FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2044285724> ?p ?o ?g. }

• W2044285724 endingPage "327" @default.
• W2044285724 startingPage "322" @default.
• W2044285724 abstract "Soil plays an important role in the global carbon cycle, and carbon sequestration in soil is important for mitigating global climate change. Historically, soil erosion led to great reductions of soil organic carbon (SOC) storage in China. Fortunately, with the economic development and remarkably effective soil erosion control measures in subtropical China over the past 20 years, soil erosion has been greatly decreased. As a result, soil organic carbon sequestration has gradually increased due to the rapid recovery of vegetation in the area. However, little information exists concerning the potential of soil carbon sequestration in the area. This paper introduces a case study in Xingguo County, Jiangxi Province, China, which used to be a typical area with significant soil loss in subtropical China. This work represents a systematic investigation of the interrelations of carbon sequestration potential with soil erosion types, altitudes, soil types and soil parent materials. In this study, 284 soil samples were collected from 151 sampling sites (51 are soil profile sites) to determine soil physicochemical properties including organic carbon content. Soil organic carbon distribution maps of the surface layer (0–20 cm) and whole profile (0–100 cm) were compiled by linking soil types to the polygons of digital soil maps using GIS. Assuming that SOC was lost following the destruction of native vegetation, these lands hold great promise for potentially sequestering carbon again. The potential of soil carbon sequestration in the study area was estimated by subtracting the organic carbon status in eroded soils from that in non-eroded soils under undisturbed forest. Results show that the potential of SOC in the surface layer is 4.47 Tg C while that in the whole profile is 12.3 Tg C for the entire county. The greatest potential for carbon sequestration (3.72 Tg C) is found in severely eroded soil, while non-eroded soil has the smallest potential. Also, soil carbon sequestration potential decreases with increasing altitude. Soils at altitudes of <300 m show the greatest potential (5.01 Tg C), while those of >800 m have the smallest potential (0.25 Tg C). Among various soil types, red earths (Humic Acrisols) have the greatest potential of carbon sequestration (5.32 Tg C), and yellow earths (Ferralic Cambisols) have the smallest (0.15 Tg C). As for soils derived from various parent materials, soils derived from phyllite possess the greatest carbon sequestration potential, and soils from Quaternary red clays have the smallest." @default.
• W2044285724 created "2016-06-24" @default.
• W2044285724 creator A5019032860 @default.
• W2044285724 creator A5037231605 @default.
• W2044285724 creator A5041833285 @default.
• W2044285724 creator A5053603075 @default.
• W2044285724 creator A5060261155 @default.
• W2044285724 creator A5070672448 @default.
• W2044285724 creator A5083413359 @default.
• W2044285724 creator A5089925843 @default.
• W2044285724 date "2009-11-01" @default.
• W2044285724 modified "2023-09-27" @default.
• W2044285724 title "Potential for soil carbon sequestration of eroded areas in subtropical China" @default.
• W2044285724 cites W1505543708 @default.
• W2044285724 cites W1988853954 @default.
• W2044285724 cites W2006799969 @default.
• W2044285724 cites W2017746769 @default.
• W2044285724 cites W2031155505 @default.
• W2044285724 cites W2041869533 @default.
• W2044285724 cites W2074103890 @default.
• W2044285724 cites W2074862013 @default.
• W2044285724 cites W2079248006 @default.
• W2044285724 cites W2081634653 @default.
• W2044285724 cites W2093806074 @default.
• W2044285724 cites W2115930599 @default.
• W2044285724 cites W2123073816 @default.
• W2044285724 cites W2124759059 @default.
• W2044285724 cites W2134406342 @default.
• W2044285724 cites W2148269536 @default.
• W2044285724 cites W2157462758 @default.
• W2044285724 cites W60470445 @default.
• W2044285724 doi "https://doi.org/10.1016/j.still.2008.12.016" @default.
• W2044285724 hasPublicationYear "2009" @default.
• W2044285724 type Work @default.
