Titlebook: Carbonaceous Aerosol; András Gelencsér Book 2004 Springer Science+Business Media B.V. 2004 Aerosols.Atmospheric chemistry.Atmospheric effe

cognizant

Truong Phung,Ibrahim Sultan,Alberto Borettied organic speciation, primarily by means of gas chromatography-mass spectrometry (GC-MS). Very often the goal of such speciation studies is to obtain information only on specific target compounds, let they be potentially toxic compounds, important source tracers, or both. Most of these studies do n

讥笑

https://doi.org/10.1007/978-1-4614-6877-6’s point of view, these consequences can be summarized as direct effects, or direct forcing when only the anthropogenic contribution is taken into account. Throughout the discussion—except for the sub-chapter dealing with light-absorbing organic compounds—organic chemistry of the aerosol will not be

guardianship

秘传

Atmospheric and Oceanographic Sciences Libraryhttp://image.papertrans.cn/c/image/221672.jpg

弄皱

Carbonaceous Aerosol978-1-4020-2887-8Series ISSN 1383-8601 Series E-ISSN 2215-162X

引导

1383-8601 e coverage of the nature and atmospheric role of carbonaceous aerosol particles, these big unknowns of the global atmosphere. Even the concept of carbonaceous aerosol has just recently grown out of atmospheric pollution studies, without ever being anchored to solidified nomenclature and terminology.

匍匐前进

Nonlinear Forced Vibration of Nanobeamst typical of most analytical determinations. No uncertainty results from the definition itself (as in the case of all other sub-categories), though serious over- or underestimation of TC concentrations may come from sampling artifacts (adsorbed volatile organic species or volatilization losses, see subchapter 2.1).

思考才皱眉

Truong Phung,Ibrahim Sultan,Alberto Boretti information only on specific target compounds, let they be potentially toxic compounds, important source tracers, or both. Most of these studies do not—and cannot—pay attention to the concentration and physical-chemical properties of organic aerosol as a whole.

inflate

Major Carbonaceous Particle Types and their Sources,t typical of most analytical determinations. No uncertainty results from the definition itself (as in the case of all other sub-categories), though serious over- or underestimation of TC concentrations may come from sampling artifacts (adsorbed volatile organic species or volatilization losses, see subchapter 2.1).

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