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甘南草地土壤微生物与理化特性
引用本文:朱炜歆,索南吉,顾振宽,陈懂懂,张世虎,杜国祯.甘南草地土壤微生物与理化特性[J].草业科学,2012,29(10):1491-1496.
作者姓名:朱炜歆  索南吉  顾振宽  陈懂懂  张世虎  杜国祯
作者单位:兰州大学干旱与草地生态教育部重点实验室,甘肃兰州,730000;兰州大学干旱与草地生态教育部重点实验室,甘肃兰州730000 兰州大学草地农业科技学院,甘肃兰州730020;中国科学院西北高原生物研究所,青海西宁810001 中国科学院高原生物适应与进化重点实验室,青海西宁810001;西北师范大学生命科学学院,甘肃兰州,730070
基金项目:国家自然科学基金重点项目,国家科技支撑计划项目
摘    要:在甘肃省甘南州境内,土壤微生物呼吸强度在不同草地类型草地上由大到小的顺序:0~15 cm深度为沼泽化草甸>高寒灌丛草甸>高寒草甸>亚高寒草甸>山地草原,15~30 cm深度为沼泽化草甸>亚高寒草甸>山地草原>高寒灌丛草甸>高寒草甸,30~60 cm深度为沼泽化草甸>山地草原>亚高寒草甸>高寒草甸>高寒灌丛草甸;微生物碳在不同草地类型草地上由大到小的顺序:0~15 cm与15~30 cm深度均为沼泽化草甸>高寒灌丛草甸>高寒草甸>亚高寒草甸>山地草原,30~60 cm深度为沼泽化草甸>亚高寒草甸>高寒灌丛草甸>高寒草甸>山地草原。同一草地类型的土壤呼吸强度、微生物碳都在各自土壤深度下随深度增加而减小,代谢熵的变化趋势刚好相反,微生物商的变化趋势不明显。土壤呼吸强度、微生物碳均分别与土壤含水量、有机碳、全氮呈极显著正相关(P<0.01),而代谢熵与之呈极显著负相关(P<0.01),微生物商与含水量、全氮呈极显著正相关(P<0.01),而与有机碳呈极显著负相关(P<0.01)。

关 键 词:青藏高原  草地类型  土壤深度  微生物量  退化程度

Soil properties associated with microbe in different types of Gannan grassland
ZHU Wei-xin,SUO Nan-ji,GU Zhen-kuan,CHEN Dong-dong,ZHANG Shi-hu,DU Guo-zhen.Soil properties associated with microbe in different types of Gannan grassland[J].Pratacultural Science,2012,29(10):1491-1496.
Authors:ZHU Wei-xin  SUO Nan-ji  GU Zhen-kuan  CHEN Dong-dong  ZHANG Shi-hu  DU Guo-zhen
Institution:1,2(1.Key Laboratory of Arid and Grassland Ecology with the Ministry of Education, Lanzhou University,Lanzhou 730000,China; 2.College of Pastoral Agriculture Science and Technology,Lanzhou University,Lanzhou 730020,China; 3.The Northwest Institute of Plateau Biology,Chinese Academy of Sciences,Xining 810001,China; 4.Key Laboratory of Adaptation and Evolution of Plateau Biota,Northwest Institute of Plateau Biology, Chinese Academy of Sciences,Xining 810001,China; 5.School of Sciences,Northwest Normal University,Lanzhou 730070,China)
Abstract:In Gannan region of Gansu province, the numerical sizes of respiration rates of different grassland type soils are: swamping meadow>alpine shrub meadow>alpine meadow>sub alpine meadow>upland meadow (0-15 cm), swamping meadow>sub alpine meadow>upland meadow>alpine shrub meadow>alpine meadow (15-30 cm), and swamping meadow>upland meadow>sub alpine meadow>alpine meadow>alpine shrub meadow (30-60 cm). The numerical sizes of soil microbial biomass carbon of different grassland type soils are: swamping meadow>alpine shrub meadow>alpine meadow>sub alpine meadow>upland meadow (0-15, 15-30 cm), and swamping meadow>sub alpine meadow>alpine shrub meadow>alpine meadow>upland meadow (30-60 cm). Respiration and microbial biomass carbon of different grassland type soils decreased with soil depth, while respiratory quotient increased and microbial quotient has no significant change. There was a significant positive correlation (P<0.01) between respiration, microbial biomass carbon and soil moisture, total organic carbon, total nitrogen, and a significant negative correlation (P<0.01) between respiratory quotient and soil moisture, total organic carbon, total nitrogen. A significant positive correlation (P<0.01) exists between microbial quotient and soil moisture, total nitrogen, while a significant negative correlation (P<0.01) exists between microbial quotient and total organic carbon.
Keywords:Tibetan plateau  grassland types  depth of soil  microbial biomass  degree of degradation
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