基于三维裂隙网络的裂隙岩体表征单元体研究

岩体表征单元体（REV）的研究一直是岩土工程中的重要问题。裂隙岩体REV是其内部复杂结构在尺寸效应上的体现,归因于岩体内裂隙系统的随机性。在三维网络模型的基础上通过计算体积节理数建立了确定岩体REV的方法。这种方法考虑了岩体内裂隙的三维空间密度的特征,采用体积节理数这一参数的收敛状况确定岩体REV的大小。建立了实际岩体的模拟裂隙系统,用一定大小的立方体来分割裂隙系统,统计不同立方体内的体积节理数,并将均值作为最终裂隙岩体的参数。将此参数作为裂隙岩体的属性,通过判别其收敛状况获得了岩体REV的尺寸。考虑了岩体不连续面的特征,建立了REV的分析模型,得出工程岩体的REV的尺寸是裂隙平均迹长的4倍的结论。     

隐伏金属矿床上升气流微粒特征、形成及迁移

结合地球化学和纳米科学技术的理论和研究方法,研究隐伏金属矿床有关微粒的形成、迁移和特征。对十多个金属矿床的研究表明,隐伏金属矿体地表沉积物中上升气流微粒样品有单个微粒和微粒聚合体,单个微粒形态有球状、近球状、不规则状、规则多边形、长柱状,微粒有晶质、非晶质和部分晶质。聚合体形态一般是不规则状、球状和近球状。它们的矿物成分主要有自然Au、自然Cu、氯化物、氧化物、硫酸盐、氢氧化物等。成矿元素Au、Cu可以自然金属或自然合金形式存在,Cu、Pb、Zn等成矿元素可以氧化物或硫酸盐等形式存在,也可以存在于氧化物、氢氧化物、氯化物、硫酸盐等微粒中作为杂质元素,这些是隐伏金属矿体的指示微粒。成矿期后,与隐伏金属矿体有关微粒主要形成于断层作用、氧化作用和生物作用。在上升气流中,微粒呈“布朗运动”。     

RUSSIAN DOLLS OR SCALE SKIPPERS? TWO GENERATIONS IN STRASBOURG*

ABSTRACT. Over the past quarter‐century academic geographers have interrogated the concept of “scale.” It had previously been conceived as an unproblematic and mechanical item in geographical representation, a device for moving “up” from the finely detailed to the general. Regular, commonsensical steps were supposed to move one from the corporeal scale to the global scale, each scale nested into the next higher. Such is the “Russian‐dolls” mode, whereby an individual considering his or her geographical identity—as in this study—would proceed hierarchically in scale from self, to city, to region, to nation, to continent. Ethnographic evidence from Strasbourg, France, however, reveals another mode: “scale skipping.” Here an individual, musing upon her or his identity, can plausibly make the leap from the individual to the supranational scale in one sentence. Instructive examples of both modes are furnished from two fifteen‐strong groups of Strasburgers, selected for their presumed attachment to the supranational‐scale ideal of “Europe.” The older group comprises professional Eurocrats; the younger group, college students returning to complete their studies in Strasbourg after attending universities elsewhere in the European Union through the Erasmus Program of study abroad.     

Modelling the runoff-sediment yield relationship using a proportional function in hilly areas of the Loess Plateau, North China

Based on data observed at the 12 small watersheds in hilly areas of the Loess Plateau, North China, the relationship between event runoff volume and sediment yield is examined. The results reveal that the runoff-sediment yield relationship at the inter-event timescale is mainly determined by the runoff-sediment concentration relationship at the intra-event timescale. In the study area, the sediment concentration tends to be stable when the flow discharge exceeds a certain critical value. Many factors that are important for determining the characteristics of low-magnitude events, such as flow discharge, particle size of fluvial sediment, and accumulation of loose material on land surfaces prior to a rainstorm, appear to have little importance for high-magnitude events. Consequently, mean sediment concentration tends to be stable for large flood events, suggesting a strong similarity between the two flow-sediment relationships at inter-and intra-event temporal scales. Furthermore, a proportional function is proposed to predict event sediment yield, and the correspondence between the predicted and observed sediment yields is examined. The performance of the model is good for high-magnitude events, especially extreme events. The applicability of the proposed model at the annual timescale is also discussed.     

Chemical weathering intensity and element migration features of the Xiashu loess profile in Zhenjiang, Jiangsu Province

The chemical weathering intensity and element migration features of the Xiashu loess profile in Zhenjiang are studied in this paper. (1) The Xiashu loess profile underwent moderate chemical weathering. It seems that the precipitation is a more important factor than the temperature in controlling the process of the chemical weathering. (2) The major elements such as Si, K, Na, Ca, Mg, Mn and P were migrated and leached, while the elements Fe and Ti were slightly enriched. The migration features of the major elements reveal that the Xiashu loess finished the primary process of chemical weathering characterized by leaching of Ca and Na, and almost reached the secondary process characterized by leaching of K. Except the elements Sr and Ga, other trace elements such as Th, Ba, Cu, Zn, Co, Ni, Cr and V were enriched. It might be caused by both the biogeochemical process and the adsorption of trace elements by clay mineral and organic materials. (3) The difference of element migration down the Xiashu loess profile reveals that the climate was warm and wet at the early-middle stage of the middle Pleistocene. At the end of the middle Pleistocene, it became dry and cool. At the early stage of the Late Pleistocene, the paleoclimate became warm and wet again. As a whole, the paleoclimate generally became drier and cooler in this region from the beginning of the middle Pleistocene.     

