基于氢氧同位素的华北平原降水入渗过程

王仕琴; 宋献方; 肖国强; 王志民; 刘鑫; 王鹏

基于氢氧同位素的华北平原降水入渗过程

1.
中国科学院地理科学与资源研究所, 中国科学院陆地水循环与地表过程重点实验室, 北京, 100101;
2.
天津地质矿产研究所, 天津, 300170

基金项目: 国家自然科学基金资助项目(40671034)

详细信息

作者简介:
王仕琴(1981- ),女,甘肃靖远人,博士研究生,主要从事水文水资源、流域水循环方向研究.E-mail:wangshiqin99@gmail.com

中图分类号: P339;P334.2

Appliance of oxygen and hydrogen isotope in the process of precipitation infiltration in the shallow groundwater areas of North China Plain

1.
Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;
2.
Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China

Funds: The study is financially supported by the National Natural Science Foundation of China(No.40671034).

摘要: 华北平原地下水浅埋区水循环主要以垂直方向上的入渗、蒸发和蒸腾的方式存在,同位素可以作为一种有效"示踪剂"揭示降水入渗补给地下水的过程。选择华北平原中、东部地下水浅埋区的衡水和沧州为典型实验点,研究不同降水特征、土壤质地和植被条件下入渗过程的差异性。结果表明,土壤非均质条件下(沧州),降水入渗补给过程中伴随着蒸发、植被蒸腾作用以及与土壤前期水分的强烈混合作用,活塞流入渗的同时土壤100 cm深度可能还存在大孔隙优先流;土壤均质条件下(衡水),降水向下均匀入渗,入渗速度较快,土壤水运动以新水基本代替老水的活塞流为主要形式,并经过强烈的蒸发浓缩作用补给地下水。
- 华北平原 /
- 稳定同位素 /
- 降水入渗 /
- 土壤水 /
- 地下水
Abstract: In the shallow groundwater areas of North China Plain water cycle mostly occurs as infiltration,evaporation and evapotranspiration in the vertical direction,in which the unsaturated zone plays an important role in precipitation and groundwater. Isotope can be used to trace the process when the precipitation infiltrates and recharges groundwater. In this paper Cangzhou and Hengshui sites are selected as the typical shallow groundwater areas to research the difference of the infiltration process under the different precipitation features,soil textures and vegetation conditions. The results show that at the site with the heterogeneous soil texture the precipitation infiltrates and moves in soil as the piston mode and the mixture effect,and the evapotranspiration effect during the infiltration process is significant in the distribution of soil water. Some evidence is provided for the existence of the preferable flow at 100 m depth. The groundwater is mainly recharged by precipitation1 However,at the homogeneous site the infiltration process is uniform and the soil water moves as piston mode,too. Both deep soil water and groundwater are totally recharged by precipitation. After precipitation the recharged groundwater experiences strong evaporation effect.
- North China Plain /
- stable isotopes /
- precipitation infiltration /
- soil water /
- groundwater

