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CN111563135A - GM(1,3) Model Urban Land Subsidence Prediction Method Combining Terrain Factors and Neural Networks - Google Patents

GM(1,3) Model Urban Land Subsidence Prediction Method Combining Terrain Factors and Neural Networks Download PDF

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CN111563135A
CN111563135A CN202010242878.1A CN202010242878A CN111563135A CN 111563135 A CN111563135 A CN 111563135A CN 202010242878 A CN202010242878 A CN 202010242878A CN 111563135 A CN111563135 A CN 111563135A
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胡庆武
周启航
艾明耀
赵鹏程
李加元
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Abstract

本发明公开了一种结合地形因子与GM(1,3)模型的城市地面沉降预测方法,包括收集待预测位置站点以及附近若干站点的历史观测资料,各观测记录包括信息有观测时间、站点地理坐标和沉降观测值,同时收集当地邻近年份DEM数据;利用地形数据提取地形因子,结合地形因子构建地理空间权重矩阵,筛选沉降预测辅助变量;使用GM(1,3)模型进行初预测,利用BP神经网络对GM(1.3)的预测误差进行修正,得到精确的沉降预测值。本发明利用沉降观测历史数据和地形数据,通过GM(1,3)模型和BP神经网络融合,实现对城市地面沉降的预测,精度达到毫米级,可以媲美精密水准观测的结果,对于城市地面沉降的防控具有重要的现实意义,可提高沉降灾害防治的效率。

Figure 202010242878

The invention discloses an urban land subsidence prediction method combining terrain factors and GM (1,3) models, which includes collecting historical observation data of a site to be predicted and several nearby sites, and each observation record includes information including observation time, site geography Coordinates and subsidence observations, while collecting local DEM data in adjacent years; using terrain data to extract terrain factors, combining terrain factors to build a geospatial weight matrix, and screening auxiliary variables for subsidence prediction; using the GM(1,3) model for initial prediction, using BP The neural network corrects the prediction error of GM(1.3), and obtains the accurate settlement prediction value. The present invention utilizes subsidence observation historical data and topographic data, and integrates GM(1,3) model and BP neural network to realize the prediction of urban land subsidence, and the accuracy reaches millimeter level, which can be comparable to the results of precise level observation. The prevention and control of subsidence has important practical significance and can improve the efficiency of subsidence disaster prevention and control.

Figure 202010242878

Description

结合地形因子与神经网络的GM(1,3)模型城市地面沉降预测 方法Prediction of Urban Land Subsidence Based on GM(1,3) Model Combining Terrain Factor and Neural Network method

技术领域technical field

本发明涉及地面沉降预测技术领域,是利用城市变形观测历史数据,采用地理空间权重矩阵与神经网络技术结合的GM(1,3)模型精确预测城市地面沉降的一种方法。The invention relates to the technical field of land subsidence prediction, and is a method for accurately predicting urban land subsidence by using historical data of urban deformation observation and using a GM(1,3) model combining geographic space weight matrix and neural network technology.

背景技术Background technique

地面沉降又称为地陷或地面下沉,是一种在自然或人为因素影响下,地表以下土体被压缩从而导致局部地表标高降低的地质现象。受到地下水、天然气与石油开采以及城市开发的影响,地面沉降现象近年来在世界范围内频发。在2003 年发布的《地质灾害防治条例》中,地面沉降现象被定义为一种“缓变性地质灾害”。据统计,截止2012年,我国有超过50个大中型城市层发生地面沉降灾害现象,其中沿海发达地区为地面沉降的高发区域,全国范围内地面沉降量总计超过200毫米的城市区域面积高达到7.9万平方公里。在过去40年中,我国因地面沉降现象而受到的损失高达3000亿元。地面沉降不仅影响社会的可持续发展,还威胁到了人类的生命安全。因此,对地面沉降的模型预测研究成为了当下的热点问题。Land subsidence, also known as subsidence or ground subsidence, is a geological phenomenon in which the soil below the surface is compressed under the influence of natural or human factors, resulting in a decrease in local surface elevation. Affected by groundwater, natural gas and oil extraction and urban development, land subsidence has occurred frequently around the world in recent years. In the "Regulations on the Prevention and Control of Geological Hazards" issued in 2003, the phenomenon of land subsidence was defined as a "slowly changing geological hazard". According to statistics, as of 2012, more than 50 large and medium-sized cities in my country have experienced land subsidence disasters. Among them, the developed coastal areas are high-incidence areas of land subsidence, and the area of urban areas with a total land subsidence of more than 200 mm nationwide is as high as 7.9%. million square kilometers. In the past 40 years, my country has suffered losses of up to 300 billion yuan due to land subsidence. Land subsidence not only affects the sustainable development of society, but also threatens the safety of human life. Therefore, the research on model prediction of land subsidence has become a hot issue at present.

