The formation of a gley is known as gleying 潜育层是通过潜育作用形成的。
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Gley soils are typical of tundra , meadows , and boggy areas 该种土壤是苔原、草地以及沼地所特有的。
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Deep gley soil 深位潜育土壤
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Gley ( glei ) a waterlogged soil lacking in oxyen , in which raw humus accumulates as a result of lack of decomposition by bacteria 潜育土：是一种氧含量低而水含量很高的土壤，由于缺少分解性细菌而在其内积累了大量的腐殖质。
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The defining feature is the gley horizon below the humus - blue - grey clay whowe color is due to ferrous iron compounds that have been reduced by microorganisms , flecked with localized areas of rust - colored oxidized ferric compounds 潜育土的一个重要特点是位于土壤腐殖质层之下，其土层呈灰蓝色是由于含有被微生物还原的亚铁离子，而且常有部分铁被氧化生成红棕色的锈斑。
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