Anthropogenic metabolism

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Anthropogenic metabolism, also referred to as metabolism of the anthroposphere, is a term used in industrial ecology, material flow analysis, and waste management to describe the material and energy turnover of human society. It emerges from the application of systems thinking to the industrial and other man-made activities and it is a central concept of sustainable development. In modern societies, the bulk of anthropogenic (man-made) material flows is related to one of the following activities: sanitation, transportation, habitation, and communication, which were "of little metabolic significance in prehistoric times". [1] Global man-made stocks of steel in buildings, infrastructure, and vehicles, for example, amount to about 25 Gigatonnes (more than three tonnes per person), a figure that is surpassed only by construction materials such as concrete. [2] Sustainable development is closely linked to the design of a sustainable anthropogenic metabolism, which will entail substantial changes in the energy and material turnover of the different human activities. Anthropogenic metabolism can be seen as synonymous to social or socioeconomic metabolism. It comprises both industrial metabolism and urban metabolism.

Contents

Negative effects

In layman's terms, anthropogenic metabolism indicates the human impact on the world by the modern industrialized world. Much of these impacts include waste management, ecological footprints, water footprints, and flow analysis (i.e., the rate at which each human depleted the energy around them). Most anthropogenic metabolism happens in developed countries. According to Rosales, "Economic growth is at present the main cause of increased climate change, and climate change is a main mechanism of biodiversity loss; because of this, economic growth is a major catalyst of biodiversity loss." [3]

A water footprint is the amount of water that each person uses in their daily lives. Most of the world's water is salt water which cannot be used in human food or water supplies. Therefore, the freshwater sources that were once plentiful are now being diminished due to anthropogenic metabolism of the growing population. The water footprint encompasses how much fresh water is needed for each consumer's needs. According to J. Allan, "there is a huge impact of water use on stores of surface and groundwater and on flows to which water is returned after use. These impacts are shown to be particularly high for manufacturing industries. For example, that there are less than 10 economies worldwide that have a significant water surplus, but that these economies have successfully met, or have the potential to meet, the water deficits of the other 190 economies. Consumers enjoy the delusion of food and water security provided by virtual water trade. [4]

In addition, the ecological footprint is a more economical and land-focused way of looking at human impact. Developed countries tend to have higher ecological footprints, which do not strictly correspond to a country's total population. According to research by Dias de Oliveira, Vaughan and Rykiel, "The Ecological Footprint...is an accounting tool based on two fundamental concepts, sustainability and carrying capacity. It makes it possible to estimate the resource consumption and waste assimilation requirements of a defined human population or economy sector in terms of corresponding productive land area." [5]

One of the major cycles that humans can contribute to that cause a major impact on climate change is the nitrogen cycle. This comes from nitrogen fertilizers that humans use. Gruber and Galloway have researched, "The massive acceleration of the nitrogen cycle caused by the production and industrial use of artificial nitrogen fertilizers worldwide has led to a range of environmental problems. Most important is how the availability of nitrogen will affect the capacity of Earth's biosphere to continue absorbing carbon from the atmosphere and to thereby continue helping to mitigate climate change." [6]

The carbon cycle is another major contributor to climate change primarily from anthropogenic metabolism. A couple examples of how humans contribute to the carbon in the atmosphere is by burning fossil fuels and deforestation. By taking a close look at the carbon cycle Peng, Thomas and Tian have discovered that, "It is recognized that human activities, such as fossil fuel burning, land-use change, and forest harvesting at a large scale, have resulted in the increase of greenhouse gases in the atmosphere since the onset of the industrial revolution. The increasing amounts of greenhouse gases, particularly CO2 in the atmosphere, is believed to have induced climate change and global warming." [7]

Impact of climate change extend beyond humans. There is a forecast for extinctions of species because of their habitats being affected. An example of this is marine animals. There are major impacts on the marine systems as a result of anthropogenic metabolism, according to Blaustein, the dramatic findings indicate that "every square kilometer [is] affected by some anthropogenic driver of ecological change". [8]

The negative effects of anthropogenic metabolism are seen through the water footprint, ecological footprint, carbon cycle, and the nitrogen cycle. Studies on the marine ecosystem that show major impacts by humans and developed countries which include more industries, thus more anthropogenic metabolism.