发明内容SUMMARY OF THE INVENTION

本发明结合地形因子与GM(1,3)模型的城市地面沉降预测方法是一种采用 GM(1,3)预测模型与地理空间权重矩阵融合技术的方法,利用沉降观测历史数据,采用GM(1,3)模型与地理空间权重矩阵变量筛选的融合方法,以达到精确预测未来沉降趋势的效果。The urban land subsidence prediction method combining the terrain factor and the GM (1,3) model of the present invention is a method using the GM (1,3) prediction model and the geographic space weight matrix fusion technology, using the historical data of subsidence observation, using the GM ( 1,3) The fusion method of the model and the variable screening of the geospatial weight matrix to achieve the effect of accurately predicting the future subsidence trend.

本发明提供一种结合地形因子与GM(1,3)模型的城市地面沉降预测方法,包括以下步骤,The invention provides an urban land subsidence prediction method combining terrain factors and GM(1,3) model, comprising the following steps:

步骤1)、收集待预测位置站点以及附近若干站点的历史观测资料,各观测记录包括信息有观测时间、站点地理坐标和沉降观测值;同时收集当地邻近年份DEM数据;Step 1), collect the historical observation data of the site to be predicted and a number of nearby sites, each observation record includes information including observation time, site geographic coordinates and subsidence observations; simultaneously collect local adjacent years DEM data;

步骤2)、地形因子提取,包括通过DEM数据以及各观测站点坐标,提取每个观测站点的高程值和坡度值;Step 2), terrain factor extraction, including extracting the elevation value and slope value of each observation site through DEM data and the coordinates of each observation site;

步骤3)、地理空间权重矩阵构建与辅助变量筛选,包括对地理空间权重矩阵根据地形因子采用反距离权重法实现构建,辅助变量则是从地理空间权重矩阵中筛选出每一个站点所对应的权重最大的两个站点得到;Step 3), the construction of the geospatial weight matrix and the screening of auxiliary variables, including the construction of the geospatial weight matrix according to the terrain factor using the inverse distance weight method, and the auxiliary variable is to filter out the weight corresponding to each site from the geospatial weight matrix The largest two sites get;

步骤4)、使用GM(1,3)模型进行初预测,包括利用地理空间权重矩阵,构建 GM(1,3)模型,进行沉降粗预测;Step 4), use the GM(1,3) model for initial prediction, including using the geospatial weight matrix to construct the GM(1,3) model, and carry out rough prediction of settlement;

步骤5)、神经网络拟合误差改正精预测,包括以GM(1,3)粗预测模型拟合预测值,将数据真值与拟合值相减得到原始数据对应期数的预测误差值;将误差值输入BP神经网络得到预测误差的拟合函数,再将预测后的误差与真实预测值叠加得到更加精确的预测结果。Step 5), correcting the precise prediction of the neural network fitting error, including fitting the predicted value with the GM(1,3) rough prediction model, and subtracting the true value of the data from the fitted value to obtain the prediction error value of the corresponding period of the original data; Input the error value into the BP neural network to obtain the fitting function of the prediction error, and then superimpose the predicted error and the real prediction value to obtain a more accurate prediction result.

而且,步骤1)中,收集预测站点历史沉降观测数据不少于至少5个站点。Moreover, in step 1), the historical subsidence observation data of the predicted stations are collected for not less than at least 5 stations.

而且,步骤3)实现方式如下,And, step 3) implementation is as follows,

首先,将p个站点的四个地形因子记为(x,y,slope,H)i,i=1,2,3....p,其中x代表站点x坐标,y代表站点y坐标,slope代表站点斜率,H代表站点初始高程值;在以上4个变量构成的欧式空间中,)计算任意两站点欧式距离;First, denote the four terrain factors of p stations as (x, y, slope, H) i , i=1, 2, 3....p, where x represents the x-coordinate of the site, y represents the y-coordinate of the site, slope represents the slope of the site, and H represents the initial elevation value of the site; in the Euclidean space composed of the above four variables, ) calculates the Euclidean distance between any two sites;

其次,采用反距离权重法构建地理空间权重矩阵R,得到任意两个站点之间的地理空间权重值;Secondly, the inverse distance weight method is used to construct the geospatial weight matrix R, and the geospatial weight value between any two stations is obtained;

最后,对任意一个站点将空间权重矩阵R相应行的权重值进行排列,取权重值最大的两个站点作为预测的辅助变量。Finally, arrange the weight values of the corresponding rows of the spatial weight matrix R for any station, and take the two stations with the largest weight values as auxiliary variables for prediction.

