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Chernozem

Chernozem (from Russian: чернозём, tr. chernozyom, IPA: [tɕɪrnɐˈzʲɵm]; "black ground"),[1][2] also called black soil, is a black-colored soil containing a high percentage of humus[3] (4% to 16%) and high percentages of phosphorus and ammonia compounds.[4] Chernozem is very fertile soil and can produce high agricultural yields with its high moisture storage capacity.[a] Chernozems are a Reference Soil Group of the World Reference Base for Soil Resources (WRB).

Chernozem
Chernozemic soil
Mollisol (USDA-NRCS)
Used inWRB, other
WRB codeCH
ProfileAhBC
Parent materialLoess
ClimateHumid continental

Distribution

 
Distribution of Chernozem soils according to the World Reference Base for Soil Resources classification:
  Dominant (more than 50% of soil cover)
  Codominant (25-50%)
  Associated (5-25%)

The name comes from the Russian terms for black and soil, earth or land (chorny + zemlya).[2][3] The soil, rich in organic matter presenting a black color, was first identified by Russian geologist Vasily Dokuchaev in 1883 in the tallgrass steppe or prairie of European Russia.

Chernozem cover about 230 million hectares of land. There are two "chernozem belts" in the world. One is the Eurasian steppe which extends from eastern Croatia (Slavonia), along the Danube (northern Serbia, northern Bulgaria (Danubian Plain), southern and eastern Romania (Wallachian Plain and Moldavian Plain), and Moldova, to northeast Ukraine across the Central Black Earth Region of Central Russia, southern Russia into Siberia. The other stretches from the Canadian Prairies in Manitoba through the Great Plains of the US as far south as Kansas.[5] Similar soil types occur in Texas and Hungary. Chernozem layer thickness may vary widely, from several centimetres up to 1.5 metres (60 inches) in Ukraine,[6] as well as the Red River Valley region in the Northern US and Canada (location of the prehistoric Lake Agassiz).

The terrain can also be found in small quantities elsewhere (for example, on 1% of Poland). It also exists in Northeast China, near Harbin. The only true chernozem in Australia is located around Nimmitabel, with some of the richest soils in the nation.[7]

Previously, there was a black market for the soil in Ukraine. The sale of agricultural land has been illegal in Ukraine since 1992 until the ban was lifted in 2020,[8] but the soil, transported by truck, was able to be sold and bought. According to Kharkiv-based "Green Front" NGO, the black market for illegally acquired chernozem in Ukraine was projected to reach approximately US$900 million per year in 2011.[9]

Canadian and United States soil classification

Chernozemic soils are a soil type in the Canadian system of soil classification and the World Reference Base for Soil Resources (WRB).

Chernozemic soil type "equivalents", in the Canadian system, WRB, and US Department of Agriculture soil taxonomy:

Canadian WRB United States
Chernozemic Kastanozem, Chernozem, Phaeozem Mollisol
Brown Chernozem Kastanozem (Aridic) Aridic Mollisol subgroups (Xerolls and Ustolls)
Dark Brown Chernozem Haplic Kastanozem Typic Mollisol subgroups
Black Chernozem Chernozem Udic Mollisol subgroups
Dark Grey Chernozem Greyzemic Phaeozem Boralfic Mollisol subgroups, Albolls
Source: Pedosphere.com.

History

Theories of Chernozem origin:

As seen in the list above, the 19th and 20th-century discussions on the pedogenesis of Chernozem originally stemmed from climatic conditions from the early Holocene to roughly 5500 BC. However, no single paleo-climate reconstruction could accurately explain geochemical variations found in Chernozems throughout central Europe. Evidence of anthropomorphic origins of stable pyrogenic carbon in Chernozem led to improved formation theories.[16] Vegetation burning could explain Chernozem's high magnetic susceptibility,[19] the highest of the major soil types.[20] Soil magnetism increases when soil minerals goethite and ferrihydrite convert to maghemite on exposure to heat.[21] Temperatures sufficient to elevate maghemite on a landscape scale indicates the influence of fire. Given the rarity of such natural phenomenon in the modern-day, magnetic susceptibility in Chernozem likely relates to control of fire by early humans.[20]

Humification can darken soils (melanization) absent a pyrogenic carbon component. Given the symphony of pedogenic processes that contribute to the formation of dark earth, the term Chernozem summarizes different types of black soils with the same appearance but different formation histories.

