Tropical peat deposits undergoing land-use change: the case of Buhandanda and Lushala peatlands (Democratic Republic of Congo)

Discovery of the world’s largest known peat deposit in the Central African Basin creates a need for the Democratic Republic of Congo (DRC) to undertake a realistic national assessment of peat carbon. In the study described here we determined physicochemical properties of the Buhandanda and Lushala p...

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Main Authors: Patrick M. Senga, Julie Talbot, Steeve Bonneville
Format: Article
Language:English
Published: International Mire Conservation Group and International Peatland Society 2023-03-01
Series:Mires and Peat
Subjects:
Online Access:http://mires-and-peat.net/media/map29/map29_09.pdf
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author Patrick M. Senga
Julie Talbot
Steeve Bonneville
author_facet Patrick M. Senga
Julie Talbot
Steeve Bonneville
author_sort Patrick M. Senga
collection DOAJ
description Discovery of the world’s largest known peat deposit in the Central African Basin creates a need for the Democratic Republic of Congo (DRC) to undertake a realistic national assessment of peat carbon. In the study described here we determined physicochemical properties of the Buhandanda and Lushala peat deposits, located in Sud-Kivu Province, to gain insights about their structure and functioning and provide a first estimate of C stocks. A change of land use (to seasonal subsistence agriculture) operating in the last few decades has dramatically modified the vegetation, which was originally dominated by mesophilic forest species. Several peat properties (pH, organic matter content, porosity, dry matter, ash and fibre contents) increased with depth in the peat profile, although some (nitrogen, nitrate, phosphate content and air-filled porosity) decreased and others (bulk density, solids density, C/N) showed no trend. The C densities of peat at the two sites were 68.60 and 60.64 kg m-3, our estimates of mean (± SD) peat thickness were 324 ± 139 and 212 ± 109 cm, and total C storage was 0.136 and 0.023 Mt, for Buhandanda and Lushala, respectively. The range of calibrated radiocarbon dates for a 200 cm deep core collected from Lushala was 648–2005 cal. AD, with a high modern carbon fraction (F14C) near the surface (at depths of 15 cm and 80 cm). Overall, our results indicated that carbon accumulation has declined at these two sites owing to the reduction in litter flux associated with land use change. Using the average C densities and peat thicknesses measured at Lushala and Buhandanda, we estimated that the total C storage in Sud-Kivu peatlands is approximately 1.23 Mt.
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spelling doaj.art-cba13e0c008b4d7a9040798a56cb76b72023-09-03T13:28:15ZengInternational Mire Conservation Group and International Peatland SocietyMires and Peat1819-754X2023-03-01290911710.19189/MaP.2022.OMB.StA.2415Tropical peat deposits undergoing land-use change: the case of Buhandanda and Lushala peatlands (Democratic Republic of Congo)Patrick M. Senga0Julie Talbot1Steeve Bonneville2Department of Environmental Sciences, University of Kinshasa, Kinshasa, Democratic Republic of CongoDepartment of Geography, University of Montreal, Montreal, CanadaDépartement de Géosciences, Environnement et Société, Université Libre de Bruxelles, BelgiumDiscovery of the world’s largest known peat deposit in the Central African Basin creates a need for the Democratic Republic of Congo (DRC) to undertake a realistic national assessment of peat carbon. In the study described here we determined physicochemical properties of the Buhandanda and Lushala peat deposits, located in Sud-Kivu Province, to gain insights about their structure and functioning and provide a first estimate of C stocks. A change of land use (to seasonal subsistence agriculture) operating in the last few decades has dramatically modified the vegetation, which was originally dominated by mesophilic forest species. Several peat properties (pH, organic matter content, porosity, dry matter, ash and fibre contents) increased with depth in the peat profile, although some (nitrogen, nitrate, phosphate content and air-filled porosity) decreased and others (bulk density, solids density, C/N) showed no trend. The C densities of peat at the two sites were 68.60 and 60.64 kg m-3, our estimates of mean (± SD) peat thickness were 324 ± 139 and 212 ± 109 cm, and total C storage was 0.136 and 0.023 Mt, for Buhandanda and Lushala, respectively. The range of calibrated radiocarbon dates for a 200 cm deep core collected from Lushala was 648–2005 cal. AD, with a high modern carbon fraction (F14C) near the surface (at depths of 15 cm and 80 cm). Overall, our results indicated that carbon accumulation has declined at these two sites owing to the reduction in litter flux associated with land use change. Using the average C densities and peat thicknesses measured at Lushala and Buhandanda, we estimated that the total C storage in Sud-Kivu peatlands is approximately 1.23 Mt.http://mires-and-peat.net/media/map29/map29_09.pdfcarbon stocksgreenhouse gasmountain peatlandpeat soilsubsistence agriculture
spellingShingle Patrick M. Senga
Julie Talbot
Steeve Bonneville
Tropical peat deposits undergoing land-use change: the case of Buhandanda and Lushala peatlands (Democratic Republic of Congo)
Mires and Peat
carbon stocks
greenhouse gas
mountain peatland
peat soil
subsistence agriculture
title Tropical peat deposits undergoing land-use change: the case of Buhandanda and Lushala peatlands (Democratic Republic of Congo)
title_full Tropical peat deposits undergoing land-use change: the case of Buhandanda and Lushala peatlands (Democratic Republic of Congo)
title_fullStr Tropical peat deposits undergoing land-use change: the case of Buhandanda and Lushala peatlands (Democratic Republic of Congo)
title_full_unstemmed Tropical peat deposits undergoing land-use change: the case of Buhandanda and Lushala peatlands (Democratic Republic of Congo)
title_short Tropical peat deposits undergoing land-use change: the case of Buhandanda and Lushala peatlands (Democratic Republic of Congo)
title_sort tropical peat deposits undergoing land use change the case of buhandanda and lushala peatlands democratic republic of congo
topic carbon stocks
greenhouse gas
mountain peatland
peat soil
subsistence agriculture
url http://mires-and-peat.net/media/map29/map29_09.pdf
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AT steevebonneville tropicalpeatdepositsundergoinglandusechangethecaseofbuhandandaandlushalapeatlandsdemocraticrepublicofcongo