建立高海拔矿山测量控制网的思路     

王云生 《云南地质》2012,(2):249-252

受海拔高、空气稀薄、气候无常、高差较大等自然条件的影响,高海拔地区进行测量作业与低海拔地区有很大差别。根据高海拔地区矿山特点,结合多年矿山控制测量、特别是高海拔矿山控制测量经验,讨论在高海拔地区矿山因地制宜地建立测量控制网的方法。  相似文献   

年度土地变更调查新机制之探索   总被引：2，自引：2，他引：0  

李健  张纯  徐勇  江韦希 《地理空间信息》2011,(4):156-158

介绍了武汉市土地变更调查的历史沿革情况,通过对新旧机制的对比以及分析新机制存在的问题,从而对变更调查新机制进行了探索研究。  相似文献   

Normalizing economic loss from natural disasters: A global analysis   总被引：3，自引：0，他引：3  

Eric Neumayer  Fabian Barthel 《Global Environmental Change》2011,21(1):13-24

Climate change is likely to lead to an increase in the frequency and/or intensity of certain types of natural hazards, if not globally, then at least in certain regions. All other things equal, this should lead to an increase in the economic toll from natural disasters over time. Yet, all other things are not equal since affected areas become wealthier over time and rational individuals and governments undertake defensive mitigation measures, which requires normalizing economic losses if one wishes to analyze trends in economic loss from natural disasters for detecting a potential climate change signal. In this article, we argue that the conventional methodology for normalizing economic loss is problematic since it normalizes for changes in wealth over time, but fails to normalize for differences in wealth across space at any given point of time. We introduce an alternative methodology that overcomes this problem in theory, but faces many more problems in its empirical application. Applying, therefore, both methods to the most comprehensive existing global dataset of natural disaster loss, in general we find no significant upward trends in normalized disaster damage over the period 1980-2009 globally, regionally, for specific disasters or for specific disasters in specific regions. Due to our inability to control for defensive mitigation measures, one cannot infer from our analysis that there have definitely not been more frequent and/or more intensive weather-related natural hazards over the study period already. Moreover, it may still be far too early to detect a trend if human-induced climate change has only just started and will gain momentum over time.  相似文献   

Rapid earthquake loss assessment after damaging earthquakes     

M. Erdik  K. ŞeşetyanM.B. Demircioğlu  U. HancılarC. Zülfikar 《Soil Dynamics and Earthquake Engineering》2011

This article summarizes the work done over the last decades regarding the development of new approaches and setting up of new applications for earthquake rapid response systems that function to estimate earthquake losses in quasi-real time after an earthquake. After a critical discussion of relevant earthquake loss estimation methodologies, the essential features and characteristics of the available loss estimation software are summarized. Currently operating near-real-time loss estimation tools can be classified under two main categories depending on the size of area they cover: global and local systems. For the global or regional near-real-time loss estimation systems: GDACS, WAPMERR, PAGER, and NERIES-ELER methodologies are presented together with their loss estimations for the 2009 Abruzzo (L’Aquila) earthquake in Italy. Examples are provided for the local rapid earthquake loss estimation systems, including the Taiwan Earthquake Rapid Reporting System, Real-time Earthquake Assessment Disaster System in Yokohama, Real Time Earthquake Disaster Mitigation System of the Tokyo Gas Co., and Istanbul Earthquake Rapid Response System.  相似文献   

Comparing gravity and gravity gradient surveys     

Gary J. Barnes  John M. Lumley  Phill I. Houghton  Richard J. Gleave 《Geophysical Prospecting》2011,59(1):176-187

Noise levels in marine and airborne full tensor gravity gradiometer surveys together with conventional land, marine and airborne gravity surveys are estimated and analysed in gridded form, resulting in relations that detail how these different survey systems can be compared analytically. After defining survey parameters including line spacing, speed and instrument bandwidth, the relations estimate the noise levels that result on either grids of gravity (gz) or gravity gradient (Gzz) as a function of the spatial filtering often applied during geological interpretation. Such comparisons are believed to be a useful preliminary guide for survey selection and planning.  相似文献   

