。in is the potential of the source point in the first layer of soil, J 0 (λr) is the Bessel function of the first kind, A i (λ,X) and B i (λ,X) are integral kernel functions, and X is the layered The resistivity and thickness of the soil, λ is the integral constant.
当源点位于第1层土壤时,可将式(3)改写为:When the source point is located in the first layer of soil, formula (3) can be rewritten as:
其中,G1(r,z)为源点在第一层土壤的格林函数,h0源点的埋深,f(λ)为包含土壤分层结构参数的积分核函数。Among them, G 1 (r,z) is the Green's function whose source point is in the first layer of soil, h 0 is the buried depth of the source point, and f(λ) is the integral kernel function including the soil layer structure parameters.
f(λ)表达式为:The expression of f(λ) is:
(2)格林函数的分段采样计算(2) Segmented sampling calculation of Green's function
定义新的积分核函数(即第二积分核函数)F(λ):Define a new integral kernel function (that is, the second integral kernel function) F(λ):
F(λ)随着土壤层数的增加,并无法得到其解析表达式。为保证近似表达式能够很好的逼近实际的函数F(λ),需要研究F(λ)的分布规律,z0为场点距离点源的垂直距离。As the number of soil layers increases, F(λ) cannot obtain its analytical expression. In order to ensure that the approximate expression can well approximate the actual function F(λ), the distribution law of F(λ) needs to be studied, and z 0 is the vertical distance between the field point and the point source.
令点源埋深h0为0.8m,z0为0.006m(将电位的计算位置选择在半径为0.006m的圆钢接地导体表面)。选取土壤电阻率具有单调性的水平2层土壤到水平5层土壤,计算分层土壤的F(λ)。Let the point source buried depth h0 be 0.8m, z0 be 0.006m (choose the calculation position of the potential on the surface of the round steel grounding conductor with a radius of 0.006m). Select horizontal 2-layer soil to horizontal 5-layer soil with monotonic soil resistivity, and calculate F(λ) of layered soil.
其中水平5层土壤参数ρ1=50,ρ2=100,ρ3=150,ρ4=200,ρ5=250,h1=2,h2=1,h3=1.5,h4=1,水平4层土壤参数为ρ1,ρ2,ρ3,ρ4和h1,h2,h3,2层土壤和3层土壤以此类推。复杂水平8层土壤的参数为ρ1=100,ρ2=550,ρ3=250,ρ4=190,ρ5=30,ρ6=900,ρ7=350,ρ8=50,h1=2,h2=10,h3=30,h4=130,h5=50,h6=350,h7=450。计算结果如附图2所示。Among them, soil parameters of horizontal 5 layers ρ 1 =50, ρ 2 =100, ρ 3 =150, ρ 4 =200, ρ 5 =250, h 1 =2, h 2 =1, h 3 =1.5, h 4 =1 , the horizontal 4-layer soil parameters are ρ 1 , ρ 2 , ρ 3 , ρ 4 and h 1 , h 2 , h 3 , and so on for 2-layer soil and 3-layer soil. The parameters of complex horizontal 8-layer soil are ρ 1 =100, ρ 2 =550, ρ 3 =250, ρ 4 =190, ρ 5 =30, ρ 6 =900, ρ 7 =350, ρ 8 =50, h 1 =2, h 2 =10, h 3 =30, h 4 =130, h 5 =50, h 6 =350, h 7 =450. The calculation results are shown in Figure 2.
图2表明1)F(λ)在土壤电阻率单调时,任意多层土壤的F(λ)分布规律均与水平2层相似;2)复杂分层土壤的F(λ)分布是可能存在多个极值点。Figure 2 shows that 1) when F(λ) is monotonous in soil resistivity, the distribution of F(λ) in any multi-layered soil is similar to that of horizontal 2 layers; 2) the distribution of F(λ) in complex layered soil may have multiple an extreme point.