See also

Notes

  1. ^ Prolonged use may still require replenishment with fertilizers because it easily can get depleted of nutrities.

References

  • IUSS Working Group WRB: World Reference Base for Soil Resources, fourth edition. International Union of Soil Sciences, Vienna 2022. ISBN 979-8-9862451-1-9 ([1]).
  1. ^ Russia Investment and Business Guide. International Business Publications. 2007. p. 63. ISBN 9781433041686. Retrieved 11 January 2018.
  2. ^ a b "chernozem | Etymology, origin and meaning of chernozem by etymonline". www.etymonline.com. Retrieved 5 October 2022.
  3. ^ a b "Chernozem". Merriam-Webster Online Dictionary. 2008. Retrieved 7 July 2008.
  4. ^ "How Chemical Pre-Treatments in Particle Size Analysis Impact Wind Erosion Modeling". AZoM.com. 28 July 2021. Retrieved 30 August 2022.
  5. ^ Ecology of Arable Land – Perspectives and Challenges by M. Clarholm and L. Bergström ISBN 978-94-010-6950-2
  6. ^ Ukraine: Soils in Encyclopædia Britannica
  7. ^ KG McQueen. "The Tertiary Geology And Geomorphology Of The Monaro: The Perspective In 1994" Centre For Australian Regolith Studies, Canberra 1994
  8. ^ "Ukraine lifts ban on sale of farmland in bid to receive international funds". Euronews. Euronews. 31 March 2020.
  9. ^ Black market for rich black earth, Kyiv Post (9 November 2011)
  10. ^ Wallerius J. G. Agriculturae fundamenta chemica, åkerbrukets chemiska grunder. Upsaliae, 1761. 8, 4, 322 p.; The natural and chemical elements of agriculture. London, York: Bell, Etherington, 1770. 198 p.
  11. ^ 'Lomonosov M. V. § 125. // On the strata of the Earth: a translation of "O sloiakh zemnykh" (1763) / translated by S. M. Rowland, S. Korolev. Boulder: Geological Soc. of America, 2012. 41 p. (Special paper; 485) "And so, there is no doubt that black soil is not primordial matter, but that it has been produced by the decomposition of animal and plant bodies over time"
  12. ^ a b Geikie, A. (1875), Life of Sir Roderick I, Murchison, vol. 1, ASIN B0095632AU
  13. ^ Fedotova, Anastasia A. (August 2010), "The Origins of the Russian Chernozem Soil (Black Earth): Franz Joseph Ruprecht's 'Geo-Botanical Researches into the Chernozem' of 1866", Environment and History, 16 (3): 271–293, doi:10.3197/096734010x519762, JSTOR 20723789
  14. ^ Dokoutchaief B. Tchernozème (terre noire) de la Russie d'Europe. St.-Ptb.: Soc. Imp. libre économ., 1879. 66 p. (Comptes-rendus Soc. Imp. libre économ. T. 4).
  15. ^ Dokuchaev V. V. Russian Chernozem (1883) // Israel Program for Scientific Translations Ltd. (for USDA-NSF), S. Monson, Jerusalem, 1967. (Translated from Russian into English by N. Kaner)
  16. ^ a b Eckmeier, Eileen; Gerlach, Renate; Gehrt, Ernst; Schmidt, Michael W.I. (2007), (PDF), Geoderma, 139 (3–4): 288–299, Bibcode:2007Geode.139..288E, doi:10.1016/j.geoderma.2007.01.009, archived from the original (PDF) on 8 March 2016
  17. ^ Schmidt, M.W.I.; Skjemstad, J.O.; Jäger, C. (2002), "Carbon isotope geochemistry and nanomorphology of soil black carbon: Black chernozemic soils in central Europe originate from ancient biomass burning", Global Biogeochemical Cycles, 16 (4): 70–1–70–8, Bibcode:2002GBioC..16.1123S, doi:10.1029/2002GB001939, S2CID 56045817, These data challenge the common paradigm that chernozems are zonal soils with climate, parent material and bioturbation dominating soil formation, and introduce fire as a novel, important factor in the formation of these soils
  18. ^ Eckmeier, E. (2007), Detecting prehistoric fire-based farming using biogeochemical markers (Dissertation), University of Zurich, Faculty of Science., doi:10.5167/uzh-3752, It is now an open question as to whether Neolithic settlers did indeed prefer to grow crops where Chernozems occurred or if Neolithic burning formed the chernozemic soils.
  19. ^ Eckmeier, Eileen; Gerlach, Renate; Gehrt, Ernst; Schmidt, Michael W.I. (2007), (PDF), Geoderma, 139 (3–4): 288–299, Bibcode:2007Geode.139..288E, doi:10.1016/j.geoderma.2007.01.009, archived from the original (PDF) on 8 March 2016, magnetic susceptibility of soil material may reflect past fires
  20. ^ a b Jordanova, Neli, ed. (2017). "Chapter 8 - The discriminating power of soil magnetism for the characterization of different soil types". Soil Magnetism. Academic Press. pp. 349–365. doi:10.1016/B978-0-12-809239-2.00008-5. ISBN 978-0-12-809239-2. Chernozem soils exhibit similar features worldwide and are generally characterized by significant magnetic enhancement in the upper soil horizons.
  21. ^ Nørnberg, P.; Schwertmann, U.; Stanjek, H.; Andersen, T.; Gunnlaugsson, H.P. (2004). "Mineralogy of a burned soil compared with four anomalously red Quaternary deposits in Denmark". Clay Minerals. 39 (1): 85–98. Bibcode:2004ClMin..39...85N. doi:10.1180/0009855043910122. S2CID 129974901.

