2021
DOI: 10.3390/fire4040064
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Loss and Recovery of Carbon in Repeatedly Burned Degraded Peatlands of Kalimantan, Indonesia

Abstract: Although accurate estimates of biomass loss during peat fires, and recovery over time, are critical in understanding net peat ecosystem carbon balance, empirical data to inform carbon models are scarce. During the 2019 dry season, fires burned through 133,631 ha of degraded peatlands of Central Kalimantan. This study reports carbon loss from surface fuels and the top peat layer of 18.5 Mg C ha−1 (3.5 from surface fuels and 15.0 from root/peat layer), releasing an average of 2.5 Gg (range 1.8–3.1 Gg) carbon in … Show more

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Cited by 12 publications
(9 citation statements)
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“…NDVI is one of the vegetation indices that combines the two opposite properties of canopy, NIR which covers the spectral wavelength reflected the most by the canopy and R which covers the spectral wavelength reflected the least by the canopy [81]. As a result of this property, NDVI is considered an appropriate vegetation index to study vegetation patterns across temporal or spatial scales and it has been extensively used to study post-fire landscape patterns and vegetation dynamics [79,[81][82][83][84]. Although other indices are also reported in the literature as suitable to monitor post-fire vegetation recovery, such us the Normalised Burn Ration (NBR) [77,78,85], NDVI was the first one tried in this study and gave excellent results.…”
Section: Remote Sensing Methodsmentioning
confidence: 99%
“…NDVI is one of the vegetation indices that combines the two opposite properties of canopy, NIR which covers the spectral wavelength reflected the most by the canopy and R which covers the spectral wavelength reflected the least by the canopy [81]. As a result of this property, NDVI is considered an appropriate vegetation index to study vegetation patterns across temporal or spatial scales and it has been extensively used to study post-fire landscape patterns and vegetation dynamics [79,[81][82][83][84]. Although other indices are also reported in the literature as suitable to monitor post-fire vegetation recovery, such us the Normalised Burn Ration (NBR) [77,78,85], NDVI was the first one tried in this study and gave excellent results.…”
Section: Remote Sensing Methodsmentioning
confidence: 99%
“…Gas speci c emission factors (G i ): CO 2 = 1620 g kg − 1 ; CO = 104 g kg − 1 ; N 2 O = 0.2 g kg − 1 ; CH 4 = 6.5 g kg − 1 23 GWP: CO 2 = 1; CO = 1.9; CH 4 = 25; N 2 O = 298 *emission factor is estimated from the peat mass loss as per 22 not AGB x Cf Emissions from peat are comprised of 80 or more GHGs so that CO 2 is only a part of the peat emission pro le 19,23 .…”
Section: Resultsmentioning
confidence: 99%
“…The depth of burnt peat was derived from the published literature. For the rst re, the depth of peat burnt was 33 cm 16 ; for second re we used 20 cm (average of relative depth burnt of rst and second res 21 ; for frequent res ( re frequency < 10 year) we used 10 cm 21 and for fourth and more res we used 2 cm 21 and data from our eld study in degraded peatlands of Central Kalimantan 22 .…”
Section: Datasetmentioning
confidence: 99%
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“…Many research and reviews put pressure on tropical peat fire monitoring or susceptibility assessments (Vetrita et al, 2021;Prasetyo et al, 2022;Taufik et al, 2022), peat consumption during fire occurrence (Che Azmi et al, 2021;Volkova et al, 2021), gas and particulate emissions from burned peat (Hirano et al, 2013;Crippa et al, 2016) and rehabilitation or restoration of burned peat (Scheper et al, 2021;Yuwati et al, 2021). However, little attention has been paid to the bio-physicochemical changes of peat after being burned.…”
Section: Introductionmentioning
confidence: 99%