Deciphering the nitrate sources and processes in the Ganga river using dual isotopes of nitrate and Bayesian mixing model

被引:18
|
作者
Kumar, Anurag [1 ,4 ]
Ajay, Ajay [1 ]
Dasgupta, Bibhasvata [1 ]
Bhadury, Punyasloke [2 ,3 ]
Sanyal, Prasanta [1 ,2 ]
机构
[1] Indian Inst Sci Educ & Res Kolkata, Dept Earth Sci, Mohanpur 741246, India
[2] Indian Inst Sci Educ & Res Kolkata, Ctr Climate & Environm Studies, Mohanpur 741246, India
[3] Indian Inst Sci Educ & Res Kolkata, Dept Biol Sci, Integrat Taxon & Microbial Ecol Res Grp, Mohanpur 741246, India
[4] Birbal Sahni Inst Palaeosciences, Lucknow 226007, India
关键词
Nitrate source; Isotopic composition of dissolved NO 3; Bayesian mixing model; Assimilation; Nitrification; ANTHROPOGENIC NITROGEN INPUTS; GLOBAL PATTERNS; FLUXES; BAY; OXYGEN; DENITRIFICATION; ESTUARY; BENGAL; WATER; N-15;
D O I
10.1016/j.envres.2022.114744
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The dual isotopes of dissolved NO3- (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 NO3- concentration in the lower stretch of the river Ganga varied between 4.1 and 64.1 mu M 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%o for 815NNO3- and -1.2 to +11.0%o for 818ONO3-. The spatial NO3- concentration during the post-monsoon season varied between 23.2 and 57.7 mu M, 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%o for 815NNO3- and -4.6 to +5.2%o for 818ONO3-. 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 postmonsoon 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 NO3established 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.
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页数:13
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