Further reading

  • W. Zech, P. Schad, G. Hintermaier-Erhard: Soils of the World. Springer, Berlin 2022, Chapter 5.3.2. ISBN 978-3-540-30460-9

External links

  • profile photos (with classification) WRB homepage
  • IUSS profile photos (with classification) IUSS World of Soils

chernozem, from, russian, чернозём, chernozyom, tɕɪrnɐˈzʲɵm, black, ground, also, called, black, soil, black, colored, soil, containing, high, percentage, humus, high, percentages, phosphorus, ammonia, compounds, very, fertile, soil, produce, high, agricultura. Chernozem from Russian chernozyom tr chernozyom IPA tɕɪrnɐˈzʲɵm black ground 1 2 also called black soil is a black colored soil containing a high percentage of humus 3 4 to 16 and high percentages of phosphorus and ammonia compounds 4 Chernozem is very fertile soil and can produce high agricultural yields with its high moisture storage capacity a Chernozems are a Reference Soil Group of the World Reference Base for Soil Resources WRB ChernozemChernozemic soilMollisol USDA NRCS Used inWRB otherWRB codeCHProfileAhBCParent materialLoessClimateHumid continental Contents 1 Distribution 2 Canadian and United States soil classification 3 History 4 See also 5 Notes 6 References 7 Further reading 8 External linksDistribution Edit Distribution of Chernozem soils according to the World Reference Base for Soil Resources classification Dominant more than 50 of soil cover Codominant 25 50 Associated 5 25 The name comes from the Russian terms for black and soil earth or land chorny zemlya 2 3 The soil rich in organic matter presenting a black color was first identified by Russian geologist Vasily Dokuchaev in 1883 in the tallgrass steppe or prairie of European Russia Chernozem cover about 230 million hectares of land There are two chernozem belts in the world One is the Eurasian steppe which extends from eastern Croatia Slavonia along the Danube northern Serbia northern Bulgaria Danubian Plain southern and eastern Romania Wallachian Plain and Moldavian Plain and Moldova to northeast Ukraine across the Central Black Earth Region of Central Russia southern Russia into Siberia The other stretches from the Canadian Prairies in Manitoba through the Great Plains of the US as far south as Kansas 5 Similar soil types occur in Texas and Hungary Chernozem layer thickness may vary widely from several centimetres up to 1 5 metres 60 inches in Ukraine 6 as well as the Red River Valley region in the Northern US and Canada location of the prehistoric Lake Agassiz The terrain can also be found in small quantities elsewhere for example on 1 of Poland It also exists in Northeast China near Harbin The only true chernozem in Australia is located around Nimmitabel with some of the richest soils in the nation 7 Previously there was a black market for the soil in Ukraine The sale of agricultural land has been illegal in Ukraine since 1992 until the ban was lifted in 2020 8 but the soil transported by truck was able to be sold and bought According to Kharkiv based Green Front NGO the black market for illegally acquired chernozem in Ukraine was projected to reach approximately US 900 million per year in 2011 9 Canadian and United States soil classification EditChernozemic soils are a soil type in the Canadian system of soil classification and the World Reference Base for Soil Resources WRB Chernozemic soil type equivalents in the Canadian system WRB and US Department of Agriculture soil taxonomy Canadian WRB United StatesChernozemic Kastanozem Chernozem Phaeozem MollisolBrown Chernozem Kastanozem Aridic Aridic Mollisol subgroups Xerolls