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

养分化学计量比对稻田土壤葡萄糖矿化及其激发效应的影响
引用本文:汤珍珠,祝贞科,沈冰洁,胡亚军,王 娟,庞 静,童成立,葛体达,吴金水.养分化学计量比对稻田土壤葡萄糖矿化及其激发效应的影响[J].土壤学报,2017,54(1):246-254.
作者姓名:汤珍珠  祝贞科  沈冰洁  胡亚军  王 娟  庞 静  童成立  葛体达  吴金水
作者单位:1. 湖北大学资源环境学院,武汉 430062; 中国科学院亚热带农业生态研究所农业生态系统过程重点实验室,长沙 410125;2. 中国科学院亚热带农业生态研究所农业生态系统过程重点实验室,长沙,410125;3. 中国科学院亚热带农业生态研究所农业生态系统过程重点实验室,长沙 410125; 中南林业科技大学环境科学与工程学院,长沙 410004;4. 湖北大学资源环境学院,武汉,430062
基金项目:国家自然科学基金项目(41430860,41371304),湖南省自然科学基金项目(2016JJ3132)和中国科学院战略性先导科技专项(XDB15020401)资助
摘    要:选择13C-葡萄糖作为稻田土壤典型易利用态外源有机碳,通过室内培养试验,研究不同C/N/P/S计量比条件下,葡萄糖分解矿化的动态规律及其激发效应。结果表明,稻田土壤中葡萄糖-碳(C)快速矿化,60 d培养实验后,有65.5%~74.6%的葡萄糖-C矿化。养分元素的添加使土壤中葡萄糖-C快速转化碳库的比例逐渐由58%增加至65%,从而使葡萄糖-C矿化率提高了3.9%~12.5%,养分元素的添加量与葡萄糖-C快速转化碳库的比例和矿化率均表现出显著的正相关关系(R2=0.63,p0.05;R2=0.83,p0.05)。葡萄糖-C矿化过程中,导致稻田土壤碳的累积负激发效应为-370~-570 mg kg-1,养分元素添加比例越大,其负激发效应越强,二者呈显著的负相关性(R2=0.66,p0.05)。研究表明,稻田土壤中易利用态碳的矿化受C/N/P/S元素计量比的影响,高比例养分元素的添加,促进土壤中易利用态碳的矿化,抑制土壤原有有机质的分解,增强负激发效应。本研究可为深入了解稻田生态系统碳循环、实现农田土壤肥力提升和温室气体减排提供理论依据。

关 键 词:稻田土壤  有机碳矿化  激发效应  养分元素计量学
收稿时间:2/7/2016 12:00:00 AM
修稿时间:9/9/2016 12:00:00 AM

Effect of Stoichiometric Ratio of Soil Nutrients on Mineralization and Priming Effect of Glucose in Paddy Soil
TANG Zhenzhu,ZHU Zhenke,SHEN Bingjie,HU Yajun,WANG Juan,PANG Jing,TONG Chengli,GE Tida and WU Jinshui.Effect of Stoichiometric Ratio of Soil Nutrients on Mineralization and Priming Effect of Glucose in Paddy Soil[J].Acta Pedologica Sinica,2017,54(1):246-254.
Authors:TANG Zhenzhu  ZHU Zhenke  SHEN Bingjie  HU Yajun  WANG Juan  PANG Jing  TONG Chengli  GE Tida and WU Jinshui
Institution:School of Resources and Environmental Science, Hubei University,Key Laboratory of Agro Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences,Key Laboratory of Agro Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences,Key Laboratory of Agro Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences,Key Laboratory of Agro Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences,School of Resources and Environmental Science, Hubei University,Key Laboratory of Agro Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences,Key Laboratory of Agro Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences and Key Laboratory of Agro Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences
Abstract:Objective]The turnover of liable organic carbon(C)sources in soil is a key component of the cycle of soil carbon. Liable C sources(i.e. glucose),derived from C deposition in rhizosphere and other extraneous C inputs,are important sources of the C pool in the soil. Therefore,studying the turnover of liable C sources as affected by stoichiometric ratio of soil nutrients may help reveal mechanisms of the eco-stoichiometric regulation of the turnover of extraneous C in paddy soil. Method]In this study,an in-lab incubation experiment was conducted using 13C-glucose as extraneous organic C typical in paddy soil to explore quantitatively dynamics of decompositing mineralization and priming effect of glucose as affected by C/N/P/S stoichiometric ratio. Result]Results show that glucose was rapidly mineralized in the paddy soil so that 65.5% to 74.6% of the added glucose-C was mineralized after 60 d of incubation. The addition of nutrient elements not only increased glucose mineralization rate,but also raised the proportion of glucose-C available to soil microbes from 58% to 65%,thus accelerating glucose turnover rate in the soil. The amount of nutrient elements added was found significantly and positively related to both proportion of the microbe-available C pool in and mineralization rate(R2 = 0.63,p <0.05;R2 = 0.83,p<0.05)of glucose C,which suggests that the addition of nutrient elements promoted the microbial utilization of extraneous C in the soil,and stoichiometric ratio of the nutrient elements regulated the dynamic of glucose mineralization. With the addition of glucose-C,the decomposition of the soil native organic matter was inhibited,and the cumulative negative priming effect was -370 to -570 mg kg-1. The higher the amount of nutrient elements added,the stronger the negative priming effect observed,and the two were obviously in negative correlation(R2 = 0.66,p<0.05), indicating that the soil microbes preferentially utilize the added glucose-C to sustain their growth. The supply of N,P and S reduced the dependence of microbes on nutrient elements in the soil native organic matter,and thereby slow down the decomposition of soil organic matter. Conclusion]Mineralization of liable C in paddy soil is affected by C/N/P/S stoichiometric ratio. The addition of a high ratio of nutrient elements promotes mineralization of liable C in paddy soil,inhibits decomposition of native soil organic matter,and intensify negative priming effect. All the findings in this study demonstrate that application of liable C and fertilizers to paddy soils could effectively inhibit decomposition of soil native organic matter,and stimulate accumulation of soil organic matter,thus building up soil fertility.
Keywords:Paddy soil  Organic carbon mineralization  Priming effect  Nutrient stoichiometry
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《土壤学报》浏览原始摘要信息
点击此处可从《土壤学报》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