祁连山古浪河流域径流组分特征

doi:10.7522/j.issn.1000-0240.2018.1145

冰川冻土 ›› 2019, Vol. 41 ›› Issue (4): 918-925.doi: 10.7522/j.issn.1000-0240.2018.1145

祁连山古浪河流域径流组分特征

桂娟^1,2, 李宗省¹, 冯起¹, 张德栋³, 吕越敏^1,2, 袁瑞丰¹

1. 中国科学院西北生态环境资源研究院内陆河流域生态水文重点实验室/甘肃省祁连山生态研究中心, 甘肃兰州 730000;
2. 中国科学院大学, 北京 100049;
3. 甘肃省水文水资源局, 甘肃兰州 730000

收稿日期:2018-09-12 修回日期:2018-12-11 出版日期:2019-08-25 发布日期:2019-11-28
通讯作者: 李宗省,E-mail:lizxhhs@163.com. E-mail:lizxhhs@163.com
作者简介:桂娟(1994-),女,甘肃金塔人,2018年在西北师范大学获学士学位,现为中国科学院西北生态环境资源研究院在读硕士研究生,从事高寒山区同位素水文过程研究.E-mail:guijuan6894@163.com
基金资助:
中国科学院青年创新促进会优秀会员人才计划项目（2013274）；国家重点研发计划项目（2017YFC0404305）；城市与区域生态国家重点实验室开放基金项目（SKLURE2018-2-6）；国家自然科学基金项目（91547102）资助

Characteristics of runoff components in the Gulang River basin of the Qilian Mountains

GUI Juan^1,2, LI Zongxing¹, FENG Qi¹, ZHANG Dedong³, Lü Yuemin^1,2, YUAN Ruifeng¹

1. Key Laboratory of Ecohydrology of Inland River Basin, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences/Gansu Qilian Mountains Ecological Research Center, Lanzhou 730000, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China;
3. Gansu Hydrology and Water Resources Bureau, Lanzhou 730000, China

Received:2018-09-12 Revised:2018-12-11 Online:2019-08-25 Published:2019-11-28

摘要/Abstract

摘要： 为了探究气候变暖、冰冻圈急剧萎缩背景下祁连山内陆河的水文状况，依据古浪河流域所采集的各类水体样品和相关观测数据，分析了各水体稳定同位素特征及其所指示的环境意义，并进行了径流分割。结果表明：（1）与降水相比，河水稳定同位素年际变化较小，从季节变化角度来看，河水δ¹⁸O值夏季 > 秋季 > 春季 > 冬季，反映了不同季节蒸发强度的差异。（2）泉水稳定同位素特征与河水相似，年际变化较为稳定，表明山区河水与泉水之间可能存在转换过程。（3）由于土壤水分交换、地表土壤蒸发、植被蒸腾以及土壤水和地下水之间的同位素差异，引起土壤水同位素组成的梯度差异比较明显，土壤水δ¹⁸O由地表向下经历了富集―贫化―富集的过程，d-excess变化则与之相反。（4）径流分割结果显示大气降水对古浪河流域出山径流的补给率高达76%±2.4%，冻土层上水补给为24%±2.4%。

关键词: 稳定同位素, 径流分割, 水文过程, 冻土层上水, 土壤水

Abstract: In order to explore the hydrology of inland rivers in the Qilian Mountains under the background of global warming and cryosphere shrinking,based on the samples of various waters collected in the Gulang River basin and relevant observation data,the stable isotope characteristics of each water and the environmental significance indicated by them were analyzed,and runoff segmentation was conducted. The main conclusions are as follows:(1)Compared with that in precipitation,the annual variation of stable isotope in river is relatively small. The value of δ¹⁸O in river is in summer > in autumn > in spring > in winter,reflecting the difference of intensity in various seasons. (2)The stable isotope characteristics of spring water are similar to those in river which the annual variation is relatively stable,showing that there are many conversion processes between river water and spring water in mountainous areas. (3)Due to the isotope differences among soil water recharge,surface soil evaporation and vegetation transpiration,as well as between soil water and ground water,the gradient differences of soil water isotope composition are relatively obvious. (4)The result of the segmentation of runoff of the mean runoff shows that the recharge ratio of precipitation in the Gulang River basin is up to 76%±2.4%, and that of supra-permafrost water is 24%±2.4%.

