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1.
据1989年1月10日获悉,作为人们担心在首都圈发生直下型大地震(“南关东大地震”)的防灾对策,日本国土厅正为将东京的23区等指定为“地震防灾对策推进地区(暂名)”进行讨论研究。为此,他们打算在1月底听取由日本中央防灾会议指定加强地震防灾对策地区专门委员会研究讨论的有关预测地震  相似文献   

2.
我国减灾救灾法制建设以采取母子法模式为宜,尽早制定"减灾救灾基本法",用以指导和规范防灾减灾、备灾、救灾及灾后重建等环节的立法。在此基础上,以制定《防灾减灾法》为依托完善防灾减灾法律制度,以灾害准备金立法为重心完善备灾法律制度,以《自然灾害救助条例》为依托完善救灾法律制度,以《汶川地震灾后恢复重建条例》为基础完善灾后恢复重建法律制度,同时推进减灾救灾团体及人员奖惩保障立法,最终实现减灾救灾的法治化目标。  相似文献   

3.
为了防备在发生关东大地震同样震级的东京直下型大地震等灾害时首相官邸等中央发布指令的设施遭到毁灭性打击的情况,中曾根首相已确定了如下设想:在立川市建设“立川大防灾基地”,同时设立“第二首都官邸”,作为基地内的灾害对策总部的中枢。  相似文献   

4.
1983年3月18日,日本第274届灾害科学研究会在东京召开。地震防灾对策加强地区判定会成员、地震预报联络会副会长力武常次在会上作了“关于东京直下型地震”的报告。  相似文献   

5.
1999年4月日本制定的“推进新的地震调查研究——推进地震观测、测量、调查及研究的综合性基本措施”,迄今已有10年。其问,日本地震调查研究的环境正在发生着变化。例如,预测今后30年中将以很高的概率发生造成重大灾害的东海、东南海、南海和首都直下型等地震。  相似文献   

6.
山西省地震防灾协调组(扩大)会议于1992年3月4日在太原召开。省地震防灾协调组成员,全省各地市及省直有关厅局51个单位共60余人出席了会议。 大会由王敬副组长主持。协调组组长、山西省人民政府副省长吴达才在会上作了题为《防患于未然 为减轻地震灾害损失而努力》的报告。他在报告中强调指出,王茂林书记王森浩省长对如何加强抗震减灾工作做了重要批示,这对搞好抗震防灾工作有很重要的指导意义。吴达才同志从5个方面对防震减灾工作做了具体部署,并要求要充分发挥各级政府在地震防灾减灾工作中的主导和职能作用。各地要继续抓好地震监测预报,为地震防灾工作提供可靠的决策依据,同时应注意增强全社会的地震防灾意  相似文献   

7.
地震与城市     
正如国土厅向国会提交的防灾白皮书所述的那样,今年日本的震灾对策正在根据已公布的《灾害对策基本法》和《震灾对策推进纲要》把重点放在以下几个方面:(1)促进城市防灾化;(2)加强防灾体制和提高防灾意识;(3)促进地震预报工作。这样,作为国家来说也是把城市地震防灾化列为重点,并明确规定了基本方针和政策。可实际情况是,若使其具体化则会遇到各种难题,付诸实现还需要漫长的时间。虽然在城市  相似文献   

8.
<正>日本实施的地震防灾战略设定了总的战略目标,由于总战略是由5大地震防灾战略组成的,总战略的指标是在5大地震战略目标实施后的基础上综合设定的,并且5大地震防灾战略的目标设定均是按统一的要求、统一项目、格式、流程、方案预设的~([1-3])。这里仅以东海地震防灾战略为例,介绍日本地震防灾战略的具体推进实施情况(表1,图1)。  相似文献   

