夏季越南东北外海暖水的时空变化特征及其机理研究

Due to orographic blockage, a weak wind wake occurs in summer off northeast Vietnam in the South China Sea. Under the wind wake, warm water is observed from both high-resolution satellite data and hydrographic observations. The wake of warm water forms in June, continues to mature in July and August, starts to decay in September, and disappears in October. The warm water wake also shows robust diurnal variation – it intensifies during the day and weakens in the night. Warm water wakes can be generated through wind-induced mixing and thermal(latent heat flux) processes. In this paper, a mixed layer model is used to evaluate the relative importance of the two processes on seasonal and diurnal timescales, respectively. The results demonstrate that thermal processes make a greater contribution to the wake than wind-induced mixing processes on a seasonal timescale, while the warm water wake is dominated by wind-induced mixing processes on a diurnal timescale.     

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Knowing into oblivion: Clearing wastelands and imagining emptiness in Vietnamese New Urban Zones

Lands cleared for Vietnamese New Urban Zones are commonly described as ‘wastelands’ (??t hoang) in need of development. But clearing these lands in Vietnam's densely populated urban areas requires evicting large numbers of urban residents. How is it possible to render populated spaces as empty wastelands? This paper juxtaposes new ethnographic research in Ho Chi Minh City against historical scholarship on Vietnamese concepts of ‘clearing the wasteland’ and colonial civilizing projects of mise en valeur. In doing so, the article describes these concepts as parallel legitimizing strategies that effectively enable developers and planners to render previously occupied and utilized lands as empty, uninhabited wastelands. The article shows that the same narrative structure used in these earlier contexts is used to justify current urban development projects.     

Transformation of Fish Corrals in Nha Phu Lagoon,Vietnam: livelihood changes and implications

ABSTRACT

Coastal fisheries in Nha Phu lagoon, Vietnam, have encountered dramatic transformation in recent decades. Socio-economic and environmental impacts are examined through the case of fish corrals. The intensification and expansion of fish corrals has helped some households to enhance their income and livelihood assets. Technological and access-related changes associated with this transformation have also resulted in lower incomes, and even pushed poorer households into indebtedness by undermining their livelihood assets. The privatisation of common pool resources has also led to marginalisation of the poor, increasing inequality in access to natural resources and social differentiation, as not all households are able to benefit from the technological changes taking place, while access to natural resources is increasingly concentrated among the wealthier households who are driving this process. A range of measures are needed to alleviate poverty and promote more diverse sustainable livelihood development in fishing communities around the lagoon.     

广西对越边贸口岸的空间分析

广西是我国对越边贸的主要省区，拥有全方位开发的口岸，由于区位，交通条件的差异性，口岸群的空间结构具有明显的层次，并在边贸业迹上有所表现，为了优化广西边贸口岸的空间结构，文中提出了突出重点把凭祥、东兴建成现代化边贸口岸、培育特色口岸经济，加大边贸的开放力度、提高口岸群的整体水平，以及建立新型的边境贸易空间组织－边境贸易开发等对策建议。     

东南亚断裂构造的演化

本研究项目是采用诸如地质学解释、影像判读和地球物理探测等多种方法相结合进行的。在所得结果的基础上参考了越南国内外同行的一些资料编制了东南亚、越南及邻区的断裂构造图．其比例尺分别为1：4百万和1：1百万。分析所得结果显示出东南亚断裂构造演化的下列情况：1)在现今地质结构方面东南亚是欧亚岩石圈板块的东南部分．由一条消减带围绕．这条消减带的伸展从Myanmer开始,通过Nicobar,Java Timor直到东菲律宾。东南亚被Song Hong(即红河)断裂,Three Pagodas断裂和Hainam-Natuna断裂等2级断裂系统分成3个微板块。2)在早新生代．东南亚是分为5个微板块的。它们的分界断裂中有2个一级断裂(中央东海扩张带和Lupar-Kuching消减带)和3个二级断裂(即上述3个)。3)上述绝大多数二和三级断裂从晚新生代起活化且继承了从早新生代即已发生和发展了的二、三级断裂,但在某些条件下．运动方向却完全变成了相反,尤其是走滑运动的方向。我们的研究结果表明：在这一地区内,盆地、隆起、岩浆侵入、褶皱和局部断裂等构造的形成都取决于这些沿着一、二级走滑断裂的微板块运动。     

