Laboratory Measurements of the Effects of Methane/Tetrahydrofuran Concentration and Grain Size on the P-Wave Velocity of Hydrate-Bearing Sand

2011 ◽  
Vol 25 (5) ◽  
pp. 2076-2082 ◽  
Author(s):  
Feng-Guang Li ◽  
Chang-Yu Sun ◽  
Qin Zhang ◽  
Xiao-Xiang Liu ◽  
Xu-Qiang Guo ◽  
...  
1999 ◽  
Author(s):  
J. W. Ju ◽  
L. Weng ◽  
Y. Liu

Abstract This investigation focuses on experimental study of the effects of the exciting frequency and the grain (aggregate) size upon the ultrasonic P-wave velocity and the wave attenuation characteristics such as the peak-to-peak amplitude and dominant frequency-shift when performing the ultrasonic nondestructive evaluation of concrete. Furthermore, this presentation studies the extent of wave attenuation as influenced by different grain (aggregate) sizes with or without the well-distributed embedded micro-damage under different exciting frequencies. The damage index or damage assessment of concrete is certainly linked to the reduction in the ultrasonic P-wave velocity, the reduction in the peak-to-peak amplitude response, and the increase in frequency-shift through a damaged concrete specimen. In this study, we cast concrete cylinders with five different aggregate sizes in our laboratory, including some mortar samples without coarse aggregates. In addition, small styrofoam particles are mixed into the control samples in all batches to simulate microvoids in damaged concrete. The exciting frequency ranges from a low frequency at 50 kHz to a demium frequency at 300 to 400 kHz to demonstrate the frequency effect upon the ultrasonic NDE of concrete for each batch. The grain size also affects the concrete microstructure and influences the propagation and attenuation of ultrasonic waves through undamaged and damaged concrete specimens.


2021 ◽  
Author(s):  
Dariusz Chlebowski ◽  
Zbigniew Burtan

AbstractA variety of geophysical methods and analytical modeling are applied to determine the rockburst hazard in Polish coal mines. In particularly unfavorable local conditions, seismic profiling, active/passive seismic tomography, as well as analytical state of stress calculating methods are recommended. They are helpful in verifying the reliability of rockburst hazard forecasts. In the article, the combined analysis of the state of stress determined by active seismic tomography and analytical modeling was conducted taking into account the relationship between the location of stress concentration zones and the level of rockburst hazard. A longwall panel in the coal seam 501 at a depth of ca.700 m in one of the hard coal mines operating in the Upper Silesian Coal Basin was a subject of the analysis. The seismic tomography was applied for the reconstruction of P-wave velocity fields. The analytical modeling was used to calculate the vertical stress states basing on classical solutions offered by rock mechanics. The variability of the P-wave velocity field and location of seismic anomaly in the coal seam in relation to the calculated vertical stress field arising in the mined coal seam served to assess of rockburst hazard. The applied methods partially proved their adequacy in practical applications, providing valuable information on the design and performance of mining operations.


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