陆地溶解有机碳向河流系统横向运输的历史趋势和驱动因素
Mahdi Andre Nakhavali1, Ronny Lauerwald2, Pierre Regnier3
1International Institute for Applied Systems Analysis (IIASA), Laxenburg, Austria.
The Science of the total environment
|February 1, 2024
概括
大气中的二氧化碳施肥显著增加了全球17%的溶解有机碳 (DOC) 泄漏到河流中. 气候变化也影响了DOC的动态,特别是在北极地区,而土地利用变化起到了很小的作用.
科学领域:
- 环境科学 环境科学
- 地球系统科学 地球系统科学
- 生物地质化学生物地质化学
背景情况:
- 溶解有机碳 (DOC) 对陆地碳循环和陆地-水域流动至关重要.
- 以前的研究主要集中在影响DOC浸的土地利用变化上,低估了其他因素.
研究的目的:
- 从1860年到2010年,模拟和分析DOC入全球河流的时空模式.
- 量化大气二氧化碳受精和气候变化对DOC出的影响.
- 重新评估土地利用变化在DOC出中的作用.
主要方法:
- 使用基于过程的陆地生态系统模型JULES-DOCM.
- 从1860年到2010年,全球模拟的DOC出模式.
- 采用了因数模拟方法来隔离二氧化碳施肥的影响.
主要成果:
- 到2010年,全球DOC水量增加了17%,达到292 Tg C yr-1 .
- 大气中的二氧化碳施肥是主要的驱动因素,提高了植被生产力和土壤碳.
- 北极地区显示出气候变化的显著影响,有时超过二氧化碳的影响;热带地区由于土壤湿度/温度变化而增加较小.
- 发现土地利用变化的影响比先前假设的要小.
结论:
- 大气中的二氧化碳施肥和气候变化是DOC出的主要调节因素.
- 这些发现提升了对陆地碳动态和全球碳预算的理解.
- 对二氧化碳和气候的DOC浸出反应的区域差异需要进行本地研究.
相关概念视频
The Carbon Cycle
37.6K
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.
37.6K
The Sulfur Cycle
44.2K
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...
44.2K
What are Biogeochemical Cycles?
31.9K
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
31.9K
The Water Cycle
24.5K
The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
24.5K
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
The Phosphorus Cycle
36.9K
Unlike carbon, water, and nitrogen, phosphorus is not present in the atmosphere as a gas. Instead, most phosphorus in the ecosystem exists as compounds, such as phosphate ions (PO43-), found in soil, water, sediment and rocks. Phosphorus is often a limiting nutrient (i.e., in short supply). Consequently, phosphorus is added to most agricultural fertilizers, which can cause environmental problems related to runoff in aquatic ecosystems.
36.9K


