An open-accessed inventory of landslides triggered by the MS 6.8 Luding earthquake,China on September 5, 2022     

《地震研究进展（英文）》2023,3(1):100181

This study constructs a preliminary inventory of landslides triggered by the M_S 6.8 Luding earthquake based on field investigation and human-computer interaction visual interpretation on optical satellite images. The results show that this earthquake triggered at least 5 007 landslides, with a total landslide area of 17.36 ?km², of which the smallest landslide area is 65 ?m² and the largest landslide area reaches 120 747 ?m², with an average landslide area of about 3 500 ?m². The obtained landslides are concentrated in the IX intensity zone and the northeast side of the seismogenic fault, and the area density and point density of landslides are 13.8%, and 35.73 ?km^?2 peaks with 2 ?km as the search radius. It should be noted that the number of landslides obtained in this paper will be lower than the actual situation because some areas are covered by clouds and there are no available post-earthquake remote sensing images. Based on the available post-earthquake remote sensing images, the number of landslides triggered by this earthquake is roughly estimated to be up to 10 000. This study can be used to support further research on the distribution pattern and risk evaluation of the coseismic landslides in the region, and the prevention and control of landslide hazards in the seismic area.  相似文献   

山东临朐山旺组火山集块岩和辫状河道沉积物发现的意义——对李泰来等论点的质疑,兼述山旺化石的早期研究历史     

杨慕华  李风麟  罗照华 《现代地质》1991,5(3):273

山东临朐解家河盆地山旺组底部发现火山集块岩,下部有一层岩屑质长石砂岩,具清楚的板状交错层理.证明解家河盆地附近虽有火山活动,而解家河盆地本身并非天池式封闭型古火山口.为澄清山旺组建立的年代,简述了山旺组的早期研究历史.  相似文献   

A comparison of field and laboratory analytical methods for radon site investigation     

D. K. Talbot  J. D. Appleton  T. K. Ball  M. H. Strutt 《Journal of Geochemical Exploration》1998,65(1):79-90

Soil-gas radon measurements provide a valuable tool in assessing probable indoor radon levels on a regional basis. However, in Great Britain, seasonal weather changes can cause large changes in soil-gas radon concentration. Although this does not significantly constrain systematic radon potential mapping programmes, it does cause difficulties in responding to ad-hoc requests for site-specific radon investigations. The relationship between soil-gas radon and gamma spectrometry measurements made in the field with radon released from a representative sample of soil in the laboratory has been investigated as part of a program to develop a method of radon potential mapping and site investigation which can be used at any time of the year. Multiple soil and soil-gas samples were collected from sites underlain by bedrocks with widely varying radon potentials. For each geological unit, sites both free of and covered by glacial drift deposits were sampled. Soil and soil-gas samples were taken at the same depth of 60–100 cm. The effectiveness of these radon site investigation procedures has been evaluated by studying the relationship between the soil-gas radon, gamma spectrometry and radon emanation data with an independent estimate of the radon risk. The geologic radon potential (GEORP), which is the proportion of existing dwellings which exceed the UK radon Action Level (200 Bq m⁻³) for a particular combination of solid and drift geology within a defined geographic area, has been used for this study as the independent estimate of radon risk. Soil-gas radon, radon emanation and eU (equivalent uranium by field γ spectrometry) are all good geochemical indicators of radon risk (GEORP) in Derbyshire but only soil-gas radon correlates significantly with GEORP in Northamptonshire. Radon in soil gas discriminates more effectively between sites with different radon potential in Northamptonshire if soil permeability is also taken into account. In general, measurement of soil-gas radon in the field provides the most universally applicable indicator of radon potential. If soil-gas radon concentrations cannot be determined because of climatic factors, for example when the soil profile is waterlogged, measurement of radon emanation in the laboratory or measurement of eU can be used as radon potential indicators in some geological environments. This applies particularly in areas where the soil composition rather than the composition and permeability of the underlying rock or superficial deposits are the dominant controls of radon potential. It appears, therefore, that it may be necessary to use different radon site investigation methods according to the specific factors controlling radon emanation from the ground. In some cases no method will provide a reliable indicator of radon risk under unfavourable climatic conditions.  相似文献   

探地雷达在大面积场区岩土工程勘察中的应用：以苏丹喀土穆炼油厂为例     

刘红军  贾永刚 《海岸工程》1998,17(4):41-46

探地雷达是利用超高频脉冲电磁波深测地下介质分布的一种地球物理勘探方法,由于其高效快捷、高分辨率等特征,在浅层与超浅层地质调查中应用越来越广泛。本文以苏丹喀土穆炼油厂区勘察为例,介绍探地雷达在大面积场区岩土工程勘察中的应用,本次勘察目的是详细查明厂区岩土层分布、进行基岩风化带的划分、查明场区构造破碎带发育状况。由于采用了地质雷达探测,钻孔数由原先的500多个孔减少到了63个,工期由原来的6个月缩短为1个半月,大大缩短了勘察周期,节省了勘察经费,尤其对涉外工程,大大降低了间接费用。  相似文献   

