Relationships of saturation and B horizon colour patterns in soils of three hydrosequences in south-central Michigan, USA

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Abstract. Relationships between soil colour patterns and depth and duration of water tables were studied using piezometers in three soil hydrosequences. A colour index was developed to quantify matrix colour, size and colour of mottles, and continuity and colour of clay films. It correlated well with duration of saturation when above 5°C (r= 0.88) and with duration of total saturation (r= 0.87). The colour index is useful to evaluate soils for various land uses.