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951.
本文提出了以地理空间数据为支撑,结合手机信令、POI等多源数据刻画城市居民出行特征的方法。首先将信令数据与地理信息区块绑定,根据时间特征和地理区块的社会属性,识别居民的基本职住娱信息;然后综合民生POI点、出行特征拓展关键词、图谱等多源数据,运用工作日通勤分析模型和节假日出行特征提取模型,识别用户的通勤距离、通勤方式、日均通勤频次、周均工作时长、节假日出行场景、出行频次、驻留时长等内容,并形成涵盖职住娱信息的出行特征类标签集。以成都市为例,采集连续1个月的手机信令数据和同时期的POI等数据,验证了该方法的可行性,该成果作为反映城市实际人口规模数量和空间分布特征的城市人口地图大数据产品的重要内容,为政府部门、商企用户开展相关分析业务提供数据支撑。 相似文献
952.
为探究不同测量方法获取浅沟数据的精度,本文以元谋干热河谷区浅沟为例,采用RTK、三维激光扫描、近景摄影测量等多种测量方法获取浅沟数据,建立DEM并提取浅沟形态参数,对比近景摄影测量以不同方式获取标记坐标后建立DEM的差异,同时以测针板实测浅沟横剖面为参照,对比分析不同测量方法获取浅沟横剖面的精度。结果表明:RTK获取密度较低的点数据,建立的DEM较粗糙,仅体现沟缘大致走向;近景摄影测量+RTK方法测得的DEM高程整体低于近景摄影测量+全站仪所得DEM高程;利用三维激光扫描仪和近景摄影测量+全站仪两种方法获取数据所提取的浅沟形态参数精度较高;对比浅沟横剖面,横剖面近景摄影测量+全站仪测量所得与实测横剖面重合度较高。因此,利用近景摄影测量+全站仪进行浅沟测量,在精度、效率等方面优势较大。 相似文献
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955.
Dawei Lv Jitao Chen Zengxue Li Guiqiang Zheng Cuiyu Song Haiyan Liu Yanru Meng Dongdong Wang 《Resource Geology》2014,64(4):332-345
The Huanghebei Coalfield, one of the coal production bases in North China, was considered as a coalfield without coal‐bed methane (CBM) during past decades. In recent years, however, CBM has been discovered in coal‐bearing successions. In order to understand the CBM geological characteristics and accumulation process in this area, fifteen coal samples were collected and analyzed with respect to coal maceral and reflectance. The result shows that the gas distribution is uneven and the content varies in different areas even for the same coal bed. The storage of CBM is affected by geological factors such as burial depth, geological structures, and magmatic intrusion, among which the former two are more important in the formation of CBM. Deep burial of coal beds with the presence of cap‐rock mudstone can seal CBM. The CBM is also accumulated and preserved at the place where normal faults are distributed. Magmatic intrusion causes contact metamorphism and controls the CBM formation by heating the coal‐bearing successions. The obtained data indicate the geological conditions in northeastern Zhaoguan Mine are preferable for CBM formation and conservation; recent exploration estimates the CBM geological reserves up to 282.16 Mm3 and average of reserve abundance at 0.1662 × 108 m3 km?2. The Changqing Mine is a potential prospect in terms of CBM exploration since its geological conditions (structures and burial depth) are similar to the Zhaoguan Mine and its cap rock is even better. 相似文献
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957.
为支撑地质条件复杂地区的水文地质、工程地质和环境地质调查研究,在皖江经济带沿江丘陵平原区通过系统分析第四纪地层的岩性、结构、构造等组合,以地貌以及第四系成因、沉积相和沉积物物源为指标,结合已有区域第四纪研究成果以及年代地层和岩石地层划分标准,进行皖江沿江丘陵平原区“第四纪地质单元”划分,共划分出冲积-湖积平原地质单元、洪积-坡积岗地地质单元和残积-剥蚀丘陵地质单元3个一级地质单元,总结了7种类型第四纪地层结构组合及其特征,为区域水文地质和工程地质调查与研究奠定了基础。 相似文献
958.
