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地下水同位素国际研讨会在京召开

已有 5342 次阅读 2013-11-11 20:01 |个人分类:科研笔记|系统分类:科研笔记| 国际会议, 研讨会, 地下水, 同位素

       地下水动力学与补给研究中同位素与水化学数据处理分析与解释国际学术会议(以下简称“地下水同位素国际研讨会”)于2013114日至8日在北京召开。此次会议是受国际原子能机构委托,我所和院工程地质力学重点实验室具体承办的国际组织区域性会议。来自亚太地区14个国家的代表和我国代表60余人参加了会议。 

  大会开幕式由我所庞忠和研究员主持,国际原子能机构(IAEA)技术官员M. Choudhry博士中国国家原子能机构(CAEA)项目官员刘汉思先生、我所所长助理郭敬辉研究员等先后致词。 

  本次会议有26位代表作了大会报告,重点围绕地下水补给区与补给量的确定,地下水运动的动力学等主题。涉及大气降水同位素背景值,地表水径流分割,地下水地表水相互作用等相关内容。我所庞忠和研究员、黄天明副研究员、孔彦龙博士后、李捷博士生分别在报告中重点介绍了中国同位素文学及其在地下水补给与循环研究中的应用方面取得的新进展,重点评述了水汽判源与降水过程刻画、地表地下水相互作用、地下水入渗补给、古气候古水文等方面的应用,具体介绍了该课题组近年来在地下水同位素研究中取得的新成果。与会代表认为地下水补给与循环的研究对于地下水资源的可持续开发利用与保护具有重要意义。环境同位素在确定地下水起源、补给、运动、混合、定年等方面具有突出的优越性。一方面广泛地用于研究多种水文地质过程机理,另一方面,越来越多地用于标定地下水水流与溶质运移数值模型,为地下水资源管理提供支撑。希望今后加强相互交流合作。 

  会议期间,亚太地区项目协调组召开了专门会议,重点交流与评估了在国际原子能机构水资源合作项目(RAS7022)框架下各国取得的进展。包括中国在内的14个国家分别提交了国家报告,在评估进展的基础上制定了后两年的工作计划。国外代表们还考察了北京市地下水监测网回龙观代表性观测井等设施,以及建设中的通州区张家湾的地下水科学试验基地,包括北京市地面沉降观测场、地下水一井多层监测点、水盐运移试验场和三维弥散试验场等,增进了对北京市地下水工作的了解。 

[中科院地质所报道]

会 议 日 程

时间

地点:北京外国专家大厦二楼多功能厅

9:00-9:20

开幕式(主持人:庞忠和)

9:20-9:40

全体参会人员合影

114日上午       主持人:庞忠和、Manzoor Choudhry

9:40-10:05

Manzoor Choudhry

国际原子能机构

Water Resources Program at the IAEA

10:05-10:30

庞忠和

中科院

地质与地球所

Groundwater Studies Using Isotopes and Other Environmental Tracers in China during 1992-2012: A Review

10:30-10:55

文冬光

中国地质调查局

Applications of isotope technologies in hydrogeological survey of main basins in China (特邀报告)

10:55-11:15

11:15-11:40

Suzanne Hollins

Australian Nuclear Science and Technology Organisation

Radiocarbon dating and the challenges in revealing the “age” of groundwater-an example from an evaporation-dominated system in arid Australia

11:40-12:05

陈宗宇

中国地科院

水环所

Sustainability of intensively exploited aquifer systems in the North China Plain-Insights from environmental tracers

(特邀报告)

12:05-13:30

114日下午        主持人:陈宗宇、Suzanne Hollins

13:30-13:55

Uwe Morgenstern

GNS Science - New Zealand

Time lag of the water in the Lake Rotorua catchment and delayed arrival of contaminants from past land use activities

13:55-14:20

马金珠

兰州大学

Groundwater availability and renewal in the Northwest China

(特邀报告)

14:20-14:45

Janchivdorj Lunten

Mongolian Academy of Sciences

Ground Water Resources, Gobi Desert in Mongolia and some results of isotope application for study

