渗透系数的空间变异性是影响地下水运动和溶质迁移过程的主要因素。本文利用改进的连续随机增加方法(Successive random additional method,简称SRA)生成了渗透系数对数(lnK)具有分维Levy运动统计特征的随机场,并对生成样本的统计特征...渗透系数的空间变异性是影响地下水运动和溶质迁移过程的主要因素。本文利用改进的连续随机增加方法(Successive random additional method,简称SRA)生成了渗透系数对数(lnK)具有分维Levy运动统计特征的随机场,并对生成样本的统计特征进行了分析验证,同时应用蒙特卡罗方法研究含水层渗透系数的空间变异性对地下水运动和溶质迁移过程的影响。结果表明:Levy指数α越小,渗透系数空间变异性越强。当研究区域渗透系数的对数lnK增量符合Levy稳定分布时,其纵向流速对数lnv增量同样具有Levy稳定分布,且所对应的Levy指数αlnK与αlnv的大小基本一致。污染羽一阶矩纵向分量Mx随lnK平均值的增大而增大,而与α的大小无关。同一lnK均值条件下,纵向分量Mx随时间增大而增大,横向分量My与时间无关。污染羽二阶矩分量Mxx和Myy随α的减小而增大,表明渗透系数的空间变异性越强,污染物质心的扩散范围越大。渗透系数的空间变异程度对地下水运动和溶质迁移过程的影响十分明显。展开更多
建立了三级灰度图像边缘模型的空间矩算子。首先利用LOG(Laplacian of Gaussian)算子定位速度快的特点,确定图像像素级边缘;然后在包含边缘点的邻域内利用空间矩进行边缘的亚像素定位,由Hough变换提取直线和椭圆边缘像素点;最后采用基...建立了三级灰度图像边缘模型的空间矩算子。首先利用LOG(Laplacian of Gaussian)算子定位速度快的特点,确定图像像素级边缘;然后在包含边缘点的邻域内利用空间矩进行边缘的亚像素定位,由Hough变换提取直线和椭圆边缘像素点;最后采用基于最小二乘原理的直线拟合边缘提取方法,得到亚像素级被检测直线和椭圆。对空间矩算子亚像素定位算法与像面直线和椭圆亚像素提取算法的有效性和精度进行了实验研究,实验结果表明,在测量速度相当的情况下,本文提出的算法具有较高的精度和稳定性。展开更多
建立了基于空间矩的三级灰度图像边缘模型,首先由传统LOG(Laplacian of Gaussian)算子确定图像的像素级边缘,再由灰度空间矩对像素级边缘进行亚像素定位,并用Hough变换提取基元的亚像素边缘像素点,最后通过最小二乘法曲线拟合得到亚像...建立了基于空间矩的三级灰度图像边缘模型,首先由传统LOG(Laplacian of Gaussian)算子确定图像的像素级边缘,再由灰度空间矩对像素级边缘进行亚像素定位,并用Hough变换提取基元的亚像素边缘像素点,最后通过最小二乘法曲线拟合得到亚像素级的基元特征。实验结果表明,基于空间矩亚像素边缘定位算法,以及像面直线和椭圆亚像素提取算法具有较高的精度和稳定性。展开更多
A novel subpixel corner detection method based on spatial moment is developed in this paper. Firstly, the spatial-moment-generating function, gradient magnitude and variation of gradientdirection corner are used as th...A novel subpixel corner detection method based on spatial moment is developed in this paper. Firstly, the spatial-moment-generating function, gradient magnitude and variation of gradientdirection corner are used as the decision rule of corner detection by analyzing the mathematical formula of corner-model spatial moment. Then Non-max suppression technique is utilized to detect the vertex of feature corner. Finally, in order to improve its localization performance, subpixel corner detection is implemented by the bilinear interpolation and Newton iteration method. Experiments illustrate that the spatial moment corner detector has better robustness and localization performance than Kitchen detector and Harris detector.展开更多
In this paper,the behavior of breakthrough curves(BTCs) for reactive solute transport through stratified porous media is investigated.A physical laboratory model for layered porous media was constructed,in which thin ...In this paper,the behavior of breakthrough curves(BTCs) for reactive solute transport through stratified porous media is investigated.A physical laboratory model for layered porous media was constructed,in which thin layer of gravel was sandwiched in between two thick layers of natural soil.Gravel layer and natural soil layers were hydraulically connected as single porous continuum.A constant source of tracer was connected through gravel layer and elucidated at different sampling points in the direction of flow.Flexible multiprocess non-equilibrium(MPNE) transport equation with scale-dependent dispersivity function was used to simulate experimental BTCs of reactive solute transport through layered porous media.The values of equilibrium sorption coefficient and other input parameters were obtained experimentally.The simulation of BTC was performed using MPNE model with scale-dependent dispersivity.The simulation of different scale-dependent dispersivities was then compared and it was found that for field scale of estimation of dispersivity,asymptotic and exponential dispersivity functions performed better.In continuation to the comparison of simulated BTCs obtained using different models,spatial moment analysis of each aforesaid scale-dependent dispersivity model was also done.Spatial moment analysis provides the information related to mean solute mass,rate of mass travel,and mean plume dispersion.Linear and constant dispersivities showed higher variance as compared to asymptotic and exponential dispersion functions.This supports the field applicability of asymptotic and exponential dispersivity functions.The BTCs were also found to elucidate a nonzero concentration with time,which was clearly affected by physical non-equilibrium.In natural condition,such information is required in effective aquifer remediation process.展开更多
