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水分管理对水稻生长与根际激发效应的影响特征
摘要点击 2025  全文点击 713  投稿时间:2020-07-19  修订日期:2020-08-17
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中文关键词  稻田  碳循环  水分管理  温室气体  13C-CO2连续标记法  根际激发效应
英文关键词  paddy soil  carbon cycle  water management  greenhouse gas emission  13C-CO2 continuous labeling  rhizosphere priming effect
作者单位E-mail
林森 中南林业科技大学环境科学与工程学院, 长沙 410004
中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125 
982500950@qq.com 
肖谋良 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125  
江家彬 贵州大学农学院, 贵阳 550025  
魏亮 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125  
李科林 中南林业科技大学环境科学与工程学院, 长沙 410004 csfuklli@163.com 
刘守龙 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125  
祝贞科 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125 zhuzhenke@isa.ac.cn 
葛体达 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125  
吴金水 中国科学院亚热带农业生态研究所, 亚热带农业生态过程重点实验室, 长沙 410125  
中文摘要
      作物根际沉积碳输入而引起的根际激发效应,对农田土壤碳排放通量和碳平衡起到关键的调控作用.在稻田生态系统中,由于频繁的干湿交替,土壤CO2和CH4排放以及根际激发效应明显有别于其他自然生态系统.因此,明确稻田生态系统干湿交替过程中水稻根际激发效应的方向与强度,对于减缓稻田温室气体排放具有重要意义.本研究采用13C-CO2连续标记法,结合盆栽试验,研究干湿交替和持续淹水条件下,水稻生长以及根际激发效应的响应特征.结果表明,相对于持续淹水处理,干湿交替处理使水稻地上部和根系生物量以及根冠比显著提高,并增加了土壤微生物生物量.持续淹水条件下,13CO213CH4排放通量随水稻生长由10.2 μg·(kg·h)-1和2.8 μg·(kg·h)-1(63 d)增加到16.0 μg·(kg·h)-1和3.2 μg·(kg·h)-1(75 d).而在干湿交替条件下,经过12 d的落干处理13CO213CH4排放通量分别降低了57.5%和88.1%.持续淹水条件下,CO2和CH4的根际激发效应表现为正激发效应,而且随水稻的生长而增加.而干湿交替处理下,经过12 d的落干处理,CO2和CH4的根际激发效应分别由0.29 mg·(kg·h)-1和12.3 μg·(kg·h)-1(63 d)降低到-0.39 mg·(kg·h)-1和0.07 μg·(kg·h)-1(75 d).因此,干湿交替处理,能有效促进水稻生长和降低CH4的累计排放量.合理地田间水分管理对于提高水稻产量和降低温室气体排放具有重要意义.
英文摘要
      The rhizosphere priming effect (RPE) caused by carbon inputs from crop rhizodeposits plays a key role in regulating the carbon emission flux and carbon balance of farmland soils. Due to frequent alternations between dry and wet conditions, CO2 and CH4 emissions and the RPE in paddy field ecosystems are significantly different to those of other ecosystems. Therefore, it is of great significance to determine the direction and intensity of the rice RPE under alternations of dry and wet to limit greenhouse gas emissions. In this study, using a 13C-CO2 continuous labeling method combined with a pot-based experiment, the response of rice growth and the RPE under alternating dry and wet and continuous flooding conditions was examined. The results showed that, compared with the continuous flooding treatment, the alternating dry and wet treatments significantly increased aboveground and root biomass and the root-to-root ratio, and also increased soil microbial biomass. Under continuous flooding conditions, fluxes of 13CO2 and 13CH4 increased with rice growth from 10.2 μg·(kg·h)-1 and 2.8 μg·(kg·h)-1 (63 d) to 16.0 μg·(kg·h)-1 and 3.2 μg·(kg·h)-1 (75 d), respectively. During the 12-day drying process, the emissions of 13CO2 and 13CH4 derived from rhizosphere deposited C decreased by 57.5% and 88.1%. Under continuous flooding conditions, the RPE for CO2 and CH4 were positive and increased with the growth of rice. Under the alternating dry and wet treatment, after 12 days of drying, the RPE for CO2 and CH4 was reduced from 0.29 mg·(kg·h)-1 and 12.3 μg·(kg·h)-1 (63 d) to -0.39 mg·(kg·h)-1 and 0.07 μg·(kg·h)-1 (75 d). Thus, alternating wet and dry treatment can effectively promote rice growth and reduce the cumulative emissions of CH4. Therefore, adopting appropriate field water management is of great significance for increasing rice yields and mitigating greenhouse gas emissions.

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