| 长期不同施肥对稻田土壤有机碳矿化及激发效应的影响 |
| 摘要点击 2428 全文点击 994 投稿时间：2018-05-06 修订日期：2018-05-29 |
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| 中文关键词 水稻土 长期施肥 同位素标记 有机碳矿化 激发效应 |
| 英文关键词 paddy soils long-term fertilization isotope labeling technique organic carbon mineralization priming effect |
| 作者 | 单位 | E-mail | | 马欣 | 西北农林科技大学资源环境学院, 杨凌 712100
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 | 2539393041@qq.com | | 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 | | | 唐美玲 | 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
中南林业科技大学生命科学与技术学院, 长沙 410004 | | | 徐福利 | 西北农林科技大学资源环境学院, 杨凌 712100
中国科学院水利部水土保持研究所, 杨凌 712100 | xfl@nwsuaf.edu.cn | | 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 | | | 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 | |
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| 中文摘要 |
| 通过室内模拟培养实验，结合14C同位素标记技术，研究了不施肥（CK）、单施化肥（NPK）、秸秆还田+化肥（ST）这3种施肥处理下稻田耕层土壤有机碳矿化特征及其对添加外源葡萄糖的响应特征.结果表明，56 d培养实验结束时，CK处理土壤累积矿化率（土壤原有有机碳累积矿化量/土壤总有机碳含量）达到1.64%，而NPK和ST处理较CK处理显著降低了0.34%和0.39%（P<0.05），表明长期施肥对土壤碳有一定的固持作用.长期不同施肥处理土壤对添加外源葡萄糖的响应有所不同，表现出了不同程度的激发效应.随着培养时间的推移，3种处理土壤碳矿化的激发效应由负激发效应逐渐转为正激发效应.56 d时，ST和NPK处理土壤的负累积激发效应比CK分别显著提高了22.07和9.05倍（P<0.05）.结构方程模型分析表明，土壤NH4+-N和DOC含量主要通过影响土壤MBC和MBN含量间接影响土壤累积激发效应，且NH4+-N对土壤累积激发效应有直接的显著负影响.综上所述，长期施肥降低了稻田土壤原有有机碳累积矿化率，有利于增强稻田土壤碳的固持和积累，秸秆还田加化肥效果更加明显. |
| 英文摘要 |
| A laboratory incubation experiment was conducted using the 14C isotope labeling technique to study the characteristics of organic carbon mineralization and their response to glucose addition when treated with a combination of straw and chemical fertilizer (ST), inorganic fertilizer (NPK), and non-fertilization (CK). The cumulative mineralization rate (ratio of accumulated mineralization amount to total organic carbon content) in CK reaches 1.64% at the end of incubation (56 days). The cumulative mineralization rate during NPK and ST treatments is significantly lower than that in CK (by 0.34% and 0.39%, respectively). This indicates that long-term fertilization affects the soil carbon sequestration. Varying long-term fertilization influences the response of paddy soil to glucose addition and leads to different levels of the priming effect. The priming effect on soil organic carbon mineralization of the three treatments gradually changes from negative to positive with increasing incubation time. The significantly negative cumulative priming effect in ST and NPK after 56 d is 22.07 and 9.05 times higher than that in CK, respectively. The results of the structural equation model indicate that the NH4+-N and DOC contents indirectly influence the cumulative priming effect on soil organic carbon by affecting the MBC and MBN contents. The NH4+-N concentration has a direct and significant negative effect on the cumulative priming effect. In conclusion, long-term fertilization treatments reduce the cumulative organic carbon mineralization rate of paddy soil. Fertilizer, especially the combination of straw and chemical fertilizer, enhances the soil carbon sequestration and accumulation. |
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