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961.
中国学者在暴雨滑坡、泥石流预测预报研究领域取得的成果为采用数字滑坡技术进行暴雨滑坡、泥石流预警、监测模型研究提供了宝贵的基础,应用数字滑坡技术建立暴雨滑坡、泥石流预测模型的原则是:(1)必须在滑坡、泥石流形成条件理论指导下;(2)应了解研究区地质环境及滑坡、泥石流特征;(3)就基于数字滑坡技术而言,只能选取遥感方法可能...  相似文献   
962.
三眼峪特大泥石流形成的物源条件分析   总被引:1,自引:0,他引:1  
通过对舟曲县"8.8"特大山洪泥石流三眼峪沟进行现场调查,从泥石流的岩土体类型及特征、地质构造、水文地质、新构造运动及地震等方面,对物源条件的地质环境背景进行了总结.调查结果表明:①三眼峪沟泥石流的松散固体物质主要包括崩塌堆积物、滑坡堆积物、残坡积物和冲洪积物.②三眼峪沟松散固体物质总量4079.42×104m3,流域...  相似文献   
963.
采用RT-PCR和快速扩增cDNA末端(rapid amplification of cDNA ends, RACE)技术首次克隆了曼氏无针乌贼?-肌动蛋白基因的 cDNA 全序列, 该序列全长为 2000bp, 由长 197bp 的 5’非翻译区(untranslated region, UTR), 669bp 的 3’非翻译区, 和 1134bp 的开放阅读框(open reading frame, ORF)组成。阅读框共编码 377 个氨基酸, 推算的分子量约为 42.0kDa, 理论等电点为 5.16。曼氏无针乌贼-actin 氨基酸序列中 Ile12、Ser172、Ser174、Gln223、His227、Ile231、Gly232、Ser320、Glu328、 Thr360等10个氨基酸残基具有特异性, 以及2个特殊的氨基酸残基位点和2个软体动物特有的氨基酸残基。曼氏无针乌贼?-actin 氨基酸序列与软体动物、节肢动物、脊椎动物的相似性高达 97%。NJ法系统进化分析显示曼氏无针乌贼首先与软体动物聚在一起, 然后与节肢动物聚在一起, 再与鱼类、两栖类、哺乳类聚在一起。  相似文献   
964.
研究采用GPS技术进行长距离输气(油)管道沿线地质灾害监测的理论和方法,主要分析滑坡体表面的形变,同时结合雨量监测和裂缝监测分析滑坡体的形变.研究表明:GPS技术可以有效地对地质情况复杂区域的地质灾害体进行监测,分析其滑移状态,为工程的灾前治理提供科学依据.  相似文献   
965.
The Walker circulation (WC) has always been an important issue in atmospheric science research due to the association between the WC and tropical Pacific sea surface temperature (SST), and between the WC and ENSO events. In this paper, a new index-Omega index (OMGI) - is constructed for WC characterization based on the NCEP / NCAR reanalysis data of monthly mean vertical velocity in recent 70 years (1948-2017). Results show that the OMGI can accurately depict the variation characteristics of WC on seasonal, annual and decadal time-scales. There is a significant inverse correlation between the OMGI and equatorial eastern and central Pacific SST. Meanwhile, the peak of the OMGI appears ahead of the ENSO peak, and therefore is able to reflect the SST in the equatorial Pacific. Especially, in 35 ENSO events, the peak of the OMGI appears earlier than Ni?o 3.4 index for 19 times with 2.6 months ahead on average. In 16 El Ni?o events, the peak of the OMGI occurs ahead of the El Ni?o for 9 times with 4 months ahead on average. In 19 La Ni?a events, the OMGI peak arises 10 times earlier than the La Ni?a peak, with an average of 1.4 months ahead. OMGI shows obvious leading effect and stability over ENSO events with different strengths and types of single peak and multi peaks: the peak of the OMGI keeps about 2-3 months ahead of the ENSO. Compared with other WC indexes such as UWI and SPLI, OMGI has some advantages in the ability to describe WC changes and present the probability and thetime of prediction of ENSO event peaks.  相似文献   
966.
