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[[File:{{{image}}}|{{{image_size}}}|alt={{{image_alt}}}]] {{{image_caption}}} |
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Used in: | {{{classification_system}}} |
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WRB code: | {{{code}}} |
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Profile: | {{{profile}}} |
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Key minerals: | {{{mineral}}} |
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Key process: | {{{process}}} |
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Parent material: | {{{parent_material}}} |
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Climate: | {{{climate}}} |
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pH | {{{ph}}} |
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Primary | {{{composition}}} |
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Secondary | {{{composition_secondary}}} |
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{{Infobox soil
| name =
| alternative_name =
| image =
| image_caption =
| image_size =
| type =
| classification_system =
| code =
| profile =
| mineral =
| process =
| parent_material =
| climate =
| ph =
| horizons =
| composition =
| composition_secondary =
}}
{{Infobox soil
| name = Podzol
| alternative_name = Podsol, Podosol, Spodosol, Espodossolo
| image = Podzol.jpg
| image_size = 250px
| image_caption = A stagnopodzol in upland Wales, showing the typical sequence of organic topsoil with leached grey-white subsoil with iron-rich horizon below.
| classification_system = [[World Reference Base for Soil Resources|WRB]], [[USDA soil taxonomy]], others
| code = PZ
| profile = O(Ah)EBhsC
| process = [[podzolization]]
| parent_material = quartz rich debris and sediments
| climate = [[humid continental climate|humid continental]], [[subarctic climate|subarctic]], [[oceanic climate|oceanic]], [[tropical rainforest climate|equatorial]]
}}
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