[1]	HSIEH J C,CHADWICK O A,KELLY E F,et al.Oxygen isotopic composition of soil water:quantifying evaporation and transpiration[J].Geoderma,1998,82(1/2/3):269-293.
[2]	张应华,仵彦卿,温小虎,等.环境同位素在水循环研究中的应用[J].水科学进展,2006,17(5):738-747.(ZHANG Ying-hua,CHU Yan-qin,WEN Xiao-hu,et al.Application of environmental isotopes in water cycle[J].Advances in Water Science,2006,17(5):738-747.(in Chinese))
[3]	张应华,仵彦卿.黑河流域不同水体中δ¹⁸O的变化[J].水科学进展,2007,18(6):864-870.(ZHANG Ying-hua,CHU Yan-qin.Variation of δ¹⁸O in water in Heihe river basin[J].Advances in Water Science,2007,18(6):864-870.(in Chinese))
[4]	田立德,姚檀栋,孙维贞,等.青藏高原中部土壤水中稳定同位素变化[J].土壤学报,2002,39(3):289-295.(TIAN Li-de,YAO Tan-dong,SUN Wei-zhen,et al.Stable isotope in soil water in the middle of Tibetan plateau[J].Acta Pedologica Sinica,2002,39(3):289-295.(in Chinese))
[5]	许士国,刘盈斐,孙万光.扎龙湿地包气带土壤水分垂直运移的稳定同位素研究[J].水文,2006,26(5):1-6.(XU Shi-guo,LIU Yin-fei,SUN Wan-guang.Research on the stable isotope for soil water vertical transporting in unsaturated zone of Zhalong wetland[J].Hydrology,2006,26(5):1-6.(in Chinese))
[6]	徐庆,刘世荣,安树青,等.四川卧龙亚高山暗针叶林土壤水的氢稳定同位素特征[J].林业科学,2007,43(1):8-14.(XU Qing,LIU Shi-rong,AN Shu-qin,et al.Characteristics of hydrogen stable isotope in soil water of Sub-Alpine Dark Coniferous Forest in Wolong,Sichuan province[J].Scientia Silvae Sinicae,2007,43(1):8-14.(in Chinese))
[7]	方生,陈秀玲.华北平原大气降水对土壤淋洗脱盐的影响[J].土壤学报,2005,42(5):730-736.(FANG Shen,CHEN Xiu-ling.Influence of atmospheric precipitation on soil leaching and desalinizationin the North China Plain[J].Acta Pedologica Sinica,2005,42(5):730-736.(in Chinese))
[8]	卫克勤,林瑞芬.论季风气候对我国雨水同位素组成的影响[J].地球化学,1994,23(1):33-40.(WEI KE-qin,LIN Rui-fen.The influence of the monsoon climate on the isotopic composition of precipitation in China[J].Geochimica,1994,23(1):33-40.(in Chinese))
[9]	李发东.基于环境同位素方法结合水文观测的水循环研究:以太行山区流域为例[D].北京:中国科学院研究生院,2005.(LI Fang-dong.Hydrological cycle research based on environmental isotopes and integrated hydrological experiments:Case study in a representative catchment,Taihang Mountainous[D].Beijing:Graduate School of the Cchinese Academy of Sciences.2005.(in Chinese))
[10]	LARS B,RAJINDER K,SAXENA,et al.Soil water movement estimated from isotope tracers[J].Hydrological Sciences,1987,32(4):497-519.
[11]	KUNG KJS.Preferential flow in a sandy vadose zone:Field observations[J].Geoderma,1990,46:51-58.
[12]	ZIMMERMANN U,MUNNICH K O,ROETHER W.Downward movement of soil moisture traced by means of hydrogen isotopes[C]//Isotope Techniques in the hydrologic cycle,Geophysical Monograph Series 11.[S.l.] :American Geophysical Union,1967:28-36.
[13]	CLARK I D,FRITZ P.Environmental Isotope in Hydrogeology[M].New Jersey:Lewis Publishers,1997:328.
[14]	FONTES J C,YOUSFI M,ALLISON G B.Estimation of long-term,diffuse groundwater discharge in the northern sahara using stable isotope profiles in soil water[J].Journal of Hydrology,1986,86(3/4):315-327.
[15]	周炼,刘存富,王佩仪.河北平原第四系咸水同位素组成[J].水文地质工程地质,1998(3):4-8.(ZHOU Lian,LIU Cun-fu,WANG Pei-yi.Isotope compositon of Quartnary saline water in Hebei province[J].Hydrogeology and Engineering Geology,1998(3):4-8.(in Chinese))

