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1.
正封面故事:能源和重要矿产资源消费与经济社会发展关系图。人均能源和重要矿产资源消费"S"形规律的发现,揭示了能源和矿产资源消费增长与经济社会发展内在的本质联系,提出了人类资源消费增长极限的理论问题。该理论认为随着经济社会发展,人类对能源和矿产资源的消费不会无限增长。如果能够有效控制人口数量的非理性增长,全球资源的消费或需求存在着极限值。这项由中国地质科学院全球矿产资源战  相似文献   

2.
矿产资源需求理论与模型预测   总被引:40,自引:21,他引:19       下载免费PDF全文
本文介绍了以人均矿产资源消费与人均GDP“S”形规律、矿产资源消费强度变化倒“U”形规律和矿产资源需求波次递进规律等为核心的能源和矿产资源需求理论, 以及以此为基础建立的能源与矿产资源需求综合预测模型; 系统预测了2010-2030年全球及中国一次能源、粗钢、铜、铝需求趋势, 并与其他预测方法和预测结果进行了对比, 论证了这一理论模型的先进性和预测结果的可靠性。  相似文献   

3.
2012年12月12日,国际地质科学联合会主席Roland Oberhnsli教授与秘书长Ian Lambert教授在中国地质科学院副院长、国际地科联司库董树文教授的陪同下,应邀访问了中国地质科学院全球矿产资源战略研究中心。全球矿产资源战略研究中心主任王安建教授作了题为"全球矿产资源需求旺盛—国际地科联可以做得更好"的学术报告,报告包括能源与矿产资源消费的历史背景、能源与矿产资源消费的基本规律、未来20  相似文献   

4.
本文以能源和大宗矿产资源消费与经济发展的"S"形规律为基础,总结并讨论了发达国家经济社会发展过程中,人均能源和矿产资源消费增长的极限及其与基础设施建设、城市化水平、社会财富积累以及经济结构变化的关系;指出人类对美好生活的物质追求是推动能源和矿产资源消费增长的原动力,从农业社会、工业社会到后工业化社会,随着经济发展,即人均收入或人均GDP的不断提高,城市化率、基础设施建设和社会财富积累水平持续提升,大宗商品或资源性产品消费将陆续进入准近饱和状态,消费结构的改变,致使铁、铜、铝等大宗矿产在工业化中期开始陆续到达人均消费极限值,并引起产业结构调整升级,推动经济结构变迁;进入后工业化发展阶段,以服务业为主体的国民经济体系逐渐使人均能源消费增长到达极限值;强调国家集团或大国资源消费增长极限的到来是导致全球性矿产资源消费增长周期结束的根本原因。  相似文献   

5.
依据矿产资源需求"S"形理论原理,按照经济发展程度把全球各国划分为4四个国家集团和3个典型国家,以1950—2014年钢、铜、铅、锌消费量和GDP总量为对象,概略论述了全球资源消费的3个周期,系统分析了各国家集团在不同周期对全球资源消费增长的贡献率,以及资源需求弹性的变化规律,指出大国工业化和全球经济周期决定资源需求周期,认为当前全球矿产资源需求的低迷状态还将进一步深化,至少将延续3~5年。  相似文献   

6.
中国重要矿产资源的需求预测   总被引:36,自引:22,他引:14  
王高尚  韩梅 《地球学报》2002,23(6):483-490
以往对矿产资源的中长期需求预测,大都基于纯数学模型或情景分析对已有数据的经验外推。由于缺乏对工业化过程矿产资源消费需求基本规律的把握,预测结果几乎无一例外地存在巨大偏差。笔者在深入分析工业化经济增长与矿产资源消费需求的相关关系、基本规律和模式的基础上,探讨了工业化过程中矿产资源消费从怎样的初始值通过什么样的方式到达多高的峰值,进而提取经济增长与矿产资源消费需求的模式参数,预测了中国未来30a能源、钢、铜、铝、锌的消费需求。  相似文献   

7.
我国区域性矿产资源需求差异与趋势分析   总被引:1,自引:1,他引:0       下载免费PDF全文
本文测算了我国各地区的粗钢消费量, 计算了长三角、珠三角、环渤海以及我国中、东、西部三种矿产资源消费总量以及人均消费量, 对比分析了各地区以及发达国家在同一人均GDP水平下的三种矿产资源消费差异, 分析了各地区能源、水泥、粗钢的消费趋势。研究表明, 东部地区粗钢、水泥的人均消费即将到达峰值, 而能源消费峰值的到达还需要10年时间; 中、西部地区粗钢、水泥消费峰值将在10年内到达, 能源消费峰值的到达仍需15年时间。  相似文献   

