土耳其卡赞碱矿对接井水溶开采技术创新综述          下载免费PDF全文

刘汪威  涂运中  刘海翔  张新刚  林修阔 《探矿工程》2020,47(8):14-23

土耳其卡赞碱矿钻井项目主要利用高精度中靶技术使定向水平井与垂直井在碱层中对接后进行水溶开采的方法。该项目通过长期大量的钻井工作,在已有的钻井技术与地质条件基础上,改进完善了与地层相适应的钻井技术,建立了矿区三维地质模型,设计应用了水平分支对接井,优化了钻井轨迹设计,建立起非矿层与矿层的基准物探测井响应曲线,探索出矿区地层致斜机理及相应钻井防斜措施,研究并应用了各种井底钻具组合与设备,采用了提高水平钻井轨迹控制精度的技术方法。上述多种水溶采矿钻井技术创新措施的应用,提高了矿山规划能力、降低了施工成本、提高了资源回采率、缩短了施工工期、降低了劳动强度、提高了钻进效率、减少了施工用地以及对环境的破坏。可为天然碱矿及可溶性矿产的整体矿山规划,以及钻井水溶采矿技术的提高提供借鉴。  相似文献   

北京市出租车GPS轨迹数据统计特征分析     

翟文龙  王海起  费涛  闫滨 《测绘与空间地理信息》2020,(2):79-84

以2015年5月11-17日北京市3万多辆出租车3.85亿条轨迹点数据为研究对象,对非载客段数据点进行剔除,使用R语言从居民出行距离、轨迹段持续时间、分时段出行量、出行方向及平均速度五个角度进行统计特征分析,并通过拟合得到浮动车行驶距离与持续时长所遵循的指数分布,进而发现距离衰减效应、工作日与周末的日律性,并以此分析乘客出行距离、出行时间的潜在规律。  相似文献   

基于Argo实测流场数据对5套海洋模式产品中赤道太平洋中层流的评估          下载免费PDF全文

周永远  闫运伟  邢小罡  柴扉 《海洋学研究》2020,38(3):1-9

本文以Argo轨迹资料计算的赤道太平洋中层流(1 000 m深度流场)作为实测数据,从空间结构特征和时间变化特征两方面对5套常用海洋模式产品(OFES、LICOM、HYCOM、ECCO2和SODA)进行了评估。Argo流场显示赤道太平洋中层流呈条带状结构,且存在明显的西强东弱和南强北弱特征。此外,赤道太平洋中层流存在明显的季节变化且其相位关于赤道对称。5套模式产品的评估结果表明,SODA流场与实测流场最接近,其时空变化特征都与实测流场基本一致;其次是ECCO2流场,除流场动能偏小以外,其他各方面都与实测流场一致;OFES、LICOM和HYCOM流场的模拟效果较差,但都能再现条带状结构特征。  相似文献   

一个从基于位置相关服务而收集的零星位置点中获取连续车辆轨迹的方法(英文)   总被引：1，自引：1，他引：0  

李响  张喜慧  林珲 《地球空间信息科学学报》2009,12(2):85-94

The paper proposes an economical and fast algorithm for deriving trajectories from sporadic tracking points collected in location-based services (LBS). Although many traffic studies or applications can benefit from the derived trajectories, the sporadic tracking points are always implicitly overlooked by most of existing map-matching algorithms. The algorithm proposed in this paper finds network paths or trajectories traveled by vehicles through augmenting GPS data with odometer data. An odometer can provide data of traveled distance which are compared with the lengths of candidate network paths in order to find the most approximate network path approaching the trajectory of a vehicle. Tracking points are classified into anchor points and non-anchor points. The former are used to divide trajectories, and the latter screen candidate network paths. An elliptic selection zone and a reduction process are applied to the selection of possible road segments composing candidate network paths. A brute-force searching algorithm is developed to find candidate network paths and calculate their lengths. A two-step screening process is designed to select the final result from candidate network paths. Finally, a series of experiments are conducted to validate the proposed algorithm. Supported by the National Natural Science Foundation of China (No.40701142), the Scientific Research Starting Foundation for Returned Overseas Chinese Scholars, Ministry of Education, China.  相似文献   

