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根系隔离和氮添加对湿性常绿阔叶林土壤碳氮组分的影响 被引量:5
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作者 陈冠陶 李顺 +4 位作者 彭天驰 邱细容 陈雨芩 马豪宇 涂利华 《应用与环境生物学报》 CAS CSCD 北大核心 2018年第1期125-131,共7页
持续增加的氮(N)沉降改变了森林生态系统土壤的养分状况和光合产物的分配,从而影响了根系分泌物质和量以及根凋落物分解过程.为揭示根系在土壤碳(C)、N组分响应N沉降增加中的作用,于2013年4月起在瓦屋山湿性常绿阔叶林中开展N添加试... 持续增加的氮(N)沉降改变了森林生态系统土壤的养分状况和光合产物的分配,从而影响了根系分泌物质和量以及根凋落物分解过程.为揭示根系在土壤碳(C)、N组分响应N沉降增加中的作用,于2013年4月起在瓦屋山湿性常绿阔叶林中开展N添加试验,N添加1年后利用壕沟法在各样地设置根系隔离子样方.N添加和根系隔离分别处理3.5年和2.5年后,取土样分析各处理腐殖土壤层(A层)和矿质土壤表层(B层)的C、N组分.结果表明:根系隔离显著降低了A层土壤的总有机C和总N含量(P〈0.05);N添加显著提高了A、B土壤层硝态N含量而降低了土壤pH值,且土壤pH值与土壤硝态N之间呈极显著的负相关关系(P〈0.05);N添加与根系隔离交互效应不显著.本研究表明根系对湿性常绿阔叶林土壤C、N储存有重要影响,而N沉降可提高土壤N可利用性并导致土壤酸化. 展开更多
关键词 根系隔离 氮沉降 碳组分 氮组分 湿性常绿落叶林
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Soil Microbial Population Dynamics along a Chronosequence of Moist Evergreen Broad-leaved Forest Succession in Southwestern China 被引量:10
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作者 ZHU Wanze CAI Xiaohu +5 位作者 LIU Xingliang WANG Jinxi CHENG Song ZHANG Xiuyan LI Dengyu LI Maihe 《Journal of Mountain Science》 SCIE CSCD 2010年第4期327-338,共12页
Little is known about whether soil microbial population dynamics are correlated with forest succession.To test the hypotheses that(1) soil microbial composition changes over successional stages,and(2) soil microbial d... Little is known about whether soil microbial population dynamics are correlated with forest succession.To test the hypotheses that(1) soil microbial composition changes over successional stages,and(2) soil microbial diversity is positively correlated with plant species diversity,we determined the soil microbial populations,community composition,and microflora diversity in evergreen broad-leaved forests along a chronosequence of vegetation succession from 5 to 300 years in southwestern China.The soil microbial community was mainly composed of bacteria(87.1-98.7% of the total microorganisms and 10 genera identified),fungi(0.3-4.0%,7 genera),and actinomycetes(2.1-9.1%,8 species and 1 genus).There were significant differences in soil microbial populations among different successional stages and within the four seasons.The seasonal variations of the soil microbial community may be associated with the seasonal changes in environmental conditions.The changes in soil microbial diversity(Shannon-Wiener index) with successional time followed one-humped,convex curves peaked at-100 years since restoration,which is identical with the trends of the aboveground plant diversity.Higher plant diversity resulting in enhanced nutrient flow and root exudation may contribute to positive relationships between the soil microbial diversity and plant diversity.Hence,decreases in soil microbial diversity in the late-successional stages appear to be related to the net loss in species richness that occurs after 100 years since restoration.Our findings confirm the intermediate disturbance hypothesis that suggests diversity peaks at midsuccessional stages. 展开更多
关键词 ACTINOMYCETES Bacteria Fungi Microbial diversity Moist evergreen broad-leavedforest Seasonal dynamics
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