干旱区研究

Arid Zone Research >

2023 , Vol. 40 >Issue 11: 1765 - 1775

DOI: https://doi.org/10.13866/j.azr.2023.11.06

Land and Water Resources

Characteristics of water and sand changes in the upper Guanchuan River and its response to precipitation and water conservation measures

  • Xiaoyu WANG ,
  • Rui MA ,
  • Fu ZHANG ,
  • Yanting HU ,
  • Lingli WANG ,
  • Chengyang JIANG ,
  • Su’e CHEN
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  • 1. College of Forestry, Gansu Agricultural University, Lanzhou 730070, Gansu, China
    2. College of Forestry Engineering, Gansu Forestry Vocational and Technical College, Tianshui 741000, Gansu, China
    3. Gansu Zhifu Ruida Ecological Environment Engineering Co. Ltd., Lanzhou 730070, Gansu, China

Received date: 2023-05-23

  Revised date: 2023-06-28

  Online published: 2023-12-01

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Abstract

In order to further explore the influence of precipitation and soil and water conservation measures on runoff sediment, and to gain an in-depth understanding of the driving factors of water and sand changes in small and medium-sized rivers of the Yellow River, M-K test, Morlet wavelet, linear regression and structural equation modeling were used to study the changes in precipitation and the area of soil and water conservation measures in the upper Guanchuan River from 1957-2021, as well as their the mechanism and process of action were studied. The results showed that annual precipitation showed a non-significant decreasing trend (P >0.05), runoff modulus and sand transport modulus showed a significant decreasing trend (P<0.05), and the area of soil and water conservation measures showed an increasing trend. The response of runoff modulus and sand transport modulus to precipitation got weakened, and the response to soil and water conservation measures was gradually strengthened; the key path of precipitation and soil and water conservation measures affecting the change of water and sand was “area of soil and water conservation measures→runoff modulus”, followed by “area of soil and water conservation measures→runoff→sand transport modulus”, then “precipitation→runoff modulus”, and finally “precipitation→runoff modulus→sand transport modulus”. The total effect of precipitation on water and sand change is 0.42 and 0.38 respectively, while the total effect of soil and water conservation measures on water and sand change is -0.72 and -0.65 respectively. The main factor affecting water and sand change in the watershed is the area of soil and water conservation measures, and the secondary factor is the amount of precipitation.

Key words： changes in water and sediment; soil and water conservation measures; structural equation model; upper Guanchuan River

Cite this article

Xiaoyu WANG , Rui MA , Fu ZHANG , Yanting HU , Lingli WANG , Chengyang JIANG , Su’e CHEN . Characteristics of water and sand changes in the upper Guanchuan River and its response to precipitation and water conservation measures[J]. Arid Zone Research, 2023 , 40(11) : 1765 -1775 . DOI: 10.13866/j.azr.2023.11.06