and Ustolls Dark Brown Chernozem Haplic Kastanozem Typic Mollisol subgroupsBlack Chernozem Chernozem Udic Mollisol subgroupsDark Grey Chernozem Greyzemic Phaeozem Boralfic Mollisol subgroups AlbollsSource Pedosphere com History EditTheories of Chernozem origin 1761 Johan Gottschalk Wallerius plant decomposition 10 1763 Mikhail Lomonosov plant and animal decomposition 11 1799 Peter Simon Pallas reeds marsh 1835 Charles Lyell loess 12 1840 Sir Roderick Murchison weathered from Jurassic marine shales 12 1850 Karl Eichwald peat 1851 A Petzgold swamps 1852 Nikifor Borisyak peat 1853 Vangengeim von Qualen silt from northern swamps 1862 Rudolf Ludwig bog on place of forests 1866 Franz Josef Ruprecht decomposed steppe grasses 13 1879 First chernozem papers translated from Russian 14 1883 Vasily Dokuchaev published his book Russian Chernozem with a complete study of this soil in European Russia 15 1929 Otto Schluter man made 16 1999 Michael W I Schmidt neolithic biomass burning 17 18 As seen in the list above the 19th and 20th century discussions on the pedogenesis of Chernozem originally stemmed from climatic conditions from the early Holocene to roughly 5500 BC However no single paleo climate reconstruction could accurately explain geochemical variations found in Chernozems throughout central Europe Evidence of anthropomorphic origins of stable pyrogenic carbon in Chernozem led to improved formation theories 16 Vegetation burning could explain Chernozem s high magnetic susceptibility 19 the highest of the major soil types 20 Soil magnetism increases when soil minerals goethite and ferrihydrite convert to maghemite on exposure to heat 21 Temperatures sufficient to elevate maghemite on a landscape scale indicates the influence of fire Given the rarity of such natural phenomenon in the modern day magnetic susceptibility in Chernozem likely relates to control of fire by early humans 20 Humification can darken soils melanization absent a pyrogenic carbon component Given the symphony of pedogenic processes that contribute to the formation of dark earth the term Chernozem summarizes different types of black soils with the same appearance but different formation histories See also EditLoam Dark earth Terra pretaNotes Edit Prolonged use may still require replenishment with fertilizers because it easily can get depleted of nutrities References EditIUSS Working Group WRB World Reference Base for Soil Resources fourth edition International Union of Soil Sciences Vienna 2022 ISBN 979 8 9862451 1 9 1 Russia Investment and Business Guide International Business Publications 2007 p 63 ISBN 9781433041686 Retrieved 11 January 2018 a b chernozem Etymology origin and meaning of chernozem by etymonline www etymonline com Retrieved 5 October 2022 a b Chernozem Merriam Webster Online Dictionary 2008 Retrieved 7 July 2008 How Chemical Pre Treatments in Particle Size Analysis Impact Wind Erosion Modeling AZoM com 28 July 2021 Retrieved 30 August 2022 Ecology of Arable Land Perspectives and Challenges by M Clarholm and L Bergstrom ISBN 978 94 010 6950 2 Ukraine Soils in Encyclopaedia Britannica KG McQueen The Tertiary Geology And Geomorphology Of The Monaro The Perspective In 1994 Centre For Australian Regolith Studies Canberra 1994 Ukraine lifts ban on sale of farmland in bid to receive international funds Euronews Euronews 31 March 2020 Black market for rich black earth Kyiv Post 9 November 2011 Wallerius J G Agriculturae fundamenta chemica akerbrukets chemiska grunder Upsaliae 1761 8 4 322 p The natural and chemical elements of agriculture London York Bell Etherington 