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Dark-Humus Residual–Hydromorphic Soils of the Slopes of the Northern Uvaly Formed on Clay Triassic Deposits

机译:在粘土三叠系沉积物上形成北方北方北方北部坡度的黑暗腐殖质残留水土

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摘要

Northern Uvaly dark-humus soils and agrozems, which formed on Triassic clay deposits, are examined. Their hydromorphic nature is identified based on determination of their organic matter properties. Nonconformity of the hydromorphic features to the current moisture conditions is found, which indicates the residual character of hydromorphism and confirms the concept that the territory of the Uvaly was uplifted during the Holocene.
机译:检查了北方的乌视黑暗腐殖质土壤和农业波子,形成在三叠纪粘土矿床上。 基于它们的有机物质特性的测定来鉴定它们的湿状性质。 发现潮湿特征的不符合目前的水分条件,这表明了湿形式的残余特性,并确认了在全新世期间封面封面的概念。

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