English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Tools annual

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Presents the access of premium content as premium feature

Premium Content

Global: Zendy Plus annual

Global: Zendy Free Plan

Já foi verificado anteriormente que certos solos do Estado de São Paulo apresentam os elementos Ca, Mg e K em formas "fixas", isto é, não trocáveis. Procurou-se neste trabalho estudar o comportamento dessas bases, frente a diversas concentrações do extrator HNQ3, desde 0,005 N até 2,000 N, comparando os resultados com os obtidos para diversos volumes do extrator acetato de amônio 1 N, pH 7. Os dados experimentais indicam que o extrator ácido retira as mesmas quantidades dos elementos Ca, Mg e K que o acetato de amônio e as variações encontradas para as diversas concentrações de HNO3 são as mesmas encontradas para volumes diferentes do acetato de amônio. Confirma-se portanto, que nos extratores ácidos são determinados os elementos trocáveis do solo. As formas "fixas" dos citados elementos são bastante resistentes à sua remoção, não sendo atacadas por ácidos à concentração 2 N. Sendo a nutrição mineral das plantas, relativamente ao Ca, Mg e K, baseada na troca com o complexo ou com a solução do solo, e não se aceitando que os vegetais possam criar condições mais enérgicas que o HNO3 2 N para solubilização das formas "fixas", conclui-se que essa nutrição só se processe através das bases trocáveis do solo. Por fim, estudam-se as variações dos teores em bases obtidas pelos extratores ácidos para solos de diversas formações geológicas e compara-se com os teores determinados pelo acetato de amônio. Some soils of the state of São Paulo possess a certain amount of bases that cannot be considered as exchangeable. The behavior of exchangeable and non-exchangeable bases in some soil types was studied by means of cation extraction with nitric acid solutions of the following concentrations: 0.005 N, 0.01 N, 0.05 N, 0.075 N, 0. 5N, 1 N, and 2 N. The exchangeable cations in the samples were determined by leaching the soil with normal ammonium acetate at pH 7, using for aliquots of the same samples 100, 200, 300, and 400 ml of the solution. Various soil types were used in these studies, including the latosols, red-yellow podzolic, and "terra-roxa", all with low content of bases. The results obtained permit the following conclusions: a) all concentrations of nitric acid tried removed the same amount of bases as was removed by the ammonium acetate method; the content variation leached by the nitric acid was identical for any volume of ammonium acetate used; b) it was confirmed that acid solutions may be employed for the determination of bases in semi-tropical soils as those of the state of São Paulo; c) non-exchangeable bases were not affected by acid solutions as strong as 2 N; d) the exchangeable property is characteristic and remains constant over a large range of acid solution concentrations; e) since the uptake of bases by plants is considered an exchange phenomenon and it is hard to conceive that plant roots may create more energetic conditions than those resulting from 2 N nitric acid treatment, it is assumed that only exchangeable bases in these soils are available for plant absorption. The amount of individual exchangeable bases is thus critical for the study of soil fertility

Bases do solo e seu comportamento frente a extratores ácidos