© 2013

Coupled Dynamics in Soil

Experimental and Numerical Studies of Energy, Momentum and Mass Transfer


Part of the Springer Theses book series (Springer Theses)

Table of contents

About this book


In arid and semi-arid areas, the main contributions to land surface processes are precipitation, surface evaporation and surface energy balancing. In the close-to-surface layer and root-zone layer, vapor flux is the dominant flux controlling these processes - process which, in turn, influence the local climate pattern and the local ecosystem. The work reported in this thesis attempts to understand how the soil airflow affects the vapor transport during evaporation processes, by using a two-phase heat and mass transfer model. The necessity of including the airflow mechanism in land surface process studies is discussed and highlighted.


Advective Effect on Evaporation Airflow Mechanism Land-Atmosphere Interaction Soil Physics Two-Phase Flow Vapour Flux in Soil

Authors and affiliations

  1. 1.University of TwenteTwenteNetherlands

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