地铁站点可达性、客流与站点商圈零售商业结构关系研究——以广州市为例

地铁与城市商业地域的结构存在极大关系。实地调查获取广州15个地铁站点商圈零售商业营业面积、地铁网络等数据,利用栅格分析方法计算不同地铁站点的可达性程度的差异性。运用回归模型分析不同地铁站点可达性、客流与站点商圈零售商业空间结构的相关关系。以广州天河市级商业中心为例,微观上分析地铁站点客流对商业中心空间结构的影响。结果表明:地铁站点交通可达性、客流量与站点零售商业营业面积存在较强关联性,但换乘站点的可达优势与客流优势在商业上未能完全体现;地铁客流与较高等级的商业存在较大的相关性,而与低等级的商业相关性小,甚至负相关;客流的增加促进了地铁附近的商业形态从传统零售业向更高级业种演化。     

翠华山水湫池及其附近崩塌堆积形成年代探疑

通过对相关史料的分析,论证了翠华山主景区崩塌堆积不可能是唐天宝年间地震诱发山崩形成的。通过实地考察,认为这些崩塌堆积不是同时发生,而是多期崩塌活动的结果,并且崩塌活动又都发生在水湫池被堰塞成湖之后。因此,水湫池不可能是唐代的地震山崩形成的。     

旅游流空间模式基本理论:问题分析及其展望

旅游流是旅游地理学的基本问题,而旅游流空间模式的研究,自20世纪50年代以来则是旅游流研究的热点问题。通过文献分析法,本文将旅游流空间模式基本理论梳理为圈层结构理论、核心边缘理论、空间扩散理论。在此基础上,揭示其存在的若干问题,包括研究中存在的"区域视角"和"旅游者个体视角"混淆的认知问题、旅游客源地和旅游目的地在区域视角下如何界定的问题、空间模式研究中广泛存在的"二元陷阱"问题、区域间旅游职能分化及其分化程度尚无科学分析的问题等。文末对未来研究进行了展望,以期从理论意义上深化旅游流基本问题的建构。需指出的是,旅游流作为"非工作流"的一种,其"流现象"、"流空间"和"流效应"同样可适用于其它形式的"流研究"。     

Transient fluid flow in and around a fault

We present the results of simple numerical experiments in which we study the evolution with time of fluid flow around and within a permeable fault embedded in a less permeable porous medium. Fluid movement is driven by an imposed vertical pressure gradient. The results show that fluid flow is controlled by two timescales: τ_f = Sl²/κ_F and τ_F = Sl²/κ_M, where S is the specific storage of the porous material, l the length of the fault, and κ_M and κ_F are the hydraulic conductivities of the porous material and the fault, respectively. Fluid flow and the associated fluid pressure field evolve through three temporal stages: an early phase [t < τ_f] during which the initial fluid pressure gradient within the fault is relaxed; a second transient stage [τ_f < t < τ_F] when fluid is rapidly expelled at one end of the fault and extracted from the surrounding rocks at the other end leading to a reduction in the pressure gradient in the intact rock; a third phase [t < τ_F] characterized by a steady‐state flow. From the numerical experiments we derive an expression for the steady‐state maximum fluid velocity in the fault and the values of the two timescales, τ_f and τ_F. A comparison indicates excellent agreement of our results with existing asymptotic solutions. For km‐scale faults, the model results suggest that steady‐state is unlikely to be reached over geological timescales. Thus, the current use of parameters such as the focusing ratio defined under the assumption of steady‐state conditions should be reconsidered.     

How should permeability be measured in fine‐grained lithologies? Evidence from the chalk

Two chalk data sets from the Central North Sea (UK/Norway and Denmark) with a similar lithological classification and porosity values (5–20%) have a difference in permeability of up to three orders of magnitude. The method of measuring permeability was different for the two data sets: samples from UK/Norway were measured by transient pulse decay (TPD), while the Danish samples were measured by routine core analysis. Petrological and petrophysical characterization of samples from the two data sets have revealed that all samples display a similar range of rock properties; the differences are not due to regional facies variations. It is likely that the low permeability values reported by TPD have more validity than routine core analyses in measuring lower porosity and permeability chalk (5–20% porosity, <0.01 mD). The fact that large sections of North Sea chalk potentially have much lower permeability than previously reported has widespread implications for petroleum migration and entrapment, and overpressure generation.     