根据F(λ)的极值点对F(λ)进行分段采样,然后采用3阶最小二乘法对第i分段上的Fi(λ)进行拟合,可得:According to the extreme points of F(λ), the F(λ) is sampled in sections, and then the third-order least square method is used to fit the F i (λ) on the i-th segment, which can be obtained as follows:
ak为拟合多项式中每一项的系数。a k is the coefficient of each term in the fitted polynomial.
分层土壤中的格林函数转化为:The Green's function in stratified soils translates to:
其中λ0为0,λn为F(λ)为0.01或者-0.01处λ的值,λ>λn时可认为F(λ)恒等于0。Where λ 0 is 0, and λ n is the value of λ when F(λ) is 0.01 or -0.01. When λ>λ n , it can be considered that F(λ) is always equal to 0.
令x=λr替换积分变量,根据Bessel函数的积分性质并结合分部积分法可求解上述积分,从而求得源点在第1层的分层土壤的格林函数G(r)。Let x=λr replace the integral variable, and according to the integral properties of the Bessel function combined with the integration by parts method, the above integral can be solved, so as to obtain the Green's function G(r) of the stratified soil whose source point is in the first layer.
(3)分段采样接地参数数值计算(3) Numerical calculation of segmental sampling grounding parameters
定义两类节点,第一类节点为e类导体节点,该节点为每一段的两个端部节点,认为外部注入电流是通过e类节点。第二类节点为m类对地(泄漏电流)节点,该节点为每一段的中点处,且该节点上仅存在泄漏电流,不与外部电气设备发生连接,无外部电流注入。Two types of nodes are defined. The first type of node is the e-type conductor node, which is the two end nodes of each segment, and the external injection current is considered to pass through the e-type node. The second type of node is the m-type ground (leakage current) node, which is the midpoint of each segment, and there is only leakage current on this node, no connection with external electrical equipment, and no external current injection.
以矩形方框接地网为例,分段数为4段,分段和实际矩形框边长保持一致,方框的四个角为外部电流注入的e类节点;电流从每一分段的中点流出,分段中点应为4个m类节点。方框接地网的分析模型如附图3和4所示。Taking the rectangular frame grounding grid as an example, the number of segments is 4 segments, and the segment length is consistent with the actual rectangular frame side length. The four corners of the frame are e-type nodes for external current injection; Points flow out, and the midpoint of the segment should be 4 m-type nodes. The analysis model of the frame ground grid is shown in Figures 3 and 4.
根据图4列写出关于所有e类节点和m类节点的节点电压方程:Write out the node voltage equations for all e-type nodes and m-type nodes according to the column in Figure 4:
其中,Yj,i为节点j和节点i的互导纳,Yj,j为节点j的自导纳,Iei为e类节点ei上的注入电流,Imi为m类节点mi上的泄漏电流。在接地网的计算过程中,Iei通常为接地电气设备的入地电流,可通过测量得到,但接地网上的泄露电流Imi为未知量,并且无法通过测量得到。为消去泄露电流变量,应仅对m类节点可列写如下节点电压方程:Among them, Y j,i is the mutual admittance between node j and node i, Y j,j is the self-admittance of node j, I ei is the injected current on the e-type node ei, I mi is the m-type node mi on leakage current. In the calculation process of the grounding grid, I ei is usually the grounding current of the grounding electrical equipment, which can be obtained by measurement, but the leakage current I mi of the grounding grid is an unknown quantity and cannot be obtained by measurement. In order to eliminate the leakage current variable, the following node voltage equation should be written only for m-type nodes:
Rj,i为m类节点的互电阻,Rj,j为m类节点的自电阻。R j,i is the mutual resistance of m-type nodes, and R j,j is the self-resistance of m-type nodes.
联立式(10)(11)消去泄露电流Imi,得到所有节点电压和注入电流Iei的矩阵方程。The simultaneous formula (10) (11) eliminates the leakage current I mi , and obtains the matrix equations of all node voltages and injection current I ei .
