CSIR-National Institute of Oceanography, Regional Centre, Visakhapatnam, 530017, India.
Dept of PNCO, School of Chemistry, Andhra University, Visakhapatnam, 530017, India.
Environ Sci Pollut Res Int. 2023 Dec;30(60):125559-125569. doi: 10.1007/s11356-023-30936-4. Epub 2023 Nov 24.
This study analyses particulate organic carbon (POC) and particulate nitrogen (PN) export from Indian monsoonal rivers to the north Indian Ocean. Indian monsoonal rivers export approximately 1.2 Tg yr (1Tg = 10 g) of POC and 0.14 Tg yr of PN, with about two-thirds entering the Bay of Bengal (0.8 and 0.1 Tg yr, respectively) and the remaining reaches to the Arabian Sea (0.4 and 0.04 Tg yr, respectively). Remarkably, just four rivers from northwest India's black soil-dominated regions contribute about half of the total POC and PN exports (0.64 and 0.06 Tg yr, respectively). This is due to substantial erosion in these catchments, resulting in suspended matter concentrations averaging 596 ± 252 mg L, significantly higher than catchments dominated by red sandy, red loamy and alluvial soils (54 ± 56 mg l). In contrast, rivers originating from catchments with heavy precipitation, a tropical wet climate, red loamy soils (with peaty and marshy characteristics), rich tropical wet evergreen and moist deciduous forests, and higher soil organic carbon content yield more POC and PN (1704 ± 383 kgC km yr and 261 ± 56 kgN km yr, respectively) than the other rivers of India (951 ± 508 kgC km yr and 120 ± 57 kgN km yr, respectively). These findings stress that the export flux and yield of POC and PN from the Indian monsoonal rivers are primarily influenced by the interplay of hydrological, lithological, environmental, and climatic conditions within the catchment, rather than river size. Moreover, this study highlights the significant impact of incorporating POC data from medium-sized rivers worldwide, as it reveals that yield is independent of river size. This calls for a re-evaluation of global POC export fluxes, taking into account hydrological, lithological, environmental, and climatic factors.
本研究分析了来自印度季风河流向北印度洋的颗粒有机碳(POC)和颗粒氮(PN)的输出。印度季风河流每年输出约 1.2 太克 POC(1Tg=10g)和 0.14 太克 PN,其中约三分之二进入孟加拉湾(分别为 0.8 和 0.1 太克/年),其余部分到达阿拉伯海(分别为 0.4 和 0.04 太克/年)。值得注意的是,来自印度西北部以黑土为主的地区的四条河流贡献了 POC 和 PN 总输出量的一半左右(分别为 0.64 和 0.06 太克/年)。这是由于这些集水区发生了大量侵蚀,导致悬浮物浓度平均为 596±252mg/L,明显高于以红砂、红壤和冲积土为主的集水区(54±56mg/L)。相比之下,起源于降水较多、热带湿润气候、红壤(具有泥炭和沼泽特征)、富含热带湿润常绿和湿润落叶林以及较高土壤有机碳含量的集水区的河流,其 POC 和 PN 的输出量更高(分别为 1704±383kgC km yr 和 261±56kgN km yr),高于印度其他河流(分别为 951±508kgC km yr 和 120±57kgN km yr)。这些发现强调了印度季风河流的 POC 和 PN 输出通量和产量主要受到集水区水文、岩石学、环境和气候条件相互作用的影响,而不是河流大小的影响。此外,本研究强调了纳入全球中等河流 POC 数据的重要性,因为它表明产量与河流大小无关。这需要重新评估全球 POC 输出通量,考虑到水文、岩石学、环境和气候因素。