而且,步骤4)实现方式如下,And, step 4) implementation mode is as follows,

首先,以待预测观测站点连续n年的高程历史观测值作为零阶累加序列,建立主变量原始序列,以经地理空间权重矩阵筛选后的两个辅助站点连续n年历史观测序列建立辅助变量序列;First, take the historical elevation observation values of the observation station to be predicted for n consecutive years as the zero-order cumulative sequence to establish the original sequence of the primary variable, and use the consecutive n-year historical observation sequence of the two auxiliary stations after screening by the geospatial weight matrix to establish the auxiliary variable sequence ;

其次,通过求解GM(1,3)方程,得到沉降预测曲线;Secondly, by solving the GM(1,3) equation, the settlement prediction curve is obtained;

最后,对主变量原始序列进行还原,得到还原后的预测值,作为预测粗预测结果。Finally, the original sequence of the main variable is restored, and the restored predicted value is obtained as the rough prediction result.

而且,步骤5)中,神经网络的特征指标优选有:Moreover, in step 5), the characteristic index of the neural network preferably has:

①BP神经网络隐藏层共1个.①The BP neural network has a total of one hidden layer.

②BP神经网络隐藏层节点为12个。②The number of hidden layer nodes of BP neural network is 12.

③BP神经网络延迟变量为3。③The delay variable of BP neural network is 3.

本发明方法的特点:对于城市地面沉降的预测具有良好的物理解释,精度达到毫米级,可以媲美精密水准观测的结果,对于城市地面沉降的防控具有重要的现实意义。本发明具有如下积极效果:城市区域地沉降的预测精度高,从而提高了对地面沉降灾害防治的准确性,同时具有良好的物理意义,有利于城市地面沉降规律的探寻。The method of the invention has the characteristics of good physical explanation for the prediction of urban land subsidence, and the accuracy reaches the millimeter level, which is comparable to the result of precise level observation, and has important practical significance for the prevention and control of urban land subsidence. The invention has the following positive effects: the prediction accuracy of urban area land subsidence is high, thereby improving the accuracy of prevention and control of land subsidence disasters, and at the same time, it has good physical meaning and is beneficial to the exploration of urban land subsidence laws.

附图说明Description of drawings

图1为本发明实施例的流程图。FIG. 1 is a flowchart of an embodiment of the present invention.

具体实施方式Detailed ways

以下结合附图和实施例具体说明本发明的技术方案。The technical solutions of the present invention will be specifically described below with reference to the accompanying drawings and embodiments.

本发明利用沉降观测历史数据,采用GM(1,3)模型与地理空间权重矩阵变量筛选的融合方法,以达到精确预测未来沉降趋势的效果。从而提高沉降预测的准确性,提高沉降灾害防治的效率。具体包括:(1)收集历史沉降观测值资料、(2) 地形因子提取、(3)地理空间权重矩阵构建与辅助变量筛选、(4)GM(1,3)模型构建、(5)BP神经网络修正、(6)沉降值预测。The present invention utilizes the historical data of settlement observation and adopts the fusion method of GM(1,3) model and the variable screening of geographic space weight matrix, so as to achieve the effect of accurately predicting the future settlement trend. Thereby, the accuracy of subsidence prediction is improved, and the efficiency of subsidence disaster prevention and control is improved. Specifically, it includes: (1) collection of historical subsidence observation data, (2) terrain factor extraction, (3) geospatial weight matrix construction and auxiliary variable screening, (4) GM(1,3) model construction, (5) BP neural network Network correction, (6) settlement value prediction.

参见图1,实施例提供一种结合地形因子与神经网络的GM(1,3)模型城市地面沉降预测方法,包括以下步骤:Referring to FIG. 1, the embodiment provides a GM(1,3) model urban land subsidence prediction method combining terrain factors and neural networks, including the following steps:

步骤1)输入待预测地点的沉降观测数据Step 1) Input the subsidence observation data of the site to be predicted

具体实施时可预先收集待预测位置站点以及附近至少5个站点的历史观测资料,各观测记录至少包含以下信息:观测时间、站点地理坐标(经纬度)、沉降观测值。同时需要收集当地邻近年份DEM数据。During specific implementation, historical observation data of the site to be predicted and at least 5 nearby sites can be collected in advance, and each observation record contains at least the following information: observation time, site geographic coordinates (latitude and longitude), and settlement observation value. At the same time, it is necessary to collect DEM data of local neighboring years.

