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_GENERAL DOCUMENTS - C1981017 (262)
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_GENERAL DOCUMENTS - C1981017 (262)
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Last modified
11/2/2020 11:08:18 AM
Creation date
6/21/2012 10:47:08 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981017
IBM Index Class Name
GENERAL DOCUMENTS
Doc Name
Bid Documents (IMP) Backfilling and Grading Plan for Preparation Plant Area
Permit Index Doc Type
General Correspondence
Media Type
D
Archive
No
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DRMS Re-OCR
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Signifies Re-OCR Process Performed
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-39- <br /> The impacts of subsidence due to mining can be expected to vary in <br /> magnitude and extent. This variation will result from a combination of <br /> numerous natural phenomenon and from the effects induced by underground <br /> mining. Surface water and ground water can both be influenced by <br /> differences in timing of mining and the physical environment. It is <br /> assumed that all mining will result in subsidence at some future point in <br /> time, although surface manifestation may require many years to occur. <br /> Therefore, control and prediction of subsidence are critical , necessary <br /> measures, which should be implemented before and during any mining <br /> activity. <br /> Natural phenomena which influence subsidence are: <br /> - Depth of overburden; <br /> - Thickness of the coal seam; <br /> - Stratiyraphy, lithology and structure of the overburden; <br /> - Topography; and <br /> - Lithology of the floor strata. <br /> Mining activities which affect subsidence are: <br /> - Size, shape, depth, location, and areal extent of workings; <br /> - Rate of development and extraction of resource; <br /> - Mining methods; and <br /> - Number of overlying and underlying coal seams mined. <br /> The possible imparts of subsidence include: <br /> - Modification of surface water hydrology - channel and <br /> watershed geometry and sediment erosion rates ; <br /> - Modification of ground water hydrology - changes in spring <br /> discharge, aquifer characteristics and recharge; <br /> - Loss of water from surface impoundments due to disruption by <br /> surface cracking; and <br /> - Increase in surficial mass movement activity - landslides and <br /> rock falls. <br /> Natural physical influences upon subsidence can be controlled to the <br /> extent that mine plans can be designed to avoid obvious hazards (e.g. , <br /> shallow workings beneath perennial streams, landslide bodies, <br /> impoundments, etc. ) , or to limit subsidence in accordance with the <br /> current state-of-the-art of ground control (engineered control of roof <br /> and pillar failures in nines) . Subsidence prediction and ground control <br /> engineering are not definitive sciences. Design engineering concepts <br /> must be verified through continuous nonitoring of surface topography, <br /> ground water hydrology and surface water hydrology. <br /> :'valuation of the impacts of subsidence upon hydrologic systems requires <br /> the collection and analysis of extensive Monitoring data consisting of <br /> surface 'water and ground 'water moni .oring ' quantity and quality) , <br /> precipitation caging, geolccical mapping, topographic surveying an,. <br />
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