Science topic

Rock Mechanics - Science topic

Rock mechanics is the theoretical and applied science of the mechanical behaviour of rock and rock masses;also compared to the geology, it is that branch of mechanics concerned with the response of rock and rock masses to the force fields of their physical environment.
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Could you please share some innovative project ideas or recent advancements in mining engineering? I'm particularly interested in areas like rock mechanics, blasting techniques, mine safety systems, and water management in mines. Your insights would be greatly appreciated! Thank you!
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Here are some innovative project ideas and recent advancements in mining engineering that could support the development of Rwanda’s artisanal mining sector:
1. Digital Mapping and Resource Estimation
• Develop a GIS-based system to map mineral-rich areas, providing artisanal miners with better access to resource data.
2. Sustainable Mining Techniques
• Introduce environmentally friendly methods, such as bioleaching, to reduce the environmental impact of small-scale mining.
3. Mechanization and Safety Enhancements
• Design affordable, low-cost equipment to improve efficiency and safety for artisanal miners.
4. Mineral Processing and Value Addition
• Develop small-scale processing technologies for minerals like coltan and tantalum, allowing miners to increase value locally.
5. Blockchain for Supply Chain Transparency
• Implement blockchain technology to ensure traceability of minerals, meeting international standards and increasing market access.
6. Water Recycling Systems
• Design water recycling solutions to address water usage challenges in artisanal mining operations.
These projects not only enhance productivity and sustainability but also align with Rwanda’s development goals by empowering artisanal miners and promoting responsible mining practices.
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International Journal of Rock Mechanics and Mining Sciences(IJRMMS)
The paper was submitted on September 13, 2022, and was rejected on January 11, 2024.
During the 485 days review cycle, there was no response, no review or suggestions made on the content of the paper, and it was ultimately rejected as not meeting the scope of publication in the journal.
Several authors waited for 485 days, only to receive an unapologetic and irresponsible response below.
Dear Professor XXX, Thank you for submitting your manuscript to International Journal of Rock Mechanics and Mining Sciences. I regret to inform you that the reviewers recommend against publishing your manuscript, and I must therefore reject it. My comments, and any reviewer comments, are below. We appreciate you submitting your manuscript to International Journal of Rock Mechanics and Mining Sciences and thank you for giving us the opportunity to consider your work. Kind regards,   Professor XXXX XXXX Editor-in-Chief International Journal of Rock Mechanics and Mining Sciences Editor and Reviewer comments:   This manuscript is primarily focused on geophysical imaging and processing techniques and in my opinion is outside the scope of IJRMMS. The work presented is largely mathematical with little rock mechanics. My recommendation is to encourage the authors to transfer their manuscript to Elsevier's Journal of Applied Geophysics, where it is better suited both in terms of interests of the readership and securing knowledgeable reviewers.
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Incredible! Some Elsevier journals aren't kidding. May this decision not discourage you for future submissions.
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International Journal of Rock Mechanics and Mining Sciences-IJRMMS
After 485 days of review, no comments were made on the content of the manuscript, and the manuscript was rejected only on the grounds that it did not meet the scope of the journal. Here are the only responses.
Dear Professor XXXXX,
Thank you for submitting your manuscript to International Journal of Rock Mechanics and Mining Sciences.
I regret to inform you that the reviewers recommend against publishing your manuscript, and I must therefore reject it. My comments, and any reviewer comments, are below.
We appreciate you submitting your manuscript to International Journal of Rock Mechanics and Mining Sciences and thank you for giving us the opportunity to consider your work.
Kind regards, Professor XXX XXXX Editor-in-Chief
International Journal of Rock Mechanics and Mining Sciences
Editor and Reviewer comments:
This manuscript is primarily focused on geophysical imaging and processing techniques and in my opinion is outside the scope of IJRMMS. The work presented is largely mathematical with little rock mechanics.
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Just resubmit somewhere that values your important work. And only wait a few weeks to hear back :)
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There is an underground powerhouse structure in the Himalayan region. In this structure, rockbolts and steel ribs were installed.