本实施例的应用实例中选用的是浙江省海盐县12个站点的1999-2016年的年度高程观测数据,1)沉降观测点的位置、名称等属性信息:其中位置为 CGCS2000经纬度坐标,名称为观测站点中文名称;2)沉降观测点1999-2016 年沉降观测值:观测值单位为米,精度达到毫米。筛选出的数据样例如表1所示:In the application example of this embodiment, the annual elevation observation data from 1999 to 2016 of 12 stations in Haiyan County, Zhejiang Province is selected. 1) Attribute information such as the location and name of the subsidence observation point: the location is the CGCS2000 latitude and longitude coordinates, and the name is Chinese name of the observation site; 2) Subsidence observation point of subsidence observation point from 1999 to 2016: the unit of observation value is meter, and the precision is millimeter. The filtered data samples are shown in Table 1:

表1浙江省海盐县沉降数据样例Table 1 Example of subsidence data in Haiyan County, Zhejiang Province

Figure BDA0002433143110000031
Figure BDA0002433143110000031

Figure BDA0002433143110000041
Figure BDA0002433143110000041

步骤2)地形因子提取:Step 2) Terrain factor extraction:

该步骤通过DEM数据以及各观测站点坐标,提取每个观测站点的高程值、坡度值。In this step, the DEM data and the coordinates of each observation site are used to extract the elevation value and slope value of each observation site.

实施例的应用实例中,根据海盐地区1999年30m分辨率ASTER DEM数据,利用ArcGIS对对应站点该年度的坡度、初始高程值进行提取,与站点高斯-克吕格坐标系定义下的X坐标、Y坐标共同构成地形因子数据,结果如表2所示In the application example of the embodiment, according to the 30m resolution ASTER DEM data in Haiyan area in 1999, ArcGIS was used to extract the slope and initial elevation value of the corresponding site in this year, and the X coordinate defined by the Gauss-Kruger coordinate system of the site, The Y coordinates together constitute the terrain factor data, and the results are shown in Table 2.

表2对应站点地形因子数据Table 2 Topographic factor data of corresponding sites

Figure BDA0002433143110000042
Figure BDA0002433143110000042

Figure BDA0002433143110000051
Figure BDA0002433143110000051

步骤3)地理空间权重矩阵的构建:Step 3) Construction of Geospatial Weight Matrix:

实施例中,地理空间权重矩阵根据地形因子采用反距离权重法构建;辅助变量则从地理空间权重矩阵中筛选出每一个站点所对应的权重最大的两个站点得到。In the embodiment, the geospatial weight matrix is constructed using the inverse distance weighting method according to the terrain factor; the auxiliary variables are obtained by filtering out the two sites with the largest weight corresponding to each site from the geospatial weight matrix.

将p个站点的四个地形因子记为(x,y,slope,H)i,i=1,2,3....p,其中x代表站点X坐标,y代表站点Y坐标,slope代表站点斜率,H代表站点初始高程值。在以上4个变量构成的欧式空间中,将任意两站点i、j在此空间的欧式距离记为 DijThe four terrain factors of p stations are recorded as (x, y, slope, H) i , i=1, 2, 3....p, where x represents the X coordinate of the station, y represents the Y coordinate of the station, and slope represents the Site slope, H represents the initial site elevation value. In the Euclidean space composed of the above four variables, the Euclidean distance of any two stations i, j in this space is recorded as D ij :

Figure BDA0002433143110000061
Figure BDA0002433143110000061

步骤3.1,采用反距离权重法构建地理空间权重矩阵R:Step 3.1, using the inverse distance weight method to construct the geospatial weight matrix R:

Figure BDA0002433143110000062
Figure BDA0002433143110000062

其中任意两个站点之间的地理空间权重值Rij可以采用下式计算:The geospatial weight value R ij between any two stations can be calculated by the following formula:

Figure BDA0002433143110000063
Figure BDA0002433143110000063

采用实验数据所得到的空间权重矩阵如表3所示:The spatial weight matrix obtained by using the experimental data is shown in Table 3:

表3地理空间权重矩阵构建实例Table 3 Examples of Geospatial Weight Matrix Construction

00 11 22 33 44 55 66 77 88 99 1010 1111 x0x0 0.510.51 0.840.84 1.041.04 0.900.90 1.151.15 1.051.05 0.940.94 0.930.93 1.391.39 0.640.64 1.001.00 x1x1 0.510.51 0.590.59 0.730.73 0.500.50 0.900.90 0.640.64 0.640.64 0.560.56 0.920.92 0.320.32 0.650.65 x2x2 0.840.84 0.590.59 0.730.73 0.390.39 0.330.33 0.420.42 0.850.85 0.680.68 0.790.79 0.300.30 0.470.47 x3x3 1.041.04 0.730.73 0.730.73 0.390.39 0.950.95 0.470.47 1.251.25 1.101.10 1.021.02 0.580.58 0.290.29 x4x4 0.900.90 0.500.50 0.390.39 0.390.39 0.630.63 0.170.17 0.910.91 0.740.74 0.710.71 0.290.29 0.170.17 x5x5 1.151.15 0.900.90 0.330.33 0.950.95 0.630.63 0.570.57 1.001.00 0.820.82 0.770.77 0.630.63 0.670.67 x6x6 1.051.05 0.640.64 0.420.42 0.470.47 0.170.17 0.570.57 0.950.95 0.760.76 0.600.60 0.420.42 0.210.21 x7x7 0.940.94 0.640.64 0.850.85 1.251.25 0.910.91 1.001.00 0.950.95 0.200.20 0.800.80 0.780.78 1.081.08 x8x8 0.930.93 0.560.56 0.680.68 1.101.10 0.740.74 0.820.82 0.760.76 0.200.20 0.630.63 0.640.64 0.910.91 x9x9 1.391.39 0.920.92 0.790.79 1.021.02 0.710.71 0.770.77 0.600.60 0.800.80 0.630.63 0.840.84 0.810.81 x10x10 0.640.64 0.320.32 0.300.30 0.580.58 0.290.29 0.630.63 0.420.42 0.780.78 0.640.64 0.840.84 0.420.42 x11x11 1.001.00 0.650.65 0.470.47 0.290.29 0.170.17 0.670.67 0.210.21 1.081.08 0.910.91 0.810.81 0.420.42

步骤3.2,任意站点辅助变量筛选:对任意一个站点i,将空间权重矩阵R 的第i行(Ri1,Ri2,…,Rip)权重值进行排列,取权重值最大的两个站点即为预测的辅助变量。Step 3.2, Screening of auxiliary variables of any site: for any site i, arrange the weight values of the i-th row (R i1 , R i2 , ..., R ip ) of the spatial weight matrix R, and take the two sites with the largest weight values, namely auxiliary variable for prediction.

从地理空间权重矩阵中筛选出每一个站点所对应的权重最大的两个站点,即可作为GM(1,3)预测的辅助预测变量,本实验数据得到的主变量与辅助变量的对应表格如表4所示。The two sites with the largest weights corresponding to each site are screened out from the geospatial weight matrix, which can be used as auxiliary predictors for GM(1,3) prediction. The corresponding tables of the main variables and auxiliary variables obtained from the experimental data are as follows shown in Table 4.

表4主变量与辅助变量对应表Table 4 Correspondence table of main variables and auxiliary variables

观测站IDObservatory ID 辅助变量1auxiliary variable 1 辅助变量2auxiliary variable 2 x0x0 x1x1 x10x10 x1x1 x4x4 x10x10 x2x2 x5x5 x10x10 x3x3 x4x4 x10x10 x4x4 x6x6 x11x11 x5x5 x2x2 x6x6 x6x6 x4x4 x11x11 x7x7 x1x1 x8x8 x7x7 x1x1 x7x7 x9x9 x6x6 x8x8 x10x10 x2x2 x4x4 x11x11 x4x4 x6 x6

步骤4)使用GM(1,3)模型进行初预测:Step 4) Use the GM(1,3) model for initial prediction:

该步骤利用地理空间权重矩阵,构建GM(1,3)模型,进行沉降粗预测。This step uses the geospatial weight matrix to construct a GM(1,3) model for rough prediction of settlement.

为引入地理空间权重矩阵的GM(1,3)进行粗预测,该步骤首先以待预测观测站点连续n年的高程历史观测值(即零阶累加序列)建立主变量原始序列,以经地理空间权重矩阵筛选后的两个辅助站点连续n年历史观测序列建立辅助变量序列,其次,通过求解GM(1,3)方程,即可得到沉降预测曲线;对主变量原始序列进行还原,得到还原后的预测值即为预测粗预测结果。In order to carry out rough prediction by introducing the GM(1,3) of the geospatial weight matrix, this step firstly establishes the original sequence of main variables based on the historical elevation observations of the observation station to be predicted for n consecutive years (ie, the zero-order cumulative sequence), and then uses the geospatial data to obtain the original sequence of primary variables. After the weight matrix screened out the consecutive n-year historical observation sequences of the two auxiliary stations, an auxiliary variable sequence is established. Secondly, by solving the GM(1,3) equation, the settlement prediction curve can be obtained; The predicted value of is the predicted coarse prediction result.

