中国地质灾害防治成效与问题对策     

刘传正  陈春利 《工程地质学报》2020,28(2):375-383

文章回顾了中国地质灾害调查评价、监测预警、综合防治、应急响应、信息化建设、技术装备、技术标准、学术研究、行业进步和法治化建设等工作业绩。中国地质灾害造成的遇难人数1995~2000年年均死亡失踪1205人,2001~2005年均死亡失踪884人,2006~2010年均死亡失踪776人(2010年数据不含甘肃舟曲县城山洪泥石流造成的1765人死亡失踪),2011~2017年均死亡失踪395人,2018年死亡失踪112人。2001~2010年发生地质灾害总数量194702处,平均1.947万处/年;直接经济损失385.3亿元,平均38.5亿元/年,平均19.8万元/处。2011~2018年发生地质灾害总数量为84718处,平均1.06万处/年;直接经济损失355.7亿元,平均44.5亿元/年,平均41.9万元/处。2001年以来城乡社区直接经济损失占国家GDP的比例不断下降,平均年降率为0.016‰。地质灾害成功预报数量占地质灾害总数的比例从2003的5%上升到2018年的20%左右。经过采取各种减灾措施,城乡社区需要应急避险人数逐渐减少。总结了存在的问题和面临的形势,如防灾文化建设薄弱、法制不健全和直接经济损失统计局限于城乡社区而未覆盖工程建设行业的地质灾害等。提出了地质灾害防治要建立政府、企业、个人、社会(包括保险业)和科技界五位一体的防灾减灾“伙伴”关系等对策。  相似文献   

东北三省城乡协调发展格局及影响因素   总被引：3，自引：2，他引：1  

黄禹铭 《地理科学》2019,39(8):1302-1311

以东北三省36个地区为研究对象,系统构建了城乡协调的指标体系,采用基尼系数、空间自相关和空间回归等方法探讨了2005年、2010年和2015年东北三省城乡协调的空间格局和影响机制。研究表明:① 东北三省城乡协调度的区域差异不断扩大且具有明显的空间集聚特征,但集聚程度趋于减弱。② 不同地区城乡协调水平变化各异。研究期内,大连市和锦州市一直处于高水平城乡协调状态,朝阳市长期处于低水平城乡协调状态。鹤岗市和七台河市城乡协调度位次上升最明显,哈尔滨市和辽源市城乡协调度位次下降最显著。③ 从空间格局来看,中级城乡协调区增多且向北移动,初级城乡协调区减少且向中部集中,“南北高,中间低”的城乡协调格局基本形成。与此同时,城乡协调的冷热点均不断收缩,空间极化效应趋于减弱。④ 城镇化和农业规模化经营是促进东北城乡协调发展的主要力量,工业化并未显著促进东北城乡协调发展且与城乡协调发展负相关,农业现代化经营对城乡协调发展有正向作用,交通因素在近些年的促进作用逐渐凸显,经济发展水平与信息化水平对东北城乡协调发展的作用还不明显。  相似文献   

Study on the urban heat island effects and its relationship with surface biophysical characteristics using MODIS imageries     

Yongnian Zeng  Wei Huang  F. Benjamin Zhan  Honghui Zhang  Huimin Liu 《地球空间信息科学学报》2010,13(1):1-7

This study assesses surface urban heat island (UHI) and its associated surface physical characteristics using remote sensing approaches. TERRA/MODIS images acquired in 2005 in three different seasons were selected to generate land surface tem-perature and surface characteristics for the Changsha-Zhuzhou-Xiangtan metropolitan area in China. The intensity of urban heat is-land effects and its seasonal variations were examined. The result showed that UHI effects were significant both in the summer and the spri...  相似文献   

Daily variability of river concentrations and fluxes: indicators based on the segmentation of the rating curve     

