固碳
植树造林
重新造林
环境科学
碳汇
生物量(生态学)
公顷
具有碳捕获和储存功能的生物能源
碳补偿
二氧化碳
碳纤维
林业
碳核算
碳循环
环境保护
气候变化
温室气体
农林复合经营
生态学
生态系统
地理
农业
生物
复合材料
材料科学
复合数
作者
Jingyun Fang,Anping Chen,Changhui Peng,Shuqing Zhao,Longjun Ci
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:2001-06-22
卷期号:292 (5525): 2320-2322
被引量:1423
标识
DOI:10.1126/science.1058629
摘要
The location and mechanisms responsible for the carbon sink in northern mid-latitude lands are uncertain. Here, we used an improved estimation method of forest biomass and a 50-year national forest resource inventory in China to estimate changes in the storage of living biomass between 1949 and 1998. Our results suggest that Chinese forests released about 0.68 petagram of carbon between 1949 and 1980, for an annual emission rate of 0.022 petagram of carbon. Carbon storage increased significantly after the late 1970s from 4.38 to 4.75 petagram of carbon by 1998, for a mean accumulation rate of 0.021 petagram of carbon per year, mainly due to forest expansion and regrowth. Since the mid-1970s, planted forests (afforestation and reforestation) have sequestered 0.45 petagram of carbon, and their average carbon density increased from 15.3 to 31.1 megagrams per hectare, while natural forests have lost an additional 0.14 petagram of carbon, suggesting that carbon sequestration through forest management practices addressed in the Kyoto Protocol could help offset industrial carbon dioxide emissions.
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