甘肃小陇山林区甘肃鼢鼠危害面积的气象预测预报技术研究   总被引：5，自引：0，他引：5  

许彦平  姚晓红  乔艳君 《地球科学进展》2011,26(8):881-886

甘肃小陇山林区位于我国四大自然植被区系（华北、华中、喜马拉雅、蒙新）交汇处的温带向亚热带过渡带,林业植物种类繁多、茂密,但区内地形、地貌复杂,气候差异大,林业生物灾害频繁,环境气候条件是其发生发展的主要制约因素。为此,进行区内林业生物灾害的气象预测预报技术研究,对林业有害生物灾害的预防、防治和林业产业发展具有显著的指导...  相似文献   

2010年中国非开挖行业调查     

颜纯文 《岩土钻凿工程》2011,(2):1-3,10

本文分析了中国地质学会非开挖技术专业委员会对2010年我国非开挖行业的调查和统计,主要是水平定向钻机的销售情况和非开挖管道修复与更换方法在管道工程施工中的应用情况,最后总结了2010年我国非开挖行业发展的几个特点。  相似文献   

高精度磁测在维西拉嘎洛铁矿勘查中的应用     

王进朝  李石磊  燕永锋  苏昌学  于斌 《云南地质》2011,30(3):332-335,361

测区引起磁异常的有磁铁矿(化)体和玄武岩,二者之间的磁性差异很大,为磁法勘探寻找磁铁矿奠定物性基础。通过磁法勘探的野外作业和室内数据整理分析,并经异常推断解释圈出矿体5个,并经坑探验证有效。  相似文献   

寻甸柯渡新村地质灾害与煤矿采矿影响分析     

吴文利  WU Wen-li 《云南地质》2011,30(2):167-170,150

不良工程地质组合导致房屋地基开裂或滑移,墙体承重失衡导致房屋结构性破裂。煤矿开采直接导致地下水位下降,部分影响建筑物地基稳定性及地面塌陷。  相似文献   

http://www.sciencedirect.com/science/article/pii/S1674987111000156   总被引：1，自引：0，他引：1  

Xiaohuan Xi  Zhongfang Yang  Yujun Cui  Shumei Sun  Chengguang Yu  Min Li 《地学前缘(英文版)》2011,2(2):115-123

Employing the Unit Soil Carbon Amount (USCA) approach, soil carbon storage was calculated across the Northeast Plain of China based on the Multi-purpose Regional Geochemical Survey conducted in 2004 – 2006 (MRGS). The results indicated that the soil organic carbon (SOC) storage in topsoil (0 – 0.2 m), subsoil (0 – 1 m) and deep soil (0 – 1.8 m) was 768.1 Mt, 2978.4 Mt and 3729.2 Mt with densities of 3327.8 t/km2, 12,904.7 t/km2 and 16,157.5 t/km2, respectively. These values were consistent with national averages, whereas the soil carbon densities showed a clear increasing trend from the southern area of the Northeast Plain (Liaoning), to the middle (Jilin) and the northern Plain (Heilongjiang) — particularly in terms of topsoil carbon density, which increased from 2284.2, to 3436.7 and 3861.5 t/km2, respectively. In comparison to carbon data obtained from the Second National Soil Survey in 1984 – 1986 (SNSS), the topsoil SOC storage values from the MRGS were found to have decreased by 320.59 Mt (29.4%), with an average annual decline of 16.0 Mt (l.73%) over the 20 years. In the southern, middle and northern areas of the plain, soil carbon densities decreased by 1060.6 t/km2, 1646.4 t/km2 and 1300.2 t/km2, respectively, with an average value of 1389.0 t/km2 for the whole plain. These findings indicate that the decrease in soil carbon density varied according to the different ecosystems and land use types. Therefore, ratios of soil carbon density were calculated in order to study the carbon dynamic balance between ecosystems, and to further explore distribution characteristics, as well as the sequestration potential of SOC.  相似文献