Key words: stable isotope, runoff segmentation, hydrological process, supra-permafrost water, soil water

中图分类号:

P339

桂娟, 李宗省, 冯起, 张德栋, 吕越敏, 袁瑞丰. 祁连山古浪河流域径流组分特征[J]. 冰川冻土, 2019, 41(4): 918-925.

GUI Juan, LI Zongxing, FENG Qi, ZHANG Dedong, Lü Yuemin, YUAN Ruifeng. Characteristics of runoff components in the Gulang River basin of the Qilian Mountains[J]. Journal of Glaciology and Geocryology, 2019, 41(4): 918-925.

参考文献

[1] Chen Rensheng,Song Yaoxuan,Kang Ersi,et al. A cryosphere hydrology observation system in a small alpine watershed of Qilian Mountains in China and its meteorology gradient[J]. Arctic,Antarctic and Alpine Research,2014,46 (2):213-231.
[2] Zhang Wenguang,Cheng Bin,Hu Zhibin,et al. Using stable isotopes to determine the water sources in alpine ecosystems on the east Qinghai Tibet Plateau,China[J]. Hydrological Process,2010,24:3270-3280.
[3] Cai M Y,Wang L,Parkes S D,et al. Stable water isotope and surface heat flux simulation using ISOLSM:evaluation against in situ measurements[J]. Journal of Hydrology,2015,523:67-78.
[4] Huai Baojuan,Li Zhongqin,Wang Shengjie,et al. RS analysis of glaciers change in the Heihe River basin,Northwest China,during the recent decades[J]. Journal of Geographical Sciences,2014,24 (6):993-1008.
[5] He Jianqiao,Song Gaoju,Jiang Xi,et al. Relation between glacial meltwater runoff and mountainous runoff in 2006 in four typical river basins of Heihe River water system[J]. Journal of Desert Research,2008,28 (6):1186-1189.[贺建桥,宋高举,蒋熹,等. 2006年黑河水系典型流域冰川融水径流与出山径流的关系[J]. 中国沙漠,2008,28 (6):1186-1189.]
[6] Wu Jinkui,Ding Yongjian,Ye Baisheng. Spatio-temporal variation of stable isotopes in precipitation in the Heihe River basin,Northwestern China[J]. Environmental Earth Sciences, 2010,61:1123-1134.
[7] Li Zongxing,Feng Qi,Liu Wei,et al. Study on the contribution from cryosphere to runoff in the cold alpine basin:a case study of Hulugou River basin in the Qilian Mountains[J]. Global and Planetary Change,2014,122:345-361.
[8] Yang Kun,Ye Baisheng,Zhou Ding,et al. Response of hydrological cycle to recent climate changes in the Tibetan Plateau[J]. Climate Change,2011,109 (3/4):517-534.
[9] Yang Yonggang,Xiao Honglang,Wei Yongping,et al. Hydrologic processes in the different landscape zones of Mafengou River basin in the alpine cold region during the melting period[J]. Journal of Hydrology,2011,409:149-156.
[10] Nie Zhenlong,Chen Zongyu,Shen Jianmei,et al. Environmental isotopes as tracers of hydrological cycle in the recharge area of the Heihe River[J]. Geography and Geo Information Science,2005,21 (1):104-107.[聂振龙,陈宗宇,申建梅,等. 应用环境同位素方法研究黑河源区水文循环特征[J]. 地理与地理信息科学,2005,21 (1):104-107.]
[11] Wang Puyu,Li Zhongqin,Gao Wenyu,et al. Glacier changes in the Heihe River basin over the past 50 years in the context of climate change[J]. Resources Science,2011,33 (3):399-407.[王璞玉,李忠勤,高闻宇,等. 气候变化背景下近50年来黑河流域冰川资源变化特征分析[J]. 资源科学,2011, 33 (3):399-407.]
