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dc.contributor.authorNoulèkoun, Florent
dc.contributor.authorBirhane, Emiru
dc.contributor.authorKassa, Habtemariam
dc.contributor.authorBerhe, Alemayehu
dc.contributor.authorMulaw Gebremichael, Zefere
dc.contributor.authorMohammed Adem, Nuru
dc.contributor.authorSyoum, Yigremachew
dc.contributor.authorMengistu, Tefera
dc.contributor.authorLemma, Bekele
dc.contributor.authorHagazi, Nigussie
dc.contributor.authorAbrha, Haftu
dc.contributor.authorMekonen Rannestad, Meley
dc.contributor.authorMensah, Sylvanus
dc.date.accessioned2021-04-16T08:18:24Z
dc.date.available2021-04-16T08:18:24Z
dc.date.issued2021-03-29
dc.identifier.urihttps://doi.org/10.1016/j.scitotenv.2021.146821
dc.identifier.urihttp://52.157.139.19:8080/xmlui/handle/123456789/44
dc.descriptionJournal Article full text: https://doi.org/10.1016/j.scitotenv.2021.146821en_US
dc.description.abstractThe establishment of grazing exclosures is widely practiced to restore degraded agricultural lands and forests. Here, we evaluated the potential of grazing exclosures to contribute to the “4 per 1000” initiative by analyzing the changes in soil organic carbon (SOC) stocks and sequestration (SCS) rates after their establishment on degraded communal grazing lands in Tigray region of Ethiopia. We selected grazing areas that were excluded from grazing for 5 to 24 years across the three agroecological zones of the region and used adjacent open grazing lands (OGLs) as control. Soil samples were collected from two depths (0–15 cm and 15–30 cm) and SOC and aboveground C stocks were quantified in both exclosures and OGLs. The mean SOC stock and SCS rate in exclosures (0–30 cm) were 31 Mg C ha−1 and 3 Mg C ha−1 year−1, which were respectively 166% and 12% higher than that in the OGLs, indicating a positive restoration effect of exclosures on SOC storage. With increasing exclosure age, SOC stock and SCS rate increased in the exclosures but decreased in the OGLs. Higher SOC stock and SCS rate were recorded in 0–15 cm than in 15–30 cm. The relative (i.e., to the SOC stock in OGLs) rates of increase in SOC stocks (70–189‰ year−1) were higher than the 4‰ year−1 and were initially high due to low initial SOC stock but declined over time after a maximum value of SOC stock is reached. Factors such as aboveground biomass, altitude, clay content and precipitation promoted SOC storage in exclosures. Our study highlights the high potential of exclosures for restoring SOC in the 0–30 cm soil depth at a rate greater than the 4‰ value. We argue that practices such as grazing exclosure can be promoted to achieve the climate change mitigation target of the “4‰” initiative.en_US
dc.publisherScience of The Total Environmenten_US
dc.relation.ispartofseries782;
dc.subjectOrganic carbon accumulation Land degradation Tree-mediated carbon sequestration Sink saturation Space-for-time approach Tigray regionen_US
dc.titleGrazing exclosures increase soil organic carbon stock at a rate greater than “4 per 1000” per year across agricultural landscapes in Northern Ethiopiaen_US
dc.typeArticleen_US
Appears in Collections:Climate Change

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