Phosphorus Dynamics in Stressed Soil Systems: Is There a Chemical and Biological Compensating Effect?

Stresses Pub Date : 2024-04-02 DOI:10.3390/stresses4020015
Bruna Arruda, Fábio Prataviera, W. F. Bejarano Herrera, Denise de Lourdes Colombo Mescolotti, Antonio Marcos Miranda Silva, H. W. Pereira de Carvalho, P. Pavinato, Fernando Dini Andreote
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Abstract

Here, we hypothesized the occurrence of a compensatory relationship between the application of P and different microbial communities in the soil, specifically in relation to the chemical and biological effects in the soil–plant–microorganisms’ interaction. We aimed to evaluate the plant–microbiota responses in plants grown in soils hosting distinct microbial communities and rates of P availability. Two experiments were carried out in a greenhouse. The first experiment evaluated four manipulated soil microbiome compositions, four P rates, and two plant species. Manipulated soil systems were obtained by the following: (i) autoclaving soil for 1 h at 121 °C (AS); (ii) inoculating AS with soil suspension dilution (AS + 10−3); (iii) heating natural soil at 80 °C for 1 h (NH80); or (iv) using natural soil (NS) without manipulation. The P rates added were 0, 20, 40, and 60 mg kg−1, and the two plant species tested were grass (brachiaria) and leguminous (crotalaria). Inorganic labile P (PAER), microbial P (PMIC), acid phosphatase activity (APASE), and shoot P uptake (PUPT) were assessed for each system. Brachiaria presented a compensatory effect for PUPT, whereby the addition of P under conditions of low microbial community enhanced P absorption capacity from the soil. However, in a system characterized by low P input, the increase in the soil biodiversity was insufficient to enhance brachiaria PUPT. Likewise, crotalaria showed a higher PUPT under high P application and low microbial community. The second experiment used three manipulated microbiome compositions: AS + 10−3; NH80; and NS and three P rates added: 0, 20, and 40 mg kg−1. In addition, two treatments were set: without and with mycorrhiza inoculation. Brachiaria showed an increase in the PUPT under low microbial communities (AS + 10−3; NH80) with P addition (20 and 40 mg kg−1 of P), but no mycorrhization was observed. In the undisturbed microbial community (NS), under no P input (0 mg kg−1 of P), brachiaria showed low mycorrhization and low PUPT. Finally, NS and the recommended P input (40 mg kg−1 of P) represented a balance between chemical and biological fertility, promoting the equilibrium between mycorrhization and PUPT.
压力土壤系统中的磷动态:是否存在化学和生物补偿效应?
在此,我们假设施用磷与土壤中不同的微生物群落之间存在一种补偿关系,特别是与土壤-植物-微生物相互作用中的化学和生物效应有关。我们的目的是评估在具有不同微生物群落和钾供应率的土壤中生长的植物的植物微生物群反应。我们在温室中进行了两项实验。第一项实验评估了四种受操纵的土壤微生物群组成、四种钾利用率和两种植物物种。操纵土壤系统是通过以下方法获得的:(i) 将土壤在 121 °C 下高压灭菌 1 小时(AS);(ii) 在 AS 中接种土壤悬浮稀释液(AS + 10-3);(iii) 将天然土壤在 80 °C 下加热 1 小时(NH80);或 (iv) 使用天然土壤(NS),不加任何处理。添加的磷比率分别为 0、20、40 和 60 毫克/千克,测试的两种植物物种分别为禾本科植物(箭竹)和豆科植物(羊角豆)。对每个系统的无机可溶性钾(PAER)、微生物钾(PMIC)、酸性磷酸酶活性(APASE)和嫩枝钾吸收量(PUPT)进行了评估。婆婆纳呈现出 PUPT 的补偿效应,即在微生物群落较低的条件下添加 P 可提高从土壤中吸收 P 的能力。然而,在一个以低钾输入为特征的系统中,土壤生物多样性的增加不足以提高帚石楠的钾吸收能力。同样,在高P施用量和低微生物群落条件下,牛筋草显示出更高的PUPT。第二个实验使用了三种受控微生物群组成:AS + 10-3、NH80 和 NS,以及三种磷添加率:0、20 和 40 毫克/千克。此外,还设置了两种处理:不接种菌根和接种菌根。在低微生物群落(AS + 10-3;NH80)条件下,添加 P(20 和 40 毫克/公斤-1 的 P)后,巴西蘑菇的 PUPT 有所提高,但没有观察到菌根。在未受干扰的微生物群落(NS)中,在无 P 投入(0 毫克/千克 P)的情况下,箭毒草的菌根化程度低,PUPT 也低。最后,NS 和建议的 P 输入量(40 毫克/千克 P)代表了化学肥力和生物肥力之间的平衡,促进了菌根和 PUPT 之间的平衡。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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