Effect of liming in plinthic and petroplinthic soils for soybean cultivation in the Brazilian Savanna

Olavo da Costa Leite, J. Luz, S. D. O. Lima, Rubens Ribeiro da Silva, R. R. Fidelis, Carmen Maria Coimbra Manhães, J. Peluzio, Osvaldo José Ferreira Júnior, Mauro Gomes dos Santos, Ismael de Oliveira Pinto, Renisson Neponuceno de Araújo Filho, Allan Deyvid Pereira da Silva, Jader Nunes Cachoeira, G. N. Scheidt
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Abstract

Agricultural expansion is advancing on marginal soils (Plinthic soils), but the liming recommendation for this soil, especially for soybean cultivation, remains unknown. This study aimed to evaluate soybean (Glycine max) responses to limestone doses in concretionary soils (plinthic and/or petroplinthic). The experiment was carried out in the greenhouse, in randomized blocks, with four soil types and six limestone doses (4x6 factorial scheme), with four replicates. Soils were: RYO: Red-Yellow Oxisols; CPP-29, CPP-72, CPP-82 corresponds to the Concretionary Petric Plinthosol with 29, 72, and 82% concretions, respectively. Limestone doses varied from 0 to 4 times for each soil, based on the recommendation of regional bulletins. Soil temperature, crop emergence, development, and soybean yield characteristics were evaluated. Results were evaluated by ANOVA, followed by the LSD test or polynomial regression adjustment (p ≤ 0.05). Soybean response to liming varied with soil types. Seedlings showed lower vigor in Plinthic soils with plinthite contents ≥72%. These soils showed higher thermal accumulation (°C), and this increase showed a strong negative correlation with soybean development and reproductive characteristics. Evidence of liming response was observed after crop stage V5. Limestone substantially improved soybean growth and development in Plinthic soils with high plinthite levels, although they had lower yield potential than low plinthite levels and Oxisol. In general, the maximum response of the crop occurred at doses ~2 times higher than that practiced in the Brazilian Savanna region, especially in Plinthic soils
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在巴西热带稀树草原种植大豆的基质土和岩石基质土中施用石灰的效果
贫瘠土壤(洼地土壤)的农业扩张正在推进,但这种土壤的石灰化建议,尤其是大豆种植的石灰化建议,仍是未知数。本研究旨在评估大豆(Glycine max)对砂礓土(lininthic 和/或 petroplinthic)中石灰石剂量的反应。实验在温室中进行,采用随机区组,有四种土壤类型和六种石灰石剂量(4x6因子方案),四次重复。土壤类型为RYO:红黄色氧化物土壤;CPP-29、CPP-72 和 CPP-82 分别对应于凝结岩质石灰质基质土壤,凝结度分别为 29%、72% 和 82%。根据地区公报的建议,每种土壤的石灰石剂量从 0 到 4 倍不等。对土壤温度、作物出苗、生长发育和大豆产量特征进行了评估。评估结果采用方差分析,然后进行 LSD 检验或多项式回归调整(p ≤ 0.05)。大豆对施用石灰的反应因土壤类型而异。在磷灰石含量≥72%的磷酸盐土壤中,幼苗的活力较低。这些土壤的热积累(℃)较高,热积累的增加与大豆的生长发育和繁殖特性呈强烈的负相关。在作物第 V5 阶段之后,观察到了石灰化反应的证据。石灰岩极大地改善了高磷酸盐土壤中大豆的生长和发育,尽管其产量潜力低于低磷酸盐土壤和 Oxisol 土壤。一般来说,作物的最大反应发生在比巴西热带稀树草原地区高出约 2 倍的剂量上,尤其是在普林西岩土壤中。
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