Related Experiment Video
Updated: Jun 21, 2026

09:01
An Ultra-clean Multilayer Apparatus for Collecting Size Fractionated Marine Plankton and Suspended Particles
Published on: April 19, 2018
Surface-level fine particle mass concentrations: from hemispheric distributions to megacity sources
1Envair/Aerochem, Placitas, NM 87043, USA. dhidy113@comcast.net
Journal of the Air & Waste Management Association (1995)
|August 4, 2009
Summary
Fine particle chemical climate knowledge has improved since 1990. Global distributions show highest concentrations near industrial areas, dominated by sulfate and organic carbon.
Area of Science:
- Atmospheric chemistry and physics
- Environmental science
- Geochemistry
Background:
- Significant advancements in understanding the chemical climate of fine particles have occurred since 1990.
- Junge's 1960s compilation provided foundational data for fine particle research.
Purpose of the Study:
- To estimate the worldwide baseline distribution of fine particle concentrations.
- To deduce the geographical distribution of fine particle characteristics.
- To analyze the composition and sources of fine particles on synoptic and continental scales.
Main Methods:
- Synthesis of disparate ground-level measurement data from all continents.
- Analysis of fine particle mass concentrations and chemical composition.
- Geographical mapping of particle characteristics and source attribution.
Main Results:
- Worldwide fine particle concentrations vary, with highest regional mass concentrations (1-80 microg/m3) near high population and industrial density areas.
- Fine particles are dominated by non-sea salt sulfate and organic carbon (approx. 25% each by mass).
- Long-range transport of pollution creates persistent regional gradients, especially in the Northern Hemisphere; data is sparse in the Southern Hemisphere.
Conclusions:
- Fine particle distribution and composition are strongly influenced by anthropogenic sources in populated and industrialized regions.
- Natural sources like dust, sea salt, and wildfires contribute significantly to intermittent particle loadings.
- Understanding fine particle chemical climate is crucial for air quality assessment and climate modeling.
Related Concept Videos
Linear Approximations
For a differentiable function of two variables, linear approximation estimates values near a known point by replacing the curved surface with its tangent plane. Consider the function\begin{equation*}f(x,y)=x^2+3y^2\end{equation*}near the point (2, 1). The exact value at this point is f(2, 1) = 22 + 3(1)2 = 4 + 3 = 7.The linear approximation of f(x, y)) near (a, b) is\begin{equation*}L(x,y)=f(a,b)+f_x(a,b)(x-a)+f_y(a,b)(y-b)\end{equation*}First, compute the partial derivatives: fx(x, y) = 2x and...
Surface Integrals of Vector Fields: Flux
Understanding the movement of air masses is fundamental to meteorological analysis and atmospheric modeling. A key component in this process is quantifying the total mass of air that flows into or out of a defined region over a specified period of time. This is achieved by evaluating the mass flux across a boundary surface, a conceptual tool that simplifies the complex dynamics of atmospheric systems.To begin, an imaginary boundary surface S is introduced, enclosing the region of interest. The...
High-Resolution Mass Spectrometry (HRMS)
The resolution of a mass spectrometer depends on the efficiency of separating ions with different ion masses. The mass of an atom is approximated to the sum of the masses of protons and neutrons inside, considering the masses of protons and neutrons as equal. However, the masses of the proton (1.6726 × 10−24 g) and neutron (1.6749 × 10−24 g) are not truly equal. There is a minor error in the expression of atomic masses relative to the simplest atom of hydrogen. For example, the mass of helium...
Maxwell-Boltzmann Distribution: Problem Solving
Individual molecules in a gas move in random directions, but a gas containing numerous molecules has a predictable distribution of molecular speeds, which is known as the Maxwell-Boltzmann distribution, f(v).
This distribution function f(v) is defined by saying that the expected number N (v1,v2) of particles with speeds between v1 and v2 is given by
This distribution function f(v) is defined by saying that the expected number N (v1,v2) of particles with speeds between v1 and v2 is given by
Mass Spectrum
A mass spectrum is the graphical representation of the relative abundance of the charged fragments in an analyte plotted against their mass-to-charge ratio (m/z). The plot's x-axis represents the ratio of the mass of the charged fragment to the number of charges it carries. The y axis of the plot represents the relative abundance of each charged species. The relative abundance is calculated from the signal intensity of each charged species recorded at the detector. The most intense signal (the...
Atomic Emission Spectroscopy: Overview
Atomic emission spectroscopy (AES) is an analytical technique used to determine the elemental composition of a sample by analyzing the light emitted from excited atoms. In AES, atoms in a sample are excited to higher energy levels by thermal energy from high-temperature sources, such as plasma, arcs, or sparks. When these excited atoms return to lower energy states, they emit light at specific wavelengths characteristic of each element. The resulting atomic emission spectrum, which consists of...