Experimental Study of Nonlinear Behaviors of A Free-Floating Body in Waves     

贺铭  任冰  邱大洪 《海洋工程》2016,(3):421-430

Nonlinear behaviors of a free-floating body in waves were experimentally investigated in the present study. The experiments were carried out for 6 different wave heights and 6 different wave periods to cover a relatively wide range of wave nonlinearities. A charge-coupled device (CCD) camera was used to capture the real-time motion of the floating body. The measurement data show that the sway, heave and roll motions of the floating body are all harmonic oscillations while the equilibrium position of the sway motion drifts in the wave direction. The drift speed is proportional to wave steepness when the size of the floating body is comparable to the wavelength, while it is proportional to the square of wave steepness when the floating body is relatively small. In addition, the drift motion leads to a slightly longer oscillation period of the floating body than the wave period of nonlinear wave and the discrepancy increases with the increment of wave steepness.  相似文献   

一种顾及时间特征的船舶轨迹DBSCAN聚类算法     

郭乃琨  陈明剑  陈锐 《测绘工程》2021,30(3):51-58

随着世界海洋经济的快速增长和各国海洋贸易的持续发展,船舶A IS系统被世界各国广泛采用,由此产生海量的船舶轨迹数据.如何对这些多维、动态的数据进行挖掘和利用,成为当前时空数据挖掘领域的研究热点之一.文中在经典DBSCAN空间聚类算法的基础上,对船舶轨迹数据进行清洗、压缩等预处理,并将其划分为特征点相连的子轨迹段,然后引...  相似文献   

Huygens probe entry and descent trajectory analysis and reconstruction techniques     

D.H. Atkinson  B. Kazeminejad  J.-P. Lebreton 《Planetary and Space Science》2005,53(5):586-593

Cassini/Huygens is a joint National Aeronautics and Space Administration (NASA)/European Space Agency (ESA)/Agenzia Spaziale Italiana (ASI) mission on its way to explore the Saturnian system. The ESA Huygens Probe is scheduled to be released from the Orbiter on 25 December 2004 and enter the atmosphere of Titan on 14 January 2005. Probe delivery to Titan, arbitrarily defined to occur at a reference altitude of 1270 km above the surface of Titan, is the responsibility of the NASA Jet Propulsion Laboratory (JPL). ESA is then responsible for safely delivering the probe from the reference altitude to the surface. The task of reconstructing the probe trajectory and attitude from the entry point to the surface has been assigned to the Huygens Descent Trajectory Working Group (DTWG), a subgroup of the Huygens Science Working Team. The DTWG will use data provided by the Huygens Probe engineering subsystems and selected data sets acquired by the scientific payload. To correctly interpret and correlate results from the probe science experiments and to provide a reference set of data for possible “ground-truthing” Orbiter remote sensing measurements, it is essential that the trajectory reconstruction be performed as early as possible in the post-flight data analysis phase. The reconstruction of the Huygens entry and descent trajectory will be based primarily on the probe entry state vector provided by the Cassini Navigation Team, and measurements of acceleration, pressure, and temperature made by the Huygens Atmospheric Structure Instrument (HASI). Other data sets contributing to the entry and descent trajectory reconstruction include the mean molecular weight of the atmosphere measured by the probe Gas Chromatograph/Mass Spectrometer (GCMS) in the upper atmosphere and the Surface Science Package (SSP) speed of sound measurement in the lower atmosphere, accelerations measured by the Central and Radial Accelerometer Sensor Units (CASU/RASU), and the probe altitude by the two probe radar altimeters during the latter stages of the descent. In the last several hundred meters, the altitude determination will be constrained by measurements from the SSP acoustic sounder. Other instruments contributing data to the entry and descent trajectory and attitude determination include measurements of the zonal wind drift by the Doppler Wind Experiment (DWE), and probe zonal and meridional drift and probe attitude by the Descent Imager and Spectral Radiometer (DISR). In this paper, the need for and the methods by which the Huygens Probe entry and descent trajectory will be reconstructed are reviewed.  相似文献   

Temporal variations in surface ozone and its precursors and meteorological effects at an urban site in China   总被引：3，自引：2，他引：3  

Jun Tu  Zong-Guo Xia  Hesheng Wang  Wenqing Li 《Atmospheric Research》2007,85(3-4):310-337