1770 198 p Lomonosov M V 125 On the strata of the Earth a translation of O sloiakh zemnykh 1763 translated by S M Rowland S Korolev Boulder Geological Soc of America 2012 41 p Special paper 485 And so there is no doubt that black soil is not primordial matter but that it has been produced by the decomposition of animal and plant bodies over time a b Geikie A 1875 Life of Sir Roderick I Murchison vol 1 ASIN B0095632AU Fedotova Anastasia A August 2010 The Origins of the Russian Chernozem Soil Black Earth Franz Joseph Ruprecht s Geo Botanical Researches into the Chernozem of 1866 Environment and History 16 3 271 293 doi 10 3197 096734010x519762 JSTOR 20723789 Dokoutchaief B Tchernozeme terre noire de la Russie d Europe St Ptb Soc Imp libre econom 1879 66 p Comptes rendus Soc Imp libre econom T 4 Dokuchaev V V Russian Chernozem 1883 Israel Program for Scientific Translations Ltd for USDA NSF S Monson Jerusalem 1967 Translated from Russian into English by N Kaner a b Eckmeier Eileen Gerlach Renate Gehrt Ernst Schmidt Michael W I 2007 Pedogenesis of Chernozems in Central Europe A review PDF Geoderma 139 3 4 288 299 Bibcode 2007Geode 139 288E doi 10 1016 j geoderma 2007 01 009 archived from the original PDF on 8 March 2016 Schmidt M W I Skjemstad J O Jager C 2002 Carbon isotope geochemistry and nanomorphology of soil black carbon Black chernozemic soils in central Europe originate from ancient biomass burning Global Biogeochemical Cycles 16 4 70 1 70 8 Bibcode 2002GBioC 16 1123S doi 10 1029 2002GB001939 S2CID 56045817 These data challenge the common paradigm that chernozems are zonal soils with climate parent material and bioturbation dominating soil formation and introduce fire as a novel important factor in the formation of these soils Eckmeier E 2007 Detecting prehistoric fire based farming using biogeochemical markers Dissertation University of Zurich Faculty of Science doi 10 5167 uzh 3752 It is now an open question as to whether Neolithic settlers did indeed prefer to grow crops where Chernozems occurred or if Neolithic burning formed the chernozemic soils Eckmeier Eileen Gerlach Renate Gehrt Ernst Schmidt Michael W I 2007 Pedogenesis of Chernozems in Central Europe A review PDF Geoderma 139 3 4 288 299 Bibcode 2007Geode 139 288E doi 10 1016 j geoderma 2007 01 009 archived from the original PDF on 8 March 2016 magnetic susceptibility of soil material may reflect past fires a b Jordanova Neli ed 2017 Chapter 8 The discriminating power of soil magnetism for the characterization of different soil types Soil Magnetism Academic Press pp 349 365 doi 10 1016 B978 0 12 809239 2 00008 5 ISBN 978 0 12 809239 2 Chernozem soils exhibit similar features worldwide and are generally characterized by significant magnetic enhancement in the upper soil horizons Nornberg P Schwertmann U Stanjek H Andersen T Gunnlaugsson H P 2004 Mineralogy of a burned soil compared with four anomalously red Quaternary deposits in Denmark Clay Minerals 39 1 85 98 Bibcode 2004ClMin 39 85N doi 10 1180 0009855043910122 S2CID 129974901 Further reading EditW Zech P Schad G Hintermaier Erhard Soils of the World Springer Berlin 2022 Chapter 5 3 2 ISBN 978 3 540 30460 9External links Edit Wikimedia Commons has media related to Chernozem Look up chernozem in Wiktionary the free dictionary profile photos with classification WRB homepage IUSS profile photos with classification IUSS World of Soils Retrieved from https en wikipedia org w index php title Chernozem amp oldid 1135715000, wikipedia, wiki, book, books, library,

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