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A process-based model for quantifying the effects of canal blocking on water table and CO<sub>2</sub> emissions in tropical peatlands

dc.contributor.authorUrzainki, Iñaki
dc.contributor.authorPalviainen, Marjo
dc.contributor.authorHökkä, Hannu
dc.contributor.authorPersch, Sebastian
dc.contributor.authorChatellier, Jeffrey
dc.contributor.authorWang, Ophelia
dc.contributor.authorMahardhitama, Prasetya
dc.contributor.authorYudhista, Rizaldy
dc.contributor.authorLaurén, Annamari
dc.contributor.departmentid4100110310
dc.contributor.orcidhttps://orcid.org/0000-0003-2426-0539
dc.contributor.organizationLuonnonvarakeskus
dc.date.accessioned2023-08-11T07:32:29Z
dc.date.accessioned2025-05-27T18:35:10Z
dc.date.available2023-08-11T07:32:29Z
dc.date.issued2023
dc.description.abstractDrainage in tropical peatlands increases CO2 emissions, the rate of subsidence, and the risk of forest fires. To a certain extent, these effects can be mitigated by raising the water table depth (WTD) using canal or ditch blocks. The performance of canal blocks in raising WTD is, however, poorly understood because the WTD monitoring data are limited and spatially concentrated around canals and canal blocks. This raises the following question: how effective are canal blocks in raising the WTD over large areas? In this work, we composed a process-based hydrological model to assess the peatland restoration performance of 168 canal blocks in a 22 000 ha peatland area in Sumatra, Indonesia. We simulated daily WTD over 1 year using an existing canal block setup and compared it to the situation without blocks. The study was performed across two contrasting weather scenarios representing dry (1997) and wet (2013) years. Our simulations revealed that, while canal blocks had a net positive impact on WTD rise, they lowered WTD in some areas, and the extent of their effect over 1 year was limited to a distance of about 600 m around the canals. We also show that canal blocks are most effective in peatlands with high hydraulic conductivity. Averaging over all modeled scenarios, blocks raised the annual mean WTD by only 1.5 cm. This value was similar in the dry (1.44 cm) and wet (1.57 cm) years, and there was a 2.13 fold difference between the scenarios with large and small hydraulic conductivities (2.05 cm versus 0.96 cm). Using a linear relationship between WTD and CO2 emissions, we estimated that, averaging over peat hydraulic properties, canal blocks prevented the emission of 1.07 Mg ha−1 CO2 in the dry year and 1.17 Mg ha−1 CO2 in the wet year. We believe that the modeling tools developed in this work could be adopted by local stakeholders aiming at a more effective and evidence-based approach to canal-blockbased peatland restoration.
dc.description.vuosik2023
dc.format.bitstreamtrue
dc.format.pagerange2099-2116
dc.identifier.olddbid496317
dc.identifier.oldhandle10024/553753
dc.identifier.urihttps://jukuri.luke.fi/handle/11111/6151
dc.identifier.urnURN:NBN:fi-fe2023081194977
dc.language.isoen
dc.okm.corporatecopublicationon
dc.okm.discipline1171
dc.okm.discipline114
dc.okm.discipline1172
dc.okm.internationalcopublicationon
dc.okm.openaccess1 = Open access -julkaisukanavassa ilmestynyt julkaisu
dc.okm.selfarchivedon
dc.publisherCopernicus GmbH
dc.relation.doi10.5194/bg-20-2099-2023
dc.relation.ispartofseriesBiogeosciences
dc.relation.issn1726-4189
dc.relation.numberinseries11
dc.relation.volume20
dc.rightsCC BY 4.0
dc.source.identifierhttps://jukuri.luke.fi/handle/10024/553753
dc.teh41007-00189301
dc.teh41007-00187801
dc.titleA process-based model for quantifying the effects of canal blocking on water table and CO<sub>2</sub> emissions in tropical peatlands
dc.typepublication
dc.type.okmfi=A1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä|sv=A1 Originalartikel i en vetenskaplig tidskrift|en=A1 Journal article (refereed), original research|
dc.type.versionfi=Publisher's version|sv=Publisher's version|en=Publisher's version|

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