[12] Li Zongxing,Feng Qi,Wang Yongsong,et al. Quantitative evaluation on the influence from cryosphere meltwater on runoff in an inland river basin of China[J]. Global and Planetary Change,2016,143:189-195.
[13] Kong Yanlong,Pang Zhonghe. Evaluating the sensitivity of glacier rivers to climate change based on hydrograph separation of discharge[J]. Journal of Hydrology,2012,434/435:121-129.
[14] Sun Congjian,Chen Yaning,Li Weihong,et al. Isotopic timeseries partitioning of streamflow components under regional climate change in the Urumqi River,Northwest China[J/OL]. Hydrological Sciences Journal,2016,61 (8)[20181128]. https://www.tandfonline.com/doi/abs/10.1080/02626667.2015.1031757.
[15] Wang Xiaoyan,Li Zhongqin,Ross E,et al. Characteristics of water isotopes and hydrograph separation during the spring flood period in Yushugou River basin,eastern Tianshan,China[J]. Earth System Science,2015,124 (1):115-124.
[16] Sun Congjian,Chen Wei. Streamflow components in inland rivers in the Tianshan Mountains,Northwest China[J]. Arid Land Geography,2017,40 (1):37-44.[孙从建,陈伟. 天山山区典型内陆河流域径流组分特征分析[J]. 干旱区地理, 2017,40 (1):37-44.]
[17] Fan Yuting,Chen Yaning,Li Xingong,et al. Characteristics of water isotopes and ice-snowmelt quantification in the Tizinafu River,north Kunlun Mountains,Central Asia[J]. Quaternary International,2015,380:116-122.
[18] Li Zongxing,Gao Yan,Wang Yamin,et al. Can monsoon moisture arrive Qilian Mountains in summer?[J]. Quaternary International,2015,358:113-125.
[19] Zhou Jiaxin,Wu Jinkui,Liu Shiwei,et al. Hydrograph separation in the headwaters of the Shule River basin:combining water chemistry and stable isotopes[J/OL]. Advances in Meteorology,2015 (2)[2018-12-07]. http://dx.doi.org/10.1155/2015/830306.
[20] Gao Xin,Zhang Shiqiang,Ye Baisheng,et al. Recent changes of glacier runoff in the Hexi inland river basin[J]. Advances in Water Science,2011,22 (3):344-350.[高鑫,张世强,叶柏生,等. 河西内陆河流域冰川融水近期变化[J]. 水科学进展,2011,22 (3):344-350.]
[21] Yin Guan,Wang Xiaodan,Gao Zhiyou,et al. Study of the hydrology of glacial runoff in Hailuogou valley,Gongga Mountain by means of isotopic tracing[J]. Journal of Glaciology and Geocryology,2008,30 (3):365-372.[尹观,王小丹,高志友,等. 贡嘎山海螺沟冰川径流水文规律的同位素示踪研究[J]. 冰川冻土,2008,30 (3):365-372.]
[22] Wang Qingfeng,Zhang Tingjun,Wu Jichun,et al. Investigation on permafrost distribution over the upper reaches of the Heihe River in the Qilian Mountains[J]. Journal of Glaciology and Geocryology,2013,35 (1):19-29.[王庆峰,张廷军,吴吉春,等. 祁连山区黑河上游多年冻土分布考察[J]. 冰川冻土,2013,35 (1):19-29.]
[23] Song Mengyuan,Li Zhongqin,Jin Shuang,et al. Characteristics of water isotopes and hydrograph separation in the Glacier No. 72 of Qingbingtan,Tomur Peak[J]. Journal of Arid Land Resources and Environment,2015,29 (3):156-160.[宋梦媛,李忠勤,金爽,等. 托木尔峰青冰滩72号冰川流域同位素特征及径流分割研究[J]. 干旱区资源与环境,2015,29 (3):156-160.]