实施例中预测具体步骤如下:主变量原始序列即为待预测观测站点连续n 年的高程历史观测值(即零阶累加序列)记为 H1 (0)=(h1 (0)(1),h1 (0)(2),h1 (0)(3),…,h1 (0)(n)),辅助变量序列即为经地理空间权重矩阵筛选后的两个辅助站点连续n年历史观测序列分别记为:The specific steps of the prediction in the embodiment are as follows: the original sequence of the main variable is the historical elevation observation value of the observation site to be predicted for consecutive n years (ie, the zero-order cumulative sequence), which is recorded as H 1 (0) = (h 1 (0) (1) ,h 1 (0) (2),h 1 (0) (3),…,h 1 (0) (n)), the auxiliary variable sequence is the consecutive n of two auxiliary stations filtered by the geospatial weight matrix The annual historical observation sequences are recorded as:

H2 (0)=(h2 (0)(1),h2 (0)(2),h2 (0)(3),…,h2 (0)(n))H 2 (0) = (h 2 (0) (1),h 2 (0) (2),h 2 (0) (3),…,h 2 (0) (n))

H2 (0)=(h3 (0)(1),h3 (0)(2),h3 (0)(3),…,h3 (0)(n))H 2 (0) = (h 3 (0) (1),h 3 (0) (2),h 3 (0) (3),…,h 3 (0) (n))

步骤4.1,按照如下步骤求解GM(1,3)方程,即可得到预测曲线:Step 4.1, follow the steps below to solve the GM(1,3) equation to get the prediction curve:

①一阶累加生成序列计算:将主变量H1与两个辅助变量H2、H3的一阶累加生成序列记为H1 (1),H2 (1),H3 (1),则:①Calculation of the first-order accumulation generation sequence: the first-order accumulation generation sequence of the main variable H 1 and the two auxiliary variables H 2 and H 3 is recorded as H 1 (1) , H 2 (1) , H 3 (1) , then :

Hi (1)=(hi (1)(1),hi (1)(2),hi (1)(3),…,hi (1)(n)) i=1,2,3Hi (1) = ( hi (1) (1), hi (1) (2), hi (1) (3),…, hi (1) (n)) i =1,2 ,3

Figure BDA0002433143110000081
Figure BDA0002433143110000081

其中,hi (1)(1),hi (1)(2),hi (1)(3),…,hi (1)(n)分别表示待预测观测站点第 1,2,3,…,n年的一阶累加值。Among them, h i (1) (1), h i (1) (2), h i (1) (3),…, h i (1) (n) represent the first, second, and third observation sites to be predicted, respectively. 3,…, first-order cumulative value of n years.

②计算主变量序列一阶累加序列的紧邻均值序列Z1 (1),其中第k个值为② Calculate the adjacent mean sequence Z 1 (1) of the first-order cumulative sequence of the main variable sequence, where the k-th value is

Figure BDA0002433143110000082
Figure BDA0002433143110000082

③构建GM(1,3)白化微分方程,方程形式如下:其中t指代观察期数③Construct the GM(1,3) whitening differential equation, the equation form is as follows: where t refers to the number of observation periods

Figure BDA0002433143110000083
Figure BDA0002433143110000083

求解中设:

Figure BDA0002433143110000084
其中Solve the middle set:
Figure BDA0002433143110000084
in

Y=[H1 (0)(2),H1 (0)(3),…,H1 (0)(n)],Y=[H 1 (0) (2),H 1 (0) (3),...,H 1 (0) (n)],

Figure BDA0002433143110000085
Figure BDA0002433143110000085

其中,a、b1、b2

Figure BDA0002433143110000087
Y、B等为求解方程的中间参数。Among them, a, b 1 , b 2 ,
Figure BDA0002433143110000087
Y, B, etc. are the intermediate parameters for solving the equation.

④对方程进行离散化并求解,得到时间响应序列方程的解为④ Discretize and solve the equation, and obtain the solution of the time response sequence equation as

Figure BDA0002433143110000086
Figure BDA0002433143110000086

其中,

Figure BDA0002433143110000091
为真实H1 (1)(k+1)的估算值,e为自然对数。in,
Figure BDA0002433143110000091
is an estimate of the true H 1 (1) (k+1), and e is the natural logarithm.

步骤4.2,对原始序列进行还原,得到还原后的预测值

Figure BDA0002433143110000092
该序列即为预测结果。Step 4.2, restore the original sequence to obtain the restored predicted value
Figure BDA0002433143110000092
This sequence is the prediction result.

Figure BDA0002433143110000093
Figure BDA0002433143110000093

其中,

Figure BDA0002433143110000094
表示还原后的预测值,即
Figure BDA0002433143110000095
in,
Figure BDA0002433143110000094
represents the predicted value after restoration, that is,
Figure BDA0002433143110000095

步骤5)神经网络拟合误差改正精预测:本发明利用BP神经网络对GM(1.3) 的预测误差进行修正,得到精确的沉降预测值。Step 5) Neural network fitting error correction and accurate prediction: The present invention uses BP neural network to correct the prediction error of GM (1.3) to obtain accurate settlement prediction value.

