Deciphering the nitrate sources and processes in the Ganga river using dual isotopes of nitrate and Bayesian mixing model
Environmental Research, ISSN: 0013-9351, Vol: 216, Issue: Pt 4, Page: 114744
2023
- 24Citations
- 4Captures
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Article Description
The dual isotopes of dissolved NO 3 - (n = 43) has been used to delineate the nitrate sources and N-cycling processes in the Ganga river. The proportional contribution of nitrate from different sources has been estimated using the Bayesian mixing model. The seasonal NO 3 - concentration in the lower stretch of the river Ganga varied between 4.1 and 64.1 μM with higher concentration during monsoon and post-monsoon season and lower concentration during the pre-monsoon and winter season. The temporal variation in the isotopic values ranged between +0.0 and +9.6‰ for δ 15 N NO3 - and −1.2 to +11.0‰ for δ 18 O NO3 -. The spatial NO 3 - concentration during the post-monsoon season varied between 23.2 and 57.7 μM, with higher values from the middle and lower values from the lower stretch of the river Ganga. The isotopic ratio during the post-monsoon season varied between −1.0 and +11.3‰ for δ 15 N NO3 - and −4.6 to +5.2‰ for δ 18 O NO3 -. The temporal dataset from the lower stretch of the river Ganga showed the dominance of nitrate derived from the nitrification of soil organic matter (SOM) (average ∼53.4%). The nitrate contribution from synthetic fertilizers was observed to be higher during the post-monsoon season (34.7 ± 23.4%) compared to that in the monsoon (25.5 ± 19.5%) and pre-monsoon (22.2 ± 19.6%) season. No significant seasonal variations were observed in the nitrate input from manure/sewage (∼13.9%). Spatial samples collected during the post-monsoon season showed higher contribution of synthetic fertilizer in the lower stretch (34.6 ± 22.7%) compared to the middle stretch (21.1 ± 18.2%), which indicates greater influence of the agricultural activity in the lower stretch. The dual isotope study of dissolved NO 3 - established that the nitrate in the Ganga river water is mostly derived from the nitrification of incoming organic compounds and is subsequently removed via assimilatory nitrate uptake. The study also emphasises significant nitrification and assimilatory nitrate removal processes operating in the mixing zone of the Ganga river and Hooghly estuary.
Bibliographic Details
http://www.sciencedirect.com/science/article/pii/S0013935122020710; http://dx.doi.org/10.1016/j.envres.2022.114744; http://www.scopus.com/inward/record.url?partnerID=HzOxMe3b&scp=85141769438&origin=inward; http://www.ncbi.nlm.nih.gov/pubmed/36368371; https://linkinghub.elsevier.com/retrieve/pii/S0013935122020710; https://dx.doi.org/10.1016/j.envres.2022.114744
Elsevier BV
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