摘要
气候变化是全球变化的主要表现之一,它对全球陆地生态系统碳循环有着巨大的影响,具体表现在气温和降水两个方面。全球生态系统碳循环有多种影响因子,本文主要阐述NPP和土壤碳呼吸与气温和降水之间的关系。研究表明,气温与NPP表现出一定的纬度地带性;气候变暖会增加土壤呼吸,不过超过最适温度,土壤呼吸减弱,表现出一定的适应性;随着降水格局的改变,在不同时间尺度和地区上,NPP与降水关系也不同;在一定降水范围内,降水量对土壤呼吸的作用是不同的。水分对土壤呼吸的抑制作用会随降水的增加而减小。
Climate change is one of the main manifestations of global change.It has a huge impact on the global terrestrial ecosystem carbon cycle,which is reflected in both temperature and precipitation.The global ecosystem carbon cycle carbon cycle has a variety of impact factors.This paper mainly describes the relationship between NPP and soil carbon respiration and temperature and precipitation.There are some conclusions:temperature and NPP show a certain latitudinal zonal;climate warming will increase soil respiration,but soil moisture is weaker than the optimum temperature,showing a certain adaptability;in the pattern of precipitation change,NPP and precipitation are different in different time scales and regions;in a certain precipitation range,the effect of precipitation on soil respiration is different.The inhibition of soil moisture on soil respiration decreases with increasing precipitation.
作者
王天华
孟素昕
崔桂善
Wang Tianhua;Meng Suxin;Cui Guishan(Department of Geography,Yanbian University,Yanji 133002,China;Research Center for Wetland,Yanbian University,Yanji 133002,China)
出处
《中国资源综合利用》
2019年第1期105-108,共4页
China Resources Comprehensive Utilization
基金
国家自然科学基金项目(项目编号:413010052)的阶段性研究成果之一
关键词
气候变化
生态系统
碳循环
净初级生产力
土壤呼吸
climate change
ecosystem
carbon cycle
net primary productivity
soil respiration