References

[1] 冯德锃, 吴栋栋, 赵玲玲, 等. 1952—2014 年饶河流域水沙变化特征及影响因素[J]. 南水北调与水利科技, 2018, 16(6): 53-59.
[1] [Feng Dezeng, Wu Dongdong, Zhao Lingling, et al. Analysis on characteristics and influence factors of runoff and sediment changes in the Raohe River basin from 1952 to 2014[J]. South to North Water Transfers and Water Science ＆ Technology, 2018, 16(6): 53-59.]
[2] 保光裕, 乜虹, 王平, 等. 黄河上游河源区不同量级降水对径流变化的影响[J]. 干旱区研究, 2021, 38(3): 704-713.
[2] [Bao Gangyu, Nie Hong, Wang Ping, et al. Research on effects of different precipitation magnitudes on runoff changes in the headwater region of the upper Yellow River[J]. Arid Zone Research, 2021, 38(3): 704-713.]
[3] 姚文艺, 高亚军, 张晓华. 黄河径流与输沙关系演变及其相关科学问题[J]. 中国水土保持科学, 2020, 18(4): 1-11.
[3] [Yao Wenyi, Gao Yajun, Zhang Xiaohua. Relationship evolution between runoff and sediment transport in the Yellow River and related scientific issues[J]. Science of Soil and Water Conservation, 2020, 18(4): 1-11.]
[4] 段雨佳, 何毅, 赵杰, 等. 人类活动对秦岭月河流域径流变化的影响分析[J]. 干旱区研究, 2023, 40(4): 605-614.
[4] [Duan Yujia, He Yi, Zhao Jie, et al. Analysis of impact of human activities on runoff changes in Yue River Basin of the Qinling Mountains[J]. Arid Zone Research, 2023, 40(4): 605-614.]
[5] 高凛. 《巴黎协定》框架下全球气候治理机制及前景展望[J]. 国际商务研究, 2022, 43(6): 54-62.
[5] [Gao Lin. Global climate governance mechanisms and prospects under the framework of the Paris Agreement[J]. International Business Research, 2022, 43(6): 54-62.]
[6] 姚春艳, 刘洪鹄, 刘竞, 等. 长江源区1980—2020年水沙变化规律[J]. 干旱区研究, 2023, 40(5): 726-736.
[6] [Yao Chunyan, Liu Honghu, Liu Jing, et al. Vatiation of runoff and sediment in the headwaters of the Yangtze River from 1980 to 2020[J]. Arid Zone Research, 2023, 40(5): 726-736.]
[7] 赵阳, 余新晓. 黄土丘陵沟壑区典型流域气候和土地利用变化对径流泥沙产量的影响[J]. 北京林业大学学报, 2013, 35(3): 39-45.
[7] [Zhao Yang, Yu Xinxiao. Effects of climate variation and land use change on runoff-sediment yield in typical watershed of loess hilly-gully region[J]. Journal of Beijing Forestry University, 2013, 35(3): 39-45.]
[8] 宁珍, 高光耀, 傅伯杰. 黄土高原流域水沙变化研究进展[J]. 生态学报, 2020, 40(1): 2-9.
[8] [Ning Zhen, Gao Guangyao, Fu Bojie. Changes in steamflow and sediment load in the catchments of the Loees Plateau, China: A review[J]. Acta Ecologica Sinica, 2020, 40(1): 2-9.]
[9] Zheng H Y, Miao C Y, Wu J W, et al. Temporal and spatial variations in water discharge and sediment load on the Loess Plateau, China: A high-density study[J]. Science of the Total Environment, 2019, 666: 875-886.
[10] Zhang F, Xing Z S, Zhao C Y, et al. Characterizing long-term soil and water erosion and their interactions withvarious conservation practices in the semi-arid Zulihebasin, Dingxi, Gansu, China[J]. Ecological Engineering, 2017, 106: 458-470.
[11] Rustomji P, Zhang X P, Hairsine P B, et al. River sediment load and concentration responses to changes in hydrology and catchment management in the Loess Plateau region of China[J]. Water Resources Research, 2008, 44(7): 1-17.
[12] Zhang J J, Zhang X P, Li R, et al. Did streamflow or suspended sediment concentration changes reduce sediment load in the middle reaches of the Yellow River[J]. Journal of Hydrology, 2017, 546: 357-369.
[13] 廖建华, 许炯心, 杨永红. 黄土高原区高含沙水流发生频率空间分异及其影响因素[J]. 水科学进展, 2008, 19(2): 160-170.
[13] [Liao Jianhua, Xu Jiongxin, Yang Yonghong. Study of the spatial differentiation of hyperconcentrated flows frequency in the Losee Plateau[J]. Advances in Water Science, 2008, 19(2): 160-170.]
[14] 赵娟. 基于 VAR 模型的典型流域水沙变化及其对降水与水土保持措施的动态响应[D]. 杨凌: 西北农林科技大学, 2019.
[14] [Zhao Juan. Impact of Soil and Water Conservation Measurements and Precipitation on River Runoff and Sediment Based on VAR Model in the Typical Area of Yellow River[D]. Yangling: Northwest A & F University, 2019.]
[15] 穆兴民, 李靖, 王飞, 等. 基于水土保持的流域降水-径流统计模型及其应用[J]. 水利学报, 2004, 49(5): 122-128.
[15] [Mu Xingmin, Li Jing, Wang Fei, et al. Rainfall-runoff statistical hydrological model based on soil and water conservation practices[J]. Journal of Hydraulic Engineering, 2004, 49(5): 122-128.]
[16] 穆兴民, 王万忠, 高鹏, 等. 黄河泥沙变化研究现状与问题[J]. 人民黄河, 2014, 36(12): 1-7.
[16] [Mu Xingmin, Wang Wanzhong, Gao Peng, et al. Progress and discussion on sediment load variation research of the Yellow River[J]. Yellow River, 2014, 36(12): 1-7.]
[17] 赵传普, 徐学选, 陈天林, 等. 关川河流域土地利用变化对径流的影响[J]. 水土保持研究, 2015, 22(3): 83-87.
[17] [Zhao Chuanpu, Xu Xuexuan, Chen Tianlin, et al. Impact of land use changes on the streamflow in Guanchuanhe Watershed[J]. Research on Soil and Water Conservation, 2015, 22(3): 83-87.]
