Siliceous soils are formed from rocks that have silica (SiO2) as a principal constituent. The parent material of siliceous soils may include quartz sands, chert, quartzite, quartz reefs, granite, rhyolite, ademellite, dellenite, quartz sandstone, quartz siltstone, siliceous tuff, among others.[1] These parent materials sometimes originate from silica-secreting organisms such as radiolarians, diatoms, or some types of sponges.[2]

Characteristics

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Soils high in siliceous parent material typically have:[1]

Agriculture

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Siliceous soils in vineyard soils have been linked to larger grapes with increased tannin content.[3][4]

See also

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References

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  1. ^ a b Gray, Jonathan; Murphy, Brian (2002). Parent material and world soil distribution. World Congress of Soil Science. Thailand. CiteSeerX 10.1.1.3.2975.
  2. ^ Schumann, Walter (1993). Handbook of Rocks, Minerals, and Gemstones. Houghton Mifflin Harcourt. ISBN 978-0395511374.
  3. ^ Conte, M., Rossini, L., Tiberi, M., Montanari, A. (2006). Verdicchio dei Castelli di Jesi vs Verdicchio di Matelica: Geomorphological control of two white wines of the Marche region (northeastern Apennines, Italy). Bollettino Della Società Geologica Italiana E Del Servizio Geologico D'Italia, 6, 41-48.
  4. ^ Burns S. (2012) The Importance of Soil and Geology in Tasting Terroir with a Case History from the Willamette Valley, Oregon. In: Dougherty P. (Eds.), The Geography of Wine (pp. 95-108). Springer, Dordrecht.