Michel Meybeck  Florentina Moatar 《水文研究》2012,26(8):1188-1207

The variability of water chemistry on a daily scale is rarely addressed due to the lack of records. Appropriate tools, such as typologies and dimensionless indicators, which permit comparisons between stations and between river materials, are missing. Such tools are developed here for daily concentrations (C), specific fluxes or yields (Y) and specific river flow (q). The data set includes 128 long‐term daily records, for suspended particulate matter (SPM), total dissolved solids (TDS), dissolved and total nutrients, totalling 1236 years of records. These 86 river basins (10³–10⁶ km²) cover a wide range of environmental conditions in semi‐arid and temperate regions. The segmentation—truncation of C–q rating curves into two parts at median flows (q₅₀) generates two exponents (b_50inf and b_50sup) that are different for 66% of the analysed rating curves. After segmentation, the analysis of records results in the definition of nine major C–q types combining concentrating, diluting or stable patterns, showing inflexions, chevron and U shapes. SPM and TDS are preferentially distributed among a few types, while dissolved and total nutrients are more widely distributed. Four dimensionless indicators of daily variability combine median (C₅₀, Y₅₀), extreme (C₉₉, Y₉₉) and flow‐weighted (C*, Y*) concentrations and yields (e.g. C₉₉/C₅₀, Y*/Y₅₀). They vary over two to four orders of magnitude in the analysed records, discriminating stations and river material. A second set of four indicators of relative variability [e.g. (Y*/Y₅₀)/(q*/q₅₀)], takes into account the daily flow variability, as expressed by q*/q₅₀ and q₉₉/q₅₀, which also vary over multiple orders of magnitude. The truncated exponent b_50sup is used to describe fluxes at higher flows accounting for 75% (TDS) to 97% (SPM) of interannual fluxes. It ranges from ? 0·61 to + 1·86 in the database. It can be regarded as the key amplificator (positive b_50sup) or reductor (negative b_50sup) of concentrations or yields variability. C₅₀, Y₅₀, b_50sup can also be estimated in discrete surveys, which provides a new perspective for quantifying and mapping water quality variability at daily scale. Copyright © 2011 John Wiley & Sons, Ltd.  相似文献   

基于GIS的甘肃省区域经济时空差异研究   总被引：2，自引：0，他引：2  

王世杰  赵军 《测绘科学》2010,35(2):170-172

区域经济差异研究一直是区域经济学、发展经济学研究的核心问题之一,也是世界各国经济发展过程中的一个普遍性问题。一直受到各国学术界和政府决策部门的普遍关注。地处中国西北地区的甘肃省,经济社会发展较为落后,省内区域经济差异问题突出。深入分析甘肃省区域经济差异演变规律及其原因对于探索落后地区经济协调发展道路具有重要的理论和实践意义。本文在总结前人研究成果的基础上,采用一系列定量测度指标,运用GIS和空间统计分析方法,研究了2000-2006年间甘肃省区域经济差异及其演变规律。基于ESDA全局和局部空间自相关分析,在GIS软件和GeoDA空间统计软件的支持下,利用甘肃省2000-2006年各市、州和县域人均GDP数据,对甘肃省县域经济的总体和局部空间差异进行了实证分析。  相似文献   

基于GIS的湖北省区域经济差异空间统计分析   总被引：2，自引：0，他引：2  

杜小娟  吴华意  龚健雅 《测绘信息与工程》2010,35(1):23-25

运用了空间统计分析和地理信息系统技术相结合的方法，分析和研究了湖北省区域经济差异，揭示了湖北省区域经济差异的空间自相关和空间集聚特征。  相似文献   

Silurian and Devonian systems     

Maxwell R. Banks  E. D. Gill  K. L. Burns 《Australian Journal of Earth Sciences》2013,60(2):177-187

The Ediacara mineral field is situated 30 km W of Beltana on the western margins of the Flinders Ranges, South Australia, and consists of silver‐lead and copper deposits in lower Cambrian carbonate rocks that contain anomalous base‐metal contents throughout the Adelaide Geosyncline. The lower Cambrian rocks, which consist of the basal Parachilna Formation and overlying Ajax Limestone, rest disconformably on the Precambrian, and at Ediacara occupy a shallow N‐S elongate syncline near the hinge zone of the Adelaide Geosyncline. The main primary ore minerals of the silver‐lead mineralization are galena and pyrite, with very minor chalcopyrite and sphalerite, and rare tetrahedrite and pearceite. The gangue consists mainly of silica (both chalcedony and quartz), with minor dolomite and rare barite. The mineralization is stratabound and occurs in conformable zones, the lowest of which commences about 30–50 m above the base of the Cambrian sequence. The host to the silver‐lead mineralization, the Ajax Limestone, can be subdivided into three units which represent a set of lithologies, structures and organic traces indicative of a shallow near‐shore carbonate environment. The silver‐lead mineralization is mainly present in sandy and laminated dolomites which were deposited in an environment ranging from sub‐tidal to bar and channel and tidal flat, respectively. Four types of mineralization have been recognized; disseminated sulphides of syngenetic and/or diagenetic origin and epigenetic concentrations along stylolites, in veins and as breccia fillings. Post‐depositional solution activity has affected a large proportion of the carbonate sequence. The effects of this activity range from stylolites through stylobreccias to solution collapse breccias. The epigenetic concentrations of mineralizations have apparently been formed by the remobilization of the disseminated sulphides during solution activity. The ore and gangue minerals of the epigenetic mineralization display both euhedral forms and distinct colloform banding, and framboidal textures have also been observed in both pyrite and galena. There is evidence of repeated episodic precipitation and no simple paragenetic sequence can be recognized. Fluid inclusions in silica and dolomite associated with the epigenetic mineralization have homogenization temperatures of 159 to 199°C and freezing temperatures that indicate the fluids to be saline brines containing NaCl with CaCl₂ and/or MgCl₂. Sulphur isotope analyses show a range of 8³⁴S values from ‐12.5 to +8.6 per mil, with no evidence of significant differences between the four types of mineralization. The data suggest deposition of the disseminated sulphides as a result of biological reduction of seawater sulphate in a system partially open with respect to sulphate supply. Subsequent remobilization of sulphides apparently involved little or no sulphur isotope fractionation. The Ediacara silver‐lead deposits have many features in common with Mississippi Valley‐type lead‐zinc deposits and appear to have similarities in terms of genesis, in that the epigenetic mineralization has been formed as a result of post‐depositional solution activity during diagenesis in a sedimentary basin. The scale of transport of the metals deposited as the epigenetic mineralization at Ediacara appears, however, to have been very much less than that of the metals in other Mississippi Valley‐type deposits.  相似文献   

