吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (3): 762-772.doi: 10.13278/j.cnki.jjuese.20170322

• 地质工程与环境工程 • 上一篇    下一篇

基于环境同位素技术的河水补给研究——以沈阳黄家傍河水源地为例

苏小四1,2, 高睿敏1, 袁文真3, 鹿帅1, 苏东1, 张丽华4, 孟祥菲4, 左恩德1   

  1. 1. 吉林大学水资源与环境研究所, 长春 130021;
    2. 吉林大学建设与工程学院, 长春 130026;
    3. 中国地质科学研究院, 北京 100037;
    4. 黑龙江九○四环境工程勘察设计院, 哈尔滨 150027
  • 收稿日期:2017-12-08 出版日期:2019-06-03 发布日期:2019-06-03
  • 作者简介:苏小四(1971-),男,教授,博士生导师,主要从事地下水资源评价与管理、同位素水文地球化学等方向的研究,E-mail:suxiaosi@163.com
  • 基金资助:
    国家自然科学基金项目(41372238)

Research on River Recharge Based on Environmental Isotope Technology: A Case Study of Huangjia Riverside Well Field in Shenyang City

Su Xiaosi1,2, Gao Ruimin1, Yuan Wenzhen3, Lu Shuai1, Su Dong1, Zhang Lihua4, Meng Xiangfei4, Zuo Ende1   

  1. 1. Institute of Water Resources and Environment, Jilin University, Changchun 130021, China;
    2. College of Construction Engineering, Jilin University, Changchun 130026, China;
    3. Chineses Academy of Geological Sciences, Beijing 100037, China;
    4. 904 Environment Surveying and Designing Academy of Heilongjiang Province, Harbin 150027, China
  • Received:2017-12-08 Online:2019-06-03 Published:2019-06-03
  • Supported by:
    Supported by National Natural Science Foundation of China (41072038)

摘要: 河水入渗补给是傍河水源地的主要补给来源,确定河水补给强度对于促进水源地长期安全的开采具有十分重要的意义。以沈阳黄家水源地为研究区,通过对比研究区河水、地下水的水化学及氢氧稳定同位素特征,分析了水源地地下水的补给来源及强度。结果表明:傍河水源地地下水主要接受河水的入渗补给和区域地下水的侧向补给;受河床沉积物和含水介质的岩性及结构在空间上的差异影响,河水入渗补给后在向地下水位漏斗中心流动的过程中具有浅层和深层两条地下水流路径,深层地下水与河水的水力联系更为紧密;河水对地下水的补给强度具有明显的时空变化特点,表现为雨季河水入渗强度明显大于旱季,并且随着与辽河距离的增加,水源地地下水获得的河水补给量呈逐渐减小的趋势。

关键词: 环境同位素技术, 河水补给, 傍河水源地, 氢氧稳定同位素

Abstract: River recharge is a main source of riverside well field, and determining the recharge intensity of groundwater is of great significance for a long-term and safe exploitation of riverside well field. By taking the Huangjia riverside well field as an example,the authors analyzed the hydro-chemical components and the hydrogen and oxygen stable isotope characteristics of river and groundwater by using hydro-chemical technology and environmental isotope technology,and determined the recharge of groundwater and spatial and temporal variation of recharge intensity. The results show that the main recharges of groundwater are river recharge and regional lateral flow recharge. There are two main types of flow path from river to production wells, i.e. shallow flow path and deep flow path. The deep groundwater has a close hydraulic relationship with the river. The recharge from river to groundwater varies significantly in time and space. In terms of temporal variation, the intensity of river water in rainy season is larger than that in dry season; while in spatial variation, the effect of river infiltration declines with the increase of the distance from river bank to pumping wells.

Key words: environmental isotope technology, river recharge, riverside well field, hydrogen and oxygen stable isotopes

中图分类号: 