文摘渗透系数的空间变异性是影响地下水运动和溶质迁移过程的主要因素。本文利用改进的连续随机增加方法(Successive random additional method,简称SRA)生成了渗透系数对数(lnK)具有分维Levy运动统计特征的随机场,并对生成样本的统计特征进行了分析验证,同时应用蒙特卡罗方法研究含水层渗透系数的空间变异性对地下水运动和溶质迁移过程的影响。结果表明:Levy指数α越小,渗透系数空间变异性越强。当研究区域渗透系数的对数lnK增量符合Levy稳定分布时,其纵向流速对数lnv增量同样具有Levy稳定分布,且所对应的Levy指数αlnK与αlnv的大小基本一致。污染羽一阶矩纵向分量Mx随lnK平均值的增大而增大,而与α的大小无关。同一lnK均值条件下,纵向分量Mx随时间增大而增大,横向分量My与时间无关。污染羽二阶矩分量Mxx和Myy随α的减小而增大,表明渗透系数的空间变异性越强,污染物质心的扩散范围越大。渗透系数的空间变异程度对地下水运动和溶质迁移过程的影响十分明显。
文摘建立了三级灰度图像边缘模型的空间矩算子。首先利用LOG(Laplacian of Gaussian)算子定位速度快的特点,确定图像像素级边缘;然后在包含边缘点的邻域内利用空间矩进行边缘的亚像素定位,由Hough变换提取直线和椭圆边缘像素点;最后采用基于最小二乘原理的直线拟合边缘提取方法,得到亚像素级被检测直线和椭圆。对空间矩算子亚像素定位算法与像面直线和椭圆亚像素提取算法的有效性和精度进行了实验研究,实验结果表明,在测量速度相当的情况下,本文提出的算法具有较高的精度和稳定性。
文摘建立了基于空间矩的三级灰度图像边缘模型,首先由传统LOG(Laplacian of Gaussian)算子确定图像的像素级边缘,再由灰度空间矩对像素级边缘进行亚像素定位,并用Hough变换提取基元的亚像素边缘像素点,最后通过最小二乘法曲线拟合得到亚像素级的基元特征。实验结果表明,基于空间矩亚像素边缘定位算法,以及像面直线和椭圆亚像素提取算法具有较高的精度和稳定性。
文摘A novel subpixel corner detection method based on spatial moment is developed in this paper. Firstly, the spatial-moment-generating function, gradient magnitude and variation of gradientdirection corner are used as the decision rule of corner detection by analyzing the mathematical formula of corner-model spatial moment. Then Non-max suppression technique is utilized to detect the vertex of feature corner. Finally, in order to improve its localization performance, subpixel corner detection is implemented by the bilinear interpolation and Newton iteration method. Experiments illustrate that the spatial moment corner detector has better robustness and localization performance than Kitchen detector and Harris detector.
文摘In this paper,the behavior of breakthrough curves(BTCs) for reactive solute transport through stratified porous media is investigated.A physical laboratory model for layered porous media was constructed,in which thin layer of gravel was sandwiched in between two thick layers of natural soil.Gravel layer and natural soil layers were hydraulically connected as single porous continuum.A constant source of tracer was connected through gravel layer and elucidated at different sampling points in the direction of flow.Flexible multiprocess non-equilibrium(MPNE) transport equation with scale-dependent dispersivity function was used to simulate experimental BTCs of reactive solute transport through layered porous media.The values of equilibrium sorption coefficient and other input parameters were obtained experimentally.The simulation of BTC was performed using MPNE model with scale-dependent dispersivity.The simulation of different scale-dependent dispersivities was then compared and it was found that for field scale of estimation of dispersivity,asymptotic and exponential dispersivity functions performed better.In continuation to the comparison of simulated BTCs obtained using different models,spatial moment analysis of each aforesaid scale-dependent dispersivity model was also done.Spatial moment analysis provides the information related to mean solute mass,rate of mass travel,and mean plume dispersion.Linear and constant dispersivities showed higher variance as compared to asymptotic and exponential dispersion functions.This supports the field applicability of asymptotic and exponential dispersivity functions.The BTCs were also found to elucidate a nonzero concentration with time,which was clearly affected by physical non-equilibrium.In natural condition,such information is required in effective aquifer remediation process.