Tongwen Zhang Yujiang YuanWenshou Wei Shulong YuRuibo Zhang Feng ChenHuaming Shang Li Qin 《Quaternary Research》2014
August–July precipitation has been reconstructed back to AD 1724 for the Mohe region in the northern Greater Higgnan Mountains, China, using Pinus sylvestris var. mongolica tree-ring width. The reconstruction explains 39% of the variance in the precipitation observed from AD 1960–2008. Some droughts noted in historical documents are precisely captured in our reconstruction. Wet periods occurred during the periods of AD 1734–1785, AD 1805–1830, AD 1863–1880, AD 1922–1961, and AD 1983–1998; while the periods of AD 1786–1804, AD 1831–1862, AD 1881–1921, and AD 1962–1982 were relatively dry. Power spectral and wavelet analyses demonstrated the existence of significant 24-yr, 12-yr, and 2-yr cycles of variability. The results of the spatial correlations suggest that our reconstruction contains climatic signals for the southern Stanovoy Range and the northern Greater Higgnan Mountains. The positive correlations between the new reconstructed precipitation series and two precipitation reconstructions indicate that our precipitation reconstruction captures broad-scale regional climatic variations. A comparison between the weakening tendency of summer monsoon and the dry period of our reconstruction reveals that the annual precipitation in the Mohe region is partly influenced by the East Asian Summer Monsoon. 相似文献
959.
An Approach for Modeling Rock Discontinuous Mechanical Behavior Under Multiphase Fluid Flow Conditions 总被引:1,自引:0,他引:1
Peng-Zhi Pan Jonny Rutqvist Xia-Ting Feng Fei Yan 《Rock Mechanics and Rock Engineering》2014,47(2):589-603
In this paper, the two computer codes TOUGH2 and RDCA (for “rock discontinuous cellular automaton”) are integrated for coupled hydromechanical analysis of multiphase fluid flow and discontinuous mechanical behavior in heterogeneous rock. TOUGH2 is a well-established code for geohydrological analysis involving multiphase, multicomponent fluid flow and heat transport; RDCA is a numerical model developed for simulating the nonlinear and discontinuous geomechanical behavior of rock. The RDCA incorporates the discontinuity of a fracture independently of the mesh, such that the fracture can be arbitrarily located within an element, while the fluid pressure calculated by TOUGH2 can be conveniently applied to fracture surfaces. We verify and demonstrate the coupled TOUGH–RDCA simulator by modeling a number of simulation examples related to coupled multiphase flow and geomechanical processes associated with the deep geological storage of carbon dioxide—including modeling of ground surface uplift, stress-dependent permeability, and the coupled multiphase flow and geomechanical behavior of fractures intersecting the caprock. 相似文献
960.
在具有相同储集砂体和相似断层输导情况下,牛庄洼陷沙三中亚段砂岩体油藏长期存在以下难以解释的现象:1)现今砂岩孔隙度分布与油气分布不一致,高孔隙砂岩不含油而低孔隙砂岩含油;2)相同物性砂岩有的含油而有的不含油,含油砂体现今物性接近,但含油级别却存在很大差异。本文从古孔隙度恢复方面分析了牛庄洼陷西部地区沙三中砂岩储层在成藏期的储集条件,并探讨了成藏期储层临界孔隙度。研究发现:1)虽然现今储层物性下限很低,部分砂岩已经致密化,但成藏期的古孔隙度分布在18%~25%范围内,远大于成藏期临界孔隙度13.9%。但由于埋藏过程的差异导致砂岩储层后期减孔幅度不同,因而现今储层物性不能反映成藏期储层物性,成藏期孔隙度高并不能代表现今孔隙度高;2)成藏期高孔隙度带与现今油气分布范围高度一致,表明在相似断层输导条件下,由于储层物性级差优势形成油气优势运移通道,导致高孔隙度带砂体含油,因此,沙三中亚段岩性油藏富集在成藏期高孔隙带中,成藏期砂岩古孔隙度是油气成藏的重要控制因素,而现今砂岩储层高孔隙带在成藏期并不一定高。牛庄洼陷西部地区沙三中亚段储层中具有高古孔隙度的砂岩仍有较大勘探潜力。 相似文献