๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

Experimental investigation on heat, moisture and salt transfer in soil

โœ Scribed by Yongping Chen; Mingheng Shi; Xiaochuan Li


Publisher
Elsevier Science
Year
2006
Tongue
English
Weight
430 KB
Volume
33
Category
Article
ISSN
0735-1933

No coin nor oath required. For personal study only.

โœฆ Synopsis


In this paper, experiments on coupled heat, moisture and salt transfer in yellow vegetable soil are conducted. A remarkable thermal permeant region in the soil column is found, along with moisture releasing, transition and absorbing zones in the soil column. The capillary flow is the dominant mechanism that governs the moisture transfer. With the moisture transfer, the salt moves from the groundwater and accumulates at the top of the column. However, with the salt accumulation, there will be a gradient of salt content and, as a result, the salt will also diffuse due to this gradient.


๐Ÿ“œ SIMILAR VOLUMES


Three-dimensional heat, moisture and air
โœ Thomas, H. R.; Rees, S. W.; Sloper, N. J. ๐Ÿ“‚ Article ๐Ÿ“… 1998 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 478 KB ๐Ÿ‘ 1 views

A new three-dimensional numerical model of coupled heat, moisture and air transfer in unsaturated soil is presented. In particular, the model accommodates moisture transfer in the form of liquid and vapour flow and heat transfer arising from conduction, convection and latent heat of vaporization. Th

A PARALLEL COMPUTING SOLUTION OF HEAT AN
โœ H. R. THOMAS; C. L. W. LI ๐Ÿ“‚ Article ๐Ÿ“… 1996 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 737 KB

New parallel software for the analysis of coupled heat and moisture transfer in unsaturated soil is developed. The model, written in a two-dimensional polar co-ordinate formulation, is based on a finite difference self-implicit method. The code is programmed in FORTRAN with message passing libraries

Three-dimensional coupled heat, moisture
โœ H. R. Thomas; H. Missoum ๐Ÿ“‚ Article ๐Ÿ“… 1999 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 233 KB ๐Ÿ‘ 2 views

A three-dimensional numerical model is presented for three-phase flow (moisture, air, and heat) in a deformable partly saturated soil with deformation calculated via a non-linear elastic theory. The present work is an extension of a two-dimensional analysis presented by Thomas and He. The objective