از ویکیپدیا، دانشنامهٔ آزاد
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[[پرونده:{{{image}}}|{{{image_size}}}|جایگزین={{{image_alt}}}]] {{{image_caption}}} |
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ردهبندی شده در: | {{{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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اقلیم: | {{{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 =
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| image =
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{{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 = [[پودزول]]
| parent material = quartz rich debris and sediments
| climate = [[اقلیم قارهای مرطوب]], [[اقلیم زیرشمالگانی]], [[اقلیم اقیانوسی]], [[اقلیم جنگلهای بارانی]]
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