基于PixelGrid系统的无人机影像空三加密及影像图制作

探讨了基于PixelGrid系统下的无人机影像空三加密方法、工艺流程及正射影像图制作。     

基于水平集的海岛（礁）提取

提出了适合航空影像区域分割的水平集运算策略,将原始影像首先进行格网分类,对分类后的海岸线格网进行水平集运算提取精确海岛（礁）边缘,并采用多核编程策略提高运算效率。实验表明该方案效果理想,能够正确提取海岛（礁）区域。     

基于ADS 40数据的现状图测绘

新疆伊犁河谷土地开发整理现状图测绘由于其作业范围广,精度要求高,采用了ADS 40数字航空摄影数据。本文主要阐述了基于ADS 40数据进行航测外业和内业完成伊犁河谷4 000 km2的现状图测绘的生产过程。     

“摄影与航空摄影”课程互动式教学模式的研究

互动式教学模式以培养学生学习的自主意识和创新能力为目标,既发挥教师的主导作用,又充分体现学生的认知主体作用。摄影与航空摄影是遥感科学与技术专业的专业基础课程,本文提出了针对该课程的互动式教学模式,并进行了课堂教学实践,总结了该模式的创新点和应用价值。     

机载LiDAR点云数据与影像数据融合

分析机载LiDAR系统获取的点云数据与影像数据的优缺点,从而取长补短,将二者进行叠加融合,并成功地将航空影像的光谱信息赋给相对应的LiDAR点云,弥补了LiDAR点云在光谱信息方面的缺陷,为LiDAR点云数据的后续处理提供重要的信息支持。     

融合航空影像的LiDAR地物点云分类

点云滤波分类是LiDAR后续应用的基础工作,在点云滤波的基础上,以航空影像为辅助条件,结合点云高程信息,设计一套地物点云的分类方法。该方法首先融合航空影像与LiDAR数据,将对应RGB值赋予每个点,根据植被的光谱特征提取出部分植被点云;然后再根据文中定义的点云高程纹理,在剩余地物点云中提取出建筑物点,最后根据回波次数信息分离出剩余植被点,完成地物点云的分类。采用北京凤凰岭地区一组机载LiDAR数据进行实验。实验结果表明,该方法能够有效地将地物点云进行分类并且满足一定的精度要求,具有一定的实用价值。     

基于航空面阵图像快速制作冰雪覆盖地区影像镶嵌图的技术

无控制点快速处理、制作高山冰雪覆盖地区影像镶嵌图的技术和方法,在新疆喀什慕士塔格峰测区,采用ERDAS9.2LPS软件和UCXp面阵数字航空相机数据,验证了该方法的可行性。     

数字航摄仪在架空送电线路上的应用研究

随着航空摄影的发展,传统航摄仪已明显表现出其局限性,数字航摄仪在影像质量及效率等多方面的优势已愈见明显,其中DMC数字航摄仪已得到广泛应用。文章结合实际生产项目,利用DMC数字航摄仪进行摄影,对摄影比例尺、控制点布控、作业流程、作业方法及加密成图等情况进行了分析和比较。     

川藏公路中段地质灾害现象的航空遥感研究

川藏公路巴塘至林芝段位于我国青藏高原东南部,该地区是现今地壳运动十分强烈的地区之一,地形起伏强烈,气候变化多样,因此地质灾害十分发育,川藏公路就穿过这样一个复杂的地区。为查明公路沿线的地质灾害分布情况,90年代初,地矿部航空物探遥感中心沿川藏公路进行了彩色红外航空摄影,比例尺为1∶6万。通过彩色红外航片的解译及野外实地观测,圈定出滑坡、泥石流及崩塌等灾害现象,并对这些灾害的强度、活动性及其对公路的影响进行分析,最后对灾害成因及治理方法提出了建议。     

Effect of pedogenesis on the stable isotopic composition of calcretes and n‐alkanes: Implications for palaeoenvironmental reconstruction

In a fluvial system, depending on sub‐aerial exposure, non‐pedogenic pond calcretes can be modified into pedogenic calcretes. The present study attempts to understand the effect of sub‐aerial exposure and pedogenesis on calcretes using carbon and oxygen isotopic composition. For this purpose, two profiles (profile‐A and profile‐B) from the same stratigraphic level in Rayka from the western part of India were selected. The profiles are separated by a distance of 500 m and showed differences in calcrete characteristics. In profile‐A, the calcretes showed pedogenic features (root traces and void filling spar) whereas calcretes in profile‐B showed non‐pedogenic characteristics (fine laminations). However, some of the calcretes in profile‐A exhibited remnants of fine laminations suggesting that initially the calcretes had a non‐pedogenic origin but were modified due to pedogenesis. In profile‐A, the carbon and oxygen isotope values of pedogenic calcrete (δ¹³C_PC and δ¹⁸O_PC) showed more variation compared with non‐pedogenic pond calcretes (δ¹³C_SPC and δ¹⁸O_SPC) in profile‐B. The δ¹³C_PC and δ¹³C_SPC values exhibited a spread of 3·0‰ and 1·3‰, respectively, and δ¹⁸O_PC and δ¹⁸O_SPC values showed a spread of 2·3‰ and 1·3‰, respectively. The differences in the isotopic composition between the two profiles suggest that pedogenesis controlled the isotopic inheritance in calcretes. In addition, the carbon isotopic composition of organic matter (δ¹³C_OM) and n‐alkanes (δ¹³C_n‐alk) that forms the basis of palaeovegetational reconstruction have also been measured to understand the effect of pedogenesis on organic matter in both of the profiles. The average δ¹³C_OM values in profile‐A and profile‐B are ?23·4‰ and ?21·1‰, respectively. The disparity in δ¹³C_OM values is a result of the difference in the sources and preservation of organic matter. However, the δ¹³C_n‐alk values show a similar trend in profile‐A and profile‐B, indicating that sources of n‐alkanes are the same in both of the profiles and δ¹³C_n‐alk values are unaffected by the pedogenic modifications.