院报 ›› 2024, Vol. 41 ›› Issue (5): 18-25.DOI: 10.11988/ckyyb.20221678

• 河湖保护与治理 • 上一篇    下一篇

羊信江流域水沙变化特征及其影响因素

邢志云1, 刘惠英1,2, 李佳伟1   

  1. 1.南昌工程学院 水利工程学院,南昌 330099;
    2. 江西省鄱阳湖流域生态水利技术创新中心,南昌 330099
  • 收稿日期:2022-12-14 修回日期:2023-07-06 出版日期:2024-05-01 发布日期:2024-05-07
  • 通讯作者: 刘惠英(1973-),女,陕西凤翔人,副教授,博士,主要从事流域水沙变化和水体监测方面的研究。E-mail:huiyingliu@nit.edu.cn
  • 作者简介:邢志云(1998-),女,山东莒南人,硕士研究生,研究方向为水文学与水资源。E-mail:zhiyunxing1024@163.com
  • 基金资助:
    国家自然科学基金项目(41761058);2022年江西省大学生创新创业训练计划项目(S202211319001)

Variation Characteristics and Influencing Factors of Water and Sediment in Yangxin River Basin

XING Zhi-yun1, LIU Hui-ying1,2, LI Jia-wei1   

  1. 1. School of Hydraulic Engineering,Nanchang Institute of Technology,Nanchang 330099,China;
    2. Jiangxi Provincial Technology Innovation Center for Ecological Water Engineering in Poyang Lake Basin, Nanchang 330099, China
  • Received:2022-12-14 Revised:2023-07-06 Online:2024-05-01 Published:2024-05-07

摘要: 为深入研究水沙变化对流域生态修复和经济可持续发展的影响,利用Mann-Kendall非参数趋势检验法、Pettitt突变检验法、Spearman秩相关系数法、累积量斜率变化率比较法对赣江上游羊信江流域1964—2020年的降雨量、径流量和输沙量的变化特征及其贡献率进行分析,确定影响流域输沙量变化的主要因素。结果表明:①羊信江流域在1964—2020年年降雨量和年径流量无显著变化,年输沙量呈显著增加趋势;②降雨量、径流量及输沙量年内分配不均,均多集中在汛期(3—6月份);③年降雨量、年径流量均未发生显著突变,年输沙量在1995年发生显著突变(P<0.01);④降雨和人类活动对输沙量增加的贡献率分别为-0.35%、100.35%。以稀土矿开采、脐橙种植、跨河公路修建为主的人类活动是导致羊信江流域水土流失的重要原因。研究成果对流域种植结构调整及矿产资源绿色开放具有重要的指导意义。

关键词: 水沙变化, 气候变化, 人类活动, 贡献率, 羊信江流域

Abstract: To delve into the impact of water and sediment variations on basin ecological restoration and sustainable economic development, we scrutinized the variations of precipitation, runoff, and sediment transport within the Yangxin River Basin in the upper reaches of Ganjiang River from 1964 to 2020 by using a variety of methods. Such methods include the Mann-Kendall nonparametric trend test, Pettitt test, Spearman rank correlation coefficient method, and cumulated slope change rate comparative method. We aimed to pinpoint the primary factors influencing sediment transport alterations. Our findings indicate the following: (1) Annual rainfall and runoff in the Yangxin River Basin remained relatively stable from 1964 to 2020, contrasting with a notable upward trend in annual sediment transport. (2) Precipitation, runoff, and sediment transport exhibit seasonal disparities, predominantly occurring in flood season (March-June). (3) While annual rainfall and runoff remained steady, a significant shift in annual sediment transport occurred in 1995 (P<0.01). (4) Rainfall and human activities contributed -0.35% and 100.35%, respectively, to the rise in sediment transport. Human activities such as rare earth mining, navel orange cultivation, and cross-river highway construction emerged as key drivers of water loss and soil erosion in the Yangxin River Basin. This research holds paramount importance for guiding the adjustments in planting strategies and promoting environmentally friendly mineral resource utilization within river basins.

Key words: water and sediment variation, climate change, human activities, contribution rate, Yangxin River basin

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