Characteristics of isotope in precipitation,river water and lake water in the Manasarovar basin of Qinghai–Tibet Plateau

The stable hydrogen and oxygen of lake, river, rain and snow waters were investigated to understand the water cycle characteristics of the drainage basin of Manasarovar Lake in Tibet. Both δD and δ ¹⁸O of river water are larger than those of lake water and the effect of altitude on both δD and δ ¹⁸O is not very significant. This phenomenon was suggested to occur because Manasarovar basin is located in Qinghai–Tibet Plateau which has low latitude, high altitude, abundant glaciers, thin air and intensive solar radiation, resulting in higher evaporation in lake water.     

Environmental effects of foreign trade and its spatial variations in mid-eastern provinces and cities of China

The studies on environmental effects of foreign trade and its spatial variations are helpful to design and implement environmental protection countermeasures.In order to eliminate the adverse effects of insufficient observation values on the accuracy of regression results and dynamic information quantity of fitting equation during empirical study,panel data of the mid-eastern provinces and cities of China from 1985 to 2007 were selected based on the adjustment of classical regression model in this paper.Panel unit root test and panel cointegration analysis method were applied to investigating the environmental effects of foreign trade and its spatial variations in the mid-eastern provinces and cities of China and its three groups divided by foreign trade dependence.The results show that all scale effects are positive,while all technical effects are negative and unable to counteract positive scale effects.Foreign trade development is regarded as an important cause for outstanding eco-environmental problems in the mid-eastern provinces and cities of China.Total effects and structural effects are significantly different among different groups because of spatial variations in environmental policies,export destinations,source of FDI,etc.Following the principle of′coordinating generality and considering differences comprehensively′,it is essential to issue a series of policies and countermeasures corresponding to differences in regional environmental effect of foreign trade,in order to coordinate the relationship between foreign trade development and eco-environment in each region.     

全球及中国周边地区资源环境科学数据库构建

 全球及中国周边地区资源环境科学数据是支撑包括全球变化在内的资源环境前沿科学研究,以及我国宏观决策制定重要的基础性支撑数据,对于保障国家安全具有重要意义。针对现阶段尚无一套完整的、标准化的全球及中国周边地区资源环境科学数据库的现状,结合中国科学院 "资源环境科学数据库建设与决策支持研究"实践工作,本文构建了包括3大体系在内的全球及中国周边地区资源环境科学数据库的基本框架,即资源环境科学数据库标准规范体系结构、全球资源环境科学数据库系统、中国周边资源环境科学数据库系统。其中,资源环境科学数据库标准规范体系结构,包括3个大类共计22类标准规范;全球资源环境科学数据库系统包括2大类、13亚类、35个小类的数据库;中国周边地区资源环境科学数据库由东北亚、东南亚、南亚和中亚4个区域共计23小类数据库构成,以期为后续相关大尺度资源环境科学数据库的构建提供探索性的借鉴。今后将进一步完善全球及中国周边地区资源环境科学数据库构建工作的深化与拓展研究。     

土质场地重力式挡土墙地震土压力振动台实验研究

汶川震区路基挡土墙震害表明,地震动荷载作用下重力式挡墙的位移、破坏与基础场地形式有关,除岩质场地和土质场地挡墙所共有的外倾形式,土质地基挡土墙还表现有整体推移及下部向外推移的倾转变形等复杂模式,因此地震土压力大小及分布也将受到这种复杂土-结相互作用的影响。基于碎石土及风化花岗岩填料的土质场地重力式挡土墙大型振动台模型实验,对挡土墙地震土压力及变形模式开展了对比研究,发现在强震作用下,土质地基挡墙因基础约束较弱而产生位移,并伴随明显的墙—土分离现象,致使实测地震土压力较之抗震设计规范计算值偏小（0.4g峰值加速度下约小6%～15%）,但作用点高度变化不大。由实验结果与现行抗震规范计算值的安全系数对比,认为对土质场地挡墙的地震土压力计算,按现行国内抗震设计规范基本能满足实际工程抗震设计需要;对于地震区挡墙设计,在允许挡墙发生少量容许位移的前提下可采用内摩擦角较大、自稳能力更好的墙背填料以减少地震土压力。     

Formation of chlorite rims and the impact of pore-lining chlorite on reservoir quality: a case study from Shiqianfeng sandstones in upper Permian of Dongpu Depression,Bohai Bay Basin,eastern China

The source material, precursor and formation processes of chlorite rims, and impact of pore-lining chlorite on reservoir quality of the Shiqianfeng sandstones, Dongpu Depression, Bohai Bay Basin, China, are studied using an integrated approach, including core observation, point-count analysis of thin-sections, scanning electron microscopy, electron microprobe analysis and cathode luminescence. The petrographic analysis shows that chlorite rims consist of grain-coating chlorite, poorly crystalline pore-lining chlorite and euhedral-crystallised pore-lining chlorite. The chemical composition shows that pore-lining chlorite is mainly Fe-rich with an average of 0.785 for Fe/(Fe+Mg) ratio. Petrographic analysis shows a large amount of volcanic dust (3.0～16.0 vol%, average of 7.93 vol%) in Shiqianfeng sandstones, which determines the formation of poorly crystalline pore-lining chlorite. Transformation of volcanic dust to smectite rims started with shallow burial depth at an early diagenetic stage, followed by in situ alteration of the smectite rims to poorly crystalline chlorite rims. Euhedral-crystallised chlorite mainly develops in sandstones with high porosity, high permeability and open flow systems. Pore-lining chlorite can inhibit quartz overgrowth but cannot effectively prevent pore-filling of authigenic quartz, carbonate and kaolinite cements, and therefore cannot prevent porosity destruction. However, the occurrence of pore-lining chlorite is a barometer of good reservoir quality and intense hydrodynamic conditions.     

Modeling the influence of urbanization on urban pluvial flooding: a scenario-based case study in Shanghai,China

Natural Hazards - Rapid urbanization has brought great productivity, prosperity and challenges to Shanghai in the last few decades. This paper focuses on the influence of urbanization on urban...     

Quantitative Analysis of Mineralization-Alteration Index about the Huize Lead-zinc district in Northeast Yunnan, China

<正>1 Introduction The super-large Huize lead-zinc ore district is one of the most representative lead-zinc deposits in Northeastern Yunnan poly-metallic deposit concentration district.So far,studies(Liu and Lin,1999;Han et al.,2007)on the type of deposits like the Huize lead-zinc deposit,focused on deposit genesis,the sources of metallogenic materials,     

Geochemistry Characteristics of Granodiorite Porphyry in the Degongniuchang Copper Deposit, Muli, Sichuan Province, China

<正>1 Introduction 1The Sanjiang region in SE Tibet Plateau and NW Yunnan is known to have formed by amalgamation of Gongwanaderived continental blocks and arc terranes as a result of oceanic subduction followed by continental