概括
埃内韦塔克环礁空气中的土壤尘埃度在1979年5个月内显著下降. 这种可能来自中国的尘埃可能对北太平洋深海沉积物有很大贡献.
科学领域:
- 大气科学 大气科学
- 海洋学 海洋学 海洋学
- 地质化学 地质化学
背景情况:
- 伊内韦塔克环礁位于太平洋的偏远地区,是监测远程大气运输的理想地点.
- 了解空气中的尘埃的来源和沉积率对于解释海洋沉积物组成和古气候记录至关重要.
研究的目的:
- 量化埃内韦塔克环礁空气中的土壤尘埃的度和时间趋势.
- 调查观察到的尘埃事件的潜在起源和沉积意义.
主要方法:
- 空气中的颗粒物被收集并分析了土壤尘埃度.
- 在五个月的时间内分析了尘埃度的时间趋势.
主要成果:
- 1979年4月,埃内韦塔克环礁空气中的土壤尘埃度被测定为2.3μg/m3.
- 度在1979年9月稳步下降至0.02μg/m3.
- 沉积速度估计大约为每1000年0.3毫米.
结论:
- 在Enewetak环礁观察到的春季尘埃事件可能起源于东亚来源,如中国.
- 计算的沉积率表明,这种尘埃是北太平洋深海沉积物的重要潜在贡献者.
相关概念视频
Global Climate Change
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.
What is Climate?
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Variation of Atmospheric Pressure
Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Boundary Layer Characteristics
When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
The Sulfur Cycle
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...
Precipitation Processes
The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...