  • P59
[1] Bouwer H. Artificial Recharge of Groundwater:Hydrogeology and Engineering[J]. Hydrogeol J, 2002, 10(1):121-142.
[2] Farnsworth C E, Hering J G. Inorganic Geochemistry and Redox Dynamics in Bank Filtration Settings[J]. Environmental Science & Technology,2011, 45(12):5079-5087.
[3] Harvey J W, Drummond J D, Martin R L, et al. Hydrogeomorphology of the Hyporheic Zone:Stream Solute and Fine Particle Interactions with a Dynamic Streambed[J]. Journal of Geophysical Research, 2012, 117:1-20.
[4] Sophocleous M. Interactions Between Groundwater and Surface Water:The State of the Science[J]. Hydrogeology Journal, 2002, 10:52-67.
[5] Masaki H, Donald O R. Effects of Groundwater Exchange on the Hydrology and Ecology of Surface Waters[J]. Journal of Groundwater Hydrology, 2001, 43:327-341.
[6] Farnsworth C E, Voegelin A, Hering J G. Manganese Oxidation Induced by Water Table Fluctuations in a Sand Column[J]. Environmental Science & Technology, 2012, 46(1):277-284.
[7] Tufenkji N, Ryan J N, Elimelech M. Peer Reviewed:The Promise of Bank Filtration[J]. Environmental Science & Technology, 2002,36(21):422A-428A.
[8] Rivett M O, Buss S R, Morgan P, et al. Nitrate Attenuation in Groundwater:A Review of Biogeochemical Controlling Processes[J]. Water Research, 2008, 42:15-32.
[9] Scanlon B R, Healy R W, Cook P G. Choosing Appropriate Techniques for Quantifying Groundwater Recharge[J]. Hydrogeology Journal, 2002, 10:18-39.
[10] Paulsen R J, Smith C F, O'Rourke D, et al. Development and Evaluation of an Ultrasonic Around Water Seepage Meter[J]. Ground Water, 2001, 39(6):904-911.
[11] Landon M K, Rus D L, Harvey F E. Comparison of Instream Methods for Measuring Hydraulic Conductivity in Sandy Streambeds[J]. Ground Water, 2001, 39(6):870-885.
[12] Otz M H, Otz H K, Otz I, et al. Surface Water/Groundwater Interaction in the Piora Aquifers, Witzerland:Evidence from Dye Tracing Tests[J]. Hydrogeology Journal, 2003, 11:228-239.
[13] Koh D C, Ha K, Lee K S, et al. Flow Paths and Mixing Properties of Groundwater Using Hydrogeochemistry and Environmental Tracers in the Southwestern Area of Jeju Volcanic Island[J]. Journal of Hydrology, 2012, 432:61-74.
[14] Soulsby C, Piegat K, Selibert J, et al. Catchment-Scale Estimates of Flow Path Partitioning and Water Storage Based on Transit Time and Runoff Modeling[J]. Hydrological Processes, 2011, 25:3960-3976.
[15] Parkin G, Birkinshaw S J, Younger P L, et al. A Numerical Modeling and Neural Network Approach to Estimate the Impact of Groundwater Abstractions on River Flows[J]. Journal of Hydrology, 2007, 339:15-28.
[16] Dutton A, Wilkinson B H, Welker J M, et al. Spatial Distribution and Seasonal Variation in 18O/16O of Modern Precipitation and River Water Across the Conterminous USA[J]. Hydrological Processes, 2005, 19(20):4121-4146.
[17] Zagana E, Obeidat M, Kuells C, et al. Chloride, Hydrochemical and Isotope Methods of Groundwater Recharge Estimation in Eastern Mediterranean Areas:A Case Study in Jordan[J]. Hydrol Process, 2007, 21:2112-2123.
[18] Kalbus E, Reinstorf F, Schirmer M. Mearsuring Methods for Groundwater-Surface Water Interactions:A Review[J]. Hydrology and Earth System Sciences, 2006, 10:873-887.
[19] Song X F, Kayane I, Tanaka T, et al. A Study of the Groundwater Cycle in Sri Lanka Using Stable Isotopes[J]. Hydrological Processes, 1999, 13(10):1479-1496.
[20] Su X S, Xu W, Du S H. In Situ Infiltration Test Usinga Reclaimed Abandoned River Bed:Managed Aquifer Recharge in Shijiazhuang City, China[J]. Environmental Journal of Solids and Structures, 2014, 71(12):5017-5025.
[21] Su X S, Lu S, Gao R M, et al. Groundwater Flow Path Determination During Riverbank Filtration Affected by Groundwater Exploitation:A Case Study of Liao River, Northeast China[J]. Hydrological Sciences Journal, 2017, 62(14):2331-2347.
[22] Guglielmi Y, Mudry J. Estimation of Spatial and Temporal Variability of Recharge Fluxes to an Alluvial Aquifer in a Foreland Area by Water Chemistry and Isotopes[J]. Ground Water, 1996, 34(6):1017-1023.
[23] Weyhenmeyer C E, Burns S J, Waber H N. Isotope Studyof Moisture Sources, Recharge Areas, and Groundwater Flow Paths Within the Eastern Batinah Coastal Plain, Sultanate of Oman[J]. Water Resources Research, 2002, 38(10):1184-1206.
[24] 张磊,秦小光,刘嘉麒,等.淮南采煤区积水来源的氢氧稳定同位素证据[J]. 吉林大学学报(地球科学版),2015,45(5):1502-1514. Zhang Lei, Qin Xiaoguang, Liu Jiaqi,et al. Characters of Hydrogen and Oxygen Stable Isotope of Different Water Bodies in Huainan Coal Mining Area[J]. Journal of Jilin University (Earth Science Edition), 2015, 45(5):1502-1514.
[25] 于静洁,宋献方,刘相超,等. 基于δD和δ18O及水化学的永定河流域地下水循环特征解析[J]. 自然资源学报,2007,22(3):415-423. Yu Jingjie, Song Xianfang, Liu Xiangchao,et al. A Study of Groundwater Cycle in Yongding River Basin by Using δD, δ18O and Hydrochemical Data[J]. Journal of Natural Resources, 2007, 22(3):415-423.
[26] 董维红,孟莹,王雨山,等. 三江平原富锦地区浅层地下水水化学特征及其形成作用[J]. 吉林大学学报(地球科学版),2017,47(2):542-553. Dong Weihong, Meng Ying, Wang Yushan, et al. Hydrochemical Characteristics and Formation of the Shallow Groundwater in Fujin, Sanjiang Plain[J]. Journal of Jilin University (Earth Science Edition), 2017, 47(2):542-553.
[27] 左恩德.沈阳市黄家傍河水源地地下水开采潜力评价[D]. 长春:吉林大学,2016. Zuo Ende. Evaluation of Groundwater Exploitation Potential in Shenyang Huangjia Water Source[D]. Changchun:Jilin University, 2016.
[1] 张磊, 秦小光, 刘嘉麒, 穆燕, 安士凯, 陆春辉, 陈永春. 淮南采煤沉陷区积水来源的氢氧稳定同位素证据[J]. 吉林大学学报(地球科学版), 2015, 45(5): 1502-1514.
[2] 刘佩贵,束龙仓. 傍河水源地地下水水流数值模拟的不确定性[J]. J4, 2008, 38(4): 639-0643.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!