Abstract
Prolonged water saturation and seasonal alternational between water logging and drainage has profound effects on soil chemical and morphological properties. Changes in the degree of water saturation affect the supply of O2 to the soil, wich in turn affects the oxidation state of important elements. The oxidation state of iron, manganese and sulfur strongly influences their solubility and colour, explaining the brown, gray, blue, black and yellow mottles often seen in periodically wet, so-called hydromorphic, soils. Redox processes often involve production or consumption of H+ and so have an important effect on soil pH too.
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
7.7. References
Brinkman, R., 1970. Ferrolysis, a hydromorphic soil forming process. Geoderma 3:199–206.
Brinkman, R., 1977. Surface-water gley soils in Bangladesh: genesis. Geoderma 17:111–144.
Brinkman, R., 1979. Ferrolysis, a soil forming process in hydromorphic conditions. Agricultural Research Reports 887: vi + 106 pp., PUDOC, Wageningen.
Buurman, P., 1980. Palaeosols in the Reading Beds (Paleocene) of Alum Bay, Isle of Wight, U.K. Sedimentology 27:593–606.
Kawaguchi, K. and Y. Matsuo, 1957. Reinvestigation of active and inactive oxides along soil profiles in time series of dry rice fields in polder lands of Kojima basin, Okayama prefecture, Japan. Soil Plant Food, 3: 29–35.
Konsten, C.J.M., N van Breemen, Supardo Suping, and J.E. Groenenberg, 1994. Effects of flooding on pH of rice-producing acid sulphate soils in Indonesia Soil Sci.Soc.Amer.J. 58,871–883.
Patrick Jr., W.H. and R.D. Delaune, 1972. Characterization of the oxidized and reduced zone in flooded soil. Soil Sci. Soc. Amer. Proc.36: 573–576.
Van Breemen, N., 1976. Genesis and solution chemistry of acid sulfate soils in Thailand. Agric. Res. Rept. 848, 263 pp. PUDOC, Wageningen.
Van Breemen, N., 1988. Redox processes of iron and sulfur involved in the formation of acid sulfate soils, p. 825–841 in J.W. Stucki et al (eds) Iron in Soils and Clay Minerals. D. Reidel Publ. Co, Dordrecht. Netherlands, 893 pp.
Van Breemen, N., W.F.J. Visser and Th. Pape, 1987. Biogeochemistry of an oak-woodland ecosystem in the Netherlands, affected by acid atmospheric deposition. Agricultural Research Reports 930, 197 pp. PUDOC, Wageningen.
Van Mensvoort, M.E.F. and Le Quang Tri, 1988. Morphology and genesis of actual acid sulphate soils without jarosite in the Ha Tien Plain, Mekong Delta, Viet Nam. p. 11–15 in: Dost, H. (ed). Selected Papers of the Dakar Symposium on Acid Sulphate Soils, Dakar, Senegal, January 1986, p. ILRI Publication 44.
Rights and permissions
Copyright information
© 1998 Kluwer Academic Publishers
About this chapter
Cite this chapter
(1998). Hydromorphic Soils. In: Soil Formation. Springer, Dordrecht. https://doi.org/10.1007/978-0-585-31788-5_7
Download citation
DOI: https://doi.org/10.1007/978-0-585-31788-5_7
Publisher Name: Springer, Dordrecht
Print ISBN: 978-0-7923-5263-1
Online ISBN: 978-0-585-31788-5
eBook Packages: Springer Book Archive