Please use this identifier to cite or link to this item: https://hdl.handle.net/1959.11/44882
Full metadata record
DC FieldValueLanguage
dc.contributor.authorPasut, Chiaraen
dc.contributor.authorTang, Fiona H Men
dc.contributor.authorMaggi, Federicoen
dc.date.accessioned2022-02-25T03:04:31Z-
dc.date.available2022-02-25T03:04:31Z-
dc.date.issued2020-04-27-
dc.identifier.citationJournal of Geophysical Research: Biogeosciences, 125(4), p. 1-20en
dc.identifier.issn2169-8961en
dc.identifier.issn2169-8953en
dc.identifier.urihttps://hdl.handle.net/1959.11/44882-
dc.description.abstract<p>Wetlands represent the most significant natural greenhouse gas (GHG) source and their annual emissions tightly depend on climatic and anthropogenic factors. Biogeochemical processes occurring in wetlands are still poorly described by mechanistic models and hence their dynamic response to environmental changes are weakly predicted. We investigated wetland GHG emissions, relevant electron acceptors and donors concentrations, and microbial composition resulting from changes in temperature, CH<sub>4</sub> plant uptake efficiency, and SO<sup>2−</sup><sub>4</sub> deposition using a mechanistic biogeochemical model (here called BAMS3) that integrates the carbon (C), nitrogen (N), and sulfur (S) cycles. Parameters constraining the coupled C-N-S cycles were retrieved from controlled experiments and were validated against independent field data of CH<sub>4</sub> emissions, and CH<sub>4</sub>(aq) and SO<sup>2−</sup><sub>4</sub> concentration profiles in a wetland in southern Michigan, USA (Shannon & White, 1994, <a href="http://hdl.handle.net/102.100.100/236252? index=1">http://hdl.handle.net/102.100.100/236252? index=1</a>). We found that +1.75 <sup>◦</sup>C increase in temperature leads to 22% and 30% increment in CH<sub>4</sub> and N<sub>2</sub>O emissions, respectively. A decrease in the CH<sub>4</sub> plant uptake efficiency causes the prevalent CH<sub>4</sub> emission pathway to become diffusion mediated and resulted in 50% increase in the daily average CH<sub>4</sub> emissions. Finally, a decreasing SO<sup>2−</sup><sub>4</sub> deposition rate can increase CH<sub>4</sub> emissions up to 5%. We conclude that the increasing GHG emissions from wetlands is a result of both environmental and anthropogenic causes rather than global warming alone. An increase in model complexity does not necessary improve the estimation of GHG emissions but it aids interpretation of intermediate processes to a greater detail.</p> <p>Plain Language Summary</p> <p>Wetlands are the largest natural source of greenhouse gasses; hence, climate change and human development have become a major concern for the conservation of these ecosystems. In this study, we explore the effect of rising temperature, plants community, and changes in nutrient input rate on the emission rate and quality in a wetland. The assessment was conducted using a mechanistic model that accounts for carbon, nitrogen, and sulfur cycles on test scenarios. The model was initially tested on field data of a wetland in southern Michigan, and then used for scenarios predictions. Results suggest that increasing the average soil temperature leads to a substantial increase in greenhouse gas emissions; in particular, methane emissions increase by 22%. Methane emissions are also affected by the plant composition, which controls the main emission pathway; small composition changes can induce high emissions variations. Finally, we showed how a change in atmospheric sulfate deposition to wetlands can control the methane emissions. We conclude that modeling coupled chemical, biological, and physical processes helped to describe wetland nutrients dynamics under both climate change and anthropogenic factors.</p>en
dc.languageenen
dc.publisherWiley-Blackwell Publishing, Incen
dc.relation.ispartofJournal of Geophysical Research: Biogeosciencesen
dc.titleA Mechanistic Analysis of Wetland Biogeochemistry in Response to Temperature, Vegetation, and Nutrient Input Changesen
dc.typeJournal Articleen
dc.identifier.doi10.1029/2019JG005437en
local.contributor.firstnameChiaraen
local.contributor.firstnameFiona H Men
local.contributor.firstnameFedericoen
local.profile.schoolSchool of Environmental and Rural Scienceen
local.profile.emailftang2@une.edu.auen
local.output.categoryC1en
local.record.placeauen
local.record.institutionUniversity of New Englanden
local.publisher.placeUnited States of Americaen
local.identifier.runningnumbere2019JG005437en
local.format.startpage1en
local.format.endpage20en
local.identifier.scopusid85091020650en
local.peerreviewedYesen
local.identifier.volume125en
local.identifier.issue4en
local.contributor.lastnamePasuten
local.contributor.lastnameTangen
local.contributor.lastnameMaggien
dc.identifier.staffune-id:ftang2en
local.profile.roleauthoren
local.profile.roleauthoren
local.profile.roleauthoren
local.identifier.unepublicationidune:1959.11/44882en
local.date.onlineversion2020-04-16-
dc.identifier.academiclevelAcademicen
dc.identifier.academiclevelAcademicen
dc.identifier.academiclevelAcademicen
local.title.maintitleA Mechanistic Analysis of Wetland Biogeochemistry in Response to Temperature, Vegetation, and Nutrient Input Changesen
local.relation.fundingsourcenoteThis work is supported by the SREI2020 EnviroSphere research program of the University of Sydney and the SREI Voucher. F. M. is also supported by the Mid Career Research Award and Sydney Research Accelerator Fellowship (SOAR) of the University of Sydney.en
local.output.categorydescriptionC1 Refereed Article in a Scholarly Journalen
local.search.authorPasut, Chiaraen
local.search.authorTang, Fiona H Men
local.search.authorMaggi, Federicoen
local.uneassociationNoen
local.atsiresearchNoen
local.sensitive.culturalNoen
local.year.available2020-
local.year.published2020-
local.fileurl.closedpublishedhttps://rune.une.edu.au/web/retrieve/4dcf22f5-c12d-44aa-aa0b-6766a86009e9en
local.subject.for2020410601 Land capability and soil productivityen
local.subject.for2020410604 Soil chemistry and soil carbon sequestration (excl. carbon sequestration science)en
local.subject.seo2020190501 Climate change modelsen
Appears in Collections:Journal Article
School of Environmental and Rural Science
Files in This Item:
1 files
File SizeFormat 
Show simple item record

SCOPUSTM   
Citations

12
checked on Dec 21, 2024

Page view(s)

912
checked on Jun 18, 2023

Download(s)

4
checked on Jun 18, 2023
Google Media

Google ScholarTM

Check

Altmetric


Items in Research UNE are protected by copyright, with all rights reserved, unless otherwise indicated.