Mine Water Recovery in the Coal Mining District of Aachen - Impacts and Measures to Control Potential Risks

2002 ◽  
pp. 1011-1020
Author(s):  
K.-H. Heitfeld ◽  
M. Heitfeld ◽  
P. Rosner ◽  
H. Sahl ◽  
K. Schetelig
Kerntechnik ◽  
2008 ◽  
Vol 73 (3) ◽  
pp. 101-107
Author(s):  
C. Wanke ◽  
S. Ritzel ◽  
R. Sachse ◽  
R. Michel

2019 ◽  
Vol 53 (2) ◽  
pp. 227-235
Author(s):  
Yanxian Liu ◽  
Luwang Chen ◽  
Yudi He ◽  
Lanting Wang ◽  
Jie Zhang ◽  
...  

2018 ◽  
Vol 25 (1-2) ◽  
Author(s):  
Radek Morcinek ◽  
Josef Zeman

Large amounts of mining waters are discharged into waterstreams in the region of Ostrava-Karviná Mining District. This paper deals with discharged mine water from the Žofie watershaft , which is located in Petrvald basin in Czech part of Upper Silesian coal basin. Mine water may affect surface watercourses, especially their sediments, which may have increased activity of radium 226Ra. The aim of this work was to evaluate geochemical evolution of the Rychvald creek with regard to the mobility of radium 226Ra and estimate the degree of influence. From the results, it is evident that the mine waters significantly affect the composition of Rychvald creek. Increased equivalent dose was measured only up to the wastewater treatment plant, which probably considerably diluted the water, consequently diminishing migration abilities of radium. From the result of physicochemical parameters it is evident that discharged mine water from the Žofie watershaft affects mainly conductivity, due to high mineralization of discharged mine water. Increased doses of the gamma radiation equivalent, which are related to the increased mass activity of radium 226Ra, were found in the sediment of the first 1 200 m of the Rychvaldské creek. However the determined increased activities of radium 226Ra do not represent neither substantial risk for human health nor important risk for the environment.


2020 ◽  
Vol 39 (1) ◽  
pp. 150-156 ◽  
Author(s):  
Gang Lin ◽  
Donglin Dong ◽  
Xiang Li ◽  
Peiwei Fan

2013 ◽  
Vol 734-737 ◽  
pp. 484-487 ◽  
Author(s):  
Mei Hua Geng ◽  
Xiu Jiang Lv ◽  
Xiao Gang Zhang

The geological structure is an important factor of gas occurrence in coal seam, and the gas occurrence in deep coal seam should be paid attention to enough because the occurrence was more controlled by geological structure and influence. Taken Fengfeng coalfield as target in this paper, the geological structure of this coalfield was described. The deep coal mining district which is monoclinic structure in Fengfeng is located in the east of Gushan anticlinoria, which the junior small anticlines and synclines of the sub-echelon are well developed. And regional fault structures are intensive, the pressure structure is the major structure among this region. The characteristics of geological structure in Fengfeng coalfield were analyzed. The tensional structure planes and pressure structure are the major effect factors, and the latter is the main form of gas occurrence in deep. Some suggestions on safe of deep mining in high gas environment is also put forward, in order to provide theoretical support for the deep coal mining and gas disaster prevention.


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