Cover crops improve soil structure and change organic carbon distribution in macroaggregate fractions

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE
Soil Pub Date : 2024-02-15 DOI:10.5194/soil-10-139-2024
Norman Gentsch, Florin Laura Riechers, Jens Boy, Dörte Schweneker, Ulf Feuerstein, Diana Heuermann, Georg Guggenberger
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Abstract

Abstract. Soil structure is sensitive to intensive soil management. It can be ameliorated by a reduction in soil cultivation and stimulation of plant and microbial mediators for aggregate formation, with the latter being a prerequisite and measure for soil quality. Cover crops (CCs) are part of an integrated approach to stabilize or improve soil quality. Thereby, the incorporation of diverse CC mixtures is hypothesized to increase the positive effects of CC applications. This study entailed an investigation of the legacy effect of CCs on soil aggregates after three crop rotations in the second main crop (winter wheat) after the last CC treatment. Four CCs (mustard, phacelia, clover, and oat) cultivated in pure stands and with a fallow treatment were compared to a mixture of the four CC species (Mix4) and a highly diverse 12-plant-species mixture (Mix12) in a long-term field experiment in Germany. The organic carbon (OC) distribution within macroaggregate fractions (16–8, 8–4, 4–2, 2–1, and <1 mm) and their aggregate stability were measured by dry- and wet-sieving methods, and the mean weight diameter (MWD) was calculated from water-stable aggregates. The results showed that, compared to the fallow, all CCs increased the MWD between 10 % and 19 % in soil under the following main crop. The average MWD increase over the fallow was slightly higher for CC mixtures (16 %) than for single CCs (12 %). Most of the OC (67.9 % on average) was stored in the <1 mm aggregate fraction, highest in the topsoil and decreasing with soil depth. The intermediate fractions (8–4 mm, 4–2 mm, 2–1 mm) stored 8.5 %, 10.5 %, and 11.0 % of the total OC, while 2.1 % was stored in the 16–8 mm fraction. Higher MWD improvement at the 20–30 cm depth also indicates additional benefits from a reduction in the cultivation depth. Structural equation modelling (SEM) suggests that single CCs were more likely to increase OC storage in small macroaggregates <1 mm, while CC mixtures were more likely to increase OC in the largest fraction (8–16 mm). Different individual CC species or mixtures exhibited varying involvement in the formation of different aggregate fractions. We provide evidence that litter quality, root morphology, and rhizosphere input, which affect microbial mediators of aggregate formation, might be the main reasons for the observed differences between CC treatments. Cover crops are valuable multifunctional tools for sustainable soil management. Here, we showed that they contribute to structure amelioration in arable soils. Increasing the functional diversity of plant species in CC mixtures could be a strategy to further enhance the positive effects of CCs in agroecosystems.
覆盖作物可改善土壤结构,改变有机碳在大颗粒组分中的分布
摘要土壤结构对密集型土壤管理很敏感。土壤结构可以通过减少土壤耕作、刺激植物和微生物介质形成团聚体来改善,而后者是土壤质量的前提和衡量标准。覆盖作物(CC)是稳定或改善土壤质量的综合方法的一部分。因此,将不同的覆盖作物混在一起可以增加覆盖作物应用的积极效果。本研究调查了三种作物轮作后,CCs 对土壤团聚体的遗留影响,以及最后一种 CC 处理后的第二种主要作物(冬小麦)。在德国的一项长期田间试验中,将纯种栽培和休耕处理的四种 CC(芥菜、法桐、三叶草和燕麦)与四种 CC 的混合物(Mix4)和高度多样化的 12 种植物混合物(Mix12)进行了比较。通过干筛法和湿筛法测量了大颗粒(16-8、8-4、4-2、2-1 和小于 1 毫米)中的有机碳(OC)分布及其聚集稳定性,并根据水稳定性聚集体计算了平均重量直径(MWD)。结果表明,与休耕相比,所有 CC 都能使下茬主要作物下的土壤的 MWD 增加 10% 到 19%。与休耕相比,CC 混合物(16%)的平均 MWD 增幅略高于单一 CC(12%)。大部分 OC(平均 67.9%)储存在小于 1 毫米的骨料部分,在表层土壤中含量最高,并随着土壤深度的增加而减少。中间部分(8-4 毫米、4-2 毫米、2-1 毫米)分别储存了总 OC 的 8.5%、10.5% 和 11.0%,而 16-8 毫米部分储存了 2.1%。20-30厘米深度的MWD改善程度较高,这也表明减少栽培深度会带来额外的好处。结构方程建模(SEM)表明,单个CC更有可能增加小于1毫米的小宏观聚集体中的OC储量,而CC混合物更有可能增加最大部分(8-16毫米)的OC储量。不同的单个CC物种或混合物在不同聚合体部分的形成过程中表现出不同的参与程度。我们提供的证据表明,影响聚合体形成的微生物介质的枯落物质量、根系形态和根圈输入可能是观察到的 CC 处理间差异的主要原因。覆盖作物是可持续土壤管理的重要多功能工具。在这里,我们发现覆盖作物有助于改善耕地土壤的结构。增加CC混合物中植物物种的功能多样性可能是进一步增强CC在农业生态系统中的积极作用的一种策略。
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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