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Registro Completo |
Biblioteca(s): |
Embrapa Pantanal. |
Data corrente: |
01/10/1997 |
Data da última atualização: |
05/04/2017 |
Autoria: |
YONKER, C. M.; SCHIMEL, D. S.; PAROUSSIS, E.; HEIL, R. D. |
Título: |
Patterns of organic carbon accumulation in a semiarid shortgrass steppe, Colorado. |
Ano de publicação: |
1988 |
Fonte/Imprenta: |
Soil Science Society of America Journal, v.52, n.2, p.478-483, 1988. |
Idioma: |
Inglês |
Conteúdo: |
Organic C accumulation was measured along an 8-km transect at a site in the semiarid shortgrass steppe of northeastern Colorado. Specific objectives of the study were to (i) measure the quantity and distribution of organic C across toposequences, (ii) test the hypothesis that a disproportionate amount of soil organic C residues in the lowlands (as defined herein), and (iii) assess the role of geomorphic history as determinant of compensatory rates of biochemical organic C transformations. Resulkts of the study showed the surface (A) horizon organic C concentration did not vary systematically among slope postiions of a give toposequences. Similarly, the mass of organic C within the surface meter of soil often did not increase with decreasing elevation across a toposequence. Mass of organic C was found to range from 2.5 kg m-3 on terrace escarpments to 10.7 kg m-3 on sandy uplands. The mass of organic C, as calculated to the BCk horizon, was highest in the lowlands. The mass of buried organic C, as calculated uniformly for a 50-cm thickness of material, represents 17% of the total organic C estimate for the site. In spite of buried soils, lowlands did not contain a disproportionate amount of total landscape organic C. |
Palavras-Chave: |
Biogeoquimica; Geomorphic history; Toposequence. |
Thesagro: |
Matéria Orgânica; Solo. |
Thesaurus Nal: |
biogeochemistry; buried soils. |
Categoria do assunto: |
-- |
Marc: |
LEADER 01909naa a2200241 a 4500 001 1791836 005 2017-04-05 008 1988 bl --- 0-- u #d 100 1 $aYONKER, C. M. 245 $aPatterns of organic carbon accumulation in a semiarid shortgrass steppe, Colorado. 260 $c1988 520 $aOrganic C accumulation was measured along an 8-km transect at a site in the semiarid shortgrass steppe of northeastern Colorado. Specific objectives of the study were to (i) measure the quantity and distribution of organic C across toposequences, (ii) test the hypothesis that a disproportionate amount of soil organic C residues in the lowlands (as defined herein), and (iii) assess the role of geomorphic history as determinant of compensatory rates of biochemical organic C transformations. Resulkts of the study showed the surface (A) horizon organic C concentration did not vary systematically among slope postiions of a give toposequences. Similarly, the mass of organic C within the surface meter of soil often did not increase with decreasing elevation across a toposequence. Mass of organic C was found to range from 2.5 kg m-3 on terrace escarpments to 10.7 kg m-3 on sandy uplands. The mass of organic C, as calculated to the BCk horizon, was highest in the lowlands. The mass of buried organic C, as calculated uniformly for a 50-cm thickness of material, represents 17% of the total organic C estimate for the site. In spite of buried soils, lowlands did not contain a disproportionate amount of total landscape organic C. 650 $abiogeochemistry 650 $aburied soils 650 $aMatéria Orgânica 650 $aSolo 653 $aBiogeoquimica 653 $aGeomorphic history 653 $aToposequence 700 1 $aSCHIMEL, D. S. 700 1 $aPAROUSSIS, E. 700 1 $aHEIL, R. D. 773 $tSoil Science Society of America Journal$gv.52, n.2, p.478-483, 1988.
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121. | ![Imagem marcado/desmarcado](/consulta/web/img/desmarcado.png) | PASTORE, J. F. B.; CAVALCANTI, T. B. Polygalaceae. In: CAVALCANTI, T. B.; RAMOS, A. E. (Org.). Flora do Distrito Federal, Brasil. Brasília, DF: Embrapa Recursos Genéticos e Biotecnologia, 2006. v. 5. p.109-179.Tipo: Capítulo em Livro Técnico-Científico | Circulação/Nível: -- - -- |
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