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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第45卷

期数:

2023年第04期

页码:

844-856

栏目:

环境与可持续发展专刊

出版日期:

2023-07-15

文章信息/Info

Title:

Variation of Water and Sediment in the Tributaries of Ningxia Section of Yellow River, China from 1989 to 2019 and Their Driving Factors

文章编号:

1672-6561(2023)04-0844-13

作者:

王传贵¹; 梅雪梅²; 3; 4*; 张国军⁵; 任正龑⁵; 张晓明⁶; 李 鹏⁷; 赵 阳⁶

(1. 郑州大学 水利与交通学院,河南 郑州 450001; 2. 郑州大学 地热与生态地质研究中心,河南 郑州 450001; 3. 郑州大学 河南省减污降碳协同工程技术研究中心,河南 郑州 450001; 4. 郑州大学 生态与环境学院,河南 郑州 450001; 5. 宁夏回族自治区水土保持监测总站,宁夏 银川 750002; 6. 中国水利水电科学研究院,北京 100038; 7. 西安理工大学 西北旱区生态水利国家重点实验室,陕西 西安 710048)

Author(s):

WANG Chuan-gui¹;  MEI Xue-mei²; 3; 4*;  ZHANG Guo-jun⁵;  REN Zheng-yan⁵;  ZHANG Xiao-ming⁶;  LI Peng⁷;  ZHAO Yang⁶

(1. School of Water Conservancy and Transportation, Zhengzhou University, Zhengzhou 450001, Henan, China; 2. Geothermal and Ecological Geology Research Center, Zhengzhou University, Zhengzhou 450001, Henan, China; 3. Research Centre of Engineering and Technology for Synergetic Control of Environmental Pollution and Carbon Emissions of Henan Province, Zhengzhou University, Zhengzhou 450001, Henan, China; 4. School of Ecology and Environment, Zhengzhou University, Zhengzhou 450001, Henan, China; 5. Ningxia Soil and Water Conservation Monitoring Station, Yinchuan 750002, Ningxia, China; 6. China Institute of Water Resources and Hydropower Research, Beijing 100038, China; 7. State Key Laboratory of Eco-hydraulics in Northwest Arid Region of China, Xi'an University of Technology, Xi'an 710048, Shaanxi, China)

关键词:

水沙变化;  突变检验;  驱动因素;  相关性检验;  减沙效益;  人类活动;  水土保持;  宁夏;  黄河

Keywords:

variation of water and sediment;  mutation test;  driving factor;  correlation test;  sediment reduction benefit;  human activity;  soil and water conservation;  Ningxia;  Yellow River

分类号:

P333

DOI:

-

文献标志码:

A

摘要:

为明确黄河宁夏段典型支流水沙变化的主要驱动因素,基于清水河泉眼山站、红柳沟鸣沙洲站、苦水河郭家桥站实测水文资料,运用滑动平均法、Mann-Kendall突变检验和双累积曲线法分析典型流域的水沙变化趋势以及突变年份,运用累积斜率法、水文法和水保法对比分析水沙变化的驱动因素。结果表明:①1989～2019年,清水河、红柳沟和苦水河流域水沙变化均表现出减少趋势; 相比来说,输沙量变化较径流量变化更显著,苦水河流域的水沙变化较清水河和红柳沟流域更显著。②人类活动在水沙变化中占据主导地位且贡献率逐渐增大; 运用累积斜率法、水文法和水保法进行水沙变化归因分析,均表明人类活动是水沙变化的主要驱动因素,其中累积斜率法和水文法计算结果比较接近。③利用水保法对清水河流域进行水沙变化归因分析,发现人类活动中减水效益占据主导地位的是淤地坝和梯田,贡献率分别为42.9%、29.0%,减沙效益占据主导地位的是淤地坝,贡献率为94.5%。

Abstract:

In order to find the main driving factors of the variation of water and sediment in the typical tributaries of Ningxia section of Yellow River, based on the measured hydrological data at Quanyanshan station of Qingshui river, Mingshazhou station of Hongliugou river and Guojiaqiao station of Kushui river, the variation trend of water and sediment, and mutation year of the typical watershed were analyzed by the sliding average method, Mann-Kendall mutation test and double accumulation curve method; the driving factors of the variation of water and sediment were analyzed by cumulative slope method, hydrology method, and soil and water conservation method. The results show that ① from 1989 to 2019, the variation of water and sediment in Qingshui river, Hongliugou river and Kushui river basins all show a decreasing trend; the variation of sediment transport is more significant than that of runoff; compared with Qingshui river and Hongliugou river basins, the variation of water and sediment in Kushui river basin is more significant. ② Human activities play a leading role in the variation of water and sediment, and the contribution rate gradually increases; the cumulative slope method, hydrology method, and soil and water conservation method used in the attribution analysis of the variation of water and sediment show that human activity is the main driving factor of the variation of water and sediment, and the cumulative slope method and hydrology method have the same results. ③ According to the soil and water conservation method used in the attribution analysis of the variation of water and sediment in Qingshui river basin, it is found that the water reduction benefits of human activities are dominated by silt dam and terraced fields, with contribute rates of 42.9% and 29.0%, respectively; silt dam is dominant in sediment reduction, with contribute rate of 94.5%.

参考文献/References:

