
Gleysol - Wikipedia
A gleysol or gley soil is a hydric soil that unless drained is saturated with groundwater for long enough to develop a characteristic gleyic colour pattern.
Gleysol | Wetland Soil, Hydromorphic, Clayey | Britannica
Gleysol, one of the 30 soil groups in the classification system of the Food and Agriculture Organization (FAO). Gleysols are formed under waterlogged conditions produced by rising …
Artificially drained Gleysols are used for arable cropping, dairy farming and horticulture. Gleysols in the tropics and subtropics are widely planted to rice. Gleysols occupy an estimated 720 …
Gleysolic Order - Soils of Canada
Gleysolic soils are wetland soils whose morphology is created by the effects of water saturation on soil processes in mineral soil horizons. The g (for gleyed) suffix is applied both to horizons …
Gleysols - ISRIC
Gleysols occur throughout the world where groundwater comes near to the surface, causing soils to become wet for a prolonged part of the year. They are particularly abundant in the low-lying …
Gleysol - an overview | ScienceDirect Topics
Gleysols are characterized by subsurface horizons with prominent redoximorphic features formed by intermittent to long-term dysoxia or anoxia.
Gleysolic soils of Canada: Genesis, distribution, and classification
Apr 19, 2011 · In the Canadian System of Soil Classification, the Gleysolic Order includes all those soils with morphologic features that provide dominant physical evidence of oxidation …
Gley Soils - SpringerLink
Feb 20, 2021 · Gley Soils form where soils are saturated for long periods due to high or perched water tables, or slow drainage. Gley Soils occur throughout New Zealand but are more …
Humic Gleysol (HG) - Agriculture and Agri-Food Canada
These soils have the general properties specified for the Gleysolic order and the Humic Gleysol great group. They differ from Orthic Humic Gleysols in that they lack a B horizon at least 10 …
Gleysols - SpringerLink
Jan 1, 2016 · Gleysols are wetland soils, which in the natural state are continuously water‐saturated within 50 cm of the surface, for long periods of time. Reduction of Fe and Mn …