8.
对于不可再生的矿产资源,由于生产和消费的迅速增长,对其研究空前地加强了.人们对矿产资源问题的注意力从来没有像现在这样大.在德意志联邦共和国汉诺威市,每隔三年召开一次矿产资源问题国际学术讨论会.1976及1979年召开的前两次会议主要探讨了地球矿产资源的潜力及影响矿产资源应用的各种问题.最新一次,即1982年召开的第三次国际讨论会则以“矿产勘查的新途径”为主题,广泛讨论了矿产资源政策;能源资源及金属非金属矿物原料的普查、勘探与评价等问题.1985年将召开新的一次讨论会.这是一个引人注目的矿产资源问题国际研讨中心.会议的东道主,联邦地球科学及自然资源研究所及下萨克森州地质调查所所长本德尔教授在1982年会议闭幕词中说:“许多国家,不论是发展中国家或是工业化  相似文献   

9.
工业部门作为终端能源消费中三大主要部门之一,对经济发展具有重要作用。本文系统分析了15个发达经济体100多年来工业部门终端能源消费与人口和经济发展(GDP)的关系,发现随着人均GDP的增长,工业部门的人均终端能源消费显现缓慢增长、加速增长、减速增长到零增长或负增长的"S"形轨迹,并可分为高、中、低三个类型。通过重点解剖美、日、德、法和意大利等典型国家工业部门终端能源消费与经济发展的历史,标定了不同类型"S"形曲线的起飞点、转折点和零增长点,讨论了工业部门终端能源消费与能源消费强度、二产比例、城市化率和人均钢铁消费的内在联系,建立了"S"形曲线的一般性数学模型。工业部门终端能源消费与经济发展定量关系的确定对于国家,特别是发展中国家把握工业化过程能源消费趋势、预测能源需求和制定相关能源政策具有重要意义。  相似文献   

10.
印度拥有全球18%的人口,消费全球约5%的一次能源,创造了全球8%左右GDP,是全球发展最快的国家之一,探讨印度未来能源需求对中国获取境外能源的影响具有重要的战略意义。本文在分析印度社会经济发展和能源消费的基础上,利用人均能源消费"S"形模型对2030年印度一次能源需求进行了预测并探讨了其对中国获取境外能源的影响。研究认为2030年以前,印度未来能源需求不会对中国境外获取天然气和铀矿资源产生较大影响。而由于中印两国石油进口量较大且与所有的增长都存在叠加,将影响全球石油的供需格局。同时鉴于两国石油进口来源地具有高度重叠性,印度未来能源需求的增加,将对中国境外获取石油资源产生重要的影响。  相似文献   

11.
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.  相似文献   

12.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

13.
Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ1 roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).  相似文献   

14.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.  相似文献   

15.
PALEOZOOLOGY     
正20140968Chen Xiaohong(Northeastern University,Shenyang 110819,China);Gong Enpu The Basic Characteristics of Early Carboniferous Coral Reef at Xiadong Village in Tianlin,Guangxi,and Its Sedimentary Environment(Acta Geologica Sinica,ISSN0001-5717,  相似文献   

16.
正20140985Chen Liang(Post-Doctoral Research Station of Mining Engineering,School of Nuclear Resources and Nuclear Fuel Engineering,University of South China,Heng-yang 421001,China);Huang Wei Composition of Major and Correlated Elements with Organic Matters and Paleoclimatic Implication for Lower Paleogene Sediments in Sanshui Basin  相似文献   

17.
正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli-  相似文献   

18.
MINERALOGY     
正20141362 Chen Juan(Laboratory for High Temperature and High Pressure Study of the Earth’s Interior,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China);Li Heping Progress in Major Element and Trace Element Analysis of Sulfide Minerals(Acta Mineralogica Sinica,ISSN1000-4734,CN52-1045/P,33(3),2013,p.351-362,5 illus.,4 tables,20 refs.)  相似文献   

19.
正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7),  相似文献   

20.
正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.)  相似文献   

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