Islam Aznarul, Hoque Md Mofizul, Ghosh Susmita, Sarkar Biplab, Mahammad Sadik, Das Balai Chandra, Islam Abu Reza Md Towfiqul, Pal Subodh Chandra, Sarkar Mohan, Khatun Modina, Chakraborty Debasish, Mallick Sahadat, Alam Edris
Department of Geography, Aliah University, 17 Gorachand Road, Kolkata, 700014, West Bengal, India.
Department of Geography, Krishnagar Government College, Nadia, Krishnanagar, 741101, West Bengal, India.
Sci Rep. 2024 Aug 29;14(1):20096. doi: 10.1038/s41598-024-70851-3.
Water pollution is a major concern for a decaying river. Polluted water reduces ecosystem services and human use of rivers. Therefore, the present study aims to assess the irrigation suitability of the Jalangi River water. A total of 34 pre-selected water samples were gathered from the source to the sink of the Jalangi River with an interval of 10 km and one secondary station's data from February 2012 to January 2022 were used for this purpose. The Piper diagram exhibits that the Jalangi River water is Na-HCO types, and the alkaline earth (Ca + Mg) outperforms alkalises (Na + K) and weak acids (HCO + CO) outperform strong acids (Cl + SO). SAR values ranging from 0.35 to 0.64 show that water is suitable for irrigation and poses no sodicity risks. The %Na results show that 91.18% of water samples are good and acceptable for irrigation. RSC levels indicate a significant alkalinity hazard, with 94.12% of samples considered inappropriate for irrigation. PI findings show that 91.18% of water samples are suitable for irrigation. Apart from the spatial water samples, seasonal water samples exhibit a wide variations as per the nature of irrigation hazards. Gibbs plot demonstrates that the weathering of rocks determined the hydro-chemical evolution of Jalangi River water. This study identifies very little evaporation dominance for pre- and post-monsoon water. The analysis of variance (ANOVA) test illustrates that there are no spatial variations in water quality while seasonal variations are widely noted (p < 0.05). The results also revealed that river water for irrigation during monsoon is suitable compared to the pre-monsoon season. Anthropogenic interventions including riverbed agriculture, and the discharge of untreated sewage from urban areas are playing a crucial role in deteriorating the water quality of the river, which needs substantial attention from the various stakeholders in a participatory, and sustainable manner.
水污染是一条逐渐衰败河流的主要问题。受污染的水会减少生态系统服务以及人类对河流的利用。因此,本研究旨在评估贾朗吉河水的灌溉适宜性。为此,从2012年2月至2022年1月,每隔10公里从贾朗吉河的源头到入海口共采集了34个预先选定的水样,并使用了一个二级站点的数据。派珀图显示,贾朗吉河水为钠-重碳酸盐类型,碱土(钙+镁)含量高于碱金属(钠+钾),弱酸(重碳酸根+碳酸根)含量高于强酸(氯离子+硫酸根)。钠吸附比(SAR)值在0.35至0.64之间,表明该水适合灌溉,不存在碱化风险。钠含量百分比结果显示,91.18%的水样灌溉适宜性良好且可接受。剩余碳酸钠(RSC)水平表明存在显著的碱化危害,94.12%的样本被认为不适宜灌溉。灌溉水质参数(PI)结果显示,91.18%的水样适合灌溉。除了空间水样外,季节性水样根据灌溉危害性质呈现出很大差异。吉布斯图表明,岩石风化决定了贾朗吉河水的水化学演化。本研究发现季风前后水的蒸发作用极小。方差分析(ANOVA)测试表明,水质不存在空间差异,但季节性差异显著(p<0.05)。结果还显示,与季风前季节相比,季风期间的河水更适合灌溉。包括河床农业和城市未经处理污水排放在内的人为干预,对河流的水质恶化起着关键作用,这需要各利益相关者以参与性和可持续的方式给予充分关注。