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

岩溶土壤4大微生物生理类群数量的时空动态特征——以贵州花江喀斯特峡谷地区为例
引用本文:魏媛,张金池,俞元春,喻理飞.岩溶土壤4大微生物生理类群数量的时空动态特征——以贵州花江喀斯特峡谷地区为例[J].新疆农业大学学报,2010,33(5):380-384.
作者姓名:魏媛  张金池  俞元春  喻理飞
作者单位:1. 贵州财经学院,资源与环境管理学院,贵阳,550004;贵州大学,林学院,贵阳,550025
2. 南京林业大学,森林资源与环境学院,南京,210037
3. 贵州大学,林学院,贵阳,550025
基金项目:"十一五"国家科技支撑计划项目,国家重点基础研究发展计划(973计划)项目,国家自然科学基金资助项目,贵州省科学技术基金 
摘    要:对贵州花江喀斯特高原生态综合治理示范区内不同植被类型下土壤4大微生物生理类群(氨化细菌、硝化细菌、纤维素分解菌及固氮菌)数量的时空动态变化进行研究。结果表明,4种植被类型土壤4大微生物生理类群中,氨化细菌数量最大,固氮菌及纤维素分解菌次之,硝化细菌数量最小,分别占微生物总数的59.13%~66.32%,29.00%~35.69%,3.71%~4.03%和0.42%~1.22%。4种植被类型不同空间层次土壤4大微生物生理类群数量变化均较大,表土层(A层)的数量为下土层(B层)的1.21~1.68倍;不同植被类型土壤4大微生物生理类群数量及其总数季节变化明显,夏季达最大,冬季最小,年际变化基本一致,总体上表现为夏季秋季春季冬季的特点(P0.05);不同植被类型同一时间土壤4大微生物生理类群总数差异较大,为3.19×105~7.64×105CFU/(g干土),表现出森林灌木林草地裸荒地的分布特点。

关 键 词:岩溶植被  土壤微生物  时空动态  贵州花江

Spatial and Temporal Dynamic Characteristics of Four Microbial Physiological Groups of Karst Soil——A Case Study of Huajiang Karst Canyon Area, Guizhou
WEI Yuan,ZHANG Jing-chi,YU Yuan-chun,YU Li-fei.Spatial and Temporal Dynamic Characteristics of Four Microbial Physiological Groups of Karst Soil——A Case Study of Huajiang Karst Canyon Area, Guizhou[J].Journal of Xinjiang Agricultural University,2010,33(5):380-384.
Authors:WEI Yuan  ZHANG Jing-chi  YU Yuan-chun  YU Li-fei
Institution:WEI Yuan1,2,ZHNAG Jing-chi3,YU Yuan-chun3,YU Li-fei2 (1.College of Resources and Environmental Management,Guizhou College of Finance and Economics,Guiyang 550004,China,2.College of Forestry,Guizhou University,Guiyang 550025,3.College of Forestry Resources and Environment,Nanjing Forestry University,Jiangsu 210037,China)
Abstract:The spatial temporal dynamic characteristics about four microbial physiological groups(ammonifiers,nitrifying bacteria,cellulose decomposing microbes,nitrogen-fixing bacteria) were studied under different karst vegetations in Ecological Synthetically Controlled Demonstration Area in Karst plateau of Huajiang area in Guizhou.The results indicated that the amount of ammonifiers was the highest(59.13%~66.32%),which was followed by nitrogen-fixing bacteria and cellulose decomposing microbes(29.00%~35.69% and 3.71%~4.03%),nitrifying bacteria was the lowest one(0.42%~1.22%) there was great change of four microbial physiological groups of karst soil under different vegetations.The amount of four microbial physiological groups was extremely diversity in distinct vertical layers under four different vegetations.The amount of the groups in surface soil(level A) was 1.21~1.68 times higher than that in underlayer soil(level B).The seasonal changes of the amount of four microbial physiological groups and their total amount were significant under different vegetations,which came to the highest level in summer and the lowest in winter.Their annual change was almost the same.Generally speaking,the amount of the groups was the highest in summer,then in autumn,then in spring and was the lowest in winter(P〈0.05).Total amount of microbial physiological groups was much different under different vegetations.It ranged from 3.19×105 CFU/(g dry soil) to 7.64×105 CFU/(g dry soil),which showed distribution characteristics of the groups as follows: the amount of the groups in forest was higher than that in shrubbery,and followed by meadow and badlands.
Keywords:karst vegetation  soil-microorganisms  spatiotemporal dynamics  Huajiang area in Guizhou  
本文献已被 CNKI 维普 万方数据 等数据库收录!
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