吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (2): 495-504.doi: 10.13278/j.cnki.jjuese.20190197

• 地质工程与环境工程 • 上一篇    

乍得湖盆地典型区域降雨入渗补给地下水试验

危润初1,2,3, 姜颖迪1, 李铭远4, 杜成额4, 乔小坡1   

  1. 1. 长沙理工大学水利工程学院, 长沙 410114;
    2. 水沙科学与水灾害防治湖南省重点实验室, 长沙 410114;
    3. 洞庭湖水环境治理与生态修复湖南省重点实验室, 长沙 410114;
    4. 湖南省有色地质勘查局二四七队, 长沙 410129
  • 收稿日期:2019-09-17 发布日期:2021-04-06
  • 作者简介:危润初(1984-),男,讲师,博士,主要从事地下水水文演化等领域的研究工作,E-mail:weirunchu@163.com
  • 基金资助:
    国家自然科学基金青年项目（41602264）；湖南省自然科学基金项目（2020JJ5572，2018JJ3543）

Rainfed Recharge Experiment in Typical Plain Area of Chad Lake Basin

Wei Runchu1,2,3, Jiang Yingdi1, Li Mingyuan4, Du Cheng'e4, Qiao Xiaopo1   

  1. 1. School of Hydraulic Engineering, Changsha University of Science&Technology, Changsha 410114, China;
    2. Key Laboratory of Water-Sediment Sciences and Water Disaster Prevention of Hunan Province, Changsha 410114, China;
    3. Key Laboratory of Dongting Lake Aquatic Eco-Environmental Control and Restoration of Hunan Province, Changsha 410114, China;
    4. Hunan Non-Ferrous Metals Geology Investigation Bureau Rows 247, Changsha 410129, China
  • Received:2019-09-17 Published:2021-04-06
  • Supported by:
    Supported by the Youth Fund of National Natural Science Foundation of China (41602264) and the National Natural Science Foundation of Hunan Province (2020JJ5572,2018JJ3543)

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摘要： 针对尼日利亚北部乍得湖盆地降雨入渗补给地下水的问题，选择典型区域开展土壤剖面取样工作，采用氯离子平衡法计算各剖面降雨入渗补给量，并结合野外调查、钻探等工作研究影响降雨入渗补给的主要因素。结果表明：4个取样点（Y1、Y2、Y3、Y4）土壤剖面年平均降雨入渗补给量分别为4.9、1.5、7.9、26.2 mm/a，平均值为10.1 mm/a，年平均降雨入渗补给率仅为0.72%、0.22%、1.17%、3.87%，平均值为1.49%；研究区降雨入渗补给量很少，降雨对地下水资源的补给有限，地下水的主要补给来源为Hadejia河；研究区蒸散发量大，植物根系发达、吸水能力强，地表入渗水分多在表层土壤中或泥质层与风积砂层交界面上消耗于蒸发蒸腾，最终散失到大气中。在人类活动严重改变Hadejia河水文情势的背景下，研究区这种独特的地下水补给特征导致地下水位快速下降，使得区内正面临较严重的地下水资源枯竭问题。

关键词: 乍得湖盆地, 尼日利亚, 降雨入渗补给, 氯离子平衡法

Abstract: Four moisture samples were obtained from the unsaturated zone profiles distributed in a typical plain area of Chad Lake basin to estimate the rainfed recharge based on the chloride (Cl) mass-balance method. The rainfed recharge results of the four sampling points (Y1, Y2, Y3, Y4) are 4.9, 1.5, 7.9, and 26.2 mm/a respectively; That is, the rainfed recharge rate are only 0.72%, 0.22%, 1.17%, and 3.87% correspondingly. Based on the survey work, combined with field investigation and drilling, the reason for the small amount of rainfed recharge is that the infiltration water from the surface is mostly consumed in evapotranspiration in the surface soil or the interface between the clay layer and the aeolian sand layer, and eventually lost to the atmosphere. Undoubtedly, the research area is facing a serious problem of water resources depletion under its single recharge source of Hadejia River, which has been interrupt by local people so greatly that the amount of infiltration to groundwater has been decreasing.

Key words: Chad Lake basin, Nigeria, rainfed recharge, chloride (Cl) mass-balance method

中图分类号: 