[24] Niu Li,Ye Baisheng,Li Jing,et al. Effects of permafrost degradation on hydrological processes in typical basins in Northwest China[J]. Science in China:Earth Sciences,2011,41 (1):85-92.[牛丽,叶柏生,李静,等. 中国西北地区典型流域冻土退化对水文过程的影响[J]. 中国科学:地球科学, 2011,41 (1):85-92.]
[25] Yao Tandong,Yao Zhijun. Impacts of glacial retreat on runoff on Tibetan Plateau[J]. Chinese Journal of Nature,2010,32 (1):4-8.[姚檀栋,姚治君. 青藏高原冰川退缩对河水径流的影响[J]. 自然杂志,2010,32 (1):4-8.]
[26] Sheng Lu,Liu Mingchun,Hu Zhenghua,et al. Characteristics of climate change and its influence on growth period of crops in Shiyang River basin[J]. Agricultural Research in the Arid Areas,2013,31 (5):19-27.[盛露,刘明春,胡正华,等. 石羊河流域气候变化及对作物生育期的影响[J]. 干旱地区农业研究,2013,31 (5):19-27.]
[27] Zhang Lanying,Pang Bo,Xu Zongxue,et al. Impacts of climate change and LUCC on Gulang River basin[J]. South-toNorth Water Transfers and Water Science and Technology, 2014,12 (1):42-46.[张兰影,庞博,徐宗学,等. 古浪河流域气候变化与土地利用变化的水文效应[J]. 南水北调与水利科技,2014,12 (1):42-46.]
[28] Wang Tingting,Feng Qi,Li Zongxing,et al. Extreme climate research on Gulang River basin in eastern Qilian Mountains during 1960-2012[J]. Journal of Glaciology and Geocryology, 2018,40 (3):598-606.[王婷婷,冯起,李宗省,等. 1960-2012年祁连山东段古浪河流域极端气候事件研究[J]. 冰川冻土,2018,40 (3):598-606.]
[29] Shi Yafeng,Shen Yongping,Li Dongliang,et al. Discussion on the present climate change from warm dry to warn wet in Northwest China[J]. Quaternary Sciences,2003,23 (2):152-163.[施雅风,沈永平,李栋梁,等. 中国西北气候由暖干向暖湿转型的特征和趋势探讨[J]. 第四纪研究,2003,23 (2):152-163.]
[30] Wang Genxu,Liu Guoshuai,Li Chanji. The variability of soil thermal and hydrological dynamics with vegetation cover in a permafrost region[J]. Agricultural and Forest Meteorology, 2012,162:44-57.
[31] Li Binquan,Yu Zhongbo,Liang Zhongmin,et al. Hydrologic response of a high altitude glacierized basin in the central Tibetan Plateau[J]. Global and Planetary Change,2014,118:69-84.
[32] Hooper R P. Diagnostic tools for mixing models of stream water chemistry[J/OL]. Water Resource,2003,39 (3)[2018-1207]. https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2002WR001528.
[33] Liu Yanjun,Lu Wenjing,Wang Hongtao,et al. Improved impact assessment of odorous compounds from landfills using Monte Carlo simulation[J]. Science of the Total Environment, 2019,648:805-810.
[34] Cook P G,Grady A P O. Determining soil and groundwater use of vegetation from heat pulse,water potential and stable isotope data[J]. Oecologia,2006,148:97-107.
[35] Allison G B,Barnes C J,Hughes M W. The distribution of deuterium and δ¹⁸O in dry soils:2. experimental[J]. Journal of Hydrology,1983,64:377-397.
[36] Luo Lun,Yu Wusheng,Wan Shimin,et al. Advances in the study of stable isotope composition of leaf water in plants[J]. Acta Ecologica Sinica,2013,33 (4):1031-1041.[罗伦,余武生,万诗敏,等. 植物叶片水稳定同位素研究进展[J]. 生态学报,2013,33 (4):1031-1041.]
[37] Hagg W,Braun L N,Kuhn M. Modelling of hydrological response to climate change in glacierized Central Asian catchments[J]. Journal of Hydrology,2007,332:40-53.

