FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2805538718> ?p ?o ?g. }

• W2805538718 endingPage "174" @default.
• W2805538718 startingPage "164" @default.
• W2805538718 abstract "Soil organic carbon (SOC) is the main terrestrial carbon (C) reservoir. Land use change has depleted SOC stocks and released large amounts of C dioxide (CO2). Thus, the development of reliable tools for SOC stock monitoring at large scale is fundamental to face climate change. Argentinean Semiarid Chaco (ASC) is a deforestation hotspot, but CO2 emissions from soil has been barely assessed. Deforested area was converted into cropland or grassland. We used empirical data to model SOC stocks under native forest (SOCref) and the RothC model to estimate SOC stock change factors under cropland (Fc) and grasslands (Fg) in the ASC. These SOCref's and stock change factors were applied in a Tier 2 (T2) C inventory, following the Intergovernmental Panel on Climate Change (IPCC) proposal. We used SOC vertical distribution models to estimate SOC stock at 0–100 cm soil depth from estimated SOC stocks at 0–30 cm, the default soil depth of IPCC C inventory method. The T2 was run for 1976 through 2012 and under three hypothetical land use change scenarios for 2012 through 2032. The scenarios were: i) land use change ceases, ii) land use change rate is the half of 1996–2012 land use change rate, and iii) land use change rate remains as in 1996–2012. Estimated average SOCref stock at 0–30 cm soil depth was 40 Mg C ha−1 and varied between 35 and 51 Mg C ha−1. Cropland was the main fate of deforested area and the land use with lower SOC stocks. Stock change factors and SOC stocks estimated with T2 were within the range of the empirical data reported in the ASC. However, research about SOC dynamics and land use change is incipient in the ASC and more empirical information is needed to validate T2 estimations. Deforestation in the ASC leads to high CO2 emissions from soil and the only scenario in which those emissions would be reduced is with deforestation cessation. Soil depth considered in greenhouse gas inventories is 0–30 cm, and this strongly underestimates CO2 emissions. We demonstrated that this limitation could be overcome by using SOC vertical distribution models to estimate deep SOC stock (up to 1 m) from estimated surface SOC stock. Hence, these models could be used to improve CO2 estimations from SOC inventories." @default.
• W2805538718 created "2018-06-13" @default.
• W2805538718 creator A5042219940 @default.
• W2805538718 creator A5043256658 @default.
• W2805538718 creator A5090306071 @default.
• W2805538718 date "2018-10-01" @default.
• W2805538718 modified "2023-10-11" @default.
• W2805538718 title "Greenhouse gas inventories: Deriving soil organic carbon change factors and assessing soil depth relevance in Argentinean Semiarid Chaco" @default.
• W2805538718 cites W135029258 @default.
• W2805538718 cites W136628441 @default.
• W2805538718 cites W1510917207 @default.
• W2805538718 cites W1810287876 @default.
• W2805538718 cites W1964700776 @default.
• W2805538718 cites W1971802656 @default.
• W2805538718 cites W1981213426 @default.
• W2805538718 cites W1988543491 @default.
• W2805538718 cites W1993923136 @default.
• W2805538718 cites W1994228237 @default.
• W2805538718 cites W1995864896 @default.
• W2805538718 cites W2022485409 @default.
• W2805538718 cites W2029338493 @default.
• W2805538718 cites W2029837710 @default.
• W2805538718 cites W2034443885 @default.
• W2805538718 cites W2037739663 @default.
• W2805538718 cites W2038044415 @default.
• W2805538718 cites W2051302738 @default.
• W2805538718 cites W2052289430 @default.
• W2805538718 cites W2056194497 @default.
• W2805538718 cites W2060016601 @default.
• W2805538718 cites W2060492176 @default.
• W2805538718 cites W2062515295 @default.
• W2805538718 cites W2063248444 @default.
• W2805538718 cites W2066537743 @default.
• W2805538718 cites W2068012521 @default.
• W2805538718 cites W2079201579 @default.
• W2805538718 cites W2079389364 @default.
• W2805538718 cites W2081527758 @default.
• W2805538718 cites W2082323515 @default.
• W2805538718 cites W2084811085 @default.
• W2805538718 cites W2086901441 @default.
• W2805538718 cites W2090602773 @default.
• W2805538718 cites W2108744281 @default.
• W2805538718 cites W2124723853 @default.
• W2805538718 cites W2137810942 @default.
• W2805538718 cites W2146450953 @default.
• W2805538718 cites W2151303612 @default.
• W2805538718 cites W2166135450 @default.
• W2805538718 cites W2167869741 @default.
• W2805538718 cites W2173110961 @default.
• W2805538718 cites W2174069807 @default.
• W2805538718 cites W2185527555 @default.
• W2805538718 cites W2203223705 @default.
• W2805538718 cites W2432068731 @default.
• W2805538718 cites W2527030653 @default.
• W2805538718 cites W2945972236 @default.
• W2805538718 doi "https://doi.org/10.1016/j.catena.2018.05.041" @default.
• W2805538718 hasPublicationYear "2018" @default.
• W2805538718 type Work @default.
• W2805538718 sameAs 2805538718 @default.
• W2805538718 citedByCount "8" @default.
• W2805538718 countsByYear W28055387182019 @default.
• W2805538718 countsByYear W28055387182020 @default.
• W2805538718 countsByYear W28055387182022 @default.
• W2805538718 crossrefType "journal-article" @default.
• W2805538718 hasAuthorship W2805538718A5042219940 @default.
• W2805538718 hasAuthorship W2805538718A5043256658 @default.
• W2805538718 hasAuthorship W2805538718A5090306071 @default.
• W2805538718 hasBestOaLocation W28055387181 @default.
• W2805538718 hasConcept C100970517 @default.
• W2805538718 hasConcept C122690726 @default.
• W2805538718 hasConcept C127313418 @default.
• W2805538718 hasConcept C132651083 @default.
• W2805538718 hasConcept C159390177 @default.
• W2805538718 hasConcept C159750122 @default.
• W2805538718 hasConcept C166957645 @default.
• W2805538718 hasConcept C187320778 @default.
• W2805538718 hasConcept C18903297 @default.
• W2805538718 hasConcept C199360897 @default.
• W2805538718 hasConcept C204036174 @default.
• W2805538718 hasConcept C205649164 @default.
• W2805538718 hasConcept C22884784 @default.
• W2805538718 hasConcept C2775835988 @default.
• W2805538718 hasConcept C2777399953 @default.
• W2805538718 hasConcept C2994081031 @default.
• W2805538718 hasConcept C39432304 @default.
• W2805538718 hasConcept C39464130 @default.
• W2805538718 hasConcept C41008148 @default.
• W2805538718 hasConcept C47737302 @default.
• W2805538718 hasConcept C4792198 @default.
• W2805538718 hasConcept C509746633 @default.
• W2805538718 hasConcept C530467964 @default.
• W2805538718 hasConcept C6557445 @default.
• W2805538718 hasConcept C76886044 @default.
• W2805538718 hasConcept C86803240 @default.
• W2805538718 hasConcept C97137747 @default.
• W2805538718 hasConceptScore W2805538718C100970517 @default.
• W2805538718 hasConceptScore W2805538718C122690726 @default.
• W2805538718 hasConceptScore W2805538718C127313418 @default.

• next