High‐resolution P‐ and S‐wave reflection to detect a shallow gas sand in southeast Kansas

Author(s):  
Deidra K. Begay ◽  
Richard D. Miller ◽  
W. Lynn Watney ◽  
Jianghai Xia
2017 ◽  
Vol 22 (4) ◽  
pp. 375-384
Author(s):  
Ahmed Ismail ◽  
Adel Abdelnaby ◽  
Timothy Larson

A study was conducted to determine whether the structural failure of a house in a residential subdivision in southern Illinois was caused by the collapse of an old underground coal mine ( i.e. mine subsidence) or as a result of a landslide. The house was displaced approximately 5 m downhill towards an engineered lake behind it. To detect any old mines near the house, we acquired high-resolution S-wave seismic reflection profiles along the roads surrounding the subdivision and a series of high-resolution P-wave reflection profiles in the immediate vicinity of the house. The S-wave seismic reflection profiles imaged a strong shallow horizon that we interpreted as Pennsylvanian siltstone overlying the Mecca Quarry Shale and Colchester Coal, which had been previously mined in the area. Locally, this horizon showed no evidence of any recent mining activities. The high-resolution P-wave reflection profiles imaged a steeply dipping bedrock with a 20° dip at the house location. These results exclude mine subsidence from being the cause for the house failure. To investigate land sliding as a possible cause of the house failure, depths to bedrock from the seismic results together with the soil type information were used to model the soil materials with a Mohr-Coulomb stress-strain model. The engineering model demonstrated that a land slide is a more plausible cause for the house failure, which agrees with the seismic results.


2001 ◽  
Author(s):  
Tomio Inazaki ◽  
Naoki Kusaka ◽  
Yuzuru Ashida ◽  
Shinji Takigawa ◽  
Shigenori Yoshimi

Geophysics ◽  
2015 ◽  
Vol 80 (1) ◽  
pp. EN13-EN25 ◽  
Author(s):  
Laura Amalia Konstantaki ◽  
Ranajit Ghose ◽  
Deyan Draganov ◽  
Giovanni Diaferia ◽  
Timo Heimovaara

Understanding the processes occurring inside a landfill is important for improving the treatment of landfills. Irrigation and recirculation of leachate are widely used in landfill treatments. Increasing the efficiency of such treatments requires a detailed understanding of the flow inside the landfill. The flow depends largely on the heterogeneous distribution of density. It is, therefore, of great practical interest to determine the density distribution affecting the flow paths inside a landfill. Studies in the past have characterized landfill sites but have not led to high-resolution, detailed quantitative results. We performed an S-wave reflection survey, multichannel analysis of surface waves (MASW), and electrical resistivity survey to investigate the possibility of delineating the heterogeneity distribution in the body of a landfill. We found that the high-resolution S-wave reflection method offers the desired resolution. However, in the case of a very heterogeneous landfill and a high noise level, the processing of high-resolution, shallow reflection data required special care. In comparison, MASW gave the general trend of the changes inside the landfill, whereas the electrical resistivity (ER) survey provides useful clues for interpretation of seismic reflection data. We found that it is possible to localize fine-scale heterogeneities in the landfill using the S-wave reflection method using a high-frequency vibratory source. Using empirical relations specific to landfill sites, we then estimated the density distribution inside the landfill, along with the associated uncertainty considering different methods. The final interpretation was guided by supplementary information provided by MASW and ER tomography.


2001 ◽  
Author(s):  
Inazaki Tomio ◽  
Kusaka Naoki ◽  
Ashida Yuzuru ◽  
Takigawa Shinji ◽  
Yoshimi Shigenori

2002 ◽  
Vol 22 (16) ◽  
pp. 2291-2301 ◽  
Author(s):  
T Missiaen ◽  
S Murphy ◽  
L Loncke ◽  
J.-P Henriet

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