Kaur Simranjeet, Gani Abdul, Pathak Shray, Tiwari Reet Kamal
Department of Geography, Punjab University, Chandigarh, India.
Department of Civil Engineering, Netaji Subhas University of Technology, New Delhi, 110073, India.
Environ Geochem Health. 2025 Sep 26;47(11):459. doi: 10.1007/s10653-025-02773-6.
The fluvial morphology of rivers is highly dynamic and vulnerable to both natural processes and human interventions. This study presents a comprehensive morphological assessment of the Sutlej River in the Jalandhar region of Punjab, India, with a particular focus on the impacts of sand mining. Geomorphic indicators, including river migration, channel width, bank erosion, and bar dynamics were determined by using multi-temporal satellite imagery for the year 2014 and 2024 with respect to the year 2001. Significant temporal and regional differences in channel morphology were found by the investigation, especially at sites where sand mining is heavily practiced. A detailed geomorphometric evaluation of the basin was conducted using SRTM-derived DEMs and standard hydrological tools, revealing a dendritic drainage pattern and moderate drainage texture (4.95), indicative of relatively stable fluvial conditions. Pronounced lateral shifts were observed in proximity to 35 identified sand mining locations, as evidenced through riverbank delineation and displacement analysis conducted at 5 km intervals. Comparative assessments of sediment load between post-monsoon 2023 and pre-monsoon 2024 further highlighted sediment redistribution associated with intensive mining hotspots. The results underscored the changed sediment transport patterns, accelerated channel dynamics due to sand mining and made areas more susceptible to flooding and ecosystem loss. The findings demonstrate a clear spatial association between intensified mining activity and increased bank erosion. The lateral shift of banks in varied from 8.6 to 972.49 m, whereas the total deposition and erosion area at both the banks was determined as 1561.85 ha and 2263.41 ha respectively. The total deposited area in the study area at left and right bank was 637.65 and 924.20 ha respectively, whereas the total eroded area at left and right bank was 1247.17 and 1016.24 ha. In addition to being a sign of geomorphic instability, these changes present significant threats to the riverine ecosystem, such as habitat loss, decreased sediment connection, and heightened vulnerability to flooding. The findings underscore the urgent need for sustainable sand mining practices, reinforced by continuous geomorphological monitoring using GIS and remote sensing, to mitigate environmental impacts and support effective management of riverine ecosystems.
河流的地貌形态具有高度动态性,易受自然过程和人类干预的影响。本研究对印度旁遮普邦贾朗达尔地区的萨特莱杰河进行了全面的形态学评估,特别关注采砂的影响。通过使用2014年和2024年相对于2001年的多时相卫星图像,确定了包括河流迁移、河道宽度、河岸侵蚀和沙洲动态在内的地貌指标。调查发现河道形态存在显著的时间和区域差异,特别是在采砂活动频繁的地点。利用航天飞机雷达地形测绘任务(SRTM)获取的数字高程模型(DEM)和标准水文工具对流域进行了详细的地貌测量评估,揭示了树枝状排水模式和中等排水纹理(4.95),表明河流条件相对稳定。在35个已确定的采砂地点附近观察到明显的横向位移,通过每隔5公里进行的河岸划定和位移分析得到了证实。对2023年季风后和2024年季风前的泥沙负荷进行的比较评估进一步突出了与密集采砂热点相关的泥沙重新分布。结果强调了采砂导致的泥沙输移模式变化、河道动态加速,使区域更容易发生洪水和生态系统损失。研究结果表明强化采砂活动与河岸侵蚀增加之间存在明显的空间关联。河岸的横向位移在8.6至972.49米之间,而两岸的总淤积和侵蚀面积分别确定为1561.85公顷和2263.41公顷。研究区域左岸和右岸的总淤积面积分别为637.65公顷和924.20公顷,而左岸和右岸的总侵蚀面积分别为1247.17公顷和1016.24公顷。除了是地貌不稳定的标志外,这些变化还对河流生态系统构成重大威胁,如栖息地丧失、泥沙连通性降低以及洪水脆弱性增加。研究结果强调迫切需要可持续的采砂做法,并通过使用地理信息系统(GIS)和遥感进行持续的地貌监测加以强化,以减轻环境影响并支持河流生态系统的有效管理。