[18] 张建云, 刘九夫, 金君良, 等. 青藏高原水资源演变与趋势分析[J]. 中国科学院院刊, 2019, 34(11): 1264-1273.
[18] [Zhang Jianyun, Liu Jiufu, Jin Junliang, et al. Evolution and trend of water resources in Qinghai-Tibet Plateau[J]. Chinese Academy of Sciences, 2019, 34(11): 1264-1273.]
[19] Gao Z L, Fu Y L, Li Y H, et al. Trends of streamflow, sediment load and their dynamic relation for the catchments in the middle reaches of the Yellow River over the past five decades[J]. Hydrology and Earth System Sciences, 2012, 16(9): 3219-3231.
[20] Zhang J J, Zhang X P, Li R, et al. Did streamflow or suspended sediment concentration changes reduce sediment load in the middle reaches of the Yellow River[J]. Journal of Hydrology, 2017, 546: 357-369.
[21] 张富, 姚进忠, 雷升文, 等. 甘肃省水土保持综合治理措施效益研究[M]. 郑州, 黄河水利出版社, 2014: 218-220.
[21] [Zhang Fu, Yao Jinzhong, Lei Shengwen, et al. Study on the Benefits of Comprehensive Management Measures for Soil and Water Conservation in Gansu Province[M]. Zhengzhou: Yellow River Water Conservancy Press, 2014: 218-220.]
[22] 甄英, 杨珊, 何静, 等. 基于M-K检验法与R/S法的宜宾市降水量分析[J]. 四川师范大学学报(自然科学版), 2017, 40(3): 392-397.
[22] [Zhen Ying, Yang Shan, He Jing, et al. Analysis of precipitation in Yibin city based on M-K test and R/S method[J]. Journal of Sichuan Normal University (Natural Science), 2017, 40(3): 392-397.]
[23] 谢智博, 穆兴民, 高鹏, 等. 基于R/S和Morlet小波分析的北洛河上游径流变化特征[J]. 水土保持研究, 2022, 29(2): 139-144.
[23] [Xie Zhibo, Mu Xingmin, Gao Peng, et al. Variation characteristics of runoff in the upper reaches of Beiluo River based on R/S and Morlet wavelet analysis[J]. Research of Soil and Water Conservation, 2022, 29(2): 139-144.]
[24] Klaus F, Axel M, Hannes S. Multiscale change point inference[J]. Journal of the Royal Statistical Society: Series B (Statistical Methodology), 2014, 3: 495-580.
[25] Fabian R, Sebastian S, Martin S, et al. Controls on runoff generation along a steep climatic gradient in the Eastern Mediterranean[J]. Journal of Hydrology: Regional Studies, 2017, 9: 18-33.
[26] 委霞. 基于结构方程模型的福寿林场三种典型林分健康评价[D]. 长沙: 中南林业科技大学, 2021.
[26] [Wei Xia. Health Evaluation of three Typical Forest Stands in Fushou Forest Farm Based on Structural Equation Model[D]. Changsha: Central South University of Forestry ＆Technology, 2021.]
[27] 萨如拉, 王子瑞, 滑永春, 等. 基于结构方程模型的大兴安岭北部天然林森林生态系统恢复能力评价研究[J/OL]. 南京林业大学学报(自然科学版), 2022, 1-11. [2022-12-01].
[27] [Sa Rula, Wang Zirui, Hua Yongchun, et al. Evaluating forest ecosystem restoration ability of natural forest in northern greater khingan Mountains by a structural equation model[J/OL]. Journal of Nanjing Forestry University (Natural Sciences Edition), 2022, 1-11. [2022-12-01].]
[28] 翟宏堃, 李强, 魏晓薇. 结构方程模型统计检验力分析: 原理与方法[J]. 心理科学进展, 2022, 30(9): 2117-2143.
[28] [Zhai Hongkun, Li Qiang, Wei Xiaowei. Power analysis in structural equation modeling: Principles and methods[J]. Advances in Psychological Science, 2022, 30(9): 2117-2143.]
[29] 刘强, 穆兴民, 赵广举, 等. 延河流域水沙变化及其对降水和土地利用变化的响应[J]. 干旱区资源与环境, 2021, 35(7): 129-135.
[29] [Liu Qiang, Mu Xingmin, Zhao Guangju, et al. Runoff and sediment changes and their responses to precipitation and land use change in the Yan River Basin[J]. Journal of Arid Land Resources and Environment, 2021, 35(7): 129-135.]
[30] 刘强, 李苗苗, 罗霞飞, 等. 黄河中游河龙区间水沙变化特征及其对降水和人类活动的响应[J]. 天水师范学院学报, 2021, 41(5): 22-28.
[30] [Liu Qiang, Li Miaomiao, Luo Xiafei, et al. Variation characteristics of runoff and sediment in the Helong region of the middle Yellow River and its response to climate change and human activities[J]. Journal of Tianshui Normal University, 2021, 41(5): 22-28.]
[31] 张富, 宁建国, 景亚安, 等. 关川河流域水土保持质量效益监测及成果分析[J]. 中国水土保持, 1992, 13(2): 21-25, 65-66.
[31] [Zhang Fu, Ning Jianguo, Jing Ya’an, et al. Quality-effects Monitoring of the soil conservation works and analysis of the monitoring data in Guan-chuan watershed[J]. Soil and Water Conservation in China, 1992, 13(2): 21-25, 65-66.]
[32] 盛菲, 刘士余, 余敏琪, 等. 不同时间尺度濂水流域水沙变化及其驱动因素分析[J]. 水土保持学报, 2023, 37(3): 201-207, 217.
[32] [Sheng Fei, Liu Shiyu, Yu Mingqi, et al. Analysis of runoff and sediment variation and its driving factors in Lianshui Watershed at different time scales[J]. Journal of Soil and Water Conservation, 2023, 37(3): 201-207, 217.]
[33] 王进. 气候变化对半干旱区流域径流影响的分析研究[J]. 中国水利, 2011, 62(3): 18-19.
[33] [Wang Jin. Analysis of the impact of climate change on runoff in semi-arid watersheds[J]. China Water Resources, 2011, 62(3): 18-19.]
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