山字型构造形成的力学机制——地壳运动的力学模型之一(连载1)     

陈子光  薛爱民 《吉林大学学报(地球科学版)》1988,(3)

山字型构造为一种复杂的扭动构造体系,自从李四光教授提出以来,已有许多弹性解及数值解。本文以流变学理论研究了山字型构造的非稳定构造应力场,比较实际地反映出山字型构造体系在长期演化过程中发生、发展及形成规律。 本文在解决混合边界条件的弹性解答前提下,采用对应原理,通过拉普拉斯变换得出山字型构造的粘弹性解答。最后给出了山字型构造初期、中期、晚期的构造主应力迹线及等值线图(12幅),据此对三个时期的山字型构造各部位的构造形迹进行分析,并得出几点结论。  相似文献   

On the hydrodynamic behavior of supercooled water drops interacting with columnar ice crystals     

R. J. Schlamp  H. R. Pruppacher 《Pure and Applied Geophysics》1977,115(4):805-843

A numerical evaluation of the complete Navier-Stokes equations of motion for steady-state, incompressible flow past an infinite circular cylinder is given in terms of the stream function, vorticity, and pressure distribution past such bodies. A method is described which allows use of these flow characteristics: (1) to approximate the characteristics of air flow past hexagonal columnar ice crystals falling under gravity at terminal velocity in air, (2) to compute the trajectory of supercooled cloud drops relative to such ice crystals, and (3) to determine the efficiency with which short columnar ice crystals and needle shaped ice crystals collide with supercooled cloud drops. It is found that for all columnar type ice crystals riming is negligible if the cloud drop size is less than 5 m, and that for riming to commence short columnar crystals must have diameters larger than 50 m, while needle crystals must have diameters larger than 40 m. It is further shown that the collision efficiency cut-offs at the small drop radius and at the large drop radius end of the collision efficiency diagram can be explained on the basis of the cloud drop trajectories for these drop size ranges.  相似文献   

The origin of ozone-rich air in the middle stratosphere observed over Europe at the end of January 1979     

W. Braun  H. U. Dütsch 《Journal of Atmospheric Chemistry》1984,2(2):163-173

Daily ozone soundings over Switzerland in the winter of 1979 showed, at the end of January some extremely high values of the ozone mixing ration around the 10 mb level-9 to 10 ppm compared with a climatological mean of 6 ppm. At the same time, the temperature and ozone mixing ratio was measured by the LIMS experiment (Limb Infrared Monitor of the Stratosphere) on Nimbus 7. The single LIMS ozone profiles, as well as the LIMS 10 mb ozone maps, also showed extreme ozone maxima. Ozone transport was investigated by trajectory computations based on the LIMS geopotential height fields. Displacements and deformations of air parcel chains in 48 h were used to construct ozone maps, using the distribution on a previous day. The correspondence of such kinematically-constructed ozone maps using the actual LIMS maps is striking. This method is, thus, a strong indication of the self-consistency of the different LIMS products (ozone, temperature, geopotential) and explains the unusual ozone observations.  相似文献   

一种众源车载GPS轨迹大数据自适应滤选方法   总被引：1，自引：1，他引：0  

唐炉亮  杨雪  牛乐  常乐  李清泉 《测绘学报》2016,45(12):1455-1463

基于同步高低精度GPS轨迹数据的空间特征和GPS误差分布原理,提出了一种众源GPS车载轨迹大数据自适应分割-滤选模型。该模型首先通过角度、距离约束将完整的车载GPS轨迹数据进行分割,以轨迹分割段作为基本滤选单元;然后通过对比轨迹分割段内GPS轨迹向量与其参考基线间的相似度,按照相似度与GPS定位精度之间的量化关系指导滤选。试验结果表明,该方法可以实现车载轨迹大数据按信息提取精度需求的滤选。  相似文献   

非均匀沙运动特性试验          下载免费PDF全文

许琳娟  曹文洪  刘春晶 《水科学进展》2016,27(6):841-848

天然河流床沙通常为非均匀沙,准确把握非均匀沙颗粒运动规律是模拟和预测天然河流河床演变的基础。开展了恒定均匀流条件下的非均匀沙推移质运动水槽试验,床沙粒径范围为0.10~20 mm。利用摄像机从顶部拍摄了粗化条件下的推移质颗粒运动,获取大量非均匀沙颗粒的运动轨迹,提取了颗粒运动速度、走停时间等基本运动参数,推移质运动颗粒粒径范围为0.74~8.19 mm。试验结果表明,非均匀沙床面聚集体或大颗粒使推移质颗粒运动方向发生改变,与均匀沙成果相比,非均匀沙推移质颗粒的纵向运动速度减小,横向运动速度增大;推移质颗粒纵向运动速度遵循指数分布,单次运动速度遵循Γ分布,横向运动速度及运动速度矢量角则遵循正态分布。  相似文献   

Geostatistics applied to best-fit interpolation of orientation data     

C. Gumiaux  D. Gapais  J. P. Brun 《Tectonophysics》2003,376(3-4):241-259

Automatic methods used in geosciences to interpolate between orientation data have often limited applicability and strength, in particular where large ranges of orientations occur. In this paper, we show that geostatistical methods yield rather strong and powerful results when applied to directional data. The procedure involves the calculation of variograms, followed by a kriging interpolation of the data. In order to free from the circular property of directional data, the treatment of initial angular data sets is performed using scalar values provided by the direction cosines of double-angle values. The strength and application of the method are demonstrated by the analysis of theoretical and natural data sets. Natural examples are focused on the calculation and the analysis of cleavage trajectory maps.  相似文献   