[1] JIA L,YU K X,LI Z B,et al.Temporal and Spatial Variation of Rainfall Erosivity in the Loess Plateau of China and Its Impact on Sediment Load[J].Catena,2022,210:105931.
[2] YIN S H,GAO G Y,RAN L S,et al.Extreme Streamflow and Sediment Load Changes in the Yellow River Basin:Impacts of Climate Change and Human Activities[J].Journal of Hydrology,2023,619:129372.
[3] 张青青,钟徳钰,贾宝真.黄河中游水沙变化归因分析[J].南水北调与水利科技,2022,20(5):976-987.
ZHANG Qing-qing,ZHONG De-yu,JIA Bao-zhen.Attribution Analysis of Runoff-sediment Variation in the Middle Yellow River[J].South-to-north Water Transfers and Water Science & Technology,2022,20(5):976-987.
[4] WANG Z J,XU M Z,LIU X,et al.Quantifying the Impact of Climate Change and Anthropogenic Activities on Runoff and Sediment Load Reduction in a Typical Loess Plateau Watershed[J].Journal of Hydrology:Regional Studies,2022,39:100992.
[5] 刘晓燕.黄土高原现状产沙情势评价[J].水利学报,2023,54(1):24-33.
LIU Xiao-yan.Evaluation on Present Status of Sediment Yield in the Loess Plateau[J].Journal of Hyd-raulic Engineering,2023,54(1):24-33.
[6] MA X Q,SHI C X,PENG J,et al.Quantitative Ascription of Sediment Discharge Changes of Two Highly Sediment-loaded Tributaries of the Yellow River in China:The Importance of Selecting Rainfall Index and Timescale[J].Water,2021,13(6):845.
[7] 孙 倩,于坤霞,李占斌,等.黄河中游多沙粗沙区水沙变化趋势及其主控因素的贡献率[J].地理学报,2018,73(5):945-956.
SUN Qian,YU Kun-xia,LI Zhan-bin,et al.The Trends of Streamflow and Sediment and Their Driving Factors in the Middle Reaches of the Yellow River[J].Acta Geographica Sinica,2018,73(5):945-956.
[8] 刘 强,蔡学娅,刘君怡,等.黄河中游窟野河流域水沙关系变化特征及其成因分析[J].水土保持研究,2022,29(4):68-74.
LIU Qiang,CAI Xue-ya,LIU Jun-yi,et al.Variation Characteristics and Causes of Runoff-sediment Relationship in Kuye River Basin in the Middle Reaches of the Yellow River[J].Research of Soil and Water Conservation,2022,29(4):68-74.
[9] 夏 露,马耘秀,宋孝玉,等.黄河中游昕水河流域水沙变化及归因研究[J].水土保持学报,2021,35(6):109-115.
XIA Lu,MA Yun-xiu,SONG Xiao-yu,et al.Study on the Variation and Attribution of Runoff and Sediment in Xinshui River Watershed of Middle Yellow River[J].Journal of Soil and Water Conservation,2021,35(6):109-115.
[10] WANG H X,LIU J H,GUO W X.The Variation and Attribution Analysis of the Runoff and Sediment in the Lower Reach of the Yellow River During the Past 60 Years[J].Water Supply,2021,21(6):3193-3209.
[11] 王冰洁,李二辉,王彦君,等.黄河中游日和年输沙率-流量关系空间变化及影响因素[J].清华大学学报(自然科学版),2020,60(5):440-448.
WANG Bing-jie,LI Er-hui,WANG Yan-jun,et al.Spatial Variations and the Factors Influencing Daily and Annual Sediment Rating Curves in the Middle Yellow River Basin[J].Journal of Tsinghua Univer-sity(Science and Technology),2020,60(5):440-448.
[12] XU J,JIANG X H,SUN H T,et al.Driving Forces of Nature and Human Activities on Water and Sediment Changes in the Middle Reaches of the Yellow River in the Past 100 Years[J].Journal of Soils and Sediments,2021,21(6):2450-2464.
[13] 李慧娟,师长兴,马小晴,等.黄河中游窟野河流域水沙变化影响因素定量评估[J].资源科学,2020,42(3):499-507.
LI Hui-juan,SHI Chang-xing,MA Xiao-qing,et al.Quantification of the Influencing Factors of Runoff and Sediment Discharge Changes of the Kuye River Catchment in the Middle Reaches of the Yellow River[J].Resources Science,2020,42(3):499-507.
[14] HU J F,LI P F,ZHAO G J,et al.Effects of Climate Variability and Anthropogenic Factors on Sediment Load Reduction in the Weihe River Basin,China[J].Hydrological Processes,2022,36(4):e14562.
[15] 邱德勋,穆兴民,赵广举,等.渭河流域极端降雨变化趋势及其对水沙情势的影响[J].水土保持研究,2022,29(6):65-72.
QIU De-xun,MU Xing-min,ZHAO Guang-ju,et al.Effects of Precipitation Extremes Change on Streamflow and Sediment Load in Weihe River Basin[J].Research of Soil and Water Conservation,2022,29(6):65-72.
[16] 冯绍杰,穆兴民,高 鹏,等.泾河水沙变化特征及其影响因素分析[J].干旱区资源与环境,2022,36(10):151-157.
