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1.
韩再生 《水文地质工程地质》2005,32(2):118-120
1 会议概况国际水文地质学家协会IAH主办的第33届国际水文地质大会于2004年10月10～15日在墨西哥Zacatecas市举行,且是与拉丁美洲水文协会第7届会议联合召开的。出席该次学术会议的代表来自36个国家,约400人。本次会议的主题为:认识地下水流动—从局部到区域尺度。学术交流共分9个专题进行,分别为:(1)地下水流的环境作用;(2)水化学和同位素数据用于确定局部和区域流动;(3)坚硬岩介质中标定地下水流;(4)水流系统在污染运移中的作用;(5)局部和区域地下水系统中的补给;(6)湿地与地下水流;(7)滨海地区不同的地下水流;(8)地下水流系统模型;(9)… 相似文献
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2003年9月22日在斯洛文尼亚北部城市布莱德召开了国际水文地质学家协会IAH理事会。理事会成员、各专业委员会和国家委员会的代表共32人出席会议。IAH中国委员会的代表韩再生出席会议,陈述了IAH中国委员会提交的在中国举办2006年国际水文地质第34届大会的申请报告。会后,IAH理事会于2003年10月6日正式来函,明确将2006年国际水文地质大会委托中国主办。2006年国际水文地质学术会议期间,还将进行IAH成立50周年的纪念活动。国际水文地质学家协会IAH组织的学术活动,代表着全世界水文地质发展的各个方面。中国(原地质矿产部)曾在国际水文… 相似文献
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钟立勋 《中国地质灾害与防治学报》2006,17(3):79-79
水文地质学作为与国民经济发展密切相关的应用学科，在世界各国水资源调查、保护和管理方面发挥着重要的支撑作用。2006年是国际水文地质学家协会（IAH）成立五十周年。因此，2006年10月09日-2006年10月13日国际水文地质学家协会和中国国土资源部将在北京市联合举办“第34届国际水文地质大会”。这将是继1988年中国在桂林市成功举办“第21届国际水文地质大会”之后，再次在中国举办国际水文地质大会。 相似文献
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韩再生 《水文地质工程地质》2007,34(6):I0004-I0004
本刊讯:第35届国际水文地质大会2007年9月16~21日在葡萄牙首都里斯本市举行。本次会议由国际水文地质学家协会IAH葡萄牙分会承办。来自35个国家的400多位代表参加了会议,其中中国代表10人,分别来自中国地质调查局和中国科学院系统。本次会议的主题“地下水与生态系统”。会议共设17个专题:(1)地下水与地表水相互作用及其对河流、泉水基流和湿地可持续利用的重要性。(2)地下水水质,在依存生态系统中面临的主要过程。(3)评估和确定在依存于地下水的生态系统中地下水自然与人工补给过程中的作用。(4)在生态系统和过程中地下水污染的影响。(5)… 相似文献
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第三届“未来地下水资源危机”国际学术会议于 2 0 0 1年 6月 2 5～ 2 9日在葡萄牙的里斯本市举行。该会议由联合国教科文组织、国际水文地质学家协会等联合主办。参加这次会议的有来自五大洲 2 7个国家的 1 2 0多位专家和学者。我国向这次会议提交了 4篇论文 ,在大会上宣读论文一篇。本人受教育部的资助作为这次国际学术会议的学术委员会成员参加了会议 ,并在大会上宣读了论文。第三届“未来地下水资源危机”国际学术会议的宗旨是 :探讨新世纪地下水系统可能发生的所有问题 ,并以可持续发展的原理来解决出现的问题。会议包括 1 0个专题 ,下… 相似文献
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《水文地质工程地质》1986,(1)
国际水文地质协会于1985年9月8日至13日,在英国剑桥丘吉尔学院召开名为“水文地质为人类服务”的第18届大会,同时举行了学术讨论会。我国陈梦熊、辛奎德、袁道先及林学钰四位出席会议。 参加会议的各国代表约200多人,是一次规模较大的国际学术会议。到会代表中许多都是国际知名人士,主要有:协会顾问、英国水文地质界元老布肯博士(S.Buchan),瑞士著名岩溶水文地质学家、协会 相似文献
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韩再生 《水文地质工程地质》2004,31(3):115-116
世界地下水资源图由联合国教科文组织、世界地质图委员会、国际水文地质学家协会、国际原子能机构和德国地球科学及自然资源研究院共同组织编制,其目标是利用地理信息系统在全球尺度上汇总地下水资源,以比例尺1:25M的图件为基础,为国际社会了解世界地下水系统提供基础。2004年3月在法国巴黎召开了世界地下水资源图指导委员会工作会议,8月将在第32届国际地质大会上展示1:50M世界地下水资源图。最终的成果将于2006年国际水文地质学家协会成立50周年之际出版。 相似文献
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世界地下水资源图由联合国教科文组织、世界地质图委员会、国际水文地质学家协会、国际原子能机构和德国地球科学及自然资源研究院共同组织编制，其目标是利用地理信息系统在全球尺度上汇总地下水资源数据，以比例尺1：25M的图件为基础，为国际社会了解世界地下水系统提供基础资料。2004年3月在法国巴黎召开了世界地下水资源图指导委员会工作会议，8月将在第32届国际地质大会上展示1：50M世界地下水资源图。最终的成果将于2006年国际水文地质学家协会成立50周年之际出版。 相似文献
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国际水文地质学家协会IAH主办的第33届国际水文地质大会于2004年10月10—15日在墨西哥Zacatecas市举行。出席会议的代表来自36个国家，约400人。会议共进行5天，其中学术交流4天(含开幕式和闭幕式)，会间野外考察1天。 相似文献
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Before 1985, there were a few Chinese participators for International Association of Hydrogeologists which founded in 1956. The Chinese team composed of senior hydrogeologists attended the 17th and 18th IAH congress in 1985. More and more Chinese delegates were present at the conferences since then. The IAH National Chapter of China was first established in 1987 and organized related activities continuously since that time. The IAH members in P.R. China increased in these years. IAH congresses have been hold in China twice. The 21th congress was held in Guilin City in October, 1988. The 34th congress was held in Beijing in October, 2006. The IAH China Chapter serves for all IAH members and other scientists promoting groundwater sciences in China. There were a lot of national conferences on Hydrogeology and Groundwater sciences held almost every year since 1987. Those national conferences associate with Commission on Hydrogeology, Geology Society of China in operation. Many Chinese IAH members were the editors and responsible for the Chinese translation for the abstract of Hydrogeology Journal. The Journal of Groundwater Science and Engineering is an international journal for the natural sciences. The sponsors are IAH China chapter, Institute of Hydrogeology and Environmental Geology, CAGS. 相似文献
