Natural and anthropogenic controls on nutrient fluxes in two small rivers draining contrasting climate gradients across Southern Western Ghats, India.

IF 3 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES
Vipin T Raj, J A Gayathri, K Sreelash, D Padmalal, K Sajan, K Maya
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Abstract

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.

印度西南高止山脉两条河流中不同气候梯度的自然和人为控制对营养通量的影响。
印度南部的西高止山脉是生物多样性热点地区和主要水源,这里有多条河流受到不同气候、地质和土地利用环境的影响。本研究调查了两条小河(Bhavani和thuthapuzhai)中溶解无机氮(DIN)、溶解无机磷酸盐(DIP)和溶解二氧化硅(DSi)的时空动态,这两条小河从西高止山脉南部的不同气候带流出。在不同季节和地区共收集了150个水样,以评估营养通量及其控制因素。结果显示养分浓度存在显著的空间和季节差异。在Bhavani河,平均DIN值为112.12µg/l(季风前),1432.14µg/l(季风后)和240.98µg/l(季风后)。图萨普扎河的相应值分别为278.56µg/l、306.90µg/l和122.70µg/l。Bhavani的平均DIP浓度为8.38至16.59µg/l, Thuthapuzha的平均DIP浓度为2.69至11.01µg/l。Bhavani河的DSi水平较高,平均值在6.83至8.73毫克/升之间,而Thuthapuzha河的DSi水平为4.51至7.67毫克/升。受集约化农业和家庭污水投入的影响,特别是在半干旱区,巴瓦尼河下游的营养物质浓度增加。在Thuthapuzha,排水持续潮湿的集水区,在土地利用强度高的地区也观察到养分富集。季节性季风径流显著影响养分负荷,雨季DIN和DIP升高。耕地的高DSi水平与硅酸盐风化和土壤侵蚀有关。长期趋势表明,养分投入增加,特别是化肥的使用。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方面的作用,并强调了在西高止山脉快速变化的流域中进行综合流域管理的必要性。
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来源期刊
Environmental Monitoring and Assessment
Environmental Monitoring and Assessment 环境科学-环境科学
CiteScore
4.70
自引率
6.70%
发文量
1000
审稿时长
7.3 months
期刊介绍: Environmental Monitoring and Assessment emphasizes technical developments and data arising from environmental monitoring and assessment, the use of scientific principles in the design of monitoring systems at the local, regional and global scales, and the use of monitoring data in assessing the consequences of natural resource management actions and pollution risks to man and the environment.
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