FENG Shao-jie,MU Xing-min,GAO Peng,et al.Trends of Runoff and Sediment Loads in the Jinghe River Basin and Influencing Factors[J].Journal of Arid Land Resources and Environment,2022,36(10):151-157.
[17] 程亦菲,夏军强,周美蓉,等.一维水沙耦合模型参数敏感性分析:以2020年黄河下游洪水演进为例[J].水力发电学报,2022,41(12):100-110.
CHENG Yi-fei,XIA Jun-qiang,ZHOU Mei-rong,et al.Parameter Sensitivity Analysis of Dynamically Coupl-ed One-dimensional Morphodynamic Model:Case Stu-dy of Lower Yellow River[J].Journal of Hydroelect-ric Engineering,2022,41(12):100-110.
[18] 鲍振鑫,张建云,王国庆,等.基于水文模型与机器学习集合模拟的水沙变异归因定量识别:以黄河中游窟野河流域为例[J].水科学进展,2021,32(4):485-496.
BAO Zhen-xin,ZHANG Jian-yun,WANG Guo-qing,et al.Quantitative Assessment of the Attribution of Runoff and Sediment Changes Based on Hydrologic Model and Machine Learning:A Case Study of the Kuye River in the Middle Yellow River Basin[J].Advances in Water Science,2021,32(4):485-496.
[19] 吴 丹,夏润亮,李 涛,等.黄河水沙变化数据仓库构建关键技术研究[J].人民黄河,2022,44(10):159-162.
WU Dan,XIA Run-liang,LI Tao,et al.Study on Key Technologies of Data Warehouse Construction of Water and Sediment Change in the Yellow River[J].Yellow River,2022,44(10):159-162.
[20] MIAO J D,ZHANG X M,ZHAO Y,et al.Evolution Patterns and Spatial Sources of Water and Sediment Discharge over the Last 70 Years in the Yellow Ri-ver,China:A Case Study in the Ningxia Reach[J].Science of the Total Environment,2022,838:155952.
[21] 范俊健,赵广举,穆兴民,等.1956～2017年黄河上游水沙变化及其驱动因素[J].中国水土保持科学,2022,20(3):1-9.
FAN Jun-jian,ZHAO Guang-ju,MU Xing-min,et al.Variation of Runoff and Sediment Load and Their Driving Factors on the Upper Stream of the Yellow River from 1956 to 2017[J].Science of Soil and Water Conservation,2022,20(3):1-9.
[22] 许文龙,赵广举,穆兴民,等.近60年黄河上游干流水沙变化及其关系[J].中国水土保持科学,2018,16(6):38-47.
XU Wen-long,ZHAO Guang-ju,MU Xing-min,et al.Variations and Correlations of Runoffs and Sediment Loads in the Main Stream of the Upper Reaches of the Yellow River over the Past 60 Years[J].Science of Soil and Water Conservation,2018,16(6):38-47.
[23] 慕丹丹,褚金镝,高 博.基于小波变换的黄河宁夏段水沙变化趋势研究[J].人民黄河,2021,43(11):65-68,75.
MU Dan-dan,CHU Jin-di,GAO Bo.Evolution Law of the Runoff and Sediment Discharge in Ningxia Reach of the Yellow River Based on Wavelet Transform[J].Yellow River,2021,43(11):65-68,75.
[24] 余 欣,李其江,刘希胜,等.湟水流域水沙情势演变及驱动力分析[J].人民黄河,2022,44(9):64-70.
YU Xin,LI Qi-jiang,LIU Xi-sheng,et al.Analysis of Water and Sediment Situation Evolution and Driving Force in Huangshui River Basin[J].Yellow River,2022,44(9):64-70.
[25] YAO H F,SHI C X,SHAO W W,et al.Impacts of Climate Change and Human Activities on Runoff and Sediment Load of the Xiliugou Basin in the Upper Yellow River[J].Advances in Meteorology,2015,2015:481713.
[26] 夏 岩,张姝琪,高文冰,等.黄土高原变绿对黄河中游延河流域径流演变的影响估算[J].地球科学与环境学报,2020,42(6):849-860.
XIA Yan,ZHANG Shu-qi,GAO Wen-bing,et al.Influence of Greening Loess Plateau on Streamflow Change in Yellow River Basin of the Middle Yellow River,China[J].Journal of Earth Sciences and Environment,2020,42(6):849-860.
[27] ZHANG B Q,TIAN L,HE C S,et al.Response of Erosive Precipitation to Vegetation Restoration and Its Effect on Soil and Water Conservation over China's Loess Plateau[J].Water Resources Research,2023,59(1):e2022WR033382.
[28] 孙莉英,郑明国,蔡强国,等.张家界地区溇水流域洪水特征分析[J].陕西师范大学学报(自然科学版),2014,42(2):95-102.
SUN Li-ying,ZHENG Ming-guo,CAI Qiang-guo,et al.Analysis of Flood Characteristics in Loushui Basin of Zhangjiajie Region[J].Journal of Shaanxi Normal University(Natural Science Edition),2014,42(2):95-102.
[29] 韩建纯,李 鹏,杨 志,等.基于随机森林模型的茹河流域水沙变化及其影响因素研究[J].生态学报,2023,43(10):4190-4201.
HAN Jian-chun,LI Peng,YANG Zhi,et al.Variation and Influencing Factors of Runoff and Sediment in Ru River Basin Based on Random Forest Model[J].Acta Ecologica Sinica,2023,43(10):4190-4201.
[30] 王鸿翔,刘静航,赵颖异,等.黄河下游水沙变化与归因分析[J].人民黄河,2021,43(4):24-29,71.
WANG Hong-xiang,LIU Jing-hang,ZHAO Ying-yi,et al.Analysis of Water and Sediment Variation and Attribution in the Lower Yellow River[J].Yellow Ri-ver,2021,43(4):24-29,71.