快速、准确地判别滑坡灾害范围对灾情评估与救灾指挥至关重要。将高分辨率航空影像和机载LiDAR数据相结合,能充分利用滑坡体的光谱特征、几何形态与空间结构特征,提高滑坡识别的准确度。该文以海地地震诱发的滑坡识别为例,介绍了面向对象的滑坡识别思路及方法;针对海地滑坡灾害特点,选择了相应的灾害特征,并经反复试验设定了特征参数阈值;针对面向对象分类过程中特征组合与选择这一瓶颈问题,以河流沉积物和滑坡判别为例,通过特征组合试验与对比分析,发现基于NDVI与坡度特征组合的分类结果明显优于单一特征及其它组合模式的分类结果。与最大似然分类法相比,该方法的分类结果更为准确、精度更高。  相似文献   
967.
On July 22, 2011 and in the active region NOAA 11259 there ap- peared the event of the ejection of solar atmospheric Hα surges. According to the full-disc Hα observations of the Big Bear Solar Observatory in United States, three consecutive surges at one and the same place in the north of the main spot of the active region were discovered. The trajectories of these three surges exhib- ited the ?gure of straight lines, and their integral con?guration is like an inverted Eiffel Tower. The ?rst two surges are quite similar, and in each of them there appeared two bright points in the northern part of the main spot. After several minutes, the surges appeared in the midst of bright points. When the bright- ness of the bright points attained the maximum value, the surges spouted out from the midst of bright points. And after reaching the maximum altitude, they quickly vanished. Before the ejection of the third surge took place, no bright points appeared. Besides, its maximal altitude is merely one half of that of the ?rst two surges. Via a comparison with the SDO/HMI (Solar Dynamics Obser- vatory/Helioseismic and Magnetic Imager) data of radial magnetic ?elds, it is found that in more than one hour before the appearance of the ?rst surge there emerged bipolar magnetic ?elds in the region of ejection. Besides, in several min- utes before the ejection of each Hα surge the magnetic ?uxes of positive polarity diminished. Via our analysis it is found that there appeared reconnections be- tween the newly emerging satellite magnetic ?elds and the preexisting magnetic ?elds in the spot, and this caused the continuous ejections of Hα surges.  相似文献   
968.
969.
关于近地小行星轨道演化的初步探索   总被引:2,自引:0,他引:2  
刘林  季江徽 《天文学报》1997,38(4):337-352
本文采用改进的显式辛算法和嵌套的PKF7(8)积分器同时对86颗已命名(或编号)的近地小行星的轨道演化进行了数值研究,在103-104年的时间尺度上,给出了这些小行星轨道演化的状况以及它们与几颗大行星靠近的最小距离,特别是与地球接近的最小距离可小于0.01天文单位,甚至可能比月球还更靠近地球.  相似文献   
970.
Macroscopic frictional slip in water-saturated granular media occurs commonly during landsliding, surface faulting, and intense bedload transport. A mathematical model of dynamic pore-pressure fluctuations that accompany and influence such sliding is derived here by both inductive and deductive methods. The inductive derivation shows how the governing differential equations represent the physics of the steadily sliding array of cylindrical fiberglass rods investigated experimentally by Iverson and LaHusen (1989). The deductive derivation shows how the same equations result from a novel application of Biot's (1956) dynamic mixture theory to macroscopic deformation. The model consists of two linear differential equations and five initial and boundary conditions that govern solid displacements and pore-water pressures. Solid displacements and water pressures are strongly coupled, in part through a boundary condition that ensures mass conservation during irreversible pore deformation that occurs along the bumpy slip surface. Feedback between this deformation and the pore-pressure field may yield complex system responses. The dual derivations of the model help explicate key assumptions. For example, the model requires that the dimensionless parameterB, defined here through normalization of Biot's equations, is much larger than one. This indicates that solid-fluid coupling forces are dominated by viscous rather than inertial effects. A tabulation of physical and kinematic variables for the rod-array experiments of Iverson and LaHusen and for various geologic phenomena shows that the model assumptions commonly are satisfied. A subsequent paper will describe model tests against experimental data.  相似文献   
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