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  <titleInfo>
    <title>Potassium availability in Brazilian semiarid soils cultivated with melon</title>
  </titleInfo>
  <name type="personal">
    <namePart>Paiva, Kariolania Fortunato de</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Severo, Pedro Jorge da Silva</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Oliveira, Flávio Sarmento de</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Soares, Lauriane Almeida dos Anjos</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <name type="personal">
    <namePart>Araujo, Josinaldo Lopes</namePart>
    <role>
      <roleTerm authority="marcrelator" type="text">creator</roleTerm>
    </role>
  </name>
  <typeOfResource>text</typeOfResource>
  <genre authority="marc">periodical</genre>
  <genre authority="marc">abstract or summary</genre>
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    <issuance>continuing</issuance>
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    <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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  <abstract>

ABSTRACT - Haplic  Vertisols  and  Typic  Quartzipsamments  are  among the main classes of soils used for melon production in the Brazilian semiarid region. Potassium (K) is the nutrient most extracted by yellow melon fruits and, for this reason, high doses of potassium fertilizers are often applied to these soils. This study aimed to evaluate potassium fractions in soils of the Brazilian semiarid region, during the cultivation cycle of fertigated yellow melon.  Two  experiments  were  carried  out  with  two  types  of  soil  (Haplic  Vertisol  and  Typic  Quartzipsamment).  For  the  Vertisol, a 7 x 2 [seven evaluation periods and two soil layers (0-20 cm and 20-40 cm)] factorial arrangement was established, with four replications, totaling 56 experimental units. For the Quartzipsamment, a 9 x 2 [nine collection times and two soil layers (0-20 cm and 20-40 cm)] factorial arrangement was used, with four replications, totaling 72 experimental units. The non-exchangeable K fraction was dominant in both soils, mainly in the 0-20 cm layer, and represents an important reserve of this nutrient for melon cultivation, especially in Haplic Vertisols. The decrease in the concentrations of the soluble and exchangeable forms and the increase in the non-exchangeable form indicated an increase in the fixation of this nutrient, by fixation in the Vertisol and leaching in the Quartzipsamment, at the end of the melon cycle, when the amount of K accumulated by the plant  was lower.


KEYWORDS: Cucumismelo,  exchangeable  potassium,  potassium leaching.</abstract>
  <abstract>

RESUMO - Disponibilidade de potássio em solos da região semiárida do Brasil cultivados com melão - Vertissolos  Háplicos  e  Neossolos  Quartizarênicos  estão  entre  as  principais  classes  de  solos  utilizadas  para  a  produção  de  melão, na região semiárida do Brasil. O potássio (K) é o nutriente mais extraído pelos frutos de melão amarelo; por isso, nesses solos,sãofrequentemente aplicadas altas doses de fertilizantes potássicos. Objetivou-se avaliar as frações de K em solos da região semiárida do Brasil, durante o ciclo de cultivo do melão amarelo fertirrigado. Dois  experimentos  foram  conduzidos  em  duas  classes  de  solo  (Vertissolo Háplico e Neossolo Quartzarênico). Para o Vertissolo, os tratamentos compreenderam arranjo fatorial 7 x 2 [sete períodos de avaliação e duas camadas de solo (0-20 cm e 20-40 cm)], com quatro repetições, totalizando 56 unidades experimentais. Para o Neossolo, os tratamentos compreenderam arranjo fatorial 9 x 2 [nove épocas de coleta e duas camadas de solo (0-20 cm e 20-40 cm)], com quatro repetições, totalizando 72 unidades experimentais. A fração K não trocável foi dominante em ambos os solos, principalmente na camada de 0-20 cm, e representa importante reserva desse nutriente para o cultivo de melão, principalmente no Vertissolo. A diminuição nas concentrações das formas solúvel e trocável e o aumento da forma não trocável indicaram aumento na fixação desse nutriente, por fixação no Vertissolo e lixiviação no Neossolo, ao final do ciclo do melão, quando a quantidade de K acumulada pela planta foi menor.


PALAVRAS-CHAVE: Cucumismelo,  potássio  trocável,  lixiviação de potássio.</abstract>
  <note>
Publicação online; 28 ref.; 3 tables; Summaries (En, Pt)</note>
  <subject>
    <topic>MELÃO</topic>
  </subject>
  <subject>
    <topic>ANÁLISE DO SOLO</topic>
  </subject>
  <subject>
    <topic>FERTILIZANTE POTÁSSICO</topic>
  </subject>
  <subject>
    <topic>PRODUÇÃO VEGETAL</topic>
  </subject>
  <subject>
    <topic>FERTILIDADE DO SOLO</topic>
  </subject>
  <relatedItem type="host">
    <titleInfo>
      <title>Pesquisa Agropecuária Tropical (Brazil)</title>
    </titleInfo>
    <originInfo>
      <publisher>Goiânia-GO UFG. Escola de Agronomia 1999</publisher>
    </originInfo>
    <identifier>2024-3998</identifier>
    <identifier type="issn">1517-6398</identifier>
    <identifier type="local">BR2024003183</identifier>
    <part>
      <text>v. 50 p. 1-8; (2020)</text>
    </part>
  </relatedItem>
  <identifier type="uri">https://revistas.ufg.br/pat/article/view/63663/35538</identifier>
  <location>
    <url>https://revistas.ufg.br/pat/article/view/63663/35538</url>
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    <recordContentSource authority="marcorg">BR-BrBNA</recordContentSource>
    <recordCreationDate encoding="marc">241108</recordCreationDate>
    <recordChangeDate encoding="iso8601">20241108114150.0</recordChangeDate>
    <languageOfCataloging>
      <languageTerm authority="iso639-2b" type="code">eng</languageTerm>
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