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  <titleInfo>
    <title>Carbono, Nitrogênio, Abundância Natural de Δ13C e Δ15N do Solo sob Sistemas Agroflorestais</title>
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  <name type="personal">
    <namePart>Couto, Wanderson Henrique</namePart>
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  <name type="personal">
    <namePart>Anjos, Lúcia Helena Cunha dos</namePart>
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    </role>
  </name>
  <name type="personal">
    <namePart>Pereira, Marcos Gervasio</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Guareschi, Roni Fernandes</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Assunção, Shirlei Almeida</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Wadt, Paulo Guilherme Salvador</namePart>
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    </role>
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  <abstract>

RESUMO

O objetivo deste trabalho foi avaliar alterações nos teores de C e N e abundância natural de
δ13C e δ15N de um Cambissolo Háplico Tb distrófico em uma área com sistema agroflorestal (SAF).
Em cada área de estudo foram coletadas amostras de solo, em 8 profundidades de 0,0–1,0 m.
O delineamento experimental utilizado foi o inteiramente casualizado, em esquema de parcelas
subdivididas 2 × 8 (2 áreas florestais e 8 profundidades), com três repetições. Com exceção da
camada superficial do solo (0,0-0,10), a área de SAF está preservando os teores de C e aumentando
os teores de N (0,2-1,0) em relação à mata nativa. Ambas as áreas avaliadas apresentaram sinais
de abundância natural de δ13C referente a plantas do ciclo fotossintético C3, e a área de mata
nativa apresentou nas camadas superficiais (0,0-0,20) maiores valores de δ15N, demonstrando
maior decomposição da matéria orgânica.

Palavras-chave: reflorestamento, matéria orgânica do solo, Cambissolo.





Carbon, Nitrogen, and Natural Abundance Of Δ13C and Δ15N of Soils Under Agroforestry Systems

ABSTRACT

The aim of this study was to evaluate changes in C and N levels and in the natural abundance
of δ15N and δ13C of a Inceptisol in an agroforestry system (AFS). Soil samples were collected
from eight depth levels from 0.0-1.0 m in each studied area. The experiment was carried out in a
completely randomized 2 × 8 (2 forest areas and 8 depths) split-plot design with three replications.
Except for the topsoil (0.0-0.10), the area of this AFS has preserved content of C and increased
level of N (0.2-1.0) compared to the Forest. Both areas showed signs of natural abundance
of δ13C in plants with C3 photosynthetic pathway, and the forest area presented higher values
of δ15N in the superficial layers (0.0-0.20), indicating greater decomposition of organic matter.

Keywords: reforestation, soil organic matter, Inceptisol.</abstract>
  <note>Publicação on-line; 33 ref.; 1 table; 4 illus.; Summaries (En, Pt)</note>
  <subject>
    <topic>REFLORESTAMENTO</topic>
  </subject>
  <subject>
    <topic>MATÉRIA ORGÂNICA</topic>
  </subject>
  <subject>
    <topic>SOLO</topic>
  </subject>
  <subject>
    <topic>CAMBISSOLO</topic>
  </subject>
  <relatedItem type="host">
    <titleInfo>
      <title>Floresta e Ambiente (Brazil)</title>
    </titleInfo>
    <originInfo>
      <publisher>Rio de Janeiro-RJ Instituto de Florestas - UFRRJ 1994</publisher>
    </originInfo>
    <identifier>2025-0444</identifier>
    <identifier type="issn">1415-0980  /  ISSN 2179-8087 0nline</identifier>
    <identifier type="local">BR2026000242</identifier>
    <part>
      <text>v. 24 p. 1-8; (2017)</text>
    </part>
  </relatedItem>
  <identifier type="uri">https://www.scielo.br/j/floram/a/WRbDJwYnfq9RGvpJdXvM8Jm/?format=pdf&amp;lang=pt</identifier>
  <location>
    <url>https://www.scielo.br/j/floram/a/WRbDJwYnfq9RGvpJdXvM8Jm/?format=pdf&amp;lang=pt</url>
  </location>
  <recordInfo>
    <recordContentSource authority="marcorg">BR-BrBNA</recordContentSource>
    <recordCreationDate encoding="marc">260319</recordCreationDate>
    <recordChangeDate encoding="iso8601">20260319170941.0</recordChangeDate>
    <languageOfCataloging>
      <languageTerm authority="iso639-2b" type="code">por</languageTerm>
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