VP型垂直摆倾斜仪观测频带的分析及改进     

吕品姬  李正媛  耿丽霞  李农发  徐春阳 《大地测量与地球动力学》2020,40(5):540-545

从仪器原理、传递函数和观测数据等方面分析目前在网进行1 Hz采样的VP型垂直摆倾斜仪在2~60 s周期内的频率特性,认为该仪器可以观测到频带内的信号变化,但因处于过渡带,观测幅度较真实幅度削弱约20~40 dB。对VP型垂直摆倾斜仪观测频带进行拓展,使2~60 s周期内的观测信号由之前的过渡带进入到仪器的通频带,结果与相同采样率的其他定点形变仪器的观测效果相同,将地倾斜观测量转换为加速度表达后,其幅频特性符合全球地震背景噪声模型。改进后的VP型垂直摆倾斜仪对于远距离震级不大的同震体波震相记录效果略优于改进前,但受地脉动影响,在识别非地脉动信号时需要采用更精细的方法和手段来提高识别效果。  相似文献   

单变量特征选择的苏北地区主要农作物遥感识别   总被引：2，自引：0，他引：2  

王娜  李强子  杜鑫  张源  赵龙才  王红岩 《遥感学报》2017,21(4):519-530

遥感识别多源特征综合和特征优选是提高遥感影像分类精度的关键技术。农作物遥感识别中,识别特征的相对单一和数量过多均会导致作物识别精度不理想。随机森林(random forests)采用分类与回归树(CART)算法来生成分类树,结合了bagging和随机选择特征变量的优点,是一种有效的分类方法。单变量特征选择(univariate feature selection)能够对每一个待分类的特征进行测试,衡量该特征和响应变量之间的关系,根据得分舍弃不好的特征,优选得到的特征用于分类。本文基于随机森林和单变量特征选择,利用多时相光谱信息、植被指数信息、纹理信息及波段差值信息,设计多组分类实验方案,对江苏省泗洪县的高分一号(GF-1)和环境一号(HJ-1A)影像进行分类研究,旨在选择最佳的分类方案对实验区主要农作物进行识别和提取。实验结果表明:(1)多源信息综合的农作物分类精度明显高于单一的原始光谱特征分类,说明不同类型特征的引入能改善分类效果;(2)基于单变量特征选择算法的优选特征分类效果最佳,总体精度97.07%,Kappa系数0.96,表明了特征优选在降低维度的同时,也保证了较高的分类精度。随机森林和单变量特征选择结合的方法可以提高遥感影像的分类精度,为农作物的识别和提取研究提供了有效的方法。  相似文献   

基于华浩超算平台几何精校正模块的波段配准研究     

阳俊  张敏  李方方 《测绘与空间地理信息》2017,(1)

KOMPSAT3(阿里郎三号)卫星携带高分辨率0.7 m全色和2.8 m多光谱有效载荷,回访周期短,覆盖范围广,得到了广泛的应用。但由于受太阳辐射、大气干扰、云折射等物理因素的影响,造成波段之间在局部区域图像上发生非线性几何畸变,导致多光谱假彩色合成数据产生重叠现象,严重影响多光谱数据质量。本文针对在极端条件下产生的图像局部非线性几何畸变现象,探索国内外各种波段间配准方法,研究发现基于华浩超算平台的几何精校正算法能很好地达到波段间配准效果,消除了多光谱假彩色合成数据的影像重叠现象。  相似文献   

基于GF-1的坑塘信息精确提取方法研究     

齐永菊  裴亮  雷济升 《测绘与空间地理信息》2017,(3)

以国产高分一号2 m全色、8 m多光谱遥感影像作为数据源,选择廊坊市文安县作为研究区域,针对坑塘信息精确提取问题,采用单波段阈值法、监督分类法、面向对象方法等进行实验研究,重点研究了面向对象方法,结合运用遥感影像光谱、纹理、形状等特征,分析坑塘与其他地物之间的差异,最终实现坑塘信息的精确提取。  相似文献   

高塔,高层建筑物振动与形变的超长摆综合观测     

何世海 《地震》1997,17(4):380-388

高大建筑物（如电视塔等）在外力作用和自身老化过程中出现的形变和振动频率特性变化的监测，是灾害预测和工程检验的重要内容。具有测站移动坐标系的超长摆观测系统，可以胜任这一超宽频（0～100HZ）振动和挠曲综合观测要求。文中导出超长摆观测方程xi＝－（R~2_iQ~2_s＋P~2_i－2R_iQ_sP_icosγ_s）~(1/2)Xmsin（ωt＋θ_i）并论证了在相应参数选择下，此系统具有足够的振幅放大系数（S_i≥0．8）和振动周期观测覆盖范围；对超低频一永久形变也具有真实的监测能力（S_i＝P_i）；具有监测频带宽、动态测量范围大、无漂移、抗干扰等优点。  相似文献   

影像特征匹配的动态规划方法     

郑肇葆 《测绘学报》1992,21(4):267-271

  相似文献   

Development of composite planar fabric in mylonites along the Median Tectonic Line, southwest Japan     