顾及路网与轨迹多模特征的道路等级分类研究     

张彩丽  向隆刚  李雅丽  林志勇 《地球信息科学学报》2022,24(10):1925-1940

道路等级不仅反映在路网结构的静态骨架信息上,也蕴含在轨迹数据呈现的动态语义信息上。为解决(OpenStreetMap)OSM路网部分路段及路网生成产品等级缺失问题,本文提出一种顾及路网与轨迹多模特征的道路等级分类方法。首先通过轨迹数据的清洗、地图匹配和基于路名的路网合并实现轨迹点与命名道路的联结;然后以命名道路为分析单元,综合考虑路网及轨迹数据,在系统分析路网结构的道路几何特征、道路分布特征、道路拓扑特征及道路单双向信息基础上,进一步挖掘与融合轨迹数据蕴含的道路宽度、道路车流量、道路速度等静动态特征,形成关于道路等级的描述特征集,作为识别道路等级的基础与依据;最后以随机森林(RF)为基本分类器进行特征选择及模型训练实现道路等级识别。为验证本文方法,选取武汉市汉正街区域及二环区域,基于OSM路网数据及众源轨迹数据开展试验。该方法取得了较好的分类结果,小范围汉正街区域的验证集准确率为91.2%,大范围二环区域的验证集准确率达到80.8%。与单类特征相比,集成路网与轨迹特征极大提高了道路等级分类准确率;与原始路段形式进行道路等级分类相比,以路名重构道路形式进行道路等级分类效果更好。  相似文献   

船舶轨迹数据的Geodatabase管理方法     

陈金海  陆锋  彭国均  柯冉绚 《地球信息科学学报》2012,14(6):728-735

 船舶轨迹的自动观测记录已进入了大数据时代,其呈爆炸式增长的趋势给传统的轨迹数据管理方式带来了巨大挑战。本文针对通用船舶自动识别系统(AIS)岸基网络中船舶轨迹数据上传频率高,数据量大,覆盖范围广的特点,首先,分析了当前常见船舶轨迹数据存储方法存在的缺陷,概括了船舶轨迹数据的特征并对其进行抽象建模,然后,在时空立方体模型的基础上,提出了从抽样时刻、步进时段到每日航次的三层组织框架的建模思想,设计了Geodatabase的网格化三级时空立方体模型,实现了海洋运输船舶轨迹观测记录的Geodatabase管理方法。通过我国AIS岸基网络(温州-汕头)单日观测数据的实例验证,表明该模型存储及时空查询性能良好,且具有轨迹数据存储、查询和空间分析一体化管理的独特优势。  相似文献   

海上主航迹带边界统计推断与海西航路警戒区布局优化分析     

陈金海  陆锋  李明晓 《地球信息科学学报》2015,17(10):1196-1206

台湾海峡是东北亚各国与东南亚、印度洋沿岸各国间的海上捷径,其交通主流是通行海峡的南北向航次,然而海峡两岸启动大三通后,穿越海峡的客货运船舶日益增多,导致闽台直航航次与台湾海峡南北干线主交通流交叉现象凸显,台湾海峡西侧水域冲突日益加剧。本文根据船舶轨迹观测数据,抽样出通行海峡南北及横穿海峡的航次样本,应用轨迹栅格化方法建立统计推断模型,以概率形式表达南北干线、两岸直航的海运利用分布,推断出2种交通流的主航迹带,识别南北向交通主流与两岸直航交通支流的显著冲突区,以此调整现有警戒区设置方案。研究结果表明：轨迹统计推断法能定量化分析海西现有交通流模式,易于辨识横越海峡的船舶与通行海峡在航船舶的冲突区中心,为优化警戒区布局提供有效的方法支撑;调整后的海西警戒区中心可与台湾本岛西岸港口外侧的直航船舶通过点对接,形成海峡两岸直航的固定航线,可降低台湾海峡船舶冲突隐患,规范台湾海峡的船舶交通秩序。  相似文献   

Sediment-supply-dominated stratal architectures in a regressively stacked succession of shoreline sand bodies,Campanian Desert Member to Lower Castlegate Sandstone interval,Book Cliffs,Utah–Colorado,USA     

Simon A. J. Pattison 《Sedimentology》2020,67(1):390-430

Strongly progradational regressive stacks of shallow marine sandstones are ubiquitous in modern and ancient coastal depositional systems. Many ancient examples form prolific hydrocarbon and freshwater reservoirs in the subsurface. One of the best areas in the world to study progradational shallow marine successions is the Campanian Book Cliffs of Utah and Colorado, where the Desert Member to Lower Castlegate Sandstone interval served as a foundational data set for early sequence stratigraphic models. A strongly progradational stack of 17 parasequences comprises the Desert–Castlegate interval. Parasequences are 6·5 to 20·7 m thick. Normally regressive coarsening-upward successions are abundant, as are flat-topped, rooted foreshore sandstones. Conformable facies contacts mark the transition between the laterally adjoining nearshore terrestrial and shallow marine deposits which are genetically, temporally and spatially linked. The width of the shoreface to inner shelf facies belts varies from 4·8 to 19·9 km per parasequence, with a mean of 12·6 km. Solitary tongue shoreline trajectories are all very low to low angle ascending regressive, varying from +0·0004° to +0·171°. Stacked shoreline system trajectories are also dominantly low angle ascending regressive, with only two descending regressive trajectories, one of which intersects the depositional slope. The predominance of ascending regressive shoreline trajectories and normal regression, rarity of high frequency sequence boundaries, regressive surfaces of marine erosion and descending regressive shoreline trajectories, and absence of third-order sequence boundaries, incised valley fill deposits and no prolonged and regionally extensive sediment bypass, all point towards increasing sediment supply as the dominant driver of the Desert–Castlegate stratal architectures, while reduced accommodation (i.e. decreasing tectonic subsidence) played a secondary role.  相似文献