Technosol

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A Technosol in the FAO World Reference Base for Soil Resources [1] is a soil classification category of soil that combines soils whose properties and pedogenesis are dominated by their technical origin.[2] They contain either a significant amount of artefacts (something in the soil recognizably made or extracted from the earth by humans), some sort of geotechnical liner, or are sealed by technic hard rock (hard material created by humans, having properties unlike natural rock). They include soils from wastes (landfills, sludge, cinders, mine spoils and ashes), pavements with their underlying unconsolidated materials, soils with geomembranes and constructed soils in human-made materials. However, Technosols can also refer to a situation in which normal soil, such as a Chernozem, has been moved to a new location to act as a fill. If this fill is less than 50 cm, then the soil is called a Technosol. If fill material is greater than 50 cm deep, then the fill is designated by the original soil used to create the fill, in our example, a Chernozem. Technosols are often referred to as urban or mine soils. They are recognized in the new Russian soil classification system as Technogenic Superficial Formations.

Technosols are developed on all kinds of materials made or exposed by human activity that otherwise would not occur at the Earth’s surface. They occur mostly in urban and industrial areas, usually in small areas, and can be associated with other soil groups in a complex pattern. They are closely related to Anthrosols, which are soils created by the long term addition of organic matter to a soil, such as an old urban garden. Most of the research on Anthropogenic soils describe specific aspects of their biology, chemistry or physical properties, cultural heritage and human geography, erosion, wastes, pollution, fertilizer management, taxonomy. Very few of them,[3][4][5] try to answer to the question: How fast do they start pedogenesis (viz., differentiating horizons)? A Technosol could differentiate A and O horizons at rates of more than one centimeter per year.[6] Technosols are found throughout the world, e.g. at or near cities, roads, mines, refuse dumps, oil spills and coal fly ash deposits.

These soils are more likely to be contaminated than other soils. Many Technosols have to be treated with care as they may contain toxic substances resulting from industrial processes.

See also[edit]

References[edit]

  1. ^ FAO World Reference Base for Soil Resources
  2. ^ Rossiter, D G (2007). "Classification of Urban and Industrial Soils in the World Reference Base for Soil Resources". Journal of Soils and Sediments 7 (2): 96–100. doi:10.1065/jss2007.02.208. 
  3. ^ Bini, C., and Gaballo, S. (2006). "Pedogenic trends in anthrosols developed in sulfidic mine spoils: A case study in the Temperino mine archaeological area (Campiglia Marittima, Tuscany, Italy)". Quaternary International. 156–157 (1): 70–78. doi:10.1016/j.quaint.2006.05.033. 
  4. ^ Bokhorst, M.P., Duller, G.A.T., Van Mourik, J.M. (2005). "Optical dating of a Fimic Anthrosol in the southern Netherlands". Journal of Archaeological Science 32 (4): 547–553. doi:10.1016/j.jas.2003.11.011. 
  5. ^ Wei, C., Ni, J., Gao, M., Xie, D., and Hasegawa S. (2006). "Anthropic pedogenesis of purple rock fragments in Sichuan Basin, China". Catena 68 (1): 51–58. doi:10.1016/j.catena.2006.04.022. 
  6. ^ Scalenghe, R., Ferraris, S. (2009). "The first forty years of a Technosol". Pedosphere 19: 40–52. doi:10.1016/S1002-0160(08)60082-X.