将还原结果与真实值的误差输入时间序列神经网络中,实施例采用BP神经网络,优选地隐藏层数量为1,隐藏层节点为12,延迟变量设为3,利用神经网络算法对该网络结构进行样本训练,可以得到GM(1,3)预测误差的拟合函数。将拟合函数与预测序列进行叠加,得到最终的高精度预测值。The error between the restoration result and the real value is input into the time series neural network. The embodiment adopts the BP neural network. Preferably, the number of hidden layers is 1, the number of hidden layer nodes is 12, and the delay variable is set to 3, and the neural network algorithm is used for this network structure. After sample training, the fitting function of the prediction error of GM(1,3) can be obtained. The fitting function is superimposed with the prediction sequence to obtain the final high-precision prediction value.

经过GM(1,3)粗预测后,可以得到原始序列的GM(1,3)模型拟合预测值,将数据真值与拟合值相减即可得到原始数据对应期数的预测误差值。将误差值输入 BP神经网络即可得到预测误差的拟合函数,再将预测后的误差与真实预测值叠加既可以得到更加精确的预测结果,具体步骤如下:After GM(1,3) rough prediction, the GM(1,3) model fitting prediction value of the original sequence can be obtained, and the prediction error value of the corresponding period of the original data can be obtained by subtracting the true value of the data from the fitting value . Input the error value into the BP neural network to obtain the fitting function of the prediction error, and then superimpose the predicted error with the real prediction value to obtain a more accurate prediction result. The specific steps are as follows:

①假定需要预测的总期数为T,使用结合地形因子的GM(1,3)预测模型对T 期数据进行拟合,可以得到T期预测值与T期误差,①Assuming that the total number of periods to be predicted is T, use the GM(1,3) prediction model combined with the terrain factor to fit the T period data, and the error between the T period predicted value and the T period can be obtained,

②将误差统计序列输入时间序列神经网络后可以对误差的时间序列函数进行拟合,获得误差的拟合预测模型。② After inputting the error statistical sequence into the time series neural network, the time series function of the error can be fitted to obtain the fitting prediction model of the error.

③将神经网络误差预测模型与结合地形的GM(1,3)预测模型预测函数累加,即可以得到更加精确的沉降预测结果。③ Accumulate the prediction function of the neural network error prediction model and the GM(1,3) prediction model combined with the terrain, that is, a more accurate settlement prediction result can be obtained.

具体实施时,以上流程可采用计算机软件技术实现自动运行。运行方法的系统装置也应当在本发明的保护范围内。During specific implementation, the above process can be automatically run by using computer software technology. The system apparatus for operating the method should also be within the scope of protection of the present invention.

显然,本发明的上述实施例只是为清楚地说明本发明所作的举例,而并非是对本发明的实施方式的限定,对于本领域的普通技术人员来说,在上述说明的基础上还可以对本发明实施例进行各种改动和变型而不脱离本发明实施例的精神和范围。这样,倘若本发明实施例的这些修改和变型属于本发明权利要求及其等同技术的范围之内,则本发明也意图包含这些改动和变型在内。Obviously, the above-mentioned embodiments of the present invention are only examples for clearly illustrating the present invention, rather than limiting the embodiments of the present invention. Various changes and modifications may be made to the embodiments without departing from the spirit and scope of the embodiments of the present invention. Thus, provided that these modifications and variations of the embodiments of the present invention fall within the scope of the claims of the present invention and their equivalents, the present invention is also intended to include such modifications and variations.

Claims (5)