  • P641
[1] Scanlon B R, Keese K E, Flint A L, et al. Global Synthesis of Groundwater Recharge in Semiarid and Arid Regions[J]. Hydrological Processes, 2006, 20(15):3335-3370.
[2] Lerner D N, Issar A S, Simmers I. Groundwater Recharge:A Guide to Understanding and Estimating Natural Recharge[M]. Hannover:Heise, 1990.
[3] Gaye C B, Edmunds W M. Groundwater Recharge Estimation Using Chloride, Stable Isotopes and Tritium Profiles in the Sands of Northwestern Senegal[J]. Environmental Geology, 1996, 27(3):246-251.
[4] 尹立河, 王晓勇, 黄金廷, 等. 干旱区植被盖度增加对降水入渗补给地下水的影响:试验研究与数值模拟[J]. 地质通报, 2015, 34(11):2066-2073. Yin Lihe, Wang Xiaoyong, Huang Jinting, et al. The Impact of Vegetation Coverage Increase on Groundwater Recharge in the Arid Regions of Northwest China:Experimental and Numerical Study[J]. Geological Bulletin of China, 2015, 34(11):2066-2073.
[5] Ngatcha B N, Mudry J, Leduc C. Water Resources Management in the Lake Chad Basin:Diagnosis and Action Plan[J]. Applied Groundwater Studies in Africa, 2008, 13:65-84.
[6] Goes B J M. Estimate of Shallow Groundwater Recharge in the Hadejia-Nguru Wetlands, Semi-Arid Northeastern Nigeria[J]. Hydrogeology Journal, 1999, 7(3):294-304.
[7] Barbier E B. Upstream Dams and Downstream Water Allocation:The Case of the Hadejia-Jama'Are Floodplain, Northern Nigeria[J]. Water Resources Research, 2003, 39(11):1-9.
[8] Adelana S M A, Olasehinde P I, Bale R B, et al. An Overview of the Geology and Hydrogeology of Nigeria[J]. Applied Groundwater Studies in Africa, 2008, 13:171-197.
[9] Genik G J. Petroleum Geology of Cretaceous-Tertiary Rift Basins in Niger, Chad, and Central African Republic[J]. AAPG Bulletin, 1993, 77(8):1405-1434.
[10] 刘晓艳,陈建生,孙晓旭.采用氯离子示踪法计算沙漠降雨入渗量[J].农业工程学报,2010,26(增刊1):146-149. Liu Xiaoyan, Chen Jiansheng, Sun Xiaoxu. Application of Chloride Tracer Method to Study Replenishment Ratio of Precipitation in Desert[J]. Chinese Society of Agricultural Engineering, 2010,26(Sup.1):146-149.
[11] Newman B D, Campbell A R, Wilcox B P. Tracer-Based Studies of Soil Water Movement in Semi-Arid Forests of New Mexico[J]. Journal of Hydrology, 1997, 196(1/2/3/4):251-270.
[12] Phillips F M. Environmental Tracers for Water Movement in Desert Soils of the American Southwest[J]. Soil Science Society of America Journal, 1994, 58(1):15-24.
[13] Scanlon B R. Evaluation of Moisture Flux from Chloride Data in Desert Soils[J]. Journal of Hydrology, 1991, 128(1/2/3/4):137-156.
[14] 陈宗宇, 毕二平, 聂振龙, 等. 包气带剖面中古水文-气候信息的初步研究[J]. 地球学报, 2001, 22(4):335-339. Chen Zongyu, Bi Erping, Nie Zhenlong, et al. A Tentative Discussion on Paleohydrological and Paleoclimatical Information from Unsaturated Zone Profile[J]. Acta Geoscientica Sinica, 2001, 22(4):335-339.
[15] Goni I B, Fellman E, Edmunds W M. Rainfall Geochemistry in the Sahel Region of Northern Nigeria[J]. Atmospheric Environment, 2001, 35(25):4331-4339.
[16] Li C, Kang S, Zhang Q, et al. Major Ionic Composition of Precipitation in the Nam Co Region, Central Tibetan Plateau[J]. Atmospheric Research, 2007, 85(3/4):351-360.
[17] Safai P D, Rao P S P, Momin G A, et al. Chemical Composition of Precipitation During 1984-2002 at Pune, India[J]. Atmospheric Environment, 2004, 38(12):1705-1714.
[18] Vignaud P, Duringer P, Mackaye H T, et al. Geology and Palaeontology of the Upper Miocene Toros-Menalla Hominid Locality, Chad[J]. Nature, 2002, 418:152.
[19] Iwaco B V. Study of the Water Resources in the Komadougou-Yobe Basin[R]. Niamy:Nigeria-Niger Joint Commission for Cooperation, 1985.
[20] Carter R C, Alkali A G. Shallow Groundwater in the Northeast Arid Zone of Nigeria[J]. Quarterly Journal of Engineering Geology and Hydrogeology, 1996, 29(4):341-355.
[21] 霍思远, 靳孟贵, 梁杏. 包气带弱渗透性黏土透镜体对降雨入渗补给影响的数值模拟[J]. 吉林大学学报(地球科学版), 2013, 43(5):1579-1587. Huo Siyuan, Jin Menggui, Liang Xing. Impacts of Low-Permeability Clay Lens in Vadose Zone onto Rainfall Infiltration and Groundwater Recharge Using Numerical Simulation of Variably Saturated Flow[J]. Journal of Jilin University (Earth Science Edition), 2013, 43(5):1579-1587.
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