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901.
Ionospheric electromagnetic perturbations observed on DEMETER satellite before Chile M7.9 earthquake 下载免费PDF全文
Xuemin Zhang Jiadong Qian Xinyan Ouyang Xuhui Shen Jin an Cai Shufan Zhao 《地震科学(英文版)》2009,22(3):251-255
Based on the ionospheric electromagnetic data observed on DEMETER satellite of France, the ionospheric electromagnetic signals were analyzed within 10 days before Chile M7.9 earthquake on November 14, 2007. It is found that, low frequency electromagnetic disturbances began to increase in a large scale of latitude, and reached to a maximum one week prior to the earthquake, and at about three days before the quake, the peak values shifted to lower latitude. Taking three days as a group, spatial images of a few parameters were analyzed, from which it can be seen during the five days prior to this earthquake, the amplitude and scale of anomalies are enlarged, while the epicenter is located at the boundary of anomalous region. The anomalous tempo-spatial variation in electron density prior to the earthquake were also obtained in terms of tracing the data from revisited orbits in half a year prior to the quake. 相似文献
902.
Kunhong Li Zhining Liu Bin She Hanpeng Cai Yaojun Wang Guangmin Hu 《Geophysical Prospecting》2021,69(1):85-100
Dictionary learning is a successful method for random seismic noise attenuation that has been proven by some scholars. Dictionary learning–based techniques aim to learn a set of common bases called dictionaries from given noised seismic data. Then, the denoising process will be performed by assuming a sparse representation on each small local patch of the seismic data over the learned dictionary. The local patches that are extracted from the seismic section are essentially two‐dimensional matrices. However, for the sake of simplicity, almost all of the existing dictionary learning methods just convert each two‐dimensional patch into a one‐dimensional vector. In doing this, the geometric structure information of the raw data will be revealed, leading to low capability in the reconstruction of seismic structures, such as faults and dip events. In this paper, we propose a two‐dimensional dictionary learning method for the seismic denoising problem. Unlike other dictionary learning–based methods, the proposed method represents the two‐dimensional patches directly to avoid the conversion process, and thus reserves the important structure information for a better reconstruction. Our method first learns a two‐dimensional dictionary from the noisy seismic patches. Then, we use the two‐dimensional dictionary to sparsely represent all of the noisy two‐dimensional patches to obtain clean patches. Finally, the clean patches are patched back to generate a denoised seismic section. The proposed method is compared with the other three denoising methods, including FX‐decon, curvelet and one‐dimensional learning method. The results demonstrate that our method has better denoising performance in terms of signal‐to‐noise ratio, fault and amplitude preservation. 相似文献
903.
为了解河流大型底栖动物对环境压力的响应关系,以人类干扰程度不同的太湖流域和巢湖流域为研究区,系统调查区域内河流大型底栖动物,结合水体、沉积物理化数据及生境质量状况,运用空间分析和多元统计分析等方法,探讨了大型底栖动物多样性及典型物种对关键环境因素的响应规律.结果表明,太湖流域和巢湖流域的环境质量和大型底栖动物群落结构均差异较大,巢湖流域的生境质量优于太湖流域,巢湖流域平原区部分点位的水体营养盐(特别是氮浓度)高于太湖流域平原区.巢湖流域丘陵区的敏感型物种(主要为水生昆虫)密度远高于太湖流域丘陵区,太湖流域丘陵区的耐污型物种(寡毛纲)平均密度稍高于巢湖流域丘陵区,而巢湖流域平原区的寡毛纲霍甫水丝蚓(Limnodrilus hoffmeisteri)和苏氏尾鳃蚓(Branchiura sowerbyi)平均密度远高于太湖流域平原区.广义加性模型建立的响应关系曲线表明,栖境多样性和总氮浓度可以作为生物多样性的指示因子.铜锈环棱螺(Bellamya aeruginosa)、椭圆萝卜螺(Radix swinhoei)、河蚬(Corbicula fluminea)、霍甫水丝蚓、苏氏尾鳃蚓、黄色羽摇蚊(Chironomus flaviplumus)等特征物种与特定环境因子的响应关系显著,这些物种也可以作为环境监测的指示物种.底栖动物环境梯度的响应曲线能够定量地描述底栖动物群落对环境因子的响应关系,有利于深入了解水体水质、营养状态及生境质量与大型底栖动物群落结构的相关关系,进而预测不同人为干扰下大型底栖动物群落结构的变化趋势和演替过程. 相似文献
904.
Torsional response of pile embedded in a poroelastic medium 总被引:1,自引:0,他引:1
Yuanqiang Cai Gang Chen Changjie Xu Dazhi Wu 《Soil Dynamics and Earthquake Engineering》2006,26(12):1143-1148
The response of a cylindrical elastic pile embedded in a homogeneous poroelastic medium and subjected to torsional loading is studied for the first time. Based on the Muki's model, the pile-porous medium system is decomposed into a fictitious pile system and an extended porous medium system. The one-dimensional, vertical, elastic pile and the three-dimensional poroelastic medium are solved, respectively. Considering the mixed boundary-value conditions at the interface of pile and soil, a Fredholm's integral equation of the second kind for the bar-force is established. The force and the displacement of the pile are calculated by applying numerical quadrature. 相似文献
905.
906.
907.
The Contemporary Tectonic Strain Rate Field of Continental China Predicted from GPS Measurements and its Geodynamic Implications 总被引:7,自引:0,他引:7
In Appling studies, the strain rate in China has been computed from using different methods, resulting in quite different
estimates of the strain rate the geo-statistics from GPS velocity field of Chinese continent, we obtain the velocity value
at each little regularly spaced grid point, by kriging interpolation and the component of strain rate for each volume element,
using a method similar to the derivation of shape functions in the finite element algorithm. Therefore the distribution of
the strain rate field in whole for the Chinese continent is presented. The result shows that the orientations of principal
strain rates are consistent with those of the P and T axes of focal mechanisms. The distribution of maximum shear strain rate
clearly delineates some major active fault zones surrounding the Tibetan Plateau. The maximum shear strain rate is comparable
with that obtained from analysis of seismic moment release. In part of the Tibetan Plateau containing normal faults and pull-apart
grabens, we obtain an extensional state of strain. The absolute value of the strain rate in West China is approximately 5
times larger than that of East China, and the pattern of the strain rate field in most of the Chinese continent is controlled
by the India/Eurasia collision. 相似文献
908.
909.
本文试图探索在现有各种预报手段的基础上逐渐形成一种比较客观、比较定量的综合预报技术的可能性,並提出一种地震预报的综合概率模式,供地震部门参考,並希望广大地震预报工作者能对这个问题展开讨论。 相似文献
910.
应用云南地区地壳上地幔速度结构、电性结构和热结构等深部地球物理探测研究结果,讨论了云南地区大地震发生的深部地球介质构造背景.结果表明,上地壳高速区、壳内低速区或高导层、上地幔局部上隆、高热活动、深大断裂等深部介质构造背景的存在,与云南地区大地震的发生有着密切的联系.6,7级大震不是在任何地方都会发生,而是发生在一些具有某种深部介质构造背景的地区.5级及其以下地震的活动无显著的介质构造背景存在,其发生具有很大的随机性. 相似文献