1.一种结合地形因子与GM(1,3)模型的城市地面沉降预测方法,其特征在于:包括以下步骤,1. an urban land subsidence prediction method combining terrain factor and GM (1,3) model, is characterized in that: comprise the following steps, 步骤1)、收集待预测位置站点以及附近若干站点的历史观测资料,各观测记录包括信息有观测时间、站点地理坐标和沉降观测值;同时收集当地邻近年份DEM数据;Step 1), collect the historical observation data of the site to be predicted and a number of nearby sites, each observation record includes information including observation time, site geographic coordinates and subsidence observations; simultaneously collect local adjacent years DEM data; 步骤2)、地形因子提取,包括通过DEM数据以及各观测站点坐标,提取每个观测站点的高程值和坡度值;Step 2), terrain factor extraction, including extracting the elevation value and slope value of each observation site through DEM data and the coordinates of each observation site; 步骤3)、地理空间权重矩阵构建与辅助变量筛选,包括对地理空间权重矩阵根据地形因子采用反距离权重法实现构建,辅助变量则是从地理空间权重矩阵中筛选出每一个站点所对应的权重最大的两个站点得到;Step 3), the construction of the geospatial weight matrix and the screening of auxiliary variables, including the construction of the geospatial weight matrix according to the terrain factor using the inverse distance weight method, and the auxiliary variable is to filter out the weight corresponding to each site from the geospatial weight matrix The largest two sites get; 步骤4)、使用GM(1,3)模型进行初预测,包括利用地理空间权重矩阵,构建GM(1,3)模型,进行沉降粗预测;Step 4), using the GM(1,3) model for initial prediction, including using the geospatial weight matrix to construct the GM(1,3) model for rough prediction of settlement; 步骤5)、神经网络拟合误差改正精预测,包括以GM(1,3)粗预测模型拟合预测值,将数据真值与拟合值相减得到原始数据对应期数的预测误差值;将误差值输入BP神经网络得到预测误差的拟合函数,再将预测后的误差与真实预测值叠加得到更加精确的预测结果。Step 5), correcting the precise prediction of the neural network fitting error, including fitting the predicted value with the GM(1,3) rough prediction model, and subtracting the true value of the data from the fitted value to obtain the prediction error value of the corresponding period of the original data; Input the error value into the BP neural network to obtain the fitting function of the prediction error, and then superimpose the predicted error and the real prediction value to obtain a more accurate prediction result. 2.根据权利要求1所述的一种结合地形因子与GM(1,3)模型的城市地面沉降预测方法,其特征在于:步骤1)中,收集预测站点历史沉降观测数据不少于至少5个站点。2. a kind of urban land subsidence prediction method combining terrain factor and GM (1,3) model according to claim 1, it is characterized in that: in step 1), collect and predict site historical subsidence observation data not less than at least 5 sites. 3.根据权利要求1所述的一种结合地形因子与GM(1,3)模型的城市地面沉降预测方法,其特征在于:步骤3)实现方式如下,3. a kind of urban land subsidence prediction method combining terrain factor and GM (1,3) model according to claim 1, is characterized in that: step 3) realization mode is as follows, 首先,将p个站点的四个地形因子记为(x,y,slope,H)i,i=1,2,3....p,其中x代表站点x坐标,y代表站点y坐标,slope代表站点斜率,H代表站点初始高程值;First, denote the four terrain factors of p stations as (x, y, slope, H) i , i=1, 2, 3....p, where x represents the x-coordinate of the site, y represents the y-coordinate of the site, slope represents the slope of the site, and H represents the initial elevation value of the site; 在以上4个变量构成的欧式空间中,)计算任意两站点欧式距离;In the Euclidean space composed of the above four variables, ) calculates the Euclidean distance between any two stations; 其次,采用反距离权重法构建地理空间权重矩阵R,得到任意两个站点之间的地理空间权重值;Secondly, the inverse distance weight method is used to construct the geospatial weight matrix R, and the geospatial weight value between any two stations is obtained; 最后,对任意一个站点将空间权重矩阵R相应行的权重值进行排列,取权重值最大的两个站点作为预测的辅助变量。Finally, arrange the weight values of the corresponding rows of the spatial weight matrix R for any station, and take the two stations with the largest weight values as auxiliary variables for prediction. 4.根据权利要求1所述的一种结合地形因子与GM(1,3)模型的城市地面沉降预测方法,其特征在于:步骤4)实现方式如下,4. a kind of urban land subsidence prediction method combining terrain factor and GM (1,3) model according to claim 1, is characterized in that: step 4) realization mode is as follows, 首先,以待预测观测站点连续n年的高程历史观测值作为零阶累加序列,建立主变量原始序列,以经地理空间权重矩阵筛选后的两个辅助站点连续n年历史观测序列建立辅助变量序列;First, take the historical elevation observation values of the observation station to be predicted for n consecutive years as the zero-order cumulative sequence to establish the original sequence of the primary variable, and use the consecutive n-year historical observation sequence of the two auxiliary stations after screening by the geospatial weight matrix to establish the auxiliary variable sequence ; 其次,通过求解GM(1,3)方程,得到沉降预测曲线;Secondly, by solving the GM(1,3) equation, the settlement prediction curve is obtained; 最后,对主变量原始序列进行还原,得到还原后的预测值,作为预测粗预测结果。Finally, the original sequence of the main variable is restored, and the restored predicted value is obtained as the rough prediction result. 5.根据权利要求1或2或3或4所述的一种结合地形因子与GM(1,3)模型的城市地面沉降预测方法,其特征在于:步骤5)中,神经网络的特征指标优选有:5. a kind of urban land subsidence prediction method combining terrain factor and GM (1,3) model according to claim 1 or 2 or 3 or 4, is characterized in that: in step 5), the characteristic index of neural network is preferably Have: ①BP神经网络隐藏层共1个.①The BP neural network has a total of one hidden layer. ②BP神经网络隐藏层节点为12个。②The number of hidden layer nodes of BP neural network is 12. ③BP神经网络延迟变量为3。③The delay variable of BP neural network is 3.
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