1941
DOI: 10.1590/s0006-87051941000500001
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Avaliação da fertilidade do solo

Abstract: A-fim-de deduzir os tratamentos físicos e químicos do solo, os mais econômicos e eficientes na produção agrícola de acôrdo com as condições locais e as necessidades da cultura, foram feitos trabalhos de campo e de laboratório segundo os métodos da Secção de Solos dêste Instituto. A região estudada abrange cêrca de 10 km² de solos arenosos e pobres, situados numa zona limítrofe de duas formações geológicas pouco estudadas sob o ponto de vista agrícola. A cultura em questão é tungue (Aleurites fordii Hemsley.) E… Show more

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Cited by 15 publications
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“…The pH is one of the main indicators of soil fertility and is responsible for the adsorption and desorption reactions of chemical elements in the soil solution (Raij, 1983). Low pH conditions indicate a low availability of Ca 2+ , Mg 2+ , and K + that make up EB, which explains the positive correlation between pH and EB.…”
mentioning
confidence: 99%
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“…The pH is one of the main indicators of soil fertility and is responsible for the adsorption and desorption reactions of chemical elements in the soil solution (Raij, 1983). Low pH conditions indicate a low availability of Ca 2+ , Mg 2+ , and K + that make up EB, which explains the positive correlation between pH and EB.…”
mentioning
confidence: 99%
“…However, it is important to note the high correlation of this attribute with OM (0.89; p ≤ 0.001; Figure 2), mainly because there was a reduction of OM in the pasture environment, which contributed to reducing the CEC by approximately 0.7 cmol c dm -3 to levels considered low and medium, between 4.0 and 5.8 cmol c dm -3 . The CEC is an indicator of the potential of the soil to serve agricultural use and normally has values dependent on soil mineralogy and mainly on the OM in tropical soils (Raij, 1983). Low CEC values indicate that the soil retains few exchangeable bases, increasing the need for fertilization (Umasankareswari et al, 2022).…”
mentioning
confidence: 99%
“…1 Mq"'T No solo inicialmente eutrófico os valores de S foram diminuídos para todas as profundidades em conseqüência dos significativos decréscimos nos teores de cálcio, magnésio e potássio. Para RAIJ (1981), em culturas mais tolerantes à acidez, como é o caso da cana de açúcar, seria suficiente uma saturação por bases de 40%.…”
Section: Porosidadeunclassified