中国入境后旅游流的空间分布研究

入境旅游是中国旅游业发展的重要组成部分。海外旅游者入境后,在空间上呈现出一定的流动特征及分布规律。本文根据中国旅游统计年鉴资料和项目组旅游调查资料,将全国旅游流划分为5大基本旅游流区,为加强各分区间的联合促销及客流、信息共享提供参考依据和技术支撑。     

口岸城市入境旅游流空间扩散路径实证研究——以上海市为例

本研究以东部典型入境口岸城市上海为研究对象,以市场调查资料为数据来源,从节点、方向及路径三个角度研究上海市入境旅游流的路径转移扩散规律。研究结果显示,以上海作为入境1：7岸的入境旅游流扩散人次排前十的节点城市依次为：北京、西安、杭州、成都、南京、桂林、广州、昆明、苏州、深圳;按照旅游流扩散方向可将入境旅游流扩散方向分为四类：北向、南向、西北向和西南向,并在每个方向上分别归纳出4条扩散路径,其中上海→北京→西安这→路径人数比例最高,上海→成都→西安→北京次之,上海→西安→北京处于第三位;同时研究显示,入境旅游流的扩散存在着路径依赖及路径依赖锁定现象。     

Cyclic loading of an idealized clay‐filled fault: comparing hydraulic flow in two clay gouges

The flow of water along discontinuities, such as fractures or faults, is of paramount importance in understanding the hydrogeology of many geological settings. An experimental study was undertaken comprising two experiments on a 30° slip‐plane filled with kaolinite or Ball Clay gouge using a bespoke Angled Shear Rig (ASR). The gouge was initially loaded in equal step changes in vertical stress, followed by unloading of the sample in similar equal steps. This was followed by reloading to a new maximum stress, followed by unloading; the test history was therefore load‐unload‐reload‐unload (LURU). The transmissivity of the kaolinite and Ball Clay gouge showed a power‐law relationship with vertical stress. The LURU history showed considerable hysteresis, with flow effectively unchanged during unloading, even when vertical stress was close to zero. Reloading resulted in flow similar to that seen during unloading suggesting that the unloading‐reloading path is similar to the rebound‐reconsolidation line in classic soil mechanics. These observations show the importance of stress history on fracture flow; consideration of just the current stress acting upon a fracture may result in inaccuracies of predicted hydraulic flow. Once a new stress maximum was achieved the transmissivity of the fracture continued to reduce. No significant variation was seen in the flow response of kaolinite and Ball Clay gouge suggesting that the inclusion of illite and quartz did not have a significant influence on the form of the relationship between stress and flow, i.e. both described by a power‐law.     

Large‐scale chemical stratification of fluids in the crust: hydraulic and chemical data from the geothermal research site Urach,Germany

The Urach 3 research borehole in SW Germany has been drilled through a sedimentary cover sequence and reached gneisses of the Variscan crystalline basement at 1604 m below surface. An additional 2840 m has been drilled through fractured basement rocks. The borehole has been used for hydraulic tests in the context of a ‘hot dry rock’ (HDR) project. The sedimentary cover ranges from the Carboniferous to the Middle Jurassic (Dogger) in age and comprises mostly clastic sediments in the Paleozoic and limestone and shale in the Mesozoic. Water composition data from 10 different depths include samples from all major lithological units. The total dissolved solids (TDS) increases from the surface to about 650 m where it reaches 4.1 g l^?1 in Triassic limestone. In lower Triassic sandstones, TDS increases very sharply to 28.5 g l^?1 and the water is saturated with pure CO₂ gas. With increasing depth, TDS does not change much in the clastic sediments of the Permian and Carboniferous. The crystalline basement is marked by a very sharp increase in TDS to 55.5 g l^?1 at about 1770 m depth. TDS increases within the basement to more than 78.5 g l^?1 at about 3500 m depth. The data suggest that there is limited vertical chemical communication over long periods of time. The CO₂ gas cap in the lower Triassic sandstones requires a gastight cover. The chemical stratification of the fluids relates to the permeability structure of the crust at the Urach site and fits well with hydraulic and thermal data from the site.     

中国春运人口流动网络的富人俱乐部现象与不平衡性分析

基于“百度地图春节人口迁徙大数据”,利用加权网络的富人俱乐部系数和归一化不平衡系数方法,对2015年中国春运期间人口流动网络的富人俱乐部现象和不平衡性进行分析。研究结果表明：中国春运人口流动网络中存在明显的富人俱乐部现象,富人俱乐部城市包括北京、上海、广州、苏州、深圳和东莞,这些城市主导了超过77.66%中国城市的省际人口流动,且与这些城市之间的人口流动多属于不平衡关系,同时俱乐部城市之间、俱乐部城市与一小部分城市之间则属于平衡关系,这种流动格局很容易造成各城市在人口流动网络中的地位分化,严重影响了人口流动网络的公平性和安全性。