Tropical peat surface oscillations are a function of peat condition at North Selangor peat swamp forest, Malaysia

Ledger, Martha J.; Evans, Chris D. ORCID: https://orcid.org/0000-0002-7052-354X; Large, David J.; Evers, Stephanie; Brown, Chloe; Jovani-Sancho, A. Jonay ORCID: https://orcid.org/0000-0002-7824-0501; Callaghan, Nathan ORCID: https://orcid.org/0000-0003-0273-6161; Vane, Christopher H. ORCID: https://orcid.org/0000-0002-8150-3640; Marshall, Chris; Baskaran, Abirami; Gan, Jing Ye; Sowter, Andrew; Morrison, Keith; Sjögersten, Sofie. 2023 Tropical peat surface oscillations are a function of peat condition at North Selangor peat swamp forest, Malaysia. Frontiers in Environmental Science, 11, 1182100. 18, pp. https://doi.org/10.3389/fenvs.2023.1182100

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Official URL: http://dx.doi.org/10.3389/fenvs.2023.1182100

Abstract/Summary

Tropical peatland condition across southeast Asia is deteriorating as a result of conversion to agriculture and urban zones. Conversion begins by lowering the water table, which leads to peat decomposition, subsidence and increased risk of large-scale forest fires. Associated changes in mechanical peat properties impact the magnitude and timing of changes in peatland surface motion, making them a potential proxy for peatland condition. However, such a relationship is yet to be observed in a tropical peatland setting. This study aimed to establish whether patterns of tropical peatland surface motion were a function of peat condition at North Selangor Peat Swamp Forest in Selangor, Malaysia. Results showed that subsidence was greatest at fire-affected scrubland sites, whilst the lowest mean water table levels were found at smallholder oil palm sites. Peat condition and magnitude of tropical peat surface oscillation were significantly different between peat condition classes, whilst peat condition differed with depth. More degraded tropical peats with high bulk density throughout the peat profile due to high surface loading and low mean water table levels showed greater surface oscillation magnitudes. The dominant peat surface oscillation mechanisms present at all sites were compression and shrinkage from changes in water table level. Mean water table level and subsidence rate were related to surface oscillation magnitude. However further work towards measuring surface and within-water table range bulk densities and surface loading is required to better understand the controls on surface oscillation magnitudes.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.3389/fenvs.2023.1182100
UKCEH and CEH Sections/Science Areas:	Soils and Land Use (Science Area 2017-)
ISSN:	2296-665X
Additional Information. Not used in RCUK Gateway to Research.:	Open Access paper - full text available via Official URL link.
Additional Keywords:	tropical peat, water table, peat condition, subsidence, hydraulic conductivity, volume change, surface oscillation, peat elasticity
NORA Subject Terms:	Ecology and Environment Agriculture and Soil Science
Date made live:	15 Aug 2023 14:28 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/535603

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.3389/fenvs.2023.1182100

UKCEH and CEH Sections/Science Areas:

Soils and Land Use (Science Area 2017-)

ISSN:

2296-665X

Additional Information. Not used in RCUK Gateway to Research.:

Open Access paper - full text available via Official URL link.

Additional Keywords:

tropical peat, water table, peat condition, subsidence, hydraulic conductivity, volume change, surface oscillation, peat elasticity