9.
本文结合汶川地震总结了村镇灾害的特点,在此基础上对比城市灾害,剖析了村镇灾害发生的原因,进一步指出研究村镇灾害评价方法的必要性和紧迫性。同时就国内地震、地质灾害研究方法进行了概况总结,主要从层次分析法和基于GIS技术两个方面构建了村镇灾害研究框架详图,为研究村镇防灾减灾大纲和各种灾害防治标准提供了一些参考。  相似文献   

10.
关于推进防灾减灾与提高城市可持续发展能力的思考   总被引:9,自引:0,他引:9  
探讨了城市化导致灾害加剧对城市可持续发展构成的危害,分析了城市防灾减灾能力的现状,从发挥政府主导作用、推进科技减灾、加大防灾减灾投入等方面,提出了强化城市防灾减灾能力、实现城市可持续发展的对策和建议。  相似文献   

11.
In this paper, the changes in sediment transport over 51 years from 1955 to 2006 in the Kuye River in the Loess Plateau in China are assessed. Key factors affecting sediment yield and sediment transport, such as precipitation depth, discharge, and human activities are studied. To investigate the changes in sediment yield in this watershed, a trend analysis on sediment concentration, precipitation depth, and discharge is conducted. Precipitation depths at 2 Climate Stations (CSs), as well as discharge and sediment transport at 3 Gauging Stations (GSs) are used to assess the features of sediment transport in the Kuye River. The rtmoff modulus (defined as the annual average discharge per unit area, L/(s·km^2)) and the sediment transport modulus (defined as the annual suspended sediment transport per unit area, t/(yr km^2)) are introduced in this study to assess the changes in runoff and sediment yield for this watershed. The results show that the highest average monthly discharge during the study period in the Kuye River is 66.23 m^3/s in August with an average monthly sediment concentration of 88.9 kg/m^3. However, the highest average monthly sediment concentration during the study period in the Kuye River is 125.34 kg/m^3 and occurs in July, which has an average discharge of 42.6 m^3/s that is much less than the average monthly discharge in August. It is found that both the runoff modulus and sediment transport modulus at Wenjiachuan GS on the Kuye River has a clear downward trend. During the summer season from July to August, the sediment transport modulus at Wenjiachuan GS is much higher than those at Toudaoguai and Longmen GSs on the Yellow River. The easily erodible loess in the Kuye River watershed and the sparse vegetation are responsible for the extremely high sediment yield from the Kuye River watershed. The analyses of the grain size distribution of suspended load in the Kuye River are presented. The average monthly median grain size of suspended load in the Kuye River is largest in February and then decreases until June. In July, the average monthly median grain size of suspended load approaches another peak and decreases until September. Then, the median grain size of suspended load starts to increase until February of the following year. However, the average monthly median grain size of suspended load in the Yellow River at Toudaoguai and Longmen GSs is the smallest between early summer and late fall The median grain size in the Yellow River starts to increase in November and approaches the largest size in January.  相似文献   

12.
13.
3He/4He ratios up to 3.5 times the ratio of atmospheric He were found in groundwater samples. The3He enrichment can be attributed to radiogenic3He produced by in-situ beta-decay of3H. This shows that tritiogenic3He is accumulating in confined waters. From tritiogenic3He and3H concentrations, ages of groundwaters can be calculated. Detection of tritiogenic3He gives a tool to trace a tritium contamination which occurred in the past and cannot be assessed only by the3H counting method.  相似文献   

14.
The aim of this study is to estimate likely changes in flood indices under a future climate and to assess the uncertainty in these estimates for selected catchments in Poland. Precipitation and temperature time series from climate simulations from the EURO-CORDEX initiative for the periods 1971–2000, 2021–2050 and 2071–2100 following the RCP4.5 and RCP8.5 emission scenarios have been used to produce hydrological simulations based on the HBV hydrological model. As the climate model outputs for Poland are highly biased, post processing in the form of bias correction was first performed so that the climate time series could be applied in hydrological simulations at a catchment-scale. The results indicate that bias correction significantly improves flow simulations and estimated flood indices based on comparisons with simulations from observed climate data for the control period. The estimated changes in the mean annual flood and in flood quantiles under a future climate indicate a large spread in the estimates both within and between the catchments. An ANOVA analysis was used to assess the relative contributions of the 2 emission scenarios, the 7 climate models and the 4 bias correction methods to the total spread in the projected changes in extreme river flow indices for each catchment. The analysis indicates that the differences between climate models generally make the largest contribution to the spread in the ensemble of the three factors considered. The results for bias corrected data show small differences between the four bias correction methods considered, and, in contrast with the results for uncorrected simulations, project increases in flood indices for most catchments under a future climate.  相似文献   

