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小麦蚕豆间作体系的土壤氮矿化特征——地下部的贡献

批准号:
32060718
项目类别:
地区科学基金项目
资助金额:
35.0 万元
负责人:
肖靖秀
依托单位:
学科分类:
植物营养基础
结题年份:
2024
批准年份:
2020
项目状态:
已结题
项目参与者:
肖靖秀

项目摘要

结项摘要

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中文摘要
根系及根际淀积与土壤氮矿化过程密切相关。小麦蚕豆间作能改变地下部根系及根际过程、提高土壤氮有效性。但地下部根系及根际淀积对间作土壤氮矿化过程的影响、贡献及作用机制有待明确。基于间作田间定位试验,研究以地下部根系和根际淀积为主线,将田间原位培养、田间根系埋袋、15N田间标记-室内培养相结合,利用Illumina HiSeq和13C—NMR技术,1)研究单间作根系的还田量、分解特性及根际氮淀积量,定量间作体系地下部对土壤氮库的贡献;2)分析单间作土壤氮库的差异及有机氮矿化的周年动态、探究根系及根际淀积下的土壤氮矿化差异,揭示间作体系根系及根际淀积对土壤氮矿化过程的调控作用;3)探明单间作条件下根际微生态环境(微生物群落结构、碳库特征、胞外酶活性)的差异,解析间作体系根土互作驱动土壤氮矿化的机制。研究对全面理解豆科禾本科间作节约氮肥、调控土壤养分循环、提高土壤地力具有重要的理论和现实意义。
英文摘要
Root and rhizodeposition are closely related to soil nitrogen (N) mineralization process. Wheat and faba bean intercropping could change root biomass, root architecture and rhizodeposition, which induced increased soil N availability. However, the effects of root and rhizodeposition on intercropping soil N mineralization have not been well understood. Additionally, the belowground contribution to intercropping enhanced soil N availability and its underline mechanism are unknown. Hence, based on the several years field experiments of wheat and faba bean intercropping, the present study would be focus on below-ground root and rhizodeposition in intercropping through several experiments involving in situ field inoculation, root barrier in field and labeling with 15N in situ field-laboratory inoculation, and some key methods and techniques including Illumina HiSeq and solid 13C—NMR would be used. The mainly targets of present study are, 1), to study the amounts of root litter returned to field, the characteristic of root litter decomposition, and the N rhizodeposition under mono- and intercropping system. The contrition of root and rhizodeposition to soil N pool will be identified. 2), to analyze the difference of soil N pool between mono- and intercropped system and dynamic soil N mineralization. The regulation role of root litter and rhizodeposition on soil N mineralization will be measured. 3), to discuss the rhizosphere micro-ecological difference including rhizosphere microbial community, carbon (C) pool, and soil extracellular enzyme activity between mono- and intercropped system, and the mechanism of root-soil interaction in modulating soil N mineralization in wheat and faba bean intercropping will be revealed. The research is of scientific and practical importance not only for comprehensive understands cereal and legume intercropping saving N fertilizer, but also for intercropping regulating soil nutrients cycle and enhancing soil fertility.
土壤氮矿化是土壤氮素转化的重要过程,与土壤供氮能力和氮素流失密切相关。豆科禾本科间作可以改变地下部的根系及根际过程,提高土壤氮的有效性和作物的氮素吸收。但是,间作体系的周年氮矿化特征尚不清楚,间作体系地下部根系及根际过程对土壤氮矿化有怎样的影响,作用机制如何,均有待明确。本项目通过田间原位培养试验、室内培养试验、埋袋试验、田间定位试验等,明确小麦和蚕豆的根系还田量及根际淀积量、根系分解特征、根系化学结构,研究不同氮水平下小麦蚕豆间作体系的氮矿化周年特征,探究根系还田及根际氮沉积对土壤碳、氮含量和组分的影响及其对土壤氮矿化的影响。研究表明,小麦蚕豆种间相互作用提高0-30cm土层根系还田量和根际碳、氮沉积量15-40%。间作提高根系还田量和根际淀积量尤其是蚕豆根系和根际碳、氮还田量促进了有机碳的积累(7-12%)。小麦蚕豆种间互作最强烈的时期,间作提高了小麦和蚕豆土壤的(净)氮矿化。但是,随着小麦和蚕豆的成熟-收获,间作反而有抑制土壤氮矿化的趋势。在小麦蚕豆种间互作强烈的时期,间作增加轻组有机碳、易氧化有机碳和微生物量碳和氮,提高酸解有机氮含量和占比,为间作提高土壤净氮矿化量和氮矿化速率奠定了基础。作物成熟、收获后,间作提高土壤C/N比则抑制了土壤氮矿化。研究发现,小麦蚕豆种间相互作用提高土壤微生物量碳和氮、改变根际微生物群落结构和胞外酶活性驱动了更高土壤氮矿化速率和矿化量。其中,间作提高纤维二糖水解酶和N-乙酰-β-D-葡萄糖苷酶活性、微生物量碳和氮是间作提高土壤氮矿化的直接驱动力;其次,间作减弱酸酐菌门对土壤氮矿化的抑制作用间接促进了土壤氮矿化。研究从根土互作的角度系统揭示了间作提高土壤氮矿化的作用机制,从地下部的视角解析了间作改变土壤氮矿化的作用机制,为深入理解豆科禾本科间作提高土壤氮有效性奠定了基础。项目的实施累计发表论文10篇(1篇待发表),出版专著1部,培养硕士研究生4人。
小麦蚕豆间作调控小麦白粉病抗性的氮代谢分子机制
  • 批准号:
    31760611
  • 项目类别:
    地区科学基金项目
  • 资助金额:
    38.0万元
  • 批准年份:
    2017
  • 负责人:
    肖靖秀
  • 依托单位:
小麦蚕豆间作根际红壤磷活化及其对(无机)磷施用的响应机制
  • 批准号:
    31560581
  • 项目类别:
    地区科学基金项目
  • 资助金额:
    38.0万元
  • 批准年份:
    2015
  • 负责人:
    肖靖秀
  • 依托单位:
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