Kracmarova Martina, Uhlik Ondrej, Strejcek Michal, Szakova Jirina, Cerny Jindrich, Balik Jiri, Tlustos Pavel, Kohout Petr, Demnerova Katerina, Stiborova Hana
Department of Biochemistry and Microbiology, Faculty of Food and Biochemical Technology, University of Chemistry and Technology, Prague, Technicka 3, 166 28, Prague 6, Czech Republic.
Department of Agro-Environmental Chemistry and Plant Nutrition, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences Prague, Kamycka 129, 165 21, Prague - Suchdol, Czech Republic.
Environ Microbiome. 2022 Mar 28;17(1):13. doi: 10.1186/s40793-022-00406-4.
Although fertilization and crop rotation practices are commonly used worldwide in agriculture to maximize crop yields, their long-term effect on the structures of soil microorganisms is still poorly understood. This study investigated the long-term impact of fertilization and crop rotation on soil microbial diversity and the microbial community structure in four different locations with three soil types. Since 1996, manure (MF; 330 kg N/ha), sewage sludge (SF; 330 and SF3x; 990 kg N/ha), and NPK (NPK; 330 kg N/ha) fertilizers were periodically applied to the soils classified as chernozem, luvisol and cambisol, which are among the most abundant or fertile soils used for agricultural purposes in the world. In these soils, potato (Solanum tuberosum L.), winter wheat (Triticum aestivum L.), and spring barley (Hordeum vulgare L.) were rotated every three years.
Soil chemistry, which was significantly associated with location, fertilization, crop rotation, and the interaction of fertilization and location, was the dominant driver of soil microbial communities, both prokaryotic and fungal. A direct effect of long-term crop rotation and fertilization on the structure of their communities was confirmed, although there was no evidence of their influence on microbial diversity. Fungal and bacterial communities responded differently to fertilization treatments; prokaryotic communities were only significantly different from the control soil (CF) in soils treated with MF and SF3x, while fungal communities differed across all treatments. Indicator genera were identified for different treatments. These taxa were either specific for their decomposition activities or fungal plant pathogens. Sequential rotation of the three crops restricted the growth of several of the indicator plant pathogens.
Long-term fertilization and crop rotation significantly altered microbial community structure in the soil. While fertilization affected soil microorganisms mainly through changes in nutrient profile, crop rotations lead to the attraction and repulsion of specific plant pathogens. Such changes in soil microbial communities need to be considered when planning soil management.
尽管施肥和作物轮作做法在全球农业中普遍用于使作物产量最大化,但其对土壤微生物结构的长期影响仍知之甚少。本研究调查了施肥和作物轮作对四种不同地点、三种土壤类型的土壤微生物多样性和微生物群落结构的长期影响。自1996年以来,已定期向分类为黑钙土、淋溶土和始成土的土壤施用粪肥(MF;330千克氮/公顷)、污水污泥(SF;330和SF3x;990千克氮/公顷)以及氮磷钾(NPK;330千克氮/公顷)肥料,这些土壤是世界上用于农业目的最丰富或最肥沃的土壤之一。在这些土壤中,马铃薯(Solanum tuberosum L.)、冬小麦(Triticum aestivum L.)和春大麦(Hordeum vulgare L.)每三年轮作一次。
土壤化学与地点、施肥、作物轮作以及施肥与地点的相互作用显著相关,是土壤微生物群落(原核生物和真菌)的主要驱动因素。尽管没有证据表明长期作物轮作和施肥对微生物多样性有影响,但证实了它们对群落结构有直接影响。真菌和细菌群落对施肥处理的反应不同;原核生物群落仅在施用MF和SF3x的土壤中与对照土壤(CF)有显著差异,而真菌群落在所有处理中均有差异。确定了不同处理的指示属。这些分类群要么因其分解活动具有特异性,要么是真菌植物病原体。三种作物的顺序轮作限制了几种指示植物病原体的生长。
长期施肥和作物轮作显著改变了土壤中的微生物群落结构。施肥主要通过养分状况的变化影响土壤微生物,而作物轮作导致特定植物病原体的吸引和排斥。在规划土壤管理时需要考虑土壤微生物群落的这种变化。