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潮土
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潮土
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潮土
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Fluvo-aquic soils
潮土
发育在河流冲积物上受地下水影响,并经长期旱耕而形成的土壤。在中国第一次全国土壤普查期间,命名为淤黄土;在中国土壤分类系统(1978)和中国第二次土壤普查分类方案(1988)中,列为半水成土纲潮土土类;在中国土壤系统分类(2001)中,相当于潮湿雏形土[注];在美国土壤系统分类(1999)中,大致相当于底潜潮湿始成土[注];在世界土壤资源参比基础(2014)中,大致相当于饱和雏形土[注]或石灰性始成土[注]。曾称冲积土、浅色草甸土。
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