Based on data collected by deep seismic sounding carried out in 1999, a three-dimensional P wave velocity structure is determined with tomographic inversion. The tomographic result shows that there is a P wave low vel...Based on data collected by deep seismic sounding carried out in 1999, a three-dimensional P wave velocity structure is determined with tomographic inversion. The tomographic result shows that there is a P wave low velocity zone (LVZ) in the upper crust beneath the Tengchong volcanic area. The LVZ is in the depth of 7~8 km and may be a small magma chamber or a partial melting body. The result also shows that the LVZ is in the northeastern side of the Rehai hydrothermal field, which is located in another LVZ near the surface. The shallow LVZ may represent a well-developed fracture zone. The strong hydrothermal activity in Rehai area can attribute to the existence of fractures between two LVZs. These fractures are the channels for going upwards of the deep hot fluid.展开更多
苗期作物三维结构的精准高效重建是获取表型信息的重要基础。传统的三维重建大多基于运动恢复结构-多视图立体视觉(Structure from motion and multi-view stereo,SFM-MVS)算法,计算成本高,难以满足快速获取表型参数的需求。本研究提出...苗期作物三维结构的精准高效重建是获取表型信息的重要基础。传统的三维重建大多基于运动恢复结构-多视图立体视觉(Structure from motion and multi-view stereo,SFM-MVS)算法,计算成本高,难以满足快速获取表型参数的需求。本研究提出一种基于神经辐射场(Neural radiance fields,NeRF)的苗期作物三维建模和表型参数获取系统,利用手机获取不同视角下的RGB影像,通过NeRF算法完成三维模型的构建。在此基础上,利用点云库(Point cloud library,PCL)中的直线拟合和区域生长等算法自动分割植株,并采用距离最值遍历、圆拟合和三角面片化等算法实现了精准测量植株的株高、茎粗和叶面积等表型参数。为评估该方法的重建效率和表型参数测量精度,本研究分别选取辣椒、番茄、草莓和绿萝的苗期植株作为试验对象,对比NeRF算法与SFM-MVS算法的重建结果。结果表明,以SFM-MVS方法重建点云为基准,NeRF方法重建的各植株点云点对距离均方根误差仅为0.128~0.395 cm,两者重建质量较接近,但在重建速度方面,本文研究方法相比于SFM-MVS方法平均重建速度提高700%。此外,该方法提取辣椒苗株高、茎粗决定系数(R~2)分别为0.971和0.907,均方根误差(RMSE)分别为0.86 cm和0.017 cm,对各苗期植株叶面积提取的R~2为0.909~0.935,RMSE为0.75~3.22 cm~2,具有较高的测量精度。本研究提出的方法可以显著提高三维重建和表型参数获取效率,从而为作物育种选苗提供更为高效的技术手段。展开更多
基金State Natural Science Foundation of China (D49974020), Joint Seismological Science Foundation of China (199110) and Project (95-11-01-06) during Ninth Five-Year Plan from China Seismological Bureau.
文摘Based on data collected by deep seismic sounding carried out in 1999, a three-dimensional P wave velocity structure is determined with tomographic inversion. The tomographic result shows that there is a P wave low velocity zone (LVZ) in the upper crust beneath the Tengchong volcanic area. The LVZ is in the depth of 7~8 km and may be a small magma chamber or a partial melting body. The result also shows that the LVZ is in the northeastern side of the Rehai hydrothermal field, which is located in another LVZ near the surface. The shallow LVZ may represent a well-developed fracture zone. The strong hydrothermal activity in Rehai area can attribute to the existence of fractures between two LVZs. These fractures are the channels for going upwards of the deep hot fluid.