15.
Observations of trace gases (SO2, NH3, NO2 and O3) were made during the period 1981 to 1984 at 6 different locations representative of urban industrial, urban, nonurban, thermal power plant and marine environment. Diurnal variations of the trace gases were studied in an urban environment. Except in the urban industrial environment, the concentration of NH3 was found in the range of background values. Also, the average concentrations of NO2 and O3 at the different environments were in the order of background values. However, the concentrations of SO2 were substantially higher by about 7 times, in urban industrial and thermal power plant environments. The diurnal variations of SO2, NH3 and NO2 showed anitphase relationship with surface temperature at the urban environment station which is relatively free of industrial pollution. Discussion is centred on trace gas variations in different environments in India together with the values reported for various countries in the world.  相似文献   

16.
Changes in thermal extremes of the climate of Poland in 1951–2010 are examined. Warm extremes have become more frequent, while cold extremes have become less frequent. In the warming climate of Poland, the increase in the number of extremely warm days in a year and the decrease in the number of extremely cold days in a year have been observed. Also the increase of the maximum number of consecutive hot days in a year and the decrease of the maximum number of consecutive very cold and extremely cold days in a year have been observed. However, the trends are not of ubiquitous statistic significance, as the natural variability is strong.  相似文献   

17.
Cu concentrations in surface (river and lake) and subsurface waters are determined. The geographic pattern of Cu distribution in natural water is identified. This pattern is controlled by the difference between its concentrations in drained rocks and soils and the geochemical redox conditions of its migration. Territories with low, medium, and elevated Cu concentrations in natural waters are identified. The concentrations of Cu in natural waters of the region are found to be generally lower than the Clarke values.  相似文献   

18.
19.
Abstract

The basin area of the Ganges River in Bangladesh is extremely dependent on a regular water supply from upstream to meet requirements for agriculture, fisheries, navigation, salinity control, and domestic and industrial sectors. In 1975, India commissioned a barrage on the Ganges River at Farakka to divert a significant portion of the dry season flow in order to make the Calcutta Port navigable. Statistical analyses of discharge and water level data have been carried out to determine if significant changes have occurred in the hydrology of the Ganges system in Bangladesh in the post-Farakka period. Siltation of the Gorai River (an offtake of the Ganges River) has also been examined using the stage-discharge relationship and regression analysis. The analyses show that the diversion has caused considerable hydrological changes in the Ganges system in Bangladesh. The water supply in the dry season has been reduced substantially, while siltation of the Gorai River has increased significantly.  相似文献   

20.
In an active spreading area like Iceland, where the regional geothermal gradient is in the range 50–150°C/km, it is normally not a problem to find high enough temperature with deep drilling, but the difficulties arise with finding permeable layers at depth within the strata. Various volcanological methods can be applied in the search for aquifers and geothermal reservoir rocks. The flow pattern (as deduced from deuterium studies) indicates that the thermal water flows preferentially along high porosity stratiform horizons and dyke swarms from the recharge areas in the highlands to the hot spring areas in the lowlands. The primary porosity of the volcanic strata is dependent on the chemical composition and the mode of eruption of the volcanic units. Both the reservoir rocks and the flow channels forming the geothermal plumbing system are thought to vary from the Tertiary to the Quaternary provinces due to environmental conditions at the eruptive sites.  相似文献   

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