新型稻-罗氏沼虾轮作模式对复垦土壤理化性质、养分供应及微生物多样性的影响

Effects of a new rice-macrobrachium rosenbergii crop rotation model on reclaimed soil physicochemical properties, nutrient supply and microbial diversity

  • 摘要: 为研究新构建的稻-罗氏沼虾轮作种养系统对复垦土壤理化性质、养分供应能力及微生物多样性的影响, 以客观综合评价新建稻虾综合种养系统经济和生态效益。本研究通过现场采样、室内化学指标测定和高通量测序技术, 测定了稻-沼虾轮作模式3个不同生产阶段(放虾前、收虾后和收稻后)的两个土层(0~20 cm和20~40 cm)土壤的物理性质、还原性物质、全量和速效养分及菌群结构变化特征。结果显示: 收虾后和收稻后>2 mm土壤团聚体占比自上而下显著增加(P<0.05), 0.25~2 mm和<0.25 mm的土壤团聚体占比均大于放虾前; 收虾后20~40cm土壤还原性指标显著大于0~20 cm (P<0.05), 收虾后和收稻后有机还原性物质、Fe2+和Mn2+含量显著大于放虾前(P<0.05); 0~20 cm土壤全量和速效养分均高于20~40 cm, 收虾后土壤有机质、全氮和全磷含量显著高于放虾前(P<0.05); 收虾后0~20 cm处的OTU数量显著高于放虾前(P<0.05); 收虾后和收稻后Candidatus_SolibacterCitrobacterBacillus相对丰度显著高于放虾前(P<0.05); 土壤团聚体(0.2~2.5 mm)、全氮、全钾和毛管孔隙度是驱动土壤微生物菌群变异的主要影响因子。综上, 新建的稻-罗氏沼虾轮作模式有助于改善复垦耕层土壤物理结构、增强土壤缓冲能力、提高养分供应能力及菌群多样性, 且对0~20 cm表层土壤改善效果优于20~40 cm, 但同时可能会增加土壤次生潜育化风险。研究结果将为进一步优化稻-罗氏沼虾种养策略以最大程度发挥其经济生态效益提供理论依据。

     

    Abstract: To investigate the impacts of the newly established rice-macrobrachium rosenbergii rotation system on reclaimed soil physicochemical properties, nutrient supply capacity, and microbial diversity, and finally in order to objectively evaluate the comprehensive economic and ecological benefits of this system. This study examined the physical properties, reducing substances, total and available nutrients, and microflora structure of soil layers (0−20 cm and 20−40 cm) at three different production stages (before shrimp stock, after shrimp harvest, and after rice harvest) using field sampling, laboratory chemical analysis, and high-throughput sequencing methods. The results indicated a significant increase in the proportion of >2 mm soil aggregates from top to bottom after shrimp and rice harvesting (P<0.05). Soil bulk density, 0.25−2.0 mm, and <0.25 mm soil aggregates were all higher compared to those before shrimp stock. The soil reducing index in the 20~40 cm layer after shrimp harvest was significantly higher than that in the 0−20 cm layer (P<0.05). Additionally, the levels of organic reducing substances, Fe2+, and Mn2+ after shrimp and rice harvest were significantly higher than those before shrimp harvest (P<0.05). Total and available nutrients in the 0−20 cm soil layer were higher than those in the 20−40cm soil layer. Furthermore, the levels of soil organic matter, total and available nutrients followed the order: after shrimp harvest > after rice harvest > before shrimp stock. Additionally, the levels of organic matter, total nitrogen (TN), and total phosphorus (TP) in soil after shrimp harvest were significantly higher than those before shrimp stock (P<0.05). The number of Operational Taxonomic Units (OTUs) at 0−20 cm depth after shrimp harvest was significantly higher than that before shrimp harvest (P<0.05). Hence, the newly established rice-macrobrachium rosenbergii rotation model is advantageous in enhancing the physical structure of the topsoil, boosting soil buffer capacity, increasing nutrient supply, and enhancing microbial diversity. However, while the improvement effects are more pronounced in the 0−20 cm surface layer compared to the 20−40 cm soil layer, there is also a potential risk of soil secondary compaction. The findings of this study will serve as a theoretical foundation for optimizing rice and shrimp farming strategies, further aiming to maximize their economic and ecological benefits.

     

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