Study on the Runoff Characteristics of Ordovician Limestone Groundwater in Jinmen Coalmine

DOI

10.2991/citcs.2012.117How to use a DOI?

Keywords

limestone groundwater; piper trilinear nomograph; hydro-chemical characteristics; the type of water quality

Abstract

Based on the data of water pumping test and releasing test, we systematically analyzed the hydrochemical characteristics of the Ordovician Limestone aquifer. We sorted the data, classified the water quality of each samples, drawed piper trilinear nomograph, and delineated hydro-chemical subsections of Ordovician limestone aquifer to analyze the Ordovician limestone aquifer water runoff features. The results shown that, Ordovician limestone groundwater flowed from the northeast, the east and the south to Tianqiao Spring. From the east boundary to the west, hydro-chemical subsections were runoff area, weak runoff area and stagnation area. Ordovician limestone groundwater flowed deeper and slower to the south of Tianqiao Springs, and the type of water quality charactered as that was in stagnant zone.

Copyright

© 2012, the Authors. Published by Atlantis Press.

Open Access

This is an open access article distributed under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).

Download article (PDF)

TY  - CONF
AU  - Shasha Wang
AU  - Jiuchuan Wei
AU  - Zengxue Li
AU  - Baolai Song
PY  - 2012/11
DA  - 2012/11
TI  - Study on the Runoff Characteristics of Ordovician Limestone Groundwater in Jinmen Coalmine
BT  - Proceedings of the 2012 National Conference on Information Technology and Computer Science
PB  - Atlantis Press
SP  - 454
EP  - 456
SN  - 1951-6851
UR  - https://doi.org/10.2991/citcs.2012.117
DO  - 10.2991/citcs.2012.117
ID  - Wang2012/11
ER  -