首页 | 本学科首页   官方微博 | 高级检索  
     检索      

长期不同施肥对稻田土壤有机碳矿化及激发效应的影响
引用本文:马欣,魏亮,唐美玲,徐福利,祝贞科,葛体达,吴金水.长期不同施肥对稻田土壤有机碳矿化及激发效应的影响[J].环境科学,2018,39(12):5680-5686.
作者姓名:马欣  魏亮  唐美玲  徐福利  祝贞科  葛体达  吴金水
作者单位:西北农林科技大学资源环境学院;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;中南林业科技大学生命科学与技术学院;中国科学院水利部水土保持研究所;遵义师范学院生物与农业科...;西北农林科技大学资源环境...;中国林业科学研究院森林生...;宝鸡文理学院地理与环境学...;吉林农业大学资源与环境学...;吉林农业大学资源与环境学...;西藏自治区农牧科学院农业...;江南大学环境与土木工程学...;山东农业大学资源与环境学...;宁夏大学西北土地退化与生...
基金项目:国家自然科学基金项目(41501321);政府间国际科技创新合作重点专项(S2016G0053)
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NH+4-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NH+4-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.

关 键 词:水稻土  长期施肥  同位素标记  有机碳矿化  激发效应
收稿时间:2018/5/6 0:00:00
修稿时间:2018/5/29 0:00:00

Effects of Varying Long-term Fertilization on Organic Carbon Mineralization and Priming Effect of Paddy Soil
MA Xin,WEI Liang,TANG Mei-ling,XU Fu-li,ZHU Zhen-ke,GE Ti-da and WU Jin-shui.Effects of Varying Long-term Fertilization on Organic Carbon Mineralization and Priming Effect of Paddy Soil[J].Chinese Journal of Environmental Science,2018,39(12):5680-5686.
Authors:MA Xin  WEI Liang  TANG Mei-ling  XU Fu-li  ZHU Zhen-ke  GE Ti-da and WU Jin-shui
Institution:College of Resources and Environment, Northwest A & F University, Yangling 712100, China;Key Laboratory of Subtropical Agriculture Ecology, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China,Key Laboratory of Subtropical Agriculture Ecology, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China,Key Laboratory of Subtropical Agriculture Ecology, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China;College of Life Science and Engineering, Central South University of Forestry and Technology, Changsha 410004, China,College of Resources and Environment, Northwest A & F University, Yangling 712100, China;Institute of Soil and Water Conservation of Chinese Academy of Sciences, Ministry of Water Resources, Yangling 712100, China,Key Laboratory of Subtropical Agriculture Ecology, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China,Key Laboratory of Subtropical Agriculture Ecology, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China and Key Laboratory of Subtropical Agriculture Ecology, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Changsha 410125, China
Abstract: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.
Keywords:paddy soils  long-term fertilization  isotope labeling technique  organic carbon mineralization  priming effect
本文献已被 CNKI 等数据库收录!
点击此处可从《环境科学》浏览原始摘要信息
点击此处可从《环境科学》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号