评估美国南部森林生物能源对碳排放的影响
Fangwei Cheng1, David J Rossi2, Lilianna Gittoes1
1Andlinger Center for Energy and the Environment, Princeton University, Princeton, New Jersey 08544, United States.
Environmental science & technology
|February 17, 2025
概括
使用松木纸的森林生物能源项目可以在不到10年内实现碳回报,特别是碳捕获和储存 (CCS). 然而,硬木占主导地位的地区在项目生命周期内可能无法实现碳中和.
科学领域:
- 环境科学 环境科学
- 林业林业 林业 林业 林业
- 气候变化分析 气候变化分析
背景情况:
- 由于景观和时间的变化,从森林衍生的生物质能源中计算碳排放是复杂的.
- 了解森林生物能源对气候的影响对于可持续能源战略至关重要.
研究的目的:
- 开发一个框架来评估森林生物能源项目的动态生命周期温室气体排放.
- 确定美国南松木纸木生物能源项目的碳回报期和累积碳储存.
主要方法:
- 为动态生命周期温室气体排放评估制定了一个全面的框架.
- 将框架应用于美国南部的八个森林盆地,用于假设的生物能源项目 (2030-2060).
- 分析了森林类型,年龄分布和市场需求的变化,以计算碳回报期.
主要成果:
- 在不同的森林盆地中观察到碳回报时间的显著差异.
- 采用碳捕获和储存 (CCS) 的生物能源项目通常显示碳债务偿还速度更快.
- 在沿海平原/海湾沿岸地区,每年使用300万绿色原料和CCS的设施实现了不到10年的回报.
结论:
- 森林生物能源的碳回报高度依赖于当地生态和市场条件.
- CCS显著改善了森林生物能源项目的碳中和时间表.
- 在某些地区,如弗吉尼亚州的硬木占主导地位的地区,碳回报可能无法在30年的项目寿命内实现.
相关概念视频
The Carbon Cycle
36.9K
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.
36.9K
Global Climate Change
24.1K
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.
24.1K
Threats to Biodiversity
22.1K
There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
22.1K
The Sulfur Cycle
43.6K
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...
43.6K
Trophic Efficiency
20.3K
Trophic level transfer efficiency (TLTE) is a measure of the total energy transfer from one trophic level to the next. Due to extensive energy loss as metabolic heat, an average of only 10% of the original energy obtained is passed on to the next level. This pattern of energy loss severely limits the possible number of trophic levels in a food chain.
20.3K
Bioremediation
18.1K
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.
18.1K


