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71.
Shaolu Yu 《Urban geography》2018,39(4):563-586
Based on the ethnographic research and in-depth interviews in Flushing, Queens, New York City, this paper proposes the concept of mobilocality. Mobilocality provides a conceptual framework to examine the urban ethnic communities through the lens of mobility from a multi-scalar perspective. Mobilocality is formed by the paradox of transnational mobility and local immobility that are simultaneously embedded in everyday life of (im)migrants. It is through mobilocality where individual is ethnic, ethnic is transnational, transnational is urban. This article also suggests a placed and contextual understanding of mobility by illustrating the interrelationships among the four spatialities: mobility, place, scale and distance. The making of mobilocality is an outcome of the dialectal process among these spatialities, which involves not only spatial-temporal dimensions, but also social and cultural context. Transnationalism is far from a celebration of cosmopolitanism and diversity. Rather, it is a divergent process that generates heterogeneity and boundaries, a product of time-space distortion instead of time-space compression. 相似文献
72.
Chinese overseas industrial parks in Southeast Asia: An examination of policy mobility from the perspective of embeddedness 总被引:4,自引:2,他引:2
The development of overseas industrial parks is a key component of the Belt and Road Initiative and an expected experimental way of promoting inclusive globalization by inventing new forms of cooperation between China and local host countries. Policy mobility, a classic theory within international political geography addressing the connection between local and global policies, has implications for overseas industrial parks development. In this paper, we argue that policies are not easily moved directly from one place to another; instead, policies are embedded due to the role of local actors in policy mobility. This article first provides an overview of seven China-Southeast Asia economic and trade cooperation zones identified by the Ministry of Commerce, and analyzes their key participants. It then discusses policy mobility by looking into the roles of revenue, land, and talent in developing these industrial parks. The paper finds that these parks face challenges, such as the complicated geographical environments of host countries, huge pressure from enterprise investment capital, the lack of overseas service platforms, and underdeveloped agglomeration economies. In the light of the current situation, policy suggestions for the future sustainable development of overseas industrial parks are put forward. 相似文献
73.
Mobility Sequence of Chemical Elements During Loess Weathering—Pedogenesis,Weinan,Shaanxi Province,China 总被引:1,自引:1,他引:0
The distribution of chemical elements in the Weinan loess section shows that: (1) carbonate is the critical constituent affecting
loess chemistry. The leaching of carbonates may cause “apparent” enrichment of some other constituents. (2) CaCO3, SiO2, FeO, MgO, K2O and Na2O are mobile while Al2O3, Fe2O3 and TiO2 are inert components. The mobility sequence may follow the order of CaCO3>FeO>MgO>Na2O>K2O>SiO2>Al2O3>TiO2>Fe2O3. (3) No obvious migration is noticed of iron, except changes in valence and forms, during the pedogenic process. Little iron
has been supplied to paleosol from precipitation. (4) Carbonates and, to a lesser extent, iron are most sensitive to, and
can be therefore used as good indicators of, environmental changes.
This research project was financially supported by the National Natural Science Foundation of China (Grant No. 49672137). 相似文献
74.
75.
利用频谱分解得到的频率能量数据体进行属性提取,是烃类检测的常用手段之一.同步挤压小波变换能够提供高分辨率的时频谱,具有较好的应用潜力.本文以同步挤压小波变换为基础,提出了一套烃类检测方法,包括低频阴影检测、流体流动性估计以及高频能量衰减等,通过自适应选取优势频段,实现了多属性联合高精度刻画烃类的分布范围.实际资料处理结果与现有钻井情况吻合,具有较好的实用性,实现了对储层位置的高精度描述,对指导油气田开发具有重要的理论意义和实用价值. 相似文献
76.
Occurrence of baddeleyite (ZrO2) which is a rare mineral has been recorded in ferromanganese
nodules of Central Indian Ocean Basin (CIOB). The mineral occurs either as independent isolated
sub-rounded to elliptical grains or in clusters forming fine subhedral crystals (<3 mm) within ferromanganese
concretionary growth bands. The mode of occurrence, textural features and chemistry of the
mineral suggest detrital and possibly an authigenic origin for baddeleyite. For authigenic origin it is
proposed that zirconium might have got released either from the terrigenous sediments or the altered
seafloor rocks forming halogen complexes and subsequently it has re-precipitated in the form of baddeleyite
within manganese nodules under oxic to sub-oxic conditions. 相似文献
77.
Geochemistry and mineralogy of shallow alluvial aquifers in Daudkandi upazila in the Meghna flood plain, Bangladesh 总被引:1,自引:0,他引:1
M. Aziz Hasan Mattias von Br?mssen Prosun Bhattacharya Kazi Matin Ahmed Arif Mohiuddin Sikder Gunnar Jacks Ondra Sracek 《Environmental Geology》2009,57(3):499-511
The shallow alluvial aquifers of the delta plains and flood plains of Bangladesh, comprises about 70% of total land area are
mostly affected by elevated concentrations of arsenic (As) in groundwater exposing a population of more than 35 million to
As toxicity. Geochemical studies of shallow alluvial aquifer in the Meghna flood plain show that the uppermost yellowish grey
sediment is low in As (1.03 mg/kg) compared to the lower dark grey to black sediment (5.24 mg/kg) rich in mica and organic
matter. Sequential extraction data show that solid phase As bound to poorly crystalline and amorphous metal (Fe, Mn, Al)-oxyhydroxides
is dominant in the grey to dark grey sediment and reaches its maximum level (3.05 mg/kg) in the mica rich layers. Amount of
As bound to sulphides and organic matter also peaks in the dark grey to black sediment. Vertical distributions of major elements
determined by X-ray fluorescence (XRF) show that iron (Fe2O3), aluminum (Al2O3) and manganese (MnO) follow the general trend of distribution of As in the sediments. Concentrations of As, Mn, Fe, HCO3
−, SO4
2− and NO3
− in groundwater reflect the redox status of the aquifer and are consistent with solid phase geochemistry. Mineralogical analysis
by X-ray diffraction (XRD) and scanning electron microscopy (SEM) fitted with energy dispersive X-ray spectrometer (EDS) revealed
dominance of crystalline iron oxides and hydroxides like magnetite, hematite and goethite in the oxidised yellowish grey sediment.
