1997年印度尼西亚泥炭和森林火灾释放的碳量
Susan E Page1, Florian Siegert, John O Rieley
1Department of Geography, University of Leicester, Leicester LE1 7RH, UK. sep5@le.ac.uk
Nature
|November 8, 2002
概括
热带泥炭地储存了巨大的碳储量,对气候稳定至关重要. 1997年印度尼西亚泥炭地上的火灾释放了大量的碳,影响了全球大气中的二氧化碳水平.
科学领域:
- 环境科学 环境科学
- 气候科学 气候科学
- 生态生态学 生态生态学
背景情况:
- 热带泥炭地是重要的陆地碳汇.
- 泥炭沼泽森林受到排水和森林砍伐的威胁.
- 1997年厄尔尼诺现象在印度尼西亚的泥炭地引起了广泛的火灾.
研究的目的:
- 为量化1997年印尼泥炭地火灾造成的碳排放量.
- 评估这些排放对全球碳循环的影响.
主要方法:
- 卫星图像分析了位于中加利曼丹250万公的地区.
- 在地面测量泥炭燃烧深度.
- 将发现推断到整个印度尼西亚群岛.
主要成果:
- 研究区域的32%被烧毁,其中91.5%的被烧毁区域是泥炭地.
- 泥炭燃烧释放的碳量估计为0.190.23千兆.
- 1997年印度尼西亚泥炭和植被火灾的总碳排放量在0.81至2.57千兆之间.
结论:
- 1997年印度尼西亚的泥炭地大火是全球碳排放的主要来源.
- 这些排放量占全球每年化石燃料排放量的13-40%.
- 这些火灾导致大气二氧化碳度有史以来最大的增加.
相关概念视频
The Carbon Cycle
32.8K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
32.8K
The Sulfur Cycle
41.6K
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
41.6K
Bioremediation
17.4K
Bioremediation is the use of prokaryotes, fungi, or plants to remove pollutants from the environment. This process has been used to remove harmful toxins in groundwater as a byproduct of agricultural run-off and also to clean up oil spills.
17.4K
Global Climate Change
24.4K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
24.4K
Enthalpy and Heat of Reaction
8.3K
Combustion, commonly known as burning, is a reaction in which a substance reacts with an oxidizing agent, which in most cases is molecular oxygen, to liberate energy in the form of heat, light, or sound. The heat of combustion is also known as the enthalpy of combustion. The energy released when one mole of a substance undergoes complete combustion at constant pressure is called molar heat of combustion. Combustion reactions are exothermic; that is, they release energy, and their ΔH sign...
8.3K
Microbes and Climate Change
91
Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
91


