Experimental studies on the effects of fracture on the P and S wave velocity propagation in sedimentary rock ("Calcarenite del Salento")

被引:65
作者
Leucci, G
De Giorgi, L
机构
[1] Univ Lecce, Dipartimento Sci Mat, Osservatorio Chim Fis & Geol Ambientale, I-73100 Lecce, Italy
[2] Univ Lecce, I-73100 Lecce, Italy
关键词
fractures; seismic properties; model experiment; field experiment;
D O I
10.1016/j.enggeo.2005.12.004
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Experimental studies were carried out in laboratory in order to investigate the effects of fracture on compressional (P) wave and shear (S) wave velocity propagation and therefore the relations between seismic properties and rock mass parameters. The discontinuity index, Id, fracture density parameter C, linear fracture parameter F and the rock quality designation (RQD) were used to describe the rock mass parameters. These parameters are analyzed and then related to the seismic properties. Four vertical aligned fractures were created on an intact calcarenite block, 0.6 in long, 0.4 m thick and 0.4 in width, by sawing. The measures were carried out in four different blocks of cacarenite, having the same physical properties, and in four different phases: in first block the fractures were filled with air; in the second block the fractures were filled with "terra rossa"; in third block the fractures were filled with wet "terra rossa" and in the fourth block the fractures were filled with clay. The test results were statistically analysed using the method of least squares regression and polynomial relationships with high correlation coefficient were found between the fractured rock parameters and P-wave, S-wave velocities and V-p/V-s ratio. The investigations suggest that the P-wave and S-wave velocities decrease with increasing the fracture parameters, while the V-p/V-s, ratio increases with decreasing the fracture parameters. Furthermore the results of the experimental studies were applied on the seismic refraction tomography data acquired in a great measurements campaign undertaken in the Adriatic salentina coast (south Italy) in order to monitor the coastal erosion. The geophysical results, using the polynomial relationships between the fractured rock parameters and P-wave velocity, are in good agreement with the geomorphological and geological results. (C) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:130 / 142
页数:13
相关论文
共 21 条
[1]   INTERPRETATION OF SEISMIC DATA FROM HYDRAULIC FRACTURING EXPERIMENTS AT THE FENTON-HILL, NEW-MEXICO, HOT DRY ROCK GEOTHERMAL SITE [J].
AKI, K ;
FEHLER, M ;
AAMODT, RL ;
ALBRIGHT, JN ;
POTTER, RM ;
PEARSON, CM ;
TESTER, JW .
JOURNAL OF GEOPHYSICAL RESEARCH, 1982, 87 (NB2) :936-944
[2]   Predicting the transport properties of fractured rocks from seismic information: numerical experiments [J].
Boadu, FK .
JOURNAL OF APPLIED GEOPHYSICS, 2000, 44 (2-3) :103-113
[3]   Effects of fractures on seismic-wave velocity and attenuation [J].
Boadu, FK ;
Long, LT .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1996, 127 (01) :86-110
[4]  
BOADU FK, 1997, J APPL GEOPHYS, V36, P1
[5]  
Brown ET, 1981, ISRM SUGGESTED METHO
[6]  
Crampin S., 1980, GEOPHYSICS, V45, P361
[7]  
Deere D., 1963, ROCK MECH ENG GEOLOG, V1, P18
[8]  
Ekern A, 1995, P 35 US S ROCK MECH, P161
[10]  
Idziak A., 1988, Acta Geophysica Polonica, V36, P101