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Groundwater flow and the associated surface water flow are potential negative factors on underground tunnels. Early detection of environmental impacts on water resources is of significant importance to planning, design and construction of tunnel projects, as early detection can minimize accidents and project delays during construction. The groundwater modeling software package Groundwater Modeling System (GMS), which supports the groundwater numerical codes MODFLOW and FEMWATER, was utilized to determine the impact of tunneling excavation on the hydrogeological environment in a regional area around the tunnel and a local hot springs area, at the “Tseng-Wen Reservoir Transbasin Diversion Project”, in Taiwan. A hydrogeological conceptual model was first developed to simplify structures related to the site topography, geology and geological structure. The MODFLOW code was then applied to simulate groundwater flow pattern for the hydrogeological conceptual model in the tunnel area. The automated parameter estimation method was applied to calibrate groundwater level fluctuation and hydrogeological parameters in the region. Calibration of the model demonstrated that errors between simulated and monitored results are smaller than allowable errors. The study also observed that tunneling excavation caused groundwater to flow toward the tunnel. No obvious changes in the groundwater flow field due to tunnel construction were observed far away in the surrounding regions. Furthermore, the FEMWATER code for solving 3-D groundwater flow problems, in which hydrogeological characteristics are integrated into a geographic information system (GIS), is applied to evaluate the impact of tunnel construction on an adjacent hot spring. Simulation results indicated that the groundwater drawdown rate is less than the groundwater recharge rate, and the change to the groundwater table after tunnel construction was insignificant for the hot spring area. Finally, the groundwater flow obtained via the GMS indicated that the hydrogeological conceptual model can estimate the possible quantity of tunnel inflow and the impact of tunnel construction on the regional and local groundwater resources regime of the transbasin diversion project. 相似文献
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Hydrogeology Journal - The study defines the hydrogeological framework of the Quaternary aquifer of south Bengal Basin, India, and the impact of urbanisation on the groundwater resources in and... 相似文献
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WU Ai-min HAO Ai-bing GUO Hai-peng LIU Jing-tao ZHANG Er-yong WANG Huang WANG Xin-feng WEN Xue-ru ZHANG Cui-guang 《地下水科学与工程》2020,8(3):195-209
This paper reviewed the main achievements of hydrogeological survey in China, summarized the significant progress of hydrogeological survey over the past decade, and forecasted the key responsibilities for hydrogeological survey in the p14th Five-year Planq. The significant progress includes: China established the 1: 50 000 standard hydrogeological survey system with Chinese characteristics and produced the new generation of high-quality hydrogeological maps; the national groundwater monitoring project was completed and accepted, which marks China taking the leading position in groundwater monitoring internationally; fruitful results were achieved in the national groundwater quality survey, and groundwater quality background values were basically identified and checked; hydrogeological and environmental geological survey was continuously promoted in karst areas and the ecological restoration of rocky desertification achieved remarkable results; China strengthened layer exploration techniques for groundwater, integrating the key and practical techniques of layer exploration and monitoring; the exploration of groundwater in the poverty-stricken regions and old revolutionary base areas were effectively promoted to strongly guarantee the poverty alleviation and drinking water safety; the mystery of desert groundwater was uncovered, making up for the shortage of 1: 250 000 hydrogeological survey in the Badain Jaran Desert; and more efforts were made to conduct survey on the water resources in the basin, and to finish the unified measurement of national-scale groundwater level. 相似文献
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Qin Huanhuan Andrews Charles B. Tian Fang Cao Guoliang Luo Yong Liu Jiurong Zheng Chunmiao 《Hydrogeology Journal》2018,26(4):1061-1081
Hydrogeology Journal - Beijing, in the North China plain, is one of the few megacities that uses groundwater as its main source of water supply. Groundwater accounts for about two-thirds of the... 相似文献