See also

Related Research Articles

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An ecosystem consists of all the organisms and the physical environment with which they interact. These biotic and abiotic components are linked together through nutrient cycles and energy flows. Energy enters the system through photosynthesis and is incorporated into plant tissue. By feeding on plants and on one another, animals play an important role in the movement of matter and energy through the system. They also influence the quantity of plant and microbial biomass present. By breaking down dead organic matter, decomposers release carbon back to the atmosphere and facilitate nutrient cycling by converting nutrients stored in dead biomass back to a form that can be readily used by plants and microbes.

<span class="mw-page-title-main">Nitrogen cycle</span> Biogeochemical cycle by which nitrogen is converted into various chemical forms

The nitrogen cycle is the biogeochemical cycle by which nitrogen is converted into multiple chemical forms as it circulates among atmospheric, terrestrial, and marine ecosystems. The conversion of nitrogen can be carried out through both biological and physical processes. Important processes in the nitrogen cycle include fixation, ammonification, nitrification, and denitrification. The majority of Earth's atmosphere (78%) is atmospheric nitrogen, making it the largest source of nitrogen. However, atmospheric nitrogen has limited availability for biological use, leading to a scarcity of usable nitrogen in many types of ecosystems.

Industrial ecology (IE) is the study of material and energy flows through industrial systems. The global industrial economy can be modelled as a network of industrial processes that extract resources from the Earth and transform those resources into by-products, products and services which can be bought and sold to meet the needs of humanity. Industrial ecology seeks to quantify the material flows and document the industrial processes that make modern society function. Industrial ecologists are often concerned with the impacts that industrial activities have on the environment, with use of the planet's supply of natural resources, and with problems of waste disposal. Industrial ecology is a young but growing multidisciplinary field of research which combines aspects of engineering, economics, sociology, toxicology and the natural sciences.

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<span class="mw-page-title-main">Biogeochemical cycle</span> Chemical transfer pathway between Earths biological and non-biological parts

A biogeochemical cycle, or more generally a cycle of matter, is the movement and transformation of chemical elements and compounds between living organisms, the atmosphere, and the Earth's crust. Major biogeochemical cycles include the carbon cycle, the nitrogen cycle and the water cycle. In each cycle, the chemical element or molecule is transformed and cycled by living organisms and through various geological forms and reservoirs, including the atmosphere, the soil and the oceans. It can be thought of as the pathway by which a chemical substance cycles the biotic compartment and the abiotic compartments of Earth. The biotic compartment is the biosphere and the abiotic compartments are the atmosphere, lithosphere and hydrosphere.

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<span class="mw-page-title-main">Environmental degradation</span> Any change or disturbance to the environment perceived to be deleterious or undesirable

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<span class="mw-page-title-main">Green urbanism</span> Practice of creating communities beneficial to humans and the environment

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<span class="mw-page-title-main">Social metabolism</span> Study of materials and energy flows between nature and society

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References

  1. Brunner Paul H. and Rechberger H. (2002) Anthropogenic Metabolism and Environmental Legacies Archived December 17, 2008, at the Wayback Machine in Encyclopedia of Global Environmental Change ( ISBN   0-471-97796-9)
  2. Müller, D.B., et al. 2013. Carbon emissions of infrastructure development. Environmental Science and Technology. 47(20) 11739-11746.
  3. Rosales, J. (2008). Economic Growth, Climate Change, Biodiversity Loss: Distributive Justice for the Global North and South. Conservation Biology, 22(6), 1409-1417.
  4. Allan, J. (2009). Virtual Water in the Real World. Conservation Biology, 23(5), 1331-1332.
  5. Dias de Oliveira, M. E., Vaughan, B. E., & Rykiel, E. (2005). Ethanol as Fuel: Energy, Carbon Dioxide Balances, and Ecological Footprint. Bioscience, 55(7), 593-602.
  6. Gruber, N. Galloway, J.N. (2008). An Earth-system perspective of the global nitrogen cycle. Nature, 451, 293-296.
  7. Peng, Y., Thomas, S. C., & Tian, D. (2008). Forest management and soil respiration: Implications for carbon sequestration. Environmental Reviews, 1693-111.
  8. Blaustein, R. (2008). Global Human Impacts. Bioscience, 58(4), 376.

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