世界大都会区城际轨道交通的发展规律

通过选取世界255 个大都会区城际轨道交通样本,对城际轨道交通的发展历程、空间分布和网络特征进行了规律性总结;在此基础上,进一步分析城际轨道交通规模与大都会区人口、用地、经济规模之间的相关关系,构建多个回归模型;最后,应用于珠江三角洲区域,对其城际轨道交通的规模和布局进行预测。模型显示,世界大都会区城际轨道交通的规模与经济的相关程度最高,其次是人口和用地,而人均城际轨道规模与人均GDP和人口密度呈指数相关,其中,与人均GDP正相关,与人口密度负相关。应用模型得到,珠三角城际轨道交通的规划规模超前于现有经济发展水平,但低于人口发展水平。近期应重点建设广州、佛山、深圳、东莞4 个城市重要节点的城际轨道交通,构建广佛和广深两条走廊,并联系珠海、中山、肇庆、惠州、江门的中心城区,形成以广州为中心的放射状布局;远期则需要进一步加大广州、深圳、佛山、东莞、珠海、中山的线网密度,扩大线网的覆盖范围,并对外围的肇庆、惠州和江门适当增加联系的节点,最终形成网络状布局。     

新文化地理学视角下的国外宗教地理学研究

在文化全球化大背景下,宗教地理研究具有越来越重要的现实意义。国外宗教地理学研究在新文化地理学思潮的影响下,促生出许多新的议题和研究方向。本文依循于人文地理学中地方、景观、现代性和尺度这4 个重要概念,梳理了国外近10 年宗教地理学研究的新进展。发现其研究议题主要集中于日益重视对“非正式神圣”场所的探讨;基于人本主义研究范式下的神圣地依恋研究;随着跨国主义兴起的宗教移民身份和认同研究;宗教文化景观所暗含的政治和象征性意义的解读;宗教的多尺度分析,以及神圣与世俗间的互动分析等等。在总结国外宗教地理研究的新态势的基础上,对宗教的定义、宗教地理学与宗教性地理学的辩证关系、宗教地理学的研究趋势等进行了探讨和反思,以期为中国包括民间信仰在内的广义宗教地理的本土研究提供新的借鉴。     

山东省人口空间分布格局的多尺度分析

人口空间分布具有一定的尺度依赖性,从不同尺度上对人口空间分布格局进行分析,可以更确切、真实地揭示人口的空间分布规律,为制定区域发展规划、灾害评价、环境保护等提供科学依据。本文以山东省为研究区,运用空间自相关方法和统计相关分析方法,比较市级、县级、1 km三个尺度上人口分布的空间自相关性及其与环境—经济因子的统计相关性,试图探讨不同尺度下人口的空间分布模式及影响(指示)因素,从不同尺度揭示人口的空间分布格局特征。结果表明:①从不同尺度对人口的空间分布格局进行分析,可以得到从宏观到微观不同详细程度的信息。从市级尺度分析,可以得到山东省整体的人口空间分布特征;从县级尺度分析,可以得到山东省各市内部的人口空间分布特征;从1 km尺度分析,可以得到山东省各县内部的人口空间分布特征。②不同尺度上,人口的空间分布格局特征不同。市级和县级尺度上,人口分布受环境—经济因子的影响表现出与一些因子显著相关,而受空间集聚的作用较小;1 km尺度上,人口分布与环境—经济因子的相关性较小,而主要受空间集聚的作用,在县内部,人口往往集中分布于某一区域,呈现出典型的集聚分布模式。     

Testing mathematical uranium migration models in combined ESR/U-series dating of fossil teeth from open-air sites

Several mathematical models have been suggested to describe uranium migration kinetics for ESR dating of fossil tooth. In the present study, different U-uptake models were used to calculate ages for fossil teeth from two open-air Paleolithic sites in Nihewan Basin – Donggutuo and Hougou and compared with independent age control of the sites. For Donggutuo site, the results show that the ages of three teeth calculated by EU and AU models were much younger than magnetostratigraphic age. At Hougou site, two teeth from the top of Nihewan lacustrine deposits give the consistent EU and AU ages within errors but younger than sediment OSL age. This study indicates that mathematical modeling could not always give convincing results for the open-air sites, which may experience dramatic hydrological variations and high erosion rates.     

饱和正冻土水分迁移及冻胀模型研究

正冻土在温度梯度大的情况下,冻结锋面快速移动,孔隙水变成冰,造成原位体积膨胀;而通常在天然条件下,温度梯度都不大,水从未冻区向冻结区迁移,在某一个位置引起冰的累积,形成分凝冰。由于此诱发的冻胀要比原位冻胀大很多,因此,建立一个能够模拟土体水分迁移及分凝冰形成过程的冻胀模型尤其重要。基于第2冻胀理论,建立了饱和土体冻胀模型。在模型中,假设冻结缘中单位时间内水分迁移速度为常数,以计算冻结缘内水压力,再根据克拉方程得到冰压力。根据冰压力的大小作为分凝冰形成判据,研究中假设新的分凝冰形成以后,上一层分凝冰停止生长。模型把水分迁移和冻胀速率当作基本的未知量,模拟了与可天然土体冻胀类似的底部无压补水和顶部加压的冻胀情况。通过数值模拟与试验结果进行对比,初步验证模型的可靠性,其研究结果为实际寒区工程的冻胀预测提供参考。