Coupled Dynamics in Soil: Experimental and Numerical Studies of Energy, Momentum and Mass Transfer
Author:   Yijian Zeng
Publisher:   Springer-Verlag Berlin and Heidelberg GmbH & Co. KG
Edition:   2013 ed.
ISBN:  

9783642340727


Pages:   164
Publication Date:   14 December 2012
Format:   Hardback
Availability:   Manufactured on demand   Availability explained
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Coupled Dynamics in Soil: Experimental and Numerical Studies of Energy, Momentum and Mass Transfer


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Overview

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.

Full Product Details

Author:   Yijian Zeng
Publisher:   Springer-Verlag Berlin and Heidelberg GmbH & Co. KG
Imprint:   Springer-Verlag Berlin and Heidelberg GmbH & Co. K
Edition:   2013 ed.
Dimensions:   Width: 15.50cm , Height: 1.80cm , Length: 23.50cm
Weight:   3.967kg
ISBN:  

9783642340727


ISBN 10:   3642340725
Pages:   164
Publication Date:   14 December 2012
Audience:   College/higher education ,  Postgraduate, Research & Scholarly
Format:   Hardback
Publisher's Status:   Active
Availability:   Manufactured on demand   Availability explained
We will order this item for you from a manufactured on demand supplier.

Table of Contents

General Introduction.- Diurnal Pattern of Coupled Moisture and Heat Transport Process.- Application of Diurnal Soil Water Dynamics in Determining Effective Precipitation.- Two-Phase Mass and Heat Flow Model.- How Airflow Affects Soil Water Dynamics.- Impact of Model Physics on Retrieving Soil Moisture and Soil Temperature.- Concluding Remarks.

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