Continuous measurements of ozone and its precursors including NO, NO₂, and CO at an urban site (32°03′N, 118°44′E) in Nanjing, China during the period from January 2000 to February 2003 are presented. The effects of local meteorological conditions and distant transports associated with seasonal changed Asian monsoons on the temporal variations of O₃ and its precursors are studied by statistical, backward trajectory, and episode analyses. The diurnal variation in O₃ shows high concentrations during daytime and low concentrations during late night and early morning, while the precursors show high concentrations during night and early morning and low concentrations during daytime. The diurnal variations in air pollutants are closely related to those in local meteorological conditions. Both temperature and wind speed have significant positive correlations with O₃ and significant negative correlations with the precursors. Relative humidity has a significant negative correlation with O₃ and significant positive correlations with the precursors. The seasonal variation in O₃ shows low concentrations in late autumn and winter and high concentrations in late spring and early summer, while the precursors show high concentrations in late autumn and winter and low concentrations in summer. Local mobile and stationary sources make a great contribution to the precursors, but distant transports also play a very important role in the seasonal variations of the air pollutants. The distant transport associated with the southeastern maritime monsoon contributes substantially to the O₃ because the originally clean maritime air mass is polluted when passing over the highly industrialized and urbanized areas in the Yangtze River Delta. The high frequency of this type of air mass in summer causes the fact that a common seasonal characteristic of surface O₃ in East Asia, summer minimum, is not observed at this site. The distant transports associated with the northern continental monsoons that dominate in autumn and winter are related to the high concentrations of the precursors in these two seasons. This study can contribute to a better understanding of the O₃ pollution in vast inland of China affected by meteorological conditions and the rapid urbanization and industrialization.  相似文献   

Interplay between shoreline migration paths, architecture and pinchout distance for siliciclastic shoreline tongues: evidence from the rock record     

TORE M. LØSETH  RON J. STEEL†  JEFF P. CRABAUGH‡  MAIJA SCHELLPEPER‡ 《Sedimentology》2006,53(4):735-767

Facies, geometry and key internal stratigraphic surfaces from eight Cretaceous and Eocene clastic shoreline tongues have been documented. The regressive parts of all the studied tongues represent storm‐wave influenced strandplains, deltas or fan‐deltas, and the regressive shoreline trajectories varied from descending to ascending. The transgressive parts of the tongues are dominated by either estuarine or coastal‐plain deposits. The distance from the coeval, up‐dip non‐marine deposits to the basinward pinchout of amalgamated shoreface sandstones, measured along depositional dip, is here termed the sand pinchout distance. The study shows that the angle of regressive‐to‐transgressive turnaround (defined by the angle between the regressive and subsequent transgressive shoreline trajectories) and the process regime during turnaround largely control the sand‐pinchout distance. The amount of transgressive erosion can also partly control the pinchout distance, but this parameter was comparable for the different examples presented here. If the type of depositional system at turnaround and the depth of transgressive erosion are constant, small angles of turnaround are associated with large pinchout distances, whereas larger angles of turnaround result in smaller pinchout distances. The model developed allows sand‐pinchout distance to be predicted, using data for the landward parts of shoreline tongues. The dataset also shows that steeply rising (aggrading) shoreline trajectories tend to produce more heterolithic sandstone tongues than those formed by lower‐angle trajectories.  相似文献   

    

Yu Xing  Dai Jin  Jiang Weimei  Fan Peng 《大气科学进展》2000,17(4):617-635

It is essential to learn the temporal and spatial concentration distributions and variations of seeding agents in cloud seeding of precipitation enhancement. A three–dimensional puff trajectory model incorporating a mesoscale nonhydrostatic model has been formulated, and is applied to simulating the transporting and diffusive characteristics of multiple line sources of seeding agents within super–cooled stratus. Several important factors are taken into consideration that affect the diffusion of seeding materials such as effects of topography and vertical wind shear, temporal and spatial variation of seeding parameters and wet deposition. The particles of seeding agents are assumed to be almost inert, they have no interaction with the particles of the cloud or precipitation except that they are washed out by precipitation. The model validity is demonstrated by the analyses and comparisons of model results, and checked by the sensitivity experiments of diffusive coefficients and atmospheric stratification. The advantage of this model includes not only its exact reflection of heterogeneity and unsteadiness of background fields, but also its good simulation of transport and diffusion of multiple line sources. The horizontal diffusion rate and the horizontal transport distance have been proposed that they usually were difficult to obtain in other models. In this simulation the horizontal diffusion rate is 0.82 m s⁻¹ for average of one hour, and the horizontal average transport distance reaches 65 km after 1 h, which are closely related to the background fields.  相似文献