热带地区碳酸盐岩上覆红色风化壳的成因机理及元素演化

开展热带岩溶地区红色风化壳元素地球化学演化规律研究,有助于丰富碳酸盐岩风化成土理论的认识。在越南北部选取典型的碳酸盐岩风化剖面,分析热带气候条件下碳酸盐岩上覆红色风化壳中主量元素的物质来源和演化特征。结果表明:无论Ti/Zr的元素比值分析,Hf-Zr、Nb-Ta及Sm-Nd的元素对协变分析,还是上地壳元素平均值(UCC)标准化分析,两个剖面的上覆风化壳均显示原地残积的特征,即两个剖面是碳酸盐岩的原位风化产物。碳酸盐岩风化成土过程中,CaO、MgO淋失明显,Al_2O_3和Fe_2O_3发生富集,显示两个剖面均经历较强的风化过程,但是白云岩和灰岩剖面有一定的分异特征。越南北部白云岩风化剖面从基岩到上部土层显示出稳定的Ti-Fe元素共富集特征,而灰岩剖面中Fe的增长速率明显超过Ti。白云岩上覆风化壳经历了强烈的风化作用,其脱硅作用弱于灰岩风化剖面,而富集铝的作用强于灰岩。迁移系数的演化规律说明两个剖面中长石成分(钾长石、钠长石等)或次生矿物(伊利石等)在风化成土过程中逐渐分解,同时Al、Fe、Si等稳定元素的在风化剖面中不断富集。     

Itinerant livelihoods: Street vending‐scapes and the politics of mobility in upland socialist Vietnam

This paper explores the politics of mobility for a group of rural inhabitants attempting to diversify their livelihoods in an especially prescribed environment, namely ethnic minority street vendors living and working in upland socialist Vietnam. These Hmong, Yao and Giáy individuals face a political environment where access and trade rights shift on a near‐daily basis because of the impulses of state officials, and where ethnicity is central to determining who gets to be mobile and how. We analyse three groups of itinerant vendors—those vending on the streets of an upland tourist town, the mobile minority wholesalers who supply them and other traders, and vendors who trek with Western tourists—to reveal the nature of this trade environment, while also highlighting the ways in which ethnic minority vendors negotiate, work around and contest vending restrictions in numerous innovative ways. We find that this focus on the micro‐geographies and everyday politics of mobility is essential to understanding how rural Global South livelihoods are fashioned and diversified, in this case revealing specific relationships and negotiations regarding resource access, ethnicity, state authority and livelihood strategies.     

Subsurface eddies in the southern South China Sea detected from in-situ observation in October 2011

Two anticyclonic subsurface eddies (SSEs) are detected from the in-situ hydrography data of the southern South China Sea (SCS) during 15–25 October 2011. Both SSEs have the lens-shaped water bodies below the thermocline. Their maximum swirl speed appears at the depth of lens׳ core, which is also characterized by a dump in the T–S diagram. These eddies do not have an enclosed saline-water or warm-water body in its lens׳ core, which is different from those SSEs reported in other seas. These SSEs should be locally generated by the horizontal shear of the Southeast Vietnam Offshore Current. In the SSE generation site of the southern SCS, there is an upper-layer anticyclonic eddy (AE2) that is right above the SSE (SE2). After leaving its generation site, the eddy loses its energy source and starts to weaken. In this case, the eddy will decay quickly in the upper layer due to the restraint of the thermocline, and finally evolves into a pure subsurface eddy (i.e. SE4).     

越南西北部莱州地区新生代煌斑岩地球化学特征及其成因

越南西北部菜州地区出露的新生代煌斑岩岩脉对理解特提斯造山带东段的深部岩石圈特征和演化具有重要的地质意义.本文报道莱州地区煌斑岩的元素地球化学和Sr-Nd-Pb同位素组成特征,探讨其岩石成因.该地区煌斑岩属于钙碱性,钾质-超钾质煌斑岩特征.地球化学特征对比表明,菜州地区煌斑岩与哀牢山断裂带碱性岩具有相似的地球化学特征,但与海南和越南南部火山岩存在明显差异.分析结果表明,煌斑岩具有高的87Sr/86Sr比值、低143Nd/144Nd比值和高放射性成因Pb同位素组成特征.岩石的微量元素组成特征指示,形成煌斑岩的地幔源区可能经历过流体交代作用或沉积物组分的加入.低208Pb*/206Pb*比值暗示地幔源区富集事件是近期发生的,可能与晚古生代-早中生代印支地块向扬子地块俯冲事件有关.