14:45-15:10

Wan Zakaria Tahir

Malaysian Nuclear Agency

Assessment of Groundwater Recharge Using Environmental Isotope and In-direct Conventional Approached Techniques in the North Kelantan River Basin, Malaysia

15:10-15:30

114日下午        主持人:M. Azam TasneemViraj Edirisinghe

15:30-15:55

苏小四

吉林大学

Combined C and S isotope analysis of petroleum hydrocarbon biodegradation in a shallow contaminated aquifer

(特邀报告)

15:55-16:20

Somashekar Rayasamudra Kalegowda

Bangalore University
(INDIA)

Assessment of Source and origin of 222Rn in the groundwater of south Karnataka using isotope Hydro-chemical technique

16:20-16:45

马致远

长安大学

The evolution and indicating significance of strontium isotope in the geothermal water of basin type

16:45-17:10

蒋勇军

西南大学

Use of environmental isotopic (Sr, S and C) to trace human impacts on karst groundwater contamination from Nanshan underground river system, SW China

18:00

115日上午        主持人:马金珠Somashekar Rayasamudra Kalegowda

8:30-8:55

Viraj Edirisinghe

Atomic Energy Authority
(SRI LANKA)

Groundwater recharge study - Jaffna Peninsula - Sri Lanka: An assessment using stable isotope technique

8:55-9:20

黄天明

中科院

地质与地球所

Soil profile evolution following land-use change: Implications for groundwater quantity and quality

9:20-9:45

Paston Sidauruk

National Nuclear Energy Agency (INDONESIA)

Subsurface flow potential study in  gunung kidul karst area using isotopes technique

9:45-10:10

Nasir Ahmed

Bangladesh Atomic Energy Commision

Using Isotope Techniques to Investigate Groundwater Dynamics and Recharge Condition for Sustainable Groundwater Resource Management in Surma basin, Sylhet, North Eastern of Bangladesh

10:10-10:30

115日上午        主持人:叶淑君、Uwe Morgenstern

10:30-10:55

M. Azam Tasneem

Pakistan Atomic Energy Commission

Applying isotopes to investigate groundwater dynamics and recharge rate: case studies from Pakistan

10:55-11:20

李捷

中科院

地质与地球所

Dynamics and recharge rates of groundwater in the East Junggar Basin, NW China based on 14C and stable isotope measurements

11:20-11:45

Soledad Castaneda

Philippine Nuclear Research Institute

Application of isotope Techniques in Verifying Groundwater Recharge Processes  in Bulacan Province, Philippines

11:45-12:05

Ji-Hun Ryu

Korea Atomic Energy Research Institute

A study of isotopes (δD and δ18O) in precipitation and groundwater in the KURT site to investigate groundwater recharge and flow

12:05-13:30

115日下午        主持人:苏小四、Soledad Castaneda

13:30-13:55

Kiattipong Kamdee

Thailand Institute of Nuclear Technology

Application of isotope techniques in groundwater exploration and potential evaluation of Carbonate Aquifers in Saraburi and Lob Buri Provinces, Thailand

13:55-14:20

叶淑君

南京大学

A modified global model for predicting the tritium distribution in precipitation, 1960–2005 (特邀报告)

14:20-14:45

孔彦龙

中科院

地质与地球所

Using deuterium excess to quantify recycled moisture fraction in precipitation of an arid region

14:45-15:10

张光辉

北京普瑞亿科科技有限公司

The Novel Application of Laser Spectroscopy Technique for Stable Isotope Measurement

15:10-15:35

朱湘宁

北京理加联合科技有限公司

Utilizing cavity ring-down spectroscopy for high-precision analysis of the triple oxygen isotopic composition of water and water vapor

15:35-15:55

15:55-16:40

主题讨论Panel Discussion)(主持人:庞忠和)

16:40-17:00

闭幕式

 

 Topics of the Panel Discussion

  • How are isotope techniques applied in groundwater recharge studies in the AP region? How are they suitable for different geographical and geological settings? How are they useful for different investigation purposes?
  • What contributions can isotope techniques make to the study of groundwater dynamics? How are they applied in groundwater dynamics studies in the AP region?
  • What needs to be done in order to improve isotope data interpretation and use?

 

 

 

 

 

 



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