Table of Contents
ISRN Ecology
Volume 2011, Article ID 345851, 15 pages
Research Article

Practice of Mass Transport Model Application for Biogeochemical Redox Process in Aquifer

1Laboratory of Water Environment Engineering, International Education Center, Kyushu University, 6-10-1 Hakozaki Higashi-ku, Fukuoka 812-8581, Japan
2Geosphere Environmental Technology Corp. 6F, Hinoki Building, 2-1 Kanda, Ogawamachi, Chiyoda-ku, Tokyo 101-0052, Japan
3Kyushu University, 1-4-5 Izumigaoka, Munakata City, Fukuoka 811-4162, Japan

Received 15 July 2011; Accepted 17 August 2011

Academic Editor: P. Grenni

Copyright © 2011 Osama Eljamal et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.


Biogeochemical reduction processes are active in alluvial aquifers, because organic carbon which is indispensable for bacteria growth is abundant. As a result of reduction process, significant changes of groundwater quality take place; denitrification, reduction of manganese dioxide, iron-hydroxide, sulfate, arsenate, and methane are well known as reduction processes in an anaerobic groundwater condition. Therefore, the prediction of redox environment in an aquifer is a key subject in order to understand how the groundwater quality is affected. If the mechanism of groundwater quality formation in aquifer scale is systematically understood, impacts caused by accidents or illegal dumping can be predicted, and subsequently, an appropriate management of aquifer will be established. In the present paper, quantitative discussions are made by the numerical simulations applied for the one-dimensional column experiment and two-dimensional fresh-salt water mixing zone. Recommendation and the future subject are presented through the results of two numerical simulations.