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  <leader>04313nab a2200337 i 4500</leader>
  <controlfield tag="003">BR-BrBNA</controlfield>
  <controlfield tag="005">20250604143924.0</controlfield>
  <controlfield tag="008">250604b2019    bl.ar|pooa||| 00| 0 por |</controlfield>
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    <subfield code="a">N20</subfield>
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    <subfield code="a">Ferreira, Raphael Leone da Cruz </subfield>
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    <subfield code="a">Sato, Michel Keisuke </subfield>
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    <subfield code="a">Rodrigues, Sueli</subfield>
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    <subfield code="a">Lima, Herdjania Veras de </subfield>
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    <subfield code="a">Teixeira, Orivan Maria Marques </subfield>
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  <datafield tag="245" ind1=" " ind2=" ">
    <subfield code="a">Tr&#xE1;fego de m&#xE1;quinas agr&#xED;colas em cultivo de palma de &#xF3;leo: implica&#xE7;&#xF5;es na qualidade f&#xED;sica do solo</subfield>
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Publica&#xE7;&#xE3;o online; 25 ref.; 3 illus.; 2 tables; Summaries (En, Pt)</subfield>
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RESUMO:    Embora a palma de &#xF3;leo seja cultivada em grande escala e em diferentes tipos de  solos  no  estado  do  Par&#xE1;,  mudan&#xE7;as  nas  propriedades  f&#xED;sicas  do  solo  nestas  &#xE1;reas  n&#xE3;o  v&#xEA;m sendo monitoradas. Assim, o objetivo do trabalho foi avaliar a qualidade f&#xED;sica de um Latossolo Amarelo cultivado com palma de &#xF3;leo ap&#xF3;s 30 anos de implanta&#xE7;&#xE3;o. Amostras de solo com estrutura deformada e indeformada foram coletadas nas profundidades de 0-20 e 20-40 cm, na zona de tr&#xE1;fego. O grau de compacta&#xE7;&#xE3;o (GC) foi calculado a partir da densidade m&#xE1;xima do solo obtida pelo teste de Proctor e sua resist&#xEA;ncia &#xE0; penetra&#xE7;&#xE3;o (RP) determinada em amostras equilibradas em dez potenciais matriciais. Influ&#xEA;ncia das mudan&#xE7;as temporais da umidade do solo na RP tamb&#xE9;m foram avaliadas. Os par&#xE2;metros GC e RP demonstraram que a &#xE1;rea avaliada apresenta compacta&#xE7;&#xE3;o. O GC nas duas profundidades ficou acima de 90% sendo mais intenso na camada de 0-20 cm. Por&#xE9;m, quando avaliado pela RP, o estado de compacta&#xE7;&#xE3;o foi mais evidente na camada de 20-40 cm e, as varia&#xE7;&#xF5;es na umidade do solo ao longo de um ano mostraram que nos meses mais secos o solo apresenta valores limitantes de RP nesta camada. Desta forma, este estudo indica que o crescimento e desenvolvimento da palma de &#xF3;leo pode estar sendo restringido pela compacta&#xE7;&#xE3;o e sobretudo pela elevada resist&#xEA;ncia &#xE0; penetra&#xE7;&#xE3;o nos meses de menor disponibilidade de &#xE1;gua. 


PALAVRAS-CHAVE:   Elaeis guineensis Jacq., Resist&#xEA;ncia do solo &#xE0; penetra&#xE7;&#xE2;o, Teste de Proctor, Grau de compacta&#xE7;&#xE3;o, Opera&#xE7;&#xF5;es mecanizadas</subfield>
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ABSTRACT:    Although oil palm is cultivated on a large scale and in different soil types in the state of Par&#xE1;, changes in the soil&#x2019;s physical properties in these areas have not been evaluated. Thus, the objective of this study was to evaluate the physical quality of a Yellow Latosol cultivated with oil palm, 30 years after implantation. Soil samples with disturbed and undisturbed structure were collected at 0-20 and 20-40 cm depths, in the machinery traffic zone. The degree of compaction (DC) was calculated from the maximum soil bulk density obtained by the Proctor test, and soil penetration resistance (PR) was determined in soil samples equilibrated in ten matric potentials. Temporal changes in soil moisture in PR were also evaluated. Both parameters showed that the evaluated area has an indication of compaction. The DC in both depths was above 90% and was more severe in the 0-20 cm layer. However, when evaluated by PR, the compaction was more evident in the 20-40 cm layer, and variations in soil moisture over a year showed that in the drier months, the soil showed high values of PR in this layer. Thus, this study indicates that the growth and development of oil palm may be restricted by the soil&#x2019;s compaction and mainly by the high penetration resistance in the months of reduced water availability.  


KEYWORDS:   Elaeis guineensis Jacq., Soil penetration resistance, Proctor test, Degree of compaction, Mechanized operations</subfield>
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  <datafield tag="650" ind1=" " ind2=" ">
    <subfield code="a">LATOSSOLO AMARELO</subfield>
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  <datafield tag="650" ind1=" " ind2=" ">
    <subfield code="a">AN&#xC1;LISE DO SOLO</subfield>
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  <datafield tag="650" ind1=" " ind2=" ">
    <subfield code="a">PROPRIEDADE F&#xCD;SICO-QU&#xCD;MICA</subfield>
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    <subfield code="a">PRENSAGEM</subfield>
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  <datafield tag="650" ind1=" " ind2=" ">
    <subfield code="a">M&#xC1;QUINA AGR&#xCD;COLA</subfield>
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    <subfield code="a">PAR&#xC1;</subfield>
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  <datafield tag="773" ind1="0" ind2=" ">
    <subfield code="0">3551</subfield>
    <subfield code="9">345997</subfield>
    <subfield code="d">Bel&#xE9;m-PA Faculdade de Ci&#xEA;ncias Agr&#xE1;rias do Par&#xE1; 1999</subfield>
    <subfield code="o">2024-6646</subfield>
    <subfield code="t">Revista de Ci&#xEA;ncias Agr&#xE1;rias (Brazil)</subfield>
    <subfield code="x">1517-591X Impresso/Vers&#xE3;o online ISSN 2177-8760</subfield>
    <subfield code="g">v. 62 p. 1-7; (2019)</subfield>
    <subfield code="w">BR2025001420</subfield>
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  <datafield tag="856" ind1=" " ind2=" ">
    <subfield code="u">https://ajaes.ufra.edu.br/index.php/ajaes/article/view/2979/1545</subfield>
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    <subfield code="c">ANA</subfield>
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    <subfield code="c">331895</subfield>
    <subfield code="d">331895</subfield>
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