Yadav Amita, Pandey Jitendra
Ganga River Ecology Research Laboratory, Environmental Science Division, Centre of Advanced Study in Botany, Institute of Science, Banaras Hindu University, Varanasi, 221005, India.
Environ Monit Assess. 2017 Aug 28;189(9):475. doi: 10.1007/s10661-017-6188-8.
To determine the possible contributions of point and non-point sources to carbon and nutrient loading in the Ganga River, we analyzed N, P, and organic carbon (OC) in the atmospheric deposits, surface runoff, and in the river along a 37-km stretch from 2013 to 2015. We also assessed the trophic status of the river as influenced by such sources of nutrient input. Although the river N, P, and productivity showed a declining trend with increasing discharge, runoff DOC and dissolved reactive phosphorus (DRP) increased by 88.05 and 122.7% between the Adpr and Rjht sites, indicating contributions from atmospheric deposition (AD) coupled with land use where agriculture appeared to be the major contributor. Point source input led to increased river concentrations of NO, NH, DRP, and DOC by 10.5, 115.9, 115.2, and 67.3%, respectively. Increases in N, P, and productivity along the gradient were significantly negatively correlated with river discharge (p < 0.001), while river DOC and dissolved silica showed positive relationships. The results revealed large differences in point and non-point sources of carbon and nutrient input into the Ganga River, although these variations were strongly influenced by the seasonality in surface runoff and river discharge. Despite these variations, N and P concentrations were sufficient to enhance phytoplankton growth along the study stretch. Allochthonous input together with enhanced autotrophy would accelerate heterotrophic growth, degrading the river more rapidly in the near future. This study suggests the need for large-scale inter-regional time series data on the point and non-point source partitioning and associated food web dynamics of this major river system.
为了确定点源和非点源对恒河碳和养分负荷的可能贡献,我们在2013年至2015年期间,分析了大气沉积物、地表径流以及沿37公里河段的河流中的氮、磷和有机碳(OC)。我们还评估了受此类养分输入源影响的河流营养状况。尽管河流中的氮、磷和生产力随着流量增加呈下降趋势,但在Adpr和Rjht站点之间,径流溶解有机碳(DOC)和溶解活性磷(DRP)分别增加了88.05%和122.7%,这表明大气沉降(AD)以及农业似乎是主要贡献者的土地利用方式起到了作用。点源输入分别使河流中的NO、NH、DRP和DOC浓度增加了10.5%、115.9%、115.2%和67.3%。沿梯度方向氮、磷和生产力的增加与河流流量显著负相关(p < 0.001),而河流DOC和溶解硅呈正相关。结果表明,恒河碳和养分输入的点源和非点源存在很大差异,尽管这些变化受到地表径流和河流流量季节性的强烈影响。尽管存在这些变化,但氮和磷的浓度足以促进研究河段浮游植物的生长。外源输入与增强的自养作用将加速异养生长,在不久的将来使河流退化得更快。这项研究表明,需要关于这个主要河流系统的点源和非点源划分以及相关食物网动态的大规模区域间时间序列数据。