By Professor Mark Z. Jacobson
This publication presents a finished creation to the historical past and technology of significant pollution concerns. It starts with an creation to the fundamental atmospheric chemistry and the background of discovery of chemical compounds within the surroundings, after which strikes directly to a dialogue of the evolution of the earth's surroundings, and the constitution and composition of the present-day surroundings. It additionally deals a entire and available dialogue of the 5 significant atmospheric toxins subject matters: city outside pollution, indoor pollution, acid deposition, stratospheric ozone relief, and international weather swap.
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Additional resources for Atmospheric pollution: history, science, and regulation
2. SPECTRA OF THE RADIATION OF THE SUN AND THE EARTH Life on Earth would not have evolved to its present state without heating by solar radiation. Next, the sun’s radiation spectrum is described. Radiation is the emission or propagation of energy in the form of a photon or an electromagnetic wave. Whether radiation is considered a photon or a wave is still debated. A photon is a particle or quantum of energy that has no mass, no electric charge, and an indeﬁnite lifetime. An electromagnetic wave is a disturbance traveling through a medium, such as air or space, that transfers energy from one object to another without permanently displacing the medium itself.
In this chapter, the evolution of the background atmosphere is discussed. The discussion requires a description of the sun and its origins because sunlight has affected much of the evolution of the Earth’s atmosphere. The description also requires a discussion of the Earth’s composition and structure because the inner Earth affects atmospheric composition through outgassing, and the crust affects atmospheric composition through exchange processes, including soil-dust emission. Earth’s earliest atmosphere contained mostly hydrogen and helium.
Chlorophyll a absorbs red wavelengths more efﬁciently than does chlorophyll b, and chlorophyll b absorbs blue wavelengths more efﬁciently than does chlorophyll a. Because neither chlorophyll absorbs between 500 and 600 nm, the green part of the visible spectrum, green wavelengths are reﬂected by chlorophyll, giving leaves a green color. Photosynthetic bacteria generally appear purple, blue, green, or yellow, indicating that their pigments absorb blue, green, and/or red wavelengths to different degrees.