Hideo  Takagi 《Island Arc》1992,1(1):92-102

Abstract Mylonites along the Median Tectonic Line, southwest Japan commonly contain shear bands comprising S(-C)-Ss fabrics. This paper stresses the lithologic control on the orientation, dimension and development of shear bands by comparing the microstructure of the shear bands in different rock types (P mylonites, F mylonites, micaceous phyllonite and quartzose phyllonite). There is no significant change of the α angles (average 21–24°) between Ss and S toward the centre of the shear zone (viz. increasing the intensity of mylonitization) and it is different from the S-C relationship in a narrow sense.
The generation of the composite planar fabric can be classified into four different strain partitioning models: S only type without any slip surface (model A); S-C type (model B); S-Ss type with Ss-slip precedence (model C), and S-Ss type with S-slip precedence (model D). Model C is proposed in this paper and is similar to the model for the generation of Riedel shears in brittle shear zones. An unstable slip between porphyroclasts and the matrix during ductile flow can easily initiate shear bands. Formation of a composite planar fabric is initiated according to model A, followed by model C in conditions of increasing strain, and then model D when the angle between S and the shear zone boundary becomes small enough (α/2 = 10°) to produce S-slip. Thus the generation of the shear bands probably begins in the early stages of shear deformation and continues until the latest stages.  相似文献   

森林航空摄影比例尺和森林判读像片放大倍数的研究     

黄福奎  李留瑜  邓中畅 《遥感学报》1990,(1)

为了确定森林航空摄影的最佳比例尺和波段以及判读像片的放大倍数,我们在广东省南昆山林业遥感试验场,测定了地物光谱,拍摄了不同比例尺的多光谱片和彩色红外片,进行了内业判读、野外检测和综合分析。本文讨论了航空摄影机、胶片、地物光谱反射系数和摄影位移等因素对像片分辨力的影响,用经验关系式估算了南昆山像片的影像分辨力,阐述了内业判读和实地检测的情况。试验表明,在所试验的波长附围内绿波段表达森林影像的效果最佳,用于森林判读的影像分辨力宜放大到3.5线/毫米,若用新型航空摄影机和高分辨力胶片,则用于森林资源调查分类判读的像片比例尺可缩小到1:4.8万。  相似文献   

The Influence of Undersea Feature Naming on Delimitation of Continental Shelf: A Case Study of Japan     

Huang Wenxing  Zhu Benduo  Liu Liqiang  Zhang Jinpeng 《地球科学进展》2016,31(8):811-819

Base on the tracing study on the Japanese undersea feature naming activity, this study shows that, Japan has named Bando Basin, removed Hangetsu Trough, Shingetsu Hole and Oki-Daito Trough, and altered some features names near Ogasawara Plateau and Oki-Daito Ridge, before and after the submission for Delimitation in outer limits of continental shelves. Contrary to the general undersea feature naming rule, these actions aim to extend its continental shelf boundaries. It is suggested that the study of relationships between naming undersea feature and marine right and interest should be enhanced.  相似文献   

Discovering Crustal Deformation Bands by Processing Regional Gravity Field   总被引：1，自引：0，他引：1  

YANG Wencai  SUN Yanyun 《《地质学报》英文版》2016,90(1):66-74

Objectives: This article presents a new computational procedure to discover scratches buried in the earth's crust. We also validate this new interdisciplinary analysis method with regional gravity data located in a well-known Dabie orogenic zone for test. Methods: Based on the scratch analysis method evolved with mathematical morphology of surfaces, we present a procedure that extracts information of the crustal scratches from regional gravity data. Because the crustal scratches are positively and highly correlated to crustal deformation bands, it can be used for delineation of the crustal deformation belts. The scratches can be quantitatively characterized by calculation of the ridge coefficient function, whose high value traces delineate the deformation bands hidden in the regional gravity field. In addition, because the degree of crustal deformation is an important indicator of tectonic unit divisions, so the crust can be further divided according to the degree of crustal deformation into some tectonic units by using the ridge coefficient data, providing an objective base map for earth scientists to build tectonic models with quantitative evidence. Results: After the ridge coefficients are calculated, we can further enhance the boundary of high ridge-coefficient blocks, resulting in the so-called ridge-edge coefficient function. The high-value ridge-edge coefficients are well correlated with the edge faults of tectonic units underlay, providing accurate positioning of the base map for compilation of regional tectonic maps. In order to validate this new interdisciplinary analysis method, we select the Dabie orogenic zone as a pilot area for test, where rock outcrops are well exposed on the surface and detailed geological and geophysical surveys have been carried out. Tests show that the deformation bands and the tectonic units, which are conformed by tectonic scientists based on surface observations, are clearly displayed on the ridge and ridge-edge coefficient images obtained in this article. Moreover, these computer-generated images provide more accurate locations and geometric details. Conclusions: This work demonstrates that application of modern mathematical tools can promote the quantitative degree in research of modern geosciences, helping to open a door to develop a new branch of mathematical tectonics.  相似文献