氧化还原梯度下水稻根区有机碳矿化的碳-铁耦合机制
DOI:
CSTR:
作者:
作者单位:

1.湖南农业大学环境与生态学院;2.中国科学院亚热带农业生态研究所

作者简介:

通讯作者:

中图分类号:

基金项目:

国家自然科学基金项目(面上项目,重点项目,重大项目)


The Carbon-Iron Coupling Mechanism of Organic Carbon Mineralization in the Rice Root Zone under Redox Gradients
Author:
Affiliation:

1.College of Environment and Ecology,Hunan Agricultural University;2.Institute of Subtropical Agriculture,Chinese Academy of Science;3.CInstitute of Subtropical Agriculture,Chinese Academy of Science

Fund Project:

The National Natural Science Foundation of China (General Program, Key Program, Major Research Plan)

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    稻田土壤碳循环是固碳增汇与地力提升的关键。水稻根区作为碳循环最活跃的区域,其碳周转过程与土壤氧化还原状态及铁相变化密切相关。但目前氧化还原梯度下铁介导的有机碳矿化过程尚不明确,碳-铁耦合机制仍有待系统揭示。采用土柱和人工根系建立简化的根际微生态系统,通过水分调节(60%土壤饱和含水量、80%土壤饱和含水量、100%土壤饱和含水量、3 cm淹水)构建4个氧化还原电位梯度,以13C葡萄糖作为模拟根系分泌物,用以探究不同氧化还原状态下铁相转变对水稻根区总有机碳矿化过程及激发效应的影响。结果表明:(1)土壤氧化还原电位(Eh)降低和外源葡萄糖输入均显著提高了甲烷(CH4)和二氧化碳(CO2)的排放总量;饱和含水条件下,输入葡萄糖处理的CH4的排放增量显著高于CO2,非饱和含水条件下则反之。(2)有、无葡萄糖输入处理中,土壤可溶性有机碳(DOC)含量较培养前整体降低,但饱和含水条件下的DOC芳香度增加。Eh降低和葡萄糖输入促进了亚铁(Fe2+)还原和铁结合态有机碳(Fe-OC)释放,且Fe-OC含量变化与土壤中铁形态及CO2释放速率显著相关。(3)碳循环水解酶和氧化酶活性均受到氧化还原梯度和葡萄糖输入的显著影响。其中纤维二糖水解酶活性随Eh降低而降低,并与CH4和CO2排放速率之和负相关;饱和含水处理中的酚氧化活性高于非饱和含水处理,其活性与温室气体排放速率正相关;葡萄糖输入显著提高了氧化还原相关的酚氧化活性和过氧化氢酶活性。“铁门”和“酶闩”机制协同调控了CH4和CO2的排放过程。该研究结果可为预测亚热带富铁水稻土中根际碳的积累潜力、优化水分管理以实现稻田固碳减排提供必要参数和科学依据。

    Abstract:

    【Objective】Carbon cycling in paddy soils is crucial for carbon sequestration and soil fertility enhancement. The rice root zone, being the most active site of this cycle, exhibits carbon turnover processes that are closely linked to soil redox conditions and iron phase transformations. However, the iron-mediated organic carbon mineralization process under redox gradients remains unclear, and the carbon-iron coupling mechanism requires systematic elucidation.【Method】In this study, we established a simplified rhizosphere microcosm system by using soil columns equipped with artificial roots. Four redox potential gradients of the soil column were constructed by adjusting water conditions (60%, 80%, and 100% of soil water saturation capacity, plus 3 cm flooding), and 13C-labeled glucose was used as a model root exudate, for investigating the effects of iron phase transformation on total organic carbon mineralization and priming effect in the root zone under different redox states.【Result】The results showed that: (1) Both soil Eh reduction and exogenous glucose input significantly increased the cumulative emissions of CH4 and CO2. Under water-saturated conditions, the incremental emission of CH4 was significantly higher than that of CO2 in the glucose-amended treatments, and vice versa in the unsaturated water content. (2) In both glucose-amended and non-amended treatments, soil dissolved organic carbon (DOC) content generally decreased compared to pre-incubation levels, but the aromaticity of DOC increased under saturated conditions. Eh reduction and glucose input stimulated ferrous iron (Fe2+) reduction and iron-associated organic carbon (Fe-OC) release, with Fe-OC content variations showing significant correlations with iron speciation and CO2 emission rates. (3) The activities of carbon cycle hydrolase and oxidase were significantly affected by the redox gradient and glucose input. Cellobiohydrolase (CBH) activity decreased with decreasing Eh and showed a negative correlation with CH4+CO2 emission rates. Moreover, phenol oxidative activity was higher in the saturated water treatments than in the unsaturated water treatments and was positively correlated with the rate of gas emission. Glucose addition significantly increased the activities of phenol oxidative activity and catalase oxidases. 【Conclusion】Both the “iron gate” and “enzyme latch” mechanisms synergistically regulated CH4 and CO2 emissions. The findings provide critical parameters and a scientific basis for predicting rhizodeposited carbon sequestration potential in subtropical iron-rich paddy soil, and optimizing water management strategies to enhance carbon storage and mitigate greenhouse gas emissions in rice cultivation systems.

    参考文献
    相似文献
    引证文献
引用本文

刘斯洋,李颜,李雨霖,高威,胡腾,陈香碧,周萍,郭晓彬,吴金水.氧化还原梯度下水稻根区有机碳矿化的碳-铁耦合机制[J].土壤学报,,[待发表]
LIU Siyang, LI Yan, LI Yulin, GAO Wei, Hu Teng, CHEN Xiangbi, ZHOU Ping, GUO Xiaobin, WU Jinshui. The Carbon-Iron Coupling Mechanism of Organic Carbon Mineralization in the Rice Root Zone under Redox Gradients[J]. Acta Pedologica Sinica,,[In Press]

复制
分享
相关视频

文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2025-07-02
  • 最后修改日期:2025-12-23
  • 录用日期:2026-02-05
  • 在线发布日期:
  • 出版日期:
文章二维码