Reactive nitrogen in a clay till hill slope field system

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Field Experiments in a Fractured Clay Till 2. Solute and Colloid Transport

A field tracer experiment was conducted in a lateral flow field in the weathered and highly fractured upper 6 m of a 40-m-thick clay-rich till plain in southwestern Ontario. In the upper 3 m where fractures are closely spaced (<0.13 m) the advancing front (C/Co = 0.01) of the nonreactive solute tracers, bromide and O, migrated at rates of 0.01 to 0.07 m/d, over distances of 4 and 6 m and under ...

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ژورنال

عنوان ژورنال: Ambio

سال: 2019

ISSN: 0044-7447,1654-7209

DOI: 10.1007/s13280-019-01228-4