Raj Vipin T, Gayathri J A, Sreelash K, Padmalal D, Sajan K, Maya K
National Centre for Earth Science Studies, Thiruvananthapuram, 695011, India.
Department of Marine Sciences, Cochin University of Science and Technology, Kochi, 682016, India.
Environ Monit Assess. 2025 Jul 9;197(8):884. doi: 10.1007/s10661-025-14344-4.
The Western Ghats of southern India, a biodiversity hotspot and major water source, host several rivers influenced by diverse climatic, geological, and land-use settings. This study investigates the spatiotemporal dynamics of Dissolved Inorganic Nitrogen (DIN), Dissolved Inorganic Phosphate (DIP), and Dissolved Silica (DSi) in two small rivers-the Bhavani and the Thuthapuzha-which drain contrasting climatic zones of the southern Western Ghats. A total of 150 water samples were collected across seasons and zones to assess nutrient fluxes and their controlling factors. Results revealed substantial spatial and seasonal differences in nutrient concentrations. In the Bhavani river, mean DIN values were 112.12 µg/l (pre-monsoon), 1432.14 µg/l (monsoon), and 240.98 µg/l (post-monsoon). The corresponding values in the Thuthapuzha river were 278.56 µg/l, 306.90 µg/l, and 122.70 µg/l, respectively. Mean DIP concentrations ranged from 8.38 to 16.59 µg/l in the Bhavani and from 2.69 to 11.01 µg/l in the Thuthapuzha. DSi levels were higher in the Bhavani river, with mean values between 6.83 and 8.73 mg/l, compared to 4.51 to 7.67 mg/l in the Thuthapuzha river. Nutrient concentrations in the Bhavani increased downstream, influenced by intensive agriculture and domestic wastewater inputs, particularly in the semi-arid zones. In the Thuthapuzha, which drains a persistently humid catchment, nutrient enrichment was also observed in areas of high land-use intensity. Seasonal monsoonal runoff significantly impacted nutrient loads, with elevated DIN and DIP during the wet season. Higher DSi levels in cultivated zones were linked to silicate weathering and soil erosion. Long-term trends suggest an increase in nutrient inputs, particularly from fertilizer use. These findings highlight the role of climate, land use and anthropogenic pressure in regulating nutrient fluxes in tropical river systems and underscore the need for integrated watershed management in rapidly transforming catchments of the Western Ghats.
印度南部的西高止山脉是一个生物多样性热点地区和主要水源地,有几条受不同气候、地质和土地利用环境影响的河流。本研究调查了两条小河流——巴瓦尼河和图塔普扎河——中溶解无机氮(DIN)、溶解无机磷(DIP)和溶解硅(DSi)的时空动态,这两条河流经西高止山脉南部不同的气候区。在不同季节和区域共采集了150个水样,以评估养分通量及其控制因素。结果显示养分浓度存在显著的空间和季节差异。在巴瓦尼河中,DIN的平均值分别为112.12微克/升(季风前)、1432.14微克/升(季风期)和240.98微克/升(季风后)。图塔普扎河的相应值分别为278.56微克/升、306.90微克/升和122.70微克/升。巴瓦尼河的平均DIP浓度在8.38至16.59微克/升之间,图塔普扎河在2.69至11.01微克/升之间。巴瓦尼河的DSi水平较高,平均值在6.83至8.73毫克/升之间,而图塔普扎河为4.51至7.67毫克/升。受集约化农业和生活污水排放影响,尤其是在半干旱地区,巴瓦尼河下游的养分浓度增加。在流经持续湿润集水区的图塔普扎河,在土地利用强度高的地区也观察到了养分富集。季节性季风径流对养分负荷有显著影响,雨季DIN和DIP升高。耕地较高的DSi水平与硅酸盐风化和土壤侵蚀有关。长期趋势表明养分输入增加,尤其是来自化肥使用的养分。这些发现突出了气候、土地利用和人为压力在调节热带河流系统养分通量中的作用,并强调了在西高止山脉快速变化的集水区进行综合流域管理的必要性。