A large-scale obliquely inclined bedding rockslide, activated by a heavy rainstorm, occurred on July 8, 2020, at 7:05 (UTC?+?8) in Shiban Village, Songtao Miao Autonomous County, Guizhou Province, China. The loss of life in this event was greatly reduced owing to the local warning system for rainstorm-induced geohazards. To understand the failure characteristics, triggering factors, the genetic mechanism of the landslide, the geomorphological features, geological characteristics, hydrological conditions, and rainfall characteristics were systematically studied by a synthetic approach including field investigations, satellite imagery, unmanned aerial vehicle (UAV) photography, laboratory tests, and rainfall data statistics. The results indicated that the interface between the soft and hard rock, the well-developed joints, and the free face in front of the slope constituted the boundaries of this landslide. The concave topography at the back and southern edge of the landslide, the bare ground, and the cataclastic structure of the rock mass provided favorable conditions for the collection or infiltration of rainwater. The concentrated rainstorm was the direct trigger for the landslide, which led to a rapid inflow and retention of rainfall in the landslide through favorable landform and geological conditions. The groundwater recharge that cannot be drained in time caused the mechanical deterioration of rock mass and induced a rapid increase in pore water pressure in the landslide. Moreover, the water level of the Ganlong River at the toe of the slope also rose rapidly, and the uplift pressure in front of the slope increased accordingly. Under the combined action of these adverse factors, the overall anti-sliding force of the slope was less than the sliding force, finally resulting in the landslide. Remarkably, the local warning system for rainstorm-induced geohazards successfully forecasted the landslide, but the shortcoming is that the forecast time in advance is short. Nevertheless, the prediction has significantly reduced human casualties and provided valuable experience for the prediction of this type of landslide.
相似文献 |
|||||||
|
|||||||
|
排序方式： 共有12条查询结果，搜索用时 15 毫秒
1.
依托“西部煤炭资源高精度三维地震勘探技术”工程,对晋城矿区进行了旨在提高小断层,小陷落柱探测能力的高密度三维地震勘探。根据面元选择因素及该区地质任务,采用5m×5m网格进行野外数据采集;考虑炮检距、方位角、覆盖次数、排列片横纵比及煤层埋深（350～500m）等因素,采用中点放炮、60道接收,24次覆盖（横向4次,纵向6次）的8线16炮束状观测系统,基岩中激发。原始资料经同一处理流程后,获得5m×5m×1ms、5m×10m×1ms、10m×10m×1ms及2.5m×2.5m×1ms不同单元的三维数据体多个,通过对比可以发现小断层,小陷落柱在其小面元叠加时间剖面、顺层切片及相干切片都有清晰的反映。实例说明,小面元采集技术可以提高对小构造的纵、横向分辨能力,满足山区对三维地震精确勘探的要求。 相似文献
2.
由于随机噪声是一种频带较宽的干扰波,因此依靠单一的去噪处理方式往往难以获得清晰反映目标体的地震信息。小波变换能够较好的去除高斯噪声,保留有效波中、高频成分,提高记录的信噪比,但去除脉冲噪声的效果却并不理想;中值滤波具有良好的边缘保持特性,虽低频去噪声效果有限,但去除脉冲噪声效果明显。因此可利用二维小波变换与中值滤波优势互补的方法,进行叠前去噪处理,达到去除宽频随机噪声的目的。首先运用二维小波变换的理论,采用自适应门限阀值方法进行去噪,同时结合中值滤波方法联合去噪。模型与实际数据的应用效果表明,联合去噪方法可有效压制噪声能量、保留高频有效信号、提高地震记录信噪比与分辨率。 相似文献
3.
枣庄市山亭区位于枣庄市东北部,泰沂山区西南部,属低山丘陵区,全区大小山头1000多座,地形条件复杂,土地总面积1018．64km^2,山地丘陵占全区总面积的80％以上。山亭区的土地利用现状更新调查工作始于2004年,经过1年多的艰苦调查,查清了全区各类土地利用的现状,绘制了山亭区土地利用现状图,建成了山亭区土地利用数据库。2007年7月,山东省国土资源厅对山亭区的土地利用调查更新工作进行了验收。经验收,山亭区土地利用更新调查技术路线正确、方法先进,各项成果符合土地更新调查技术要求。 相似文献
4.
5.
三维地震勘探在干厚黄土浅煤层地区的应用 总被引：2，自引：0，他引：2
干厚黄土覆盖地区表浅层黄土结构疏松、无潜水位，对地震波吸收强烈，难以开展三维地震勘探，特别是在煤层埋深浅的干厚黄土覆盖丘陵地区。在河东煤田某矿区，经多次试验，采取“高叠加次数、小炮检距、单深井激发、组合接收”等采集技术措施，使用绿山初至折射静校正方法及浮动基准面叠加方法的资料处理技术，最终有效地压制了干扰，提高了信噪比，使反射波更加突出，成像效果明显。 相似文献
6.
7.
8.
随着情感成为城市品牌的重要资产,非营销人员介入的意义创造过程日益受到重视,从居民的角度解读情感的空间性为城市品牌研究提供了一个新的视角。运用案例研究和半结构式访谈的方法,以广州非裔聚居现象及其意义生产为例,探讨居民情感的发生如何受到媒体和生活经历的影响,审视居民情感对城市移民品牌塑造的作用,初步剖析居民情感驱动的城市移民品牌化的运作机制。研究表明,尽管地方政府并没有利用非裔聚居现象及其文化景观构建品牌叙事,但居民基于人地情感关系,感知、想象和认同地方的意义,进而无形地塑造着广州开放、包容的城市品牌。然而,居民情感也并非连续、统一的整体,城市内部的有机发展使居民与地方产生差异化的情感互动。在媒体表征与个体生活经历的影响下,居民对非裔群体的积极和消极情感分别对城市移民品牌化起到建设性和破坏性的作用。研究呼吁关注居民自下而上的情感表达对城市品牌构建的意义,以期为城市形象管理提供现实参考。 相似文献
9.
The Transition Between the Scale Domains of Ray and Effective Medium Theory and Anisotropy: Numerical Models 总被引：1，自引：0，他引：1
The anisotropy of a periodically layered isotropic medium is numerically modeled in order to study the effect of the scale
of heterogeneity on seismic observations. An important motivation is to delineate the wavelength ranges over which a pulse
propagating obliquely through the structure will be described by either ray (short wavelength) or effective medium (long wavelength)
theory. The same band-limited pulse is propagated obliquely at a variety of incidence angles through a compositionally uniform
layered structure as a function of the layer thicknesses. The resulting seismograms display similar behavior to that encountered
for normal incidence including the effects of stop- and pass-bands. Velocities determined from time picks on these seismograms
show a large difference in velocities between the long and short wavelength limits as has been previously demonstrated for
normal incidence propagation. The bulk of the transition between these two limits is independent of incidence angle and occurs
when the ratio between the wavelength and the layering thickness is near a value of 10. Two more geologically reasonable models
show that these effects are diminished with smaller contrasts between the layers. 相似文献
10.
Yu Haibing Li Changdong Zhou Jia-Qing Gu Xiaoping Duan Ying Liao Liufeng Chen Wenqiang Zhu Yinbin Long Jingjing 《Landslides》2022,19(5):1119-1130
|
| 设为首页 | 免责声明 | 关于勤云 | 加入收藏 |
|
Copyright©北京勤云科技发展有限公司 京ICP备09084417号 |