[1]	李怀恩, 贾斌凯, 成波, 郭超, 李家科. 海绵城市雨水径流集中入渗对土壤和地下水影响研究进展 . 水科学进展, 2019, 30(4): 589-600. doi: 10.14042/j.cnki.32.1309.2019.04.014
[2]	马斌, 梁杏, 靳孟贵, 李静, 牛宏. 华北平原典型区水体蒸发氢氧同位素分馏特征 . 水科学进展, 2015, 26(5): 639-648. doi: 10.14042/j.cnki.32.1309.2015.05.005
[3]	詹泸成, 陈建生, 张时音. 洞庭湖湖区降水-地表水-地下水同位素特征 . 水科学进展, 2014, 25(3): 327-335.
[4]	张光辉, 费宇红, 刘春华, 冯慧敏, 严明疆, 王金哲. 华北滹滏平原地下水位下降与灌溉农业关系 . 水科学进展, 2013, 24(2): 228-234.
[5]	谭秀翠, 杨金忠, 宋雪航, 查元源. 华北平原地下水补给量计算分析 . 水科学进展, 2013, 24(1): 73-81.
[6]	章斌, 郭占荣, 高爱国, 袁晓婕, 李开培, 马志勇. 用氢氧稳定同位素评价闽江河口区地下水输入 . 水科学进展, 2012, 23(4): 539-548. doi: CNKI:32.1309.P.20120614.2251.019
[7]	袁瑞强, 宋献方, 王鹏, 张应华, 王仕琴, 唐常源. 白洋淀渗漏对周边地下水的影响 . 水科学进展, 2012, 23(6): 751-756. doi: CNKI: 32.1309.P.20121101.1801.020
[8]	郭占荣, 黄磊, 袁晓婕, 刘花台, 李开培. 用镭同位素评价九龙江河口区的地下水输入 . 水科学进展, 2011, 22(1): 118-125.
[9]	孟玉川, 刘国东. 长江流域降水稳定同位素的云下二次蒸发效应 . 水科学进展, 2010, 21(3): 327-334.
[10]	王永森, 陈建生, 汪集旸, 童海滨, 陈亮. 降水过程中氢氧稳定同位素理论关系研究 . 水科学进展, 2009, 20(2): 204-208.
[11]	储开凤, 汪静萍. 中国水文循环与水体研究进展 . 水科学进展, 2007, 18(3): 468-474.
[12]	章光新, 邓伟, 何岩, Ramsis Salama. 中国东北松嫩平原地下水水化学特征与演变规律 . 水科学进展, 2006, 17(1): 20-28.
[13]	沈彦俊, 夏军, 张永强, 肖捷颖, 唐常源, 近藤昭彦. 陆面蒸散的双源遥感模型及其在华北平原的应用 . 水科学进展, 2006, 17(3): 371-375.
[14]	张光辉, 费宇红, 刘克岩, 王金哲. 华北平原农田区地下水开采量对降水变化响应 . 水科学进展, 2006, 17(1): 43-48.
[15]	顾慰祖, 陆家驹, 谢民, 张汝智. 乌兰布和沙漠北部地下水资源的环境同位素探讨 . 水科学进展, 2002, 13(3): 326-332.
[16]	田立德, 姚檀栋, 沈永平, 杨梅学, 叶柏生, Atusi. NUMAGUTI, Maki TSUJIMURA. 青藏高原那曲河流域降水及河流水体中氧稳定同位素研究 . 水科学进展, 2002, 13(2): 206-210.
[17]	顾慰祖, 林曾平, 费光灿, 郑平生. 环境同位素硫在大同南寒武-奥陶系地下水资源研究中的应用 . 水科学进展, 2000, 11(1): 14-20.
[18]	杨建锋. 地下水-土壤水-大气水界面水分转化研究综述 . 水科学进展, 1999, 10(2): 183-189.
[19]	顾慰祖, 刘涌, 贺祥, 邓吉友, 乔茂云. 阿拉善高原地下水的稳定同位素异常 . 水科学进展, 1998, 9(4): 333-337.
[20]	唐海行, 苏逸深, 刘炳敖. 土壤包气带中气体对入渗水流运动影响的实验研究 . 水科学进展, 1995, 6(4): 263-269.

点击查看大图

计量

文章访问数: 106
HTML全文浏览量: 57
PDF下载量: 568
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

基于氢氧同位素的华北平原降水入渗过程

作者简介:
王仕琴(1981- ),女,甘肃靖远人,博士研究生,主要从事水文水资源、流域水循环方向研究.E-mail:wangshiqin99@gmail.com

Appliance of oxygen and hydrogen isotope in the process of precipitation infiltration in the shallow groundwater areas of North China Plain

计量

基于氢氧同位素的华北平原降水入渗过程

1. 中国科学院地理科学与资源研究所, 中国科学院陆地水循环与地表过程重点实验室, 北京, 100101;

2. 天津地质矿产研究所, 天津, 300170

作者简介:
王仕琴(1981- ),女,甘肃靖远人,博士研究生,主要从事水文水资源、流域水循环方向研究.E-mail:wangshiqin99@gmail.com

English Abstract

Appliance of oxygen and hydrogen isotope in the process of precipitation infiltration in the shallow groundwater areas of North China Plain

1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;

2. Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China

全文HTML

目录

留言板

基于氢氧同位素的华北平原降水入渗过程

作者简介: 王仕琴(1981- ),女,甘肃靖远人,博士研究生,主要从事水文水资源、流域水循环方向研究.E-mail:wangshiqin99@gmail.com

Appliance of oxygen and hydrogen isotope in the process of precipitation infiltration in the shallow groundwater areas of North China Plain

计量

出版历程

基于氢氧同位素的华北平原降水入渗过程

1. 中国科学院地理科学与资源研究所, 中国科学院陆地水循环与地表过程重点实验室, 北京, 100101; 2. 天津地质矿产研究所, 天津, 300170

作者简介: 王仕琴(1981- ),女,甘肃靖远人,博士研究生,主要从事水文水资源、流域水循环方向研究.E-mail:wangshiqin99@gmail.com

English Abstract

Appliance of oxygen and hydrogen isotope in the process of precipitation infiltration in the shallow groundwater areas of North China Plain

1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2. Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China

全文HTML

目录

作者简介:
王仕琴(1981- ),女,甘肃靖远人,博士研究生,主要从事水文水资源、流域水循环方向研究.E-mail:wangshiqin99@gmail.com

1. 中国科学院地理科学与资源研究所, 中国科学院陆地水循环与地表过程重点实验室, 北京, 100101;

2. 天津地质矿产研究所, 天津, 300170

作者简介:
王仕琴(1981- ),女,甘肃靖远人,博士研究生,主要从事水文水资源、流域水循环方向研究.E-mail:wangshiqin99@gmail.com

1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;

2. Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China