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生物与非生物因素对森林土壤氮矿化的调控机制

左倩倩 王邵军

左倩倩, 王邵军. 生物与非生物因素对森林土壤氮矿化的调控机制[J]. 浙江农林大学学报. doi: 10.11833/j.issn.2095-0756.20200482
引用本文: 左倩倩, 王邵军. 生物与非生物因素对森林土壤氮矿化的调控机制[J]. 浙江农林大学学报. doi: 10.11833/j.issn.2095-0756.20200482
ZUO Qianqian, WANG Shaojun. Regulation mechanism of biotic and abiotic factors on the nitrogen mineralization of forest soil[J]. Journal of Zhejiang A&F University. doi: 10.11833/j.issn.2095-0756.20200482
Citation: ZUO Qianqian, WANG Shaojun. Regulation mechanism of biotic and abiotic factors on the nitrogen mineralization of forest soil[J]. Journal of Zhejiang A&F University. doi: 10.11833/j.issn.2095-0756.20200482

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生物与非生物因素对森林土壤氮矿化的调控机制

doi: 10.11833/j.issn.2095-0756.20200482
基金项目: 国家自然科学基金项目(32060281,31660191);国家林业局“948”项目(2015-4-39);云南省全球变化生态学研究生导师团队建设项目;云南省教育厅科学研究基金项目(自然科学类)(11070641)
详细信息
    作者简介: 左倩倩(ORCID: 0000-0001-7686-6749),从事土壤生态学研究。E-mail: qianqianzuo2009@126.com
    通信作者: 王邵军(ORCID: 0000-0001-5975-7938),教授,博士,从事土壤动物和土壤生态学研究。E-mail: shaojunwang2009@163.com
  • 中图分类号: S714

Regulation mechanism of biotic and abiotic factors on the nitrogen mineralization of forest soil

  • 摘要: 温室气体排放剧增引起全球变暖,已成为全球高度关注的生态环境问题。一氧化二氮(N2O)是大气中仅次于二氧化碳(CO2)和甲烷(CH4)的第三大温室气体,森林土壤氮矿化过程伴随着硝化和反硝化的发生,能够导致N2O的产生,进而引起大气N2O浓度的升高。森林土壤氮矿化是生物与非生物环境因素共同调控的复杂生态学过程,探明森林土壤氮矿化的影响因素及其调控机制,有助于丰富人们对森林土壤氮循环过程的认识,在全球变化研究中具有重要的地位与作用。本研究揭示森林土壤氮矿化的时空变化及影响因素,阐明非生物因素以及森林植被覆盖、森林凋落物、土壤微生物与土壤动物等生物因素对森林土壤氮矿化的影响特征及作用机制。目前,森林土壤氮矿化研究存在结果可比性不强;内容多集中于氮矿化单因素影响研究,缺乏多因子尤其是微生物-动物协同调控研究;缺乏不同气候类型及不同土地利用方式森林土壤氮矿化特征及影响机制研究;缺乏氮矿化对全球变化的响应研究等一系列问题。土壤氮矿化研究应该探索统一高效的测定方法,加强土壤微生物-动物-环境因子多因素耦合对森林土壤氮矿化影响机制研究,探讨不同气候类型及不同利用方式森林土壤氮矿化调控机制,重点阐明全球变化背景下森林土壤氮矿化的过程与机理。旨在为准确理解不同气候区森林土壤氮矿化的时空格局及其对全球气候变化的影响提供理论支撑。参69
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  • 收稿日期:  2020-07-06
  • 修回日期:  2021-01-18

生物与非生物因素对森林土壤氮矿化的调控机制

doi: 10.11833/j.issn.2095-0756.20200482
    基金项目:  国家自然科学基金项目(32060281,31660191);国家林业局“948”项目(2015-4-39);云南省全球变化生态学研究生导师团队建设项目;云南省教育厅科学研究基金项目(自然科学类)(11070641)
    作者简介:

    左倩倩(ORCID: 0000-0001-7686-6749),从事土壤生态学研究。E-mail: qianqianzuo2009@126.com

    通信作者: 王邵军(ORCID: 0000-0001-5975-7938),教授,博士,从事土壤动物和土壤生态学研究。E-mail: shaojunwang2009@163.com
  • 中图分类号: S714

摘要: 温室气体排放剧增引起全球变暖,已成为全球高度关注的生态环境问题。一氧化二氮(N2O)是大气中仅次于二氧化碳(CO2)和甲烷(CH4)的第三大温室气体,森林土壤氮矿化过程伴随着硝化和反硝化的发生,能够导致N2O的产生,进而引起大气N2O浓度的升高。森林土壤氮矿化是生物与非生物环境因素共同调控的复杂生态学过程,探明森林土壤氮矿化的影响因素及其调控机制,有助于丰富人们对森林土壤氮循环过程的认识,在全球变化研究中具有重要的地位与作用。本研究揭示森林土壤氮矿化的时空变化及影响因素,阐明非生物因素以及森林植被覆盖、森林凋落物、土壤微生物与土壤动物等生物因素对森林土壤氮矿化的影响特征及作用机制。目前,森林土壤氮矿化研究存在结果可比性不强;内容多集中于氮矿化单因素影响研究,缺乏多因子尤其是微生物-动物协同调控研究;缺乏不同气候类型及不同土地利用方式森林土壤氮矿化特征及影响机制研究;缺乏氮矿化对全球变化的响应研究等一系列问题。土壤氮矿化研究应该探索统一高效的测定方法,加强土壤微生物-动物-环境因子多因素耦合对森林土壤氮矿化影响机制研究,探讨不同气候类型及不同利用方式森林土壤氮矿化调控机制,重点阐明全球变化背景下森林土壤氮矿化的过程与机理。旨在为准确理解不同气候区森林土壤氮矿化的时空格局及其对全球气候变化的影响提供理论支撑。参69

English Abstract

左倩倩, 王邵军. 生物与非生物因素对森林土壤氮矿化的调控机制[J]. 浙江农林大学学报. doi: 10.11833/j.issn.2095-0756.20200482
引用本文: 左倩倩, 王邵军. 生物与非生物因素对森林土壤氮矿化的调控机制[J]. 浙江农林大学学报. doi: 10.11833/j.issn.2095-0756.20200482
ZUO Qianqian, WANG Shaojun. Regulation mechanism of biotic and abiotic factors on the nitrogen mineralization of forest soil[J]. Journal of Zhejiang A&F University. doi: 10.11833/j.issn.2095-0756.20200482
Citation: ZUO Qianqian, WANG Shaojun. Regulation mechanism of biotic and abiotic factors on the nitrogen mineralization of forest soil[J]. Journal of Zhejiang A&F University. doi: 10.11833/j.issn.2095-0756.20200482

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