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World Stress Map Conference - International Lithosphere Program ...

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Wednesday, October 15 th<br />

Oral Session II: <strong>Stress</strong> modelling and interpretation at reservoir scale<br />

Lithospheric stresses and their effects on mine stability in<br />

the coalfields of the United States<br />

Christopher Mark, Murali Gadde and Sandin Phillipson<br />

National Institute for Occupational Safety and Health (NIOSH, USA)<br />

cnm7@cdc.gov<br />

During the past 25 years, mining engineers have realized that many of the severe stability<br />

problems they observe in underground coal mines are related to lithospheric stresses. Signs of<br />

horizontal stress in underground mines include: (1) Persistent roof “cutting” that follows a<br />

directional pattern; (2) Roof falls that can be 300 m long, preferentially running perpendicular<br />

to the orientation of the major lithospheric stress; (3) Severe stress concentrations that occur<br />

around mined-out and caved areas. Although US coal mines tend to be relatively shallow (less<br />

than 450m deep), analysis of a data base of stress measurements collected by the authors from<br />

approximately 60 US coal mines shows that distinct regional trends correspond roughly to the<br />

regional stress fields identified by the <strong>World</strong> <strong>Stress</strong> <strong>Map</strong> project. For example, in eastern<br />

North America, the greatest horizontal stresses measured in coal mines are usually ENE, and<br />

their magnitudes are usually 2-3 times as great as the vertical, gravity stress. The authors have<br />

also conducted regression analysis of the stress measurement data base to develop equations<br />

that predict the stress magnitude as a function of overburden depth and elastic modulus of the<br />

rock in which the measurement was made. The paper compares these results from the US to<br />

stress measurements compiled by others from the coalfields of Australia, western Europe, and<br />

South Africa. Horizontal stresses can be measured directly with instrumentation, or indirectly<br />

through the technique known as stress mapping. This paper reports the results obtained from<br />

stress mapping studies conducted at 25 mines throughout the eastern US, and compares those<br />

measurements with the trends observed in the direct measurements. The paper concludes with<br />

a discussion of how mines can minimize the effect of lithospheric stresses through proper<br />

mine planning, extraction sequence, and ground support.<br />

32 3 rd <strong>World</strong> <strong>Stress</strong> <strong>Map</strong> <strong>Conference</strong>, 15.-17. October 2008 in Potsdam

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