土壤有机碳对欧洲谷物产量的积极影响降至 1.4

Ana Campos-Cáliz, Enrique Valencia, César Plaza, Gina Garland, Anna Edlinger, Chantal Herzog, Marcel G. A. van der Heijden, Samiran Banerjee, Matthias C. Rillig, Sara Hallin, Aurélien Saghaï, Fernando T. Maestre, David S. Pescador, Laurent Philippot, Ayme Spor, Sana Romdhane, Pablo García-Palacios
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引用次数: 0

摘要

引言 增加农田中的土壤有机碳 (SOC) 是一种自然的气候减缓措施,同时还能提高作物产量。然而,在广泛的气候、土壤和耕作梯度中,缺乏全面的实地研究来考察土壤有机碳对作物产量的影响。此外,人们对保水能力、土壤微生物多样性和养分供应如何调节 SOC 与作物产量之间的关系还知之甚少。 材料与方法 我们对欧洲南北梯度 3000 公里的 127 块谷物田进行了观察研究,测量了表层土壤(0-20 厘米)的有机碳含量,并收集了有关气候、土壤特性、作物产量和耕作方式的数据。此外,我们还探讨了部分地点三个土壤深度(0-20 厘米、20-40 厘米和 40-60 厘米)的作物产量、颗粒有机碳(POC)和矿质相关有机碳(MAOC)含量之间的关系。 结果 SOC 含量为 1.4% 时,相对产量增长趋于平稳,这表明欧洲梯度土壤中的 SOC 含量最适合谷物生长。即使控制了各国在气候、土壤和耕作方式上的巨大差异,SOC 与谷物产量之间的二次方关系仍然非常明显。这种关系在不同的土壤深度和不同的碳组分之间有很大的差异。MAOC 在 SOC 库中占主导地位,并与相对产量有显著关系,其最佳水平随土壤深度而变化。土壤微生物多样性和养分可用性是 SOC 与产量关系的主要驱动因素,而保水能力则没有明显的影响。 结论 我们的研究表明,SOC 是决定欧洲梯度谷物产量的关键因素,确定这一阈值可为土壤管理策略提供依据,从而根据初始 SOC 水平提高碳捕获量。尽管如此,SOC 与产量之间的复杂关系还是凸显了制定有针对性的土壤管理策略的必要性,这些策略应考虑到具体的地点条件,以优化碳储存和作物产量。
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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The Positive Effects of Soil Organic Carbon on European Cereal Yields Level Off at 1.4%

Introduction

Increasing soil organic carbon (SOC) in croplands is a natural climate mitigation effort that can also enhance crop yields. However, there is a lack of comprehensive field studies examining the impact of SOC on crop yields across wide climatic, soil, and farming gradients. Furthermore, it is largely unknown how water retention, soil microbial diversity, and nutrient availability modulate the SOC-crop yield relationship.

Materials and Methods

We conducted an observational study across 127 cereal fields along a 3000 km north-south gradient in Europe, measured topsoil (0–20 cm) organic C content, and collected data on climate, soil properties, crop yield and farming practices. Additionally, we explored the relationship between crop yield, particulate organic carbon (POC) and mineral-associated organic carbon (MAOC) contents at three soil depths (0–20, 20–40 and 40–60 cm) in a subset of sites.

Results

Relative yield increases levelled off at 1.4% SOC, indicating an optimal SOC content for cereals along a European gradient. The quadratic relationship between SOC and cereal yield was conspicuous even after controlling for large differences in climate, soil and farming practices across countries. The relationship varied significantly across soil depths and C fractions. MAOC dominated the SOC pool, and was significantly related to relative yield up to an optimal level that varied with soil depth. Soil microbial diversity and nutrient availability emerged as main drivers of the SOC-yield relationship, while water retention did not exhibit a notable influence.

Conclusions

Our study demonstrates that SOC is as a key determinant of cereal yield along a European gradient, and identifying this threshold can inform soil management strategies for improved carbon capture based on initial SOC levels. Nevertheless, the complex SOC-yield relationship highlights the necessity for tailored soil management strategies that consider specific site conditions to optimize C storage and crop yield.

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