• W2044285724 sameAs 2044285724 @default.
• W2044285724 citedByCount "27" @default.
• W2044285724 countsByYear W20442857242012 @default.
• W2044285724 countsByYear W20442857242013 @default.
• W2044285724 countsByYear W20442857242014 @default.
• W2044285724 countsByYear W20442857242015 @default.
• W2044285724 countsByYear W20442857242018 @default.
• W2044285724 countsByYear W20442857242019 @default.
• W2044285724 countsByYear W20442857242020 @default.
• W2044285724 countsByYear W20442857242022 @default.
• W2044285724 countsByYear W20442857242023 @default.
• W2044285724 crossrefType "journal-article" @default.
• W2044285724 hasAuthorship W2044285724A5019032860 @default.
• W2044285724 hasAuthorship W2044285724A5037231605 @default.
• W2044285724 hasAuthorship W2044285724A5041833285 @default.
• W2044285724 hasAuthorship W2044285724A5053603075 @default.
• W2044285724 hasAuthorship W2044285724A5060261155 @default.
• W2044285724 hasAuthorship W2044285724A5070672448 @default.
• W2044285724 hasAuthorship W2044285724A5083413359 @default.
• W2044285724 hasAuthorship W2044285724A5089925843 @default.
• W2044285724 hasConcept C107872376 @default.
• W2044285724 hasConcept C123157820 @default.
• W2044285724 hasConcept C127313418 @default.
• W2044285724 hasConcept C14168384 @default.
• W2044285724 hasConcept C142724271 @default.
• W2044285724 hasConcept C151730666 @default.
• W2044285724 hasConcept C158787203 @default.
• W2044285724 hasConcept C159390177 @default.
• W2044285724 hasConcept C159750122 @default.
• W2044285724 hasConcept C182124840 @default.
• W2044285724 hasConcept C185592680 @default.
• W2044285724 hasConcept C18903297 @default.
• W2044285724 hasConcept C22884784 @default.
• W2044285724 hasConcept C2776133958 @default.
• W2044285724 hasConcept C39432304 @default.
• W2044285724 hasConcept C39464130 @default.
• W2044285724 hasConcept C530467964 @default.
• W2044285724 hasConcept C71924100 @default.
• W2044285724 hasConcept C7959160 @default.
• W2044285724 hasConcept C86803240 @default.
• W2044285724 hasConceptScore W2044285724C107872376 @default.
• W2044285724 hasConceptScore W2044285724C123157820 @default.
• W2044285724 hasConceptScore W2044285724C127313418 @default.
• W2044285724 hasConceptScore W2044285724C14168384 @default.
• W2044285724 hasConceptScore W2044285724C142724271 @default.
• W2044285724 hasConceptScore W2044285724C151730666 @default.
• W2044285724 hasConceptScore W2044285724C158787203 @default.
• W2044285724 hasConceptScore W2044285724C159390177 @default.
• W2044285724 hasConceptScore W2044285724C159750122 @default.
• W2044285724 hasConceptScore W2044285724C182124840 @default.
• W2044285724 hasConceptScore W2044285724C185592680 @default.
• W2044285724 hasConceptScore W2044285724C18903297 @default.
• W2044285724 hasConceptScore W2044285724C22884784 @default.
• W2044285724 hasConceptScore W2044285724C2776133958 @default.
• W2044285724 hasConceptScore W2044285724C39432304 @default.
• W2044285724 hasConceptScore W2044285724C39464130 @default.
• W2044285724 hasConceptScore W2044285724C530467964 @default.
• W2044285724 hasConceptScore W2044285724C71924100 @default.
• W2044285724 hasConceptScore W2044285724C7959160 @default.
• W2044285724 hasConceptScore W2044285724C86803240 @default.
• W2044285724 hasIssue "2" @default.
• W2044285724 hasLocation W20442857241 @default.
• W2044285724 hasOpenAccess W2044285724 @default.
• W2044285724 hasPrimaryLocation W20442857241 @default.

• next