鄱阳湖富营养化调查与评价   总被引：12，自引：6，他引：6  

吕兰军 《湖泊科学》1996,8(3):241-247

为了较全面了了解鄱阳湖水体的富营养化现状,于１９９２年５月１６日－６月３０日和１９９３年１月５日－２月４日在各河入湖口,湖区,候鸟保护区及长江九江大桥断面进行了调查。  相似文献   

滆湖氮、磷平衡研究   总被引：16，自引：1，他引：15  

黄文钰  舒金华  吴延根 《湖泊科学》1996,8(4):330-336

通过１９９２￣１９９３年千岛湖水质、底质、生物和污染源调查,对其水环境质量和污染物输入作了综合评价。结果表明,千岛湖水质状况良好;但局部水域水质污染逐年加重,湖泊已属中营养状态。非点源输入量占入湖污染总量的９５％,其中５０％来自上游安徽来水。建立了对流扩散模型并进行水质预测,提出了千岛湖水环境保护对策。  相似文献   

2003年淮河大水期间MCS的普查分析   总被引：8，自引：0，他引：8  

费增坪  郑永光  王洪庆 《气象》2005,31(12):18-22

利用GEOS-9卫星红外1云图对2003年6月21日至7月22日淮河流域大水期间的MCS做了普查分析.结果发现：（1）淮河大水期间共有10个MαCS和24个MβCS,其产生频数远大于常年的平均值;（2）绝大部分MCS初生于淮河流域并且其成熟时的位置位于淮河流域是造成这次大水的主要原因之一;（3）淮河流域大水期间部分MCS的形成时间与一般MCS有所不同.最后,结合常规资料对产生MCS的天气背景进行了分类,发现该期间MCS形成的天气背景具有多样性.  相似文献   

Ring permeametry: design,operation and error analysis     

N. A. Chappell  J. L. Ternan 《地球表面变化过程与地形》1997,22(13):1197-1205

Assessment of slope stability, soil management or contaminant transport problems usually requires numerous, yet accurate point measurements of permeability. This technical note describes a new method for the rapid field assessment of permeability in near-surface soils or unconsolidated sediments. The procedure is known as ‘ring permeametry’ and is an ex situ core-based method giving measurements which can be guaranteed to be stratum-specific, unlike measurements from some in situ techniques. The potential sources of precision and bias error within the method are quantified and their effect on the uncertainty of permeability estimates is illustrated. © 1997 John Wiley & Sons, Ltd.  相似文献   

四川省地文景观和水域景观资源分类方案研讨     

曹俊  郭建强  宁志中  陈斌  彭东 《四川地质学报》2020,40(1):169-172,176

四川省位于我国西南腹地、长江上游和我国陆地三级阶梯中的一、二级阶梯之间,由于地质构造和地貌的独特性、复杂性和多样性,所形成的地文景观和水域景观等自然景观丰富、类型多样,成为中国乃至全世界地质景观最为丰富、最具特色的地区之一,按2017年底发布实施的《旅游资源分类、调查与评价》分类方案不能很好地反映出四川省地文景观和水域景观特色与亮点,为此,在充分研究国标基础上,结合其他相关规范以及全省地文景观和水域景观特色,依据资源现存状况、形态、特性、特征主要分类原则将地文景观和水域景观划分为8亚类34基本类型,其中前者4亚类21基本类型、后者4亚类13基本类型,与国标相比,取消了四川没有的海面1个亚类及其相应的3个基本类型以及不便于识别的垂直自然带1个基本类型,划分的基本类型与国标一致的有16个、修改完善的有7个、新增加的有11个。对四川景观资源分类方案进行研讨。  相似文献   

绿色工程勘察钻探实施方案探索及应用          下载免费PDF全文

马映辉  贾宏福 《探矿工程》2020,47(11):29-36

绿色勘察是新发展理念在工程勘察行业的具体体现。钻探作为工程勘察各方法中最直观的手段而不可或缺,与之相关的环境问题也相对较多。通过分析工程勘察钻探特点、可能存在的环境问题,结合实际施工经验,不断探索,提出绿色工程勘察钻探实施方案,并在川藏铁路勘察实践中加以应用。思考与总结当前绿色工程勘察尚需解决的问题。倡导勘察、设计、施工单位和相关部门共同努力构建全方位、完善的绿色工程勘察体系。  相似文献