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The International Association of Hydrogeologists (IAH): reflecting on 60 years of contributions to groundwater science and water management 总被引：2，自引：0，他引：2
The 60th anniversary of the founding of the International Association of Hydrogeologists (IAH) is an important milestone that allows pause for reflection on how the association has evolved over the years and the contributions it has made to groundwater science and water management. IAH was founded in 1956 at the 20th International Geological Congress and developed rapidly during the 1980s and 1990s in response to a growing global interest in groundwater mapping and in sound approaches to resource protection and sustainable aquifer management. Incorporated in 2000, IAH has now secured its position as the world’s leading international association specialising in groundwater with over 4,100 members in 131 countries. Much credit for this success must go to members, past and present, whose individual efforts and collaboration with sister institutions are documented here. These members have shaped the association’s goals and contributed selflessly to its scientific programmes, publications and educational and charitable activities. Looking ahead to the next 60 years, it is essential that IAH does not rest on past achievements but listens and adjusts to the needs of members while continuing to pursue its mission of furthering the understanding, wise use and protection of groundwater resources throughout the world. 相似文献
18.
Water vulnerability assessment in karst environments: a new method of defining protection areas using a multi-attribute approach and GIS tools (EPIK method) 总被引：42，自引：12，他引：30
Groundwater resources from karst aquifers play a major role in the water supply in karst areas in the world, such as in Switzerland.
Defining groundwater protection zones in karst environment is frequently not founded on a solid hydrogeological basis. Protection
zones are often inadequate and as a result they may be ineffective. In order to improve this situation, the Federal Office
for Environment, Forests and Landscape with the Swiss National Hydrological and Geological Survey contracted the Centre of
Hydrogeology of the Neuchatel University to develop a new groundwater protection-zones strategy in karst environment. This
approach is based on the vulnerability mapping of the catchment areas of water supplies provided by springs or boreholes.
Vulnerability is here defined as the intrinsic geological and hydrogeological characteristics which determine the sensitivity
of groundwater to contamination by human activities. The EPIK method is a multi-attribute method for vulnerability mapping
which takes into consideration the specific hydrogeological behaviour of karst aquifers. EPIK is based on a conceptual model
of karst hydrological systems, which suggests considering four karst aquifer attributes: (1) Epikarst, (2) Protective cover,
(3) Infiltration conditions and (4) Karst network development. Each of these four attributes is subdivided into classes which
are mapped over the whole water catchment. The attributes and their classes are then weighted. Attribute maps are overlain
in order to obtain a final vulnerability map. From the vulnerability map, the groundwater protection zones are defined precisely.
This method was applied at several sites in Switzerland where agriculture contamination problems have frequently occurred.
These applications resulted in recommend new boundaries for the karst water supplies protection-zones.
Received: 27 October 1997 · Accepted: 4 July 1998 相似文献
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Adamson James K. LaVanchy G. Thomas Stone Brandon Clark James A. Dykstra Stuart J. Taylor Matthew J. 《Hydrogeology Journal》2021,29(6):2285-2304
Hydrogeology Journal - There are sparse hydrogeological data and insufficient hydrogeological knowledge in many areas of the world reliant on groundwater. Nicaragua’s Pacific coast is one... 相似文献
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在华北平原东部,选择典型地区(地调局衡水水文地质科学试验场),开展不同层位的抽水试验工作,在充分分析研究区水文地质条件的基础上,揭示在抽水试验过程中不同层位、不同时间的地下水的水化学和同位素组成,探索地下水垂向循环特征。研究表明:研究区地下水划分为三种地下水类型,随地下水埋藏深度的增加,水质逐渐变好,地下水溶解性总固体减小,硬度降低,具有垂向分带性。第Ⅰ含水组为现代水,由大气降水补给,第Ⅱ、Ⅲ含水组为现代水与古水的混合水,水力联系密切,有浅层地下水的越流补给;第Ⅳ、Ⅴ含水组为古水,水力联系不如前者密切,没有上部含水层发生越流补给;第Ⅲ、Ⅳ含水层没有水力联系。 相似文献