Amorphous Fe-oxyhydroxides identified as grain coating in the mica and organic matter rich sediment suggests weathering of
biotite is playing a critical role as the source of Fe(III)-oxyhydroxides which in turn act as sink for As. Presence of authigenic
pyrite in the dark grey sediment indicates active reduction in the aquifer. 相似文献
78.
随着中国住房改革的推进,城市居民通过居住迁移进行住房调整的行为日趋频繁。居住迁移作为城市空间分异和重构的微观机制在城市地理学、住房研究中得到了广泛关注,然而现有研究主要考察居住迁移的发生概率和驱动因素,较少论及居住迁移中的区位选择。论文基于2018年“上海市居民住房和生活空间调查”问卷,采用生命历程和时间地理学视角,刻画居民居住迁移的时空轨迹,并使用多项逻辑斯蒂回归模型探究居住迁移前后居住区位变化的影响因素。研究发现,上海市居民居住迁移的主要区位选择为跨环线向外迁移,但不同世代、不同户口、不同住房产权的居民的居住区位选择有较大差异。生命历程中的年龄、可达性中的工作单位区位以及住房属性中的产权性质都是影响居住迁移区位选择的重要因素。 相似文献
79.
生命历程视角下的广州市居民居住迁移的时空路径 总被引:4,自引:3,他引:1
转型与重构是现阶段中国城市发展的主旋律,在这一背景下,从个体生命历程的视角研究居住迁移的时空规律和影响因素有助于从深层次理解城市空间结构重构的内置机制,同时,对公共服务设施供给和提高居民生活质量等有一定的现实意义。以2007年进行的一次入户调查资料作为基础,研究了广州市居民居住迁移时空路径的生命历程特征。结果显示,广州市居民居住迁移的时空路径呈现出年龄偏好和空间偏好两个基本规律,这两个规律可以用“N”形曲线和“微笑曲线”来表达。“N”形曲线揭示了居住迁移率随年龄变化呈现出先上升后下降最后再上升的规律。微笑曲线则揭示了老人与孩子的居住迁移的方向较为集中而中年人的居住迁移方向较为离散的特点。文章据此从不同生命历程居民居住偏好的角度分析了产生上述居住迁移宏观规律的原因。从而证实了广州市居民居住迁移的时空路径具有若干生命历程的特征,对转型期广州市住房的供给与公共设施和服务的空间配置有着积极的意义。 相似文献
80.
Permian karstic bauxite and its Quaternary derivative, in western Guangxi, southwestern, South China Block, possess a total tonnage greater than 0.5 billion tons. The primary late Permian karstic bauxite formed in reduced environment in the background of Tethyan accretionary orogenesis. And as one consequence of Cenozoic convergence of the Indian and Eurasia continents, the primary orebody was uplifted, eroded and re-sedimented within Quaternary laterite. The geochemical variation and its controls during the ore transformation from Permian to Quaternary remain poorly understood. Quaternary ore blocks comprise an inner zone of fresh ore, and then it gradually transited through a middle zone to a margin with extensive weathering. One such bauxite block was selected and further subdivided into twenty-three samples for geochemical and mineralogical analysis. The inner and middle zones contain similar mineralogical compositions, dominated by diaspore and amesite, with minor illite, anatase, goethite, pyrite, zircon, and rutile. The margin is composed of diaspore, with small amounts of amesite, boehmite, illite, goethite, anatase, kaolinite, zircon, rutile, and barite. Bauxite in all three zones is composed of mainly Al, Si, Fe, and Ti, and high contents of Zr, Cr, Li, F, S, Zn, V, Sr, Nb, Ba, and REE. Variations in Fe2+ and Fe3+ between the three zones were observed. The elements Si, Al, Fe2+, Mg, Ba, Cr, F, Li, Ni, Zn, and REE decrease from the core of the ore block outwards, corresponding to an increase in S and Fe3+. Depletions in Si, Al, Fe2+, Mg, Ba, and Cr were caused by the dissolution of amesite. Most of the Al and Si in amesite were lost during the weathering, and minor retained to form kaolinite. Depletions in Li, Ni, and Zn resulted from changes in the depositional environment between the late Permian and Quaternary. Dissolution of REE-bearing fluorocarbonates resulted in depletions of REE and F. The enrichment of Fe3+ and S was related to the precipitation of goethite, hematite, and barite in an oxidizing environment, while local enrichment of Ce resulted from the redox change of Ce3+ → Ce4+ under the same condition. This shows that the chemical composition of laterite enwrapping the bauxite also took part in Quaternary bauxite transformation. This study shows that the elements migrations during bauxite transformation were influenced by multiple independent factors except for the elemental attributes. 相似文献