Mannion Carbon and its Domestication

1. Auflage 2006
ISBN: 978-1-4020-3958-4
Verlag: Springer Netherlands
Format: PDF
Kopierschutz: 1 - PDF Watermark

E-Book, Englisch, 329 Seiten, Web PDF

Reihe: Earth and Environmental Science

Carbon is chemically versatile and is thus the body and soul of biological, geological, ecological and economic systems. Its appropriation by humans through diversion of its biogeochemical cycle has been a mainstay of development. This domestication is characterized by a number of thresholds: control of fire, development of agriculture, expansion of Europe, fossil-fuel use and biotechnology. All have exacted an environmental toll, not least being climatic change and biodiversity loss. Carbon management now and in the future is a ‘hot’ political issue.

There is no existing book which focuses on the pivotal role of carbon in the environment and society and the ways in which carbon has been domesticated in time and space to generate wealth and political advantage. Students of environmental science, geography, biology and general science will find this work invaluable as a cross-disciplinary text.

Zielgruppe

Science, general, Geography (general), Life Sciences, general, Environment, general, Environmental Management

Autoren/Hrsg.

Mannion, A.M.

Fachgebiete

• Naturwissenschaften Chemie Anorganische Chemie Festkörperchemie
• Geowissenschaften Umweltwissenschaften Umweltmanagement, Umweltökonomie
• Naturwissenschaften Biowissenschaften Biowissenschaften
• Geowissenschaften Geographie | Raumplanung Geographie: Allgemeines, Karten & Atlanten
• Geowissenschaften Umweltwissenschaften Umweltwissenschaften
• Interdisziplinäres Wissenschaften Wissenschaften Interdisziplinär Naturwissenschaften, Technik, Medizin
• Naturwissenschaften Chemie Anorganische Chemie Komplexchemie
• Interdisziplinäres Wissenschaften Wissenschaft und Gesellschaft | Kulturwissenschaften
• Naturwissenschaften Chemie Anorganische Chemie Nichtmetallische Chemie

Inhaltsverzeichnis

THE CHEMISTRY OF CARBON.- THE BIOLOGY OF CARBON.- THE GEOLOGY OF CARBON.- THE HISTORY AND CONSEQUENCES OF CARBON DOMESTICATION.- THE GEOGRAPHY OF CARBON.- THE POLITICIZATION OF CARBON.- CONCLUSION AND PROSPECT.

Leseproben

2 THE CHEMISTRY OF CARBON (p. 23)

The fact that carbon has a valency of four, i.e. in the outermost shell surrounding the nucleus of the atom there are four electrons (see Section 1.1 and Figure 1.1), is the key to why carbon is so versatile. This outermost shell can accommodate eight electrons so each carbon atom has the capacity to share electrons with as many as four different atoms, including other carbon atoms. Thus carbon has the capacity to combine with many different elements to produce a vast array of compounds.

This is one reason why carbon is so important in nature and to society. Although most carbon compounds are associated with life and are thus referred to as organic, some carbon compounds are described as mineral because they are mainly, but not always exclusively, the product of geological rather than biological processes.

Truly mineral forms of carbon include its allotropes, comprising pure carbon in various structural forms, e.g. graphite, diamond and soot (see Section 1.1 and Figure 1.2). Such substances are, however, important because they have decorative or industrial uses and their extraction from geological environments is a wealth generating activity. Many other compounds containing carbon have also been formed geologically.

Such minerals include calcite (calcium carbonate), magnesite (magnesium carbonate) and dolomite (calcium magnesium carbonate). They can also be produced biologically as shells of marine organisms, which, as they become compressed through geological processes, produce limestone and chalk. Throughout Earth history the formation and weathering of these materials has played an important role in global climate because of the link between carbon dioxide in the atmosphere and shellproducing marine organisms.

These are discussed in Chapter 4 because of their importance in the geology of carbon burial and change in atmospheric composition. The fossil fuel reservoirs are also carbon-rich minerals which are linked with life. Their formation sequestered carbon from the active biosphere, a process that also had an impact on global climate because of the withdrawal of carbon dioxide from the atmosphere.They are also discussed in Chapter 4.

However, another relatively minor group of carbonates, including malachite (copper carbonate) and rhodochrosite (manganese carbonate), are considered here because they form through geological rather than biological processes. In contrast there are millions of organic compounds. These can be classified in many different ways including a basic subdivision into two groups: naturally occurring and synthetic compounds.

The former are found in living organisms, or in the environment having been produced by living organisms whilst synthetic compounds are so-called because they are artificial, i.e. they have been created in the laboratory and do not occur in nature. They have usually been created for a specific purpose, such as pharmaceuticals, crop protection chemicals and plastics. Usually they are complex molecules and comprise many carbon atoms combined with more than one other atom.

The huge range of organic compounds means that they can also be classified as simple or complex. Simple compounds contain one or two carbon atoms combined with between one and four atoms of other elements.

Über Autor(innen)

A.M. Mannion, University of Reading, Reading, U.K.