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Nitrogen along the Hydrological Gradient of Marsh Sediments in a Subtropical Estuary

Pools, Processes, and Fluxes

Bibliographic Data

ID15513834
AuthorsWeifang Hu (0000-0003-0542-9685, Fujian Normal University), Wenlong Zhang (0000-0001-6376-3994, Fujian Normal University), Linhai Zhang (0000-0003-1009-6870, Fujian Normal University), Chuan Tong (0000-0003-2071-2876, Fujian Normal University), Zhigao Sun (0000-0002-9486-8825, Fujian Normal University), Yuehmin Chen (0000-0001-9724-5669, Fujian Normal University, corresponding author), Congsheng Zeng (Fujian Normal University, corresponding author)
Year2019
Volume16
Issue11
Pages2043-2043
Publication date2019-06-09
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueInternational Journal of Environmental Research and Public Health (JOURNAL)
Journal identifiersISSN: 1661-7827 • E-ISSN: 1660-4601
PublisherMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/ijerph16112043
PMID31181868
OpenAlexW2948533897
LanguageEN
References cited70

Knowledge on the distribution of nitrogen (N) pools, processes, and fluxes along hydrological gradients provides a comprehensive perspective to understand the underlying causal mechanisms in intertidal flats, and thus improve predictions and climate adaptation strategies. We used a space-for-time substitution method to quantify N pools, processes, and fluxes along a hydrological gradient. Further, we linked N pools and processes and investigated not only surface but also subsurface sediments. Our results showed a gradual decrease in total N (TN) and mineralization rates ( PN min ), but an increase in potential rates of nitrification ( PNR ) and denitrification ( PDNR ) under an elevated hydrological gradient, except for TN and PN min in the subsurface sediment, which accumulated on the interaction zone between the high and middle tidal flats. Most sedimentary ammonium N (NH 4 + ) and nitrate N (NO 3 - ) concentrations were similar; however, NH 4 + accumulated on the subsurface of the middle tidal flat. NO 3 - fluxes (from -0.54 to -0.35 mmol m -2 h -1 ) were uptake fluxes in the intertidal flats, but NH 4 + fluxes (-2.48-3.54 mmol m -2 h -1 ) changed from uptake to efflux in the seaward direction. Structural equation modeling of the effects of inundation frequency, underground biomass, total carbon (TC), electrical conductivity (EC), and clay proportion on the N processes revealed that these accounted for 67%, 82%, and 17% of the variance of PDNR , PN min , and PNR , respectively. Inundation frequency, underground biomass, TC, EC, and PN min effects on N pools accounted for 53%, 69%, and 98% of the variance of NH 4 + , NO 3 - , and TN, respectively. This suggests that future sea level rise may decrease N storage due to increase in coupled nitrification-denitrification and decrease in N mineralization, and the NH 4 + flux may change from sink to source in intertidal ecosystems

Ammonium · Biology · Denitrification · Estuary · Geomorphology · Hydrology (agriculture · Intertidal zone · Mineralization (soil science · Nitrate · Nitrification · Nitrogen · Nitrogen Cycle · Salt marsh · Sediment · Soil water · Chemistry · Coastal and Marine Dynamics · Coastal wetland ecosystem dynamics · Environmental Science · Marine and coastal ecosystems · Ecology · Environmental Chemistry · Geology · Oceanography · Soil Science

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Citation velocityhistorical
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