摘要
文章从土壤呼吸、土壤化学计量比、土壤碳氮循环、土壤微生物等方面综述了其对氮沉降增加的响应,结果表明:(1)土壤呼吸动态在不同气候区和不同氮沉降背景中表现不同;(2)氮沉降是土壤酸化的主要驱动因素,土壤碳氮循环也因氮沉降产生不同程度和方向的改变;(3)对于化学计量比来说,氮添加导致的土壤有效氮的增加是常见的,而对碳、磷的影响可能因地域而异;(4)土壤微生物对氮沉降引起的土壤理化性质变化是高度敏感的,并且土壤微生物量、多样性以及群落结构对氮沉降响应是高度可变的.
In this paper,the effects of increased nitrogen deposition are reviewed from the aspects of soil respiration,soil stoichiometric ratio,soil carbon and nitrogen cycle,and soil microorganisms.Specifically:(1)The dynamics of soil respiration varies in different climate zones and under different nitrogen deposition backgrounds;(2)Nitrogen deposition is the main driving factor for soil acidification,and soil carbon and nitrogen cycles are also changed to varying degrees and directions due to nitrogen deposition;(3)For the stoichiometric ratio,the increase of soil available nitrogen caused by nitrogen addition is common,while the effect on carbon and phosphorus may vary from region to region;(4)The soil microorganisms are highly sensitive to the change of soil physicochemical properties caused by nitrogen deposition.The nitrogen deposition is highly variable to soil microbial biomass,diversity and community structure.
作者
马富山
闫国永
邢亚娟
王庆贵
MA Fushan;YAN Guoyong;XING Yajuan;WANG Qinggui(College of Modern Agriculture and Ecological Environment,Heilongjiang University,150080,Harbin,Heilongjiang;School of Life Sciences,Qufu Normal University,273165,Qufu,Shandong,PRC)
出处
《曲阜师范大学学报(自然科学版)》
CAS
2023年第3期14-20,F0002,共8页
Journal of Qufu Normal University(Natural Science)
基金
国家自然科学基金(42230703)。
关键词
氮沉降
土壤呼吸
土壤碳氮循环
化学计量比
土壤微生物
nitrogen deposition
soil respiration
soil carbon and nitrogen cycle
stoichiometric ratio
soil microorganisms