青岛市经济增长引发环境污染的冲击响应模式分析     

秦云鹏  于晓黎  方景清 《中国海洋大学学报(自然科学版)》2010,40(2)

经济的不断发展造成了极大的环境污染,需要人们用科学的手段对经济发展和造成的环境污染之间的关系进行客观判断。采用主成分分析法、格兰杰因果检验以及基于VAR的脉冲响应函数对青岛市的经济发展与环境污染二者间关系进行分析,结果发现由于环境承载力的存在,经济增长造成环境污染在很大程度上受到时滞的影响,经济增长引发环境问题是渐进的、长期的,所以在发展经济时不能只顾眼前利益而忽视对环境的长期影响,要注重可持续发展。  相似文献   

中国产业发展与布局的关联法则   总被引：6，自引：2，他引：6  

贺灿飞  朱晟君 《地理学报》2020,75(12):2684-2698

产业地理学研究产业空间分布及其动态演化规律。基于地理邻近性的集聚理论揭示了产业地理不平衡分布的内在机制。演化经济地理学借鉴演化经济学的历史视角,从历史角度考察经济活动空间分布的渐进演化机制,认为地理邻近性不是产业地理格局演化的充分必要条件,以认知邻近性为核心的多维邻近性能够提供更好的解释。本文从认知邻近视角系统地分析了中国区域产业发展与布局动态演化规律,总结出中国产业发展与布局的“关联法则”,即一个企业或区域进入（或退出）某项经济活动的概率是该企业或地区拥有的基于相关知识基础的经济活动的函数。本文全面地回顾了关联法则涉及的关键概念,梳理企业和区域尺度的实证研究成果,讨论关联法则在中国的适用性及其补充和拓展。本文指出：① 在认知邻近视角下,基于资源转换和组织学习等理论基础,关联法则研究了企业或区域发展新产业与现有产业之间的关系。② 关联法则不仅适用于中国企业和区域尺度,还会影响区域经济发展、创新和韧性等。③ 外部联系、冲击以及内部制度环境等可能会降低区域产业动态对本地产业基础的依赖性。关联法则指出中国区域需培育内生发展模式,围绕现有区域能力、技术和知识积累发展区域产业和实现区际产业优化布局与分工,逐步建立相关多样化的产业体系,增强区域韧性,支撑国内经济循环。  相似文献   

中国交通行业实施环境经济政策的协同控制效应研究     

邢有凯  刘峥延  毛显强  高玉冰  何峰  余红 《气候变化研究进展》2021,17(4):379-387

目前,交通行业已成为中国局地大气污染物和温室气体的重要排放来源之一,而且随着交通运输规模的不断扩大,与工业和生活排放相比,交通排放贡献占比呈相对增加趋势。文中构建了“CGE-CIMS联合模型”,对中国交通行业实施环境经济政策的局地大气污染物和CO₂协同控制效应进行量化评估。结果显示,与BAU情景相比,环境税、碳税、成品油消费税以及政策组合情景均促进了交通行业的电力消费替代汽油、柴油等石油制品,即使考虑政策实施后电力消费增加导致的间接排放,各情景下综合大气污染物协同减排量（ICER）仍为正值,即各项环境经济政策均具有较好的协同控制局地大气污染物和CO₂的效果。本文最后提出了包括聚焦高排放交通工具,以补贴低碳交通方式配合绿色税制改革,以及电力行业低碳发展等交通行业实施环境经济政策的配套措施建议。  相似文献