Abstract
To study the complex flow of water in soils, the concepts of the residence time theory have been applied. Tritiated water (HTO) was used as a tracer in humus to obtain experimental response curves for a laboratory system and a theoretical flow model was constructed and fitted to the data. The purpose of this work was to establish a flow model for a subsequent ion exchange model (Part II of this paper). Our utlimate goal is to apply the experimental techniques and the models developed to the study of natural systems.
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