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Comparison of sources with different solubilities for Mn supply and retranslocation along with soybean development
Journal of Plant Nutrition ( IF 2.1 ) Pub Date : 2021-06-28 , DOI: 10.1080/01904167.2021.1943437
Rafaela Alenbrant Migliavacca 1 , Marcos Henrique Feresin Gomes 2 , Risely Ferraz-Almeida 1 , Eduardo de Almeida 2 , José Lavres 3 , Hudson Wallace Pereira de Carvalho 2 , Rafael Otto 1
Affiliation  

Abstract

Foliar sprays with micronutrients are widely employed in agricultural production as an alternative to improve soil fertilization and plant nutritional status. We hypothesized that less water-soluble sources of manganese (Mn; MnCO3) could serve as a slow-release source compared to a water-soluble source (MnSO4.H2O). Our goal here was to evaluate Mn-sources (MnSO4.H2O and MnCO3) and rates (150; 250; 350; and 450 g ha−1) sprayed in the 3rd and 4th trifoliate leaflets of soybean growing in clayey and sandy soil under controled conditions. In phenological stages V7 (vegetative period) and R1 (reproductive period), dry matter, height, the diameter of the stem, and Mn-content in the shoot, stem, and in the trifoliate leaflets were determined. Results showed that the application of Mn resulted in an augmented Mn-content in the 3rd and 4th trifoliate leaflets (sandy) and the 3rd and 5th trifoliate (clayey). The MnSO4.H2O promoted Mn-retranslocation from the 3rd/4th trifoliate to the stem and the 5th/6th trifoliate. However, MnCO3 was accumulated in the 3rd/4th trifoliate. The Mn-rates presented a linear response in sandy soil and quadratic response in clayey soil. Clayey soil was characterized by the higher Mn-contents in the stem, while sandy soil presented the higher Mn-contents in the 3rd, 4th, 5th, and 6th trifoliate. Our results suggest that MnSO4.H2O is more effective in increasing Mn-content in soybean leaves during plant development due to the Mn-retranslocation to sink organs (5th/6th trifoliate leaflets and shoot).



中文翻译:

不同溶解度的锰供应来源比较以及大豆发育过程中的再转移

摘要

含有微量营养素的叶面喷洒广泛用于农业生产,作为改善土壤施肥和植物营养状况的替代方法。我们假设与水溶性来源 (MnSO 4 .H 2 O)相比,水溶性较差的锰来源 (Mn; MnCO 3 ) 可用作缓释来源。我们的目标是评估在第 34喷洒的Mn 源(MnSO 4 .H 2 O 和 MnCO 3)和比率(150;250;350;和 450 g ha -1在受控条件下在粘土和沙质土壤中生长的大豆的三叶小叶。在物候阶段 V7(营养期)和 R1(繁殖期),干物质、高度、茎的直径和枝条、茎和三叶小叶中的锰含量被确定。结果表明,Mn的应用导致了3增强Mn含量和4枳小叶(沙)和3和5枳(粘质)。所述的MnSO 4 ·H 2 ö从促进锰retranslocation 3/ 4枳到杆和5/ 6枳。然而,锰3积累在第 3/4三叶中。Mn 比率在砂质土壤中呈线性响应,在粘土中呈二次响应。粘质土壤的特点是在茎高锰含量,而砂土在3呈现的更高的Mn-内容RD,4,5及6枳。我们的结果表明,MnSO 4 .H 2 O 在植物发育过程中更有效地增加大豆叶片中的 Mn 含量,这是由于 Mn 重新转移到汇器官(5/6三叶小叶和枝条)。

更新日期:2021-06-28
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