Mining Research 1962
DOI: 10.1016/b978-1-4832-8307-4.50040-4
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The Time Factor in Mining Subsidence

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1973
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Cited by 6 publications
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“…In the temporal dimension, ground subsidence is not uniform over time. Subsidence of a ground point with respect to time can be described as the inverse S-shaped curve (or, time function curve) [28][29][30]. By making the first derivative of the curve, the subsidence velocity curve of the point can be obtained, as shown in Figure 11, which shows the velocity curve derived from the GNSS-IR based ground subsidence observations during the experimental campaign.…”
Section: Temporal Characteristics Of Ground Subsidence In the Study Areamentioning
confidence: 99%
“…In the temporal dimension, ground subsidence is not uniform over time. Subsidence of a ground point with respect to time can be described as the inverse S-shaped curve (or, time function curve) [28][29][30]. By making the first derivative of the curve, the subsidence velocity curve of the point can be obtained, as shown in Figure 11, which shows the velocity curve derived from the GNSS-IR based ground subsidence observations during the experimental campaign.…”
Section: Temporal Characteristics Of Ground Subsidence In the Study Areamentioning
confidence: 99%
“…This time in turn is controlled by the depth and the angle of draw (because these factors determine the critical area) as well as by the rate of advance. Typical longwall advance rates are 0.3-1.2 m per day, and "high-speed" longwall face advance in coal is about 1.5 m per day (Whetton and King, 1961;National Coal Board, 1952, 1963. The maximum longwall face advance reported was approximately 5.5 m per day in a bedded quartzite in South Africa (Cook, 1967).…”
Section: Rate Of Advancementioning
confidence: 99%