祁连山古浪河流域径流组分特征

Characteristics of runoff components in the Gulang River basin of the Qilian Mountains

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

推荐阅读 0

[1]	何天豪, 高红凯, 李向应, 韩添丁, 贺志华, 张志才, 段峥, 刘敏, 丁永建. 水稳定同位素示踪的冰川流域水文模拟及不确定性研究[J]. 冰川冻土, 2021, 43(4): 1130-1143.
[2]	刘宏超, 马俊杰, 李韧. 基于KNN机器学习方法对青藏高原唐古拉地区表层土壤水热状况的模拟[J]. 冰川冻土, 2021, 43(4): 1243-1252.
[3]	赵海鹏, 吕明侠, 王一博, 杨文静, 刘鑫, 白炜. 青藏高原风火山流域坡面尺度活动层土壤水热时空变化特征[J]. 冰川冻土, 2020, 42(4): 1158-1168.
[4]	赵求东, 赵传成, 秦艳, 苌亚平, 王建. 天山南坡高冰川覆盖率的木扎提河流域水文过程对气候变化的响应[J]. 冰川冻土, 2020, 42(4): 1285-1298.
[5]	刘乐, 孙宏义, 蔡忠兰, 张建新, 李东泽. 兰州新区黄土工程开挖边坡植被重建初期土壤水分初步研究[J]. 冰川冻土, 2020, 42(3): 1007-1016.
[6]	石玉东, 王圣杰, 张明军, 李昱锋, 宋洋. OIPC和RCWIP降水氢氧稳定同位素数据在新疆天山地区的适用性[J]. 冰川冻土, 2020, 42(3): 974-985.
[7]	赵强, 吴从林, 罗平安, 王康, 李红珍, 黄介生. 冻融期东北农田土壤温度和水分变化规律及影响因素分析[J]. 冰川冻土, 2020, 42(3): 986-995.
[8]	戴黎聪, 柯浔, 张法伟, 杜岩功, 李以康, 郭小伟, 李茜, 林丽, 曹广民. 青藏高原季节冻土区土壤冻融过程水热耦合特征[J]. 冰川冻土, 2020, 42(2): 390-398.
[9]	刘峰, 李忠勤, 郝嘉楠, 梁鹏斌, 王芳龙, 张慧. 额尔齐斯河源春季水化学及稳定同位素特征研究[J]. 冰川冻土, 2020, 42(1): 234-242.
[10]	王愿斌, 王佳铭, 樊媛媛, 陈娟, Miles Dyck, 金会军, 何海龙. 土壤水分特征曲线模型模拟性能评价[J]. 冰川冻土, 2019, 41(6): 1448-1455.
[11]	李宗省, 冯起, 李宗杰, 吕越敏, 袁瑞丰, 桂娟, 李永格, 张百娟, 薛健. 祁连山北坡稳定同位素生态水文学研究的初步进展与成果应用[J]. 冰川冻土, 2019, 41(5): 1044-1052.
[12]	李洪源, 赵求东, 吴锦奎, 丁永建, 秦甲, 韦虹, 曾帝. 疏勒河上游径流组分及其变化特征定量模拟[J]. 冰川冻土, 2019, 41(4): 907-917.
[13]	周苏娥, 张明军, 王圣杰, 孟鸿飞, 张亚宁, 余秀秀. 基于Stewart模型改进方案的新疆降水同位素的云下蒸发效应比较[J]. 冰川冻土, 2019, 41(2): 304-315.
[14]	章新平, 关华德, 张新主, 张婉君, 姚天次. 下垫面蒸发和云中凝结分馏对降水稳定同位素影响的数值试验——空间分布的比较[J]. 冰川冻土, 2017, 39(3): 455-468.
[15]	章新平, 关华德, 张新主, 张婉君, 姚天次. 下垫面蒸发和云中凝结分馏对降水稳定同位素影响的数值试验——时间变化的比较(以长沙降水同位素为例)[J]. 冰川冻土, 2017, 39(3): 469-478.