Rock Fracture and Blasting 2016
DOI: 10.1016/b978-0-12-802688-5.00003-8
|View full text |Cite
|
Sign up to set email alerts
|

Rock Fracture and Rock Strength

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

2
41
0
3

Year Published

2017
2017
2024
2024

Publication Types

Select...
5
3

Relationship

0
8

Authors

Journals

citations
Cited by 58 publications
(46 citation statements)
references
References 31 publications
2
41
0
3
Order By: Relevance
“…We argue that this is less possible in the heavy-rain zone of this study, because Miller (2008) found that the rain-triggered earthquakes occurred exclusively in karst geology where the rainwater can quickly flow into the underground karst network to induce earthquakes. In this study, the heavy-rain zone is mainly in the southern Central Ranges with primarily metamorphic rocks where its permeability is much lower than the karst areas (Ho, 1988;Wang et al, 2004;Zhang, 2016). This is consistent with our observation that no clear changes in seismicity are observed in the following weeks in the heavy-rain zone either defined as the 2-m contour or the 1.5-m contour (Figures 1a and 11).…”
Section: Seismicity In the Heavy-rain Zone In Weeks Before And After ...supporting
confidence: 90%
“…We argue that this is less possible in the heavy-rain zone of this study, because Miller (2008) found that the rain-triggered earthquakes occurred exclusively in karst geology where the rainwater can quickly flow into the underground karst network to induce earthquakes. In this study, the heavy-rain zone is mainly in the southern Central Ranges with primarily metamorphic rocks where its permeability is much lower than the karst areas (Ho, 1988;Wang et al, 2004;Zhang, 2016). This is consistent with our observation that no clear changes in seismicity are observed in the following weeks in the heavy-rain zone either defined as the 2-m contour or the 1.5-m contour (Figures 1a and 11).…”
Section: Seismicity In the Heavy-rain Zone In Weeks Before And After ...supporting
confidence: 90%
“…In shock waves, characteristic impedance (Z) is defined as (e.g., Cooper 1996;Zhang 2016) where is the density of the material in which a shock wave is propagating and D is the velocity of the shock wave. Notice that D and ρ are variables rather than constants in shock waves.…”
Section: Shock Wavesmentioning
confidence: 99%
“…Characteristic impedance was suggested for evaluation and classification of rock masses, because the characteristic impedance of rock mass could represent the geological structures of the rock mass, e.g., joints, faults, bedding, and mineral composition, to a certain extent (Zhang 2016). Following this suggestion, Zhang et al (2020a) found six empirical relations between the characteristic impedance and main mechanical properties such as Young's modulus, Poisson's ratio, mode I fracture toughness and uniaxial compressive, tensile and shear strengths of intact rock, based on a great number of intact rock tests.…”
Section: Introductionmentioning
confidence: 99%
“…The process takes place under the action of local disturbing forces exceeding the internal rock forces [2], [3]. Under the specified conditions, rock efforts result from the action of hard tools, hydraulic flows, and the developed waves and fields of diverse nature [6]. In this context, further progress and improvement are mainly accounted for rock-breaking tools if general approaches to the idea of the applied drilling techniques have been maintained.…”
Section: Analysis Of Recent Studies and Publicationsmentioning
confidence: 99%
“…buckling, chipping, cutting, crushing etc.) [6] is a distinctive feature of the majority of production methods of well drilling resulting in its fragmentation. Nevertheless, the examples cannot limit possible alternatives of a well bottom advance within the rock mass.…”
Section: Singling-out a Previously Unsolved Part Of The General Problemmentioning
confidence: 99%