Study on the Runoff Characteristics of Ordovician Limestone Groundwater in Jinmen Coalmine
Shasha Wang, Jiuchuan Wei, Zengxue Li, Baolai Song
Available Online November 2012.
- https://doi.org/10.2991/citcs.2012.117How to use a DOI?
- limestone groundwater; piper trilinear nomograph; hydro-chemical characteristics; the type of water quality
- 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.
- Open Access
- This is an open access article distributed under the CC BY-NC license.
Cite this article
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 - 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 - https://doi.org/10.2991/citcs.2012.117 ID - Wang2012/11 ER -