土壤碳循环在全球气候变暖上具有重要的作用，也越来越受到人们的关注。
Soil carbon cycle plays an important role in global warming and concerns for it have been increased.
湖滨带等水陆交错区土壤碳循环是全球碳循环的一个重要的组成部分，但相关方面的研究还相当缺乏。
Soil carbon cycle in aquatic-terrestrial ecotone (e. g. , riparian zone) is an important component of global carbon cycle, but few researches are made on it.
土壤碳循环模型是定量实现土壤碳循环的模拟和预测的必不可少的手段，同时也是综合不同因子及其相互作用的有力工具。
The model of soil carbon cycling is important in carrying out simulating and predicting soil carbon cycling and is a effect tool synthesizing different factors and their interactions.
据邦德·兰姆伯蒂说，研究人员可能错误地理解了碳循环在北极土壤中起作用的方式。
According to Bond-Lamberty, researchers might have a flawed understanding of how carbon cycling works in Arctic soil.
最后提出应加强对土壤有机质周转模型、有机质组分，尤其是活性有机质以及有机质与全球碳循环关系的研究。
In the last part of this paper, some issues to be further researched were put forward, including the turnover model of som, its components, and its relationship with global carbon cycle.
土壤碳是陆地生态系统碳循环的重要组成部分。
Soil carbon is an important part of terrestrial ecosystem carbon cycle.
森林土壤在全球碳循环研究中占有重要位置，但其动力学特征等相关的数据却非常匮乏。
Forest soil plays an important role in global carbon cycle, but emphasized a lack of fundamental knowledge of soil carbon dynamics.
碳循环是一个生物地质化学循环圈，碳通过此循环在生物圈、土壤圈、地层、水圈、大气中交流。
The carbon cycle is the biogeochemical cycle by which carbon is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of the Earth.
土壤有机碳库在全球碳循环中起着重要作用。
Soil organic carbon pool plays an important role in global carbon cycle.
土壤碳是全球碳循环中的重要组成部分，土地利用方式的改变对土壤碳的源和汇具有很大的影响。
Soil carbon is a significant component of global carbon cycling, the change of land use pattern has a great influence on soil carbon source or sink.
干旱土壤占全球陆地总面积的40 %，因此，它在全球碳循环中占有重要的地位。
Dryland does most in global carbon cycling because it occupies 40% of the earths surface.
随着全球变暖趋势逐渐明显，土壤呼吸对温度的敏感性已成为陆地生态系统碳循环研究的重要内容之一。
With global warming, the response of soil respiration to it has been an important study field in global change issue.
森林土壤呼吸是陆地生态系统土壤呼吸的重要组成部分，其动态变化将会对全球碳循环产生深远的影响。
Forest soil respiration is an important part of the soil respiration in terrestrial ecosystems, the dynamic changes of which will bring far-reaching influence on the global carbon cycling.
土壤有机碳（SOC）是全球碳循环的重要组成部分，它具有直接影响全球碳平衡。
Soil organic carbon (SOC) is an important component of the global carbon cycle, and it has direct effects on the global carbon balance.
土壤有机碳是全球碳循环的重要组成部分，而大型土壤动物对土壤碳库的稳定性起着重要的决定作用。
Soil organic matter plays an important role in global carbon cycle; soil macrofauna are key organisms controlling soil carbon stability.
土壤有机质中的碳是地球碳库的重要组成部分，它参与全球碳循环。土壤有机质分解而产生的CO2和CH4是重要的温室气体。
The carbon in soil organic matter (SOM) is a significant component of the earth's carbon reservoirs, and participates in the global carbon circulation.
碳被人们以各种各样的形式应用最后转化为二氧化碳，然后进入大气中等待c 4植被来进行消耗并把它转化为土壤碳，从而最终完成了碳循环。
Carbon in its many forms converted by man to CO2e sits in the atmosphere awaiting the day C4 vegetation factory to consume it to make soil carbon completing the carbon Cycle.
碳被人们以各种各样的形式应用最后转化为二氧化碳，然后进入大气中等待c 4植被来进行消耗并把它转化为土壤碳，从而最终完成了碳循环。
Carbon in its many forms converted by man to CO2e sits in the atmosphere awaiting the day C4 vegetation factory to consume it to make soil carbon completing the carbon Cycle.
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