上述分析是以简单节点的电网络模型,可将式(10)(11)推广至任意节点得:The above analysis is based on the electrical network model of simple nodes, and formulas (10) (11) can be extended to any node:
RIm=Um (13)RI m =U m (13)
其中Yee和Ymm分别为e类节点的自导和m类节点的自导,Yem和Yme相等,为e类节点和m类节点的互导。Ue为e类节点的节点电压,Um为m类节点的节点电压,Ie表示e类节点的注入电流,Im表示m类节点的泄露电流,R为m类节点的互电阻或自电阻。Among them, Y ee and Y mm are the self-guidance of e-type nodes and m-type nodes respectively, and Y em and Y me are equal, which are the mutual conductance of e-type nodes and m-type nodes. U e is the node voltage of e-type nodes, U m is the node voltage of m-type nodes, I e is the injection current of e-type nodes, I m is the leakage current of m-type nodes, R is the mutual resistance or self-resistance of m-type nodes resistance.
联立式(12)(13)可得:Simultaneous formula (12) (13) can get:
根据式(14)可求解出接地网上任意节点的电位,进一步根据式(11)可求得每个m类节点的泄露电流Imi。将每段的泄露电流Imi视作点源,采用叠加原理则可求得任意接地装置的接地电阻和地表电位分布。上述计算可实现不等电位任意接地装置的接地参数计算。According to formula (14), the potential of any node on the grounding grid can be obtained, and further according to formula (11), the leakage current I mi of each type m node can be obtained. The leakage current I mi of each segment is regarded as a point source, and the grounding resistance and ground potential distribution of any grounding device can be obtained by using the superposition principle. The above calculation can realize the calculation of the grounding parameters of any grounding device with different potentials.
本发明主要针对接地装置的低频稳态特性,忽略接地装置的感性部分,式(14)中的导纳变为了电导。目标节点和相邻的节点通过接地导体连接,和其他节点是通过土壤介质连接。导体的电导远大于土壤介质的电导,节点的自电导可近似认为是相邻分段金属导体的电导,可得m类节点的自电导和互电导为:The present invention mainly aims at the low-frequency steady-state characteristics of the grounding device, ignoring the inductive part of the grounding device, and the admittance in formula (14) becomes conductance. The target node is connected to the adjacent nodes through the ground conductor, and the other nodes are connected through the soil medium. The conductance of the conductor is much greater than that of the soil medium, and the self-conductance of the node can be approximately considered as the conductance of the adjacent segmented metal conductor. The self-conductance and mutual conductance of the m-type nodes can be obtained as:
其中,ρ为金属导体电阻率,S为导体截面积,l为分段导体长度,为导体电导率。Among them, ρ is the resistivity of the metal conductor, S is the cross-sectional area of the conductor, l is the length of the segmented conductor, and is the conductivity of the conductor.
e类节点的自电导为:The self-conductance of the e-type node is:
其中,N表示总共有N段导体与端部节点e连接,ρi连接在节点e上的第i段导体的电阻率,Si为第i段导体截面积,li为第i段导体的长度。Among them, N represents a total of N segments of conductors connected to the end node e, ρ i is the resistivity of the i-th segment conductor connected to node e, S i is the cross-sectional area of the i-th segment conductor, l i is the i-th segment conductor's length.
目标节点和非相邻节点的互电导,则需通过分层土壤中点源的格林函数求解。点电流源的物理意义是微段上的线电流密度,前已假设电流在每一分段上均匀分布。匹配点选择在每一分段中点处,源点段在匹配点处产生的互电阻为:The mutual conductance of the target node and non-adjacent nodes needs to be solved by the Green's function of the point source in the layered soil. The physical meaning of the point current source is the linear current density on the micro-segment, and it has been assumed that the current is uniformly distributed on each segment. The matching point is selected at the midpoint of each segment, and the mutual resistance generated by the source segment at the matching point is:
其中Ii为第i段的泄露电流,单位为A,li为第i分段的长度,ds为对源点微段li的曲线积分。G为分层土壤的格林函数,rj为第j个分段中点的位置向量,ri为第i个分段中点的位置向量。Among them, I i is the leakage current of the i-th segment, and the unit is A, l i is the length of the i-th segment, and ds is the curve integral of the micro-segment l i of the source point. G is the Green's function of the layered soil, r j is the position vector of the midpoint of the jth segment, and r i is the position vector of the midpoint of the ith segment.