[31] 汪 岗,范 昭.黄河水沙变化研究(第一卷)[M].郑州:黄河水利出版社,2002.
WANG Gang,FAN Zhao.Study on the Change of Water and Sediment of the Yellow River(Volume Ⅰ)[M].Zhengzhou:The Yellow River Water Conservancy Press,2002.
[32] 冉大川,张 栋,焦 鹏,等.西柳沟流域近期水沙变化归因分析[J].干旱区资源与环境,2016,30(5):143-149.
RAN Da-chuan,ZHANG Dong,JIAO Peng,et al.Analysis on the Attribution of Water and Sediment Changes in Xiliugou Basin[J].Journal of Arid Land Resources and Environment,2016,30(5):143-149.
[33] 赵 越.祖厉河流域水沙变化特征及水土保持减水减沙效益研究[D].兰州:甘肃农业大学,2016.
ZHAO Yue.Study on Variation Characteristics of Water and Sediment and Sediment Reduction Benefits of Water and Soil Conservation in Zuli River Basin[D].Lanzhou:Gansu Agricultural University,2016.
[34] 蒋凯鑫.黄河中游多沙粗沙区典型流域水沙变化归因对比分析[D].西安:西安理工大学,2020.
JIANG Kai-xin.Attributional Comparative Analysis of Runoff and Sediment Discharge Change in Typical Basins in Rich and Coarse Sediment Area in the Middle Reaches of the Yellow River[D].Xi'an:Xi'an University of Technology,2020.
[35] 岳志春,马晓阳,田福昌.黄河宁夏段近期水沙变化及河势演变分析[J].水利水电技术,2018,49(2):117-123.
YUE Zhi-chun,MA Xiao-yang,TIAN Fu-chang.Analysis on Recent Water-sediment Variation and River Regime Evolution of Ningxia Section of Yellow River[J].Water Resources and Hydropower Engineering,2018,49(2):117-123.
[36] 朱婉依,李昆鹏,李丽珂,等.黄河宁夏段水沙演变规律及冲淤空间分布特征研究[J].人民黄河,2022,44(8):28-33.
ZHU Wan-yi,LI Kun-peng,LI Li-ke,et al.Evolution Law of Water and Sediment and Spatial Distribution Characteristics of Erosion and Deposition in the Ning-xia Section of the Yellow River[J].Yellow River,2022,44(8):28-33.
[37] 马进国,郑艳爽,张晓华,等.宁夏清水河流域水沙变化特点分析[J].水利水运工程学报,2020(4):57-63.
MA Jin-guo,ZHENG Yan-shuang,ZHANG Xiao-hua,et al.Analysis on the Characteristics of Flow and Se-diment Variation in Qingshui River Basin of Ningxia[J].Hydro-science and Engineering,2020(4):57-63.
[38] 傅彦超,王友胜,杨 志,等.近30年苦水河水沙变化特征及成因分析[J].水土保持研究,2023,30(1):224-232.
FU Yan-chao,WANG You-sheng,YANG Zhi,et al.Analysis of Characteristics and Causes of Water and Sediment Changes in Recent 30 Years[J].Research of Soil and Water Conservation,2023,30(1):224-232.
[39] 蒋凯鑫,于坤霞,曹文洪,等.黄土高原典型流域水沙变化归因对比分析[J].农业工程学报,2020,36(4):143-149.
JIANG Kai-xin,YU Kun-xia,CAO Wen-hong,et al.Attributional Comparative Analysis of Runoff and Se-diment Change in Typical Basin of Loess Plateau[J].Transactions of the Chinese Society of Agricultural Engineering,2020,36(4):143-149.
[40] 胡春宏,张晓明.论黄河水沙变化趋势预测研究的若干问题[J].水利学报,2018,49(9):1028-1039.
HU Chun-hong,ZHANG Xiao-ming.Several Key Questions in the Researches of Runoff and Sediment Changes and Trend Predictions in the Yellow River[J].Journal of Hydraulic Engineering,2018,49(9):1028-1039.
[41] 肖培青,王玲玲,杨吉山,等.大暴雨作用下黄土高原典型流域水土保持措施减沙效益研究[J].水利学报,2020,51(9):1149-1156.
XIAO Pei-qing,WANG Ling-ling,YANG Ji-shan,et al.Study on Sediment Reduction Benefits of Soil and Water Conservation Measures in Typical Watersheds in the Loess Plateau Under the Heavy Rainfall[J].Journal of Hydraulic Engineering,2020,51(9):1149-1156.
[42] 郑佳芸,李军华,田世民,等.近70年黄河宁夏河段干支流水沙变化规律[J].泥沙研究,2023,48(3):38-44.
ZHENG Jia-yun,LI Jun-hua,TIAN Shi-min,et al.Variation of Water and Sediment in Main Stream and Tributaries of Ningxia Reach in the Yellow River in Recent 70 Years[J].Journal of Sediment Research,2023,48(3):38-44.

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备注/Memo

备注/Memo:

收稿日期:2022-09-08; 修回日期:2023-01-09投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(32201627); 宁夏回族自治区水利科技项目(SBZZ-J-2021-13,SBZZ-J-2021-12); 郑州大学院士团队科研启动基金项目(134-32340370,134-32340364); 中国水利水电科学研究院基本科研业务费专项资金项目(SE0145B022022)
作者简介:王传贵(1999-),男,河南驻马店人,工学硕士研究生,E-mail:wangchuangui@gs.zzu.edu.cn。
*通讯作者:梅雪梅(1992-),女,河南商丘人,直聘副教授,农学博士,E-mail:mxm0115@126.com。

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