Enhanced N 2 O Production Induced by Soil Salinity at a Specific Range

Yawei Li, Junzeng Xu, Boyi Liu, Haiyu Wang, Zhiming Qi, Qi Wei, Linxian Liao and Shimeng Liu
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Yawei Li: State Key Laboratory of Hydrology—Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China
Junzeng Xu: State Key Laboratory of Hydrology—Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China
Boyi Liu: College of Agricultural Science and Engineering, Hohai University, Nanjing 210098, China
Haiyu Wang: College of Agricultural Science and Engineering, Hohai University, Nanjing 210098, China
Zhiming Qi: Department of Bioresource Engineering, McGill University, Sainte-Anne-de-Bellevue, QC H9X 3V9, Canada
Qi Wei: College of Agricultural Science and Engineering, Hohai University, Nanjing 210098, China
Linxian Liao: College of Agricultural Science and Engineering, Hohai University, Nanjing 210098, China
Shimeng Liu: College of Agricultural Science and Engineering, Hohai University, Nanjing 210098, China

IJERPH, 2020, vol. 17, issue 14, 1-12

Abstract: Nitrous oxide (N 2 O) as a by-product of soil nitrogen (N) cylces, its production may be affected by soil salinity which have been proved to have significant negative effect on soil N transformation processes. The response of N 2 O production across a range of different soil salinities is poorly documented; accordingly, we conducted a laboratory incubation experiment using an array of soils bearing six different salinity levels ranging from 0.25 to 6.17 dS m −1 . With ammonium-rich organic fertilizer as their N source, the soils were incubated at three soil moisture ( θ ) levels—50%, 75% and 100% of field capacity ( θ fc )—for six weeks. Both N 2 O fluxes and concentrations of ammonium, nitrite and nitrate (NH 4 + -N, NO 2 − -N and NO 3 − -N) were measured throughout the incubation period. The rates of NH 4 + -N consumption and NO 3 − -N accumulation increased with increasing soil moisture and decreased with increasing soil salinity, while the accumulation of NO 2 − -N increased first then decreased with increasing soil salinity. N 2 O emissions were significantly promoted by greater soil moisture. As soil salinity increased from 0.25 to 6.17 dS m −1 , N 2 O emissions from soil first increased then decreased at all three soil moisture levels, with N 2 O emissions peaking at electric conductivity (EC) values of 1.01 and 2.02 dS m −1 . N 2 O emissions form saline soil were found significantly positively correlated to soil NO 2 − -N accumulation. The present results suggest that greater soil salinity inhibits both steps of nitrification, but that its inhibition of nitrite oxidation is stronger than that on ammonia oxidation, which leads to higher NO 2 − -N accumulation and enhanced N 2 O emissions in soil with a specific salinity range.

Keywords: soil salinity; N 2 O emission; soil inorganic N; nitrification (search for similar items in EconPapers)
JEL-codes: I I1 I3 Q Q5 (search for similar items in EconPapers)
Date: 2020
References: View complete reference list from CitEc
Citations: View citations in EconPapers (1)

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