为了进一步提高计算精度,通常将源点段在匹配点段处产生的电位平均值作为匹配点的电位系数,其表达式需要对匹配点所在微段进行一次积分并求平均值,如下:In order to further improve the calculation accuracy, the average potential generated by the source point segment at the matching point segment is usually used as the potential coefficient of the matching point, and its expression needs to be integrated and averaged once for the micro-segment where the matching point is located, as follows:
其中lj为匹配点所在微段的长度。Where l j is the length of the micro-segment where the matching point is located.
本实时例以水平接地极在三种不同水平分层土壤中的泄露电流分布和接地电阻计算为例,不同分层土壤的参数如表1所示。In this real-time example, the leakage current distribution and grounding resistance calculation of the horizontal ground electrode in three different horizontal layered soils is taken as an example. The parameters of different layered soils are shown in Table 1.
1、水平接地极直径为12mm,故半径r0=0.006m=z0,埋深为0.8m,故h0=0.8m。将h0和z0代入式(7)可以得到具体的积分核函数。以较小步长对进行采样,得到该核函数对应的所有极值点。然后采用3阶最小二乘法对第i分段上的Fi(λ)进行拟合,并通过替换积分变量,再根据Bessel函数的积分性质并结合分部积分法,从而求得源点在第1层的分层土壤的格林函数G(r)。1. The diameter of the horizontal grounding pole is 12mm, so the radius r 0 =0.006m=z 0 , and the buried depth is 0.8m, so h 0 =0.8m. The specific integral kernel function can be obtained by substituting h 0 and z 0 into formula (7). Sampling with a smaller step size to get all the extreme points corresponding to the kernel function. Then use the third-order least squares method to fit F i (λ) on the i-th segment, and replace the integral variable, and then according to the integral properties of the Bessel function and the integration by parts method, the source point at Green's function G(r) for layer 1 stratified soil.
2、水平接地极长度10m,分为10段,即m类节点编号从1到10,1A电流从1号m类节点的端点注入,如图5所示。接地极电导率ρ为1e-7,每段长度l=1m,接地极截面积S可由导体直径算出。由此可由式(17)算出m类节点自电导,由于没有e节点,其它电导系数均为0。再由式(13)可求解出接地网上任意节点的电位,进一步根据式(10)可求得每个m类节点的泄露电流Imi。2. The length of the horizontal ground electrode is 10m, which is divided into 10 sections, that is, the number of the m-type nodes is from 1 to 10, and the 1A current is injected from the terminal of the No. 1 m-type node, as shown in Figure 5. The conductivity ρ of the ground electrode is 1e-7, the length of each section is l=1m, and the cross-sectional area S of the ground electrode can be calculated from the diameter of the conductor. From this, the self-conductance of m-type nodes can be calculated by formula (17). Since there is no e-node, the other conductance coefficients are all 0. Then, the potential of any node on the grounding grid can be obtained from formula (13), and the leakage current I mi of each type m node can be obtained further according to formula (10).
3、根据以上求得的第一层土壤的格林函数以及每个节点的泄露电流,即可由式(17)求出接地电阻值。并将计算结果与CDEGS软件计算结果比较,如附图6和表2所示,证明本发明提出的方法的准确性。3. According to the Green's function of the first layer of soil obtained above and the leakage current of each node, the grounding resistance value can be obtained by formula (17). And the calculation result is compared with the CDEGS software calculation result, as shown in accompanying drawing 6 and table 2, proves the accuracy of the method that the present invention proposes.
表1分层土壤参数Table 1 Layered soil parameters
表2水平接地极接地电阻Table 2 Horizontal ground electrode ground resistance
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