The rockbolts have load holding capacity of 57 tons but due to improper installation and poor rockmass condition, the final load-holding capacity of the rockbolt varies between 30 tons to 57 tons.
The load is increasing on the underground structure and at several locations, rockbolts are failing because the load reached 45 tons.
At the same time, steel rib has a compression capacity of 1.06 MN/m2 but at a few steel ribs, it has reached 1.33 MN/m2.
What are the geotechnical risks involved in such a situation in this underground rockmass structure?
What corrective measures would be necessary to handle such a situation in this underground rockmass structure?
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Dear Vikalp Kumar Please do recommend my answer if helpful
Choosing the wrong type of rock bolt in an underground structure can lead to failure and compromise the stability and safety of the structure. Corrective measures should be taken promptly to address such issues. Here are some recommended corrective measures:
1. **Site Assessment and Evaluation:**
- Conduct a thorough assessment of the site, including geological conditions, rock type, stress distribution, and other relevant factors.
- Reevaluate the load-bearing capacity and structural requirements to ensure that the selected rock bolts are appropriate for the specific conditions.
2. **Engineering Analysis:**
- Engage geotechnical and structural engineers to perform a detailed analysis of the failure and determine the root causes.
- Assess the load-carrying capacity of the original rock bolts and identify any design flaws or miscalculations.
3. **Selection of Appropriate Rock Bolts:**
- Choose rock bolts that are suitable for the geological and structural conditions of the underground environment.
- Consider factors such as rock type, stress levels, and the required load-bearing capacity when selecting new rock bolts.
4. **Implementation of Monitoring Systems:**
- Install monitoring systems to continuously assess the performance and behavior of the rock bolts.
- Implement instrumentation such as strain gauges, displacement sensors, or other relevant devices to detect any signs of stress or movement.
5. **Reinforcement and Redesign:**
- Reinforce the failed rock bolt locations with additional support or alternative reinforcement methods.
- Redesign the structural support system if necessary, incorporating lessons learned from the failure.
6. **Quality Control and Assurance:**
- Implement stringent quality control measures during the installation of new rock bolts to ensure proper installation and adherence to design specifications.
- Regularly inspect and maintain the rock bolts to identify any potential issues before they escalate.
7. **Training and Education:**
- Provide training to personnel involved in the selection, installation, and monitoring of rock bolts.
- Ensure that the engineering and maintenance teams are aware of best practices and lessons learned from the failure.
8. **Documentation and Reporting:**
- Document the failure incident, including the identified causes and implemented corrective measures.
- Share this information within the organization and with relevant stakeholders to prevent similar mistakes in future projects.
9. **Continuous Monitoring and Feedback:**
- Establish a continuous monitoring and feedback system to track the performance of the structure over time.
- Regularly review the effectiveness of corrective measures and make adjustments as needed.
By taking these corrective measures, it is possible to address the issues caused by the wrong choice of rock bolts and enhance the stability and safety of the underground structure.
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Rock mechanics
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Dear Doctor
Go To
Influence of some rock strength properties on jaw crusher performance in granite quarry
By BM OLALEYE
Elsevier, Mining Science and Technology (China)
Volume 20, Issue 2, March 2010, Pages 204-208
"Abstract
The influence of rock strength properties on Jaw Crusher performance was carried out to determine the effect of rock strength on crushing time and grain size distribution of the rocks. Investigation was conducted on four different rock samples namely marble, dolomite, limestone and granite which were representatively selected from fragmented lumps in quarries. Unconfined compressive strength and Point load tests were carried out on each rock sample as well as crushing time and size analysis. The results of the strength parameters of each sample were correlated with the crushing time and the grain size distribution of the rock types. The results of the strength tests show that granite has the highest mean value of 101.67 MPa for Unconfined Compressive Strength (UCS) test, 6.43 MPa for Point Load test while dolomite has the least mean value of 30.56 MPa for UCS test and 0.95 MPa for Point Load test. According to the International Society for Rock Mechanic (ISRM) standard, the granite rock sample may be classified as having very high strength and dolomite rock sample, low strength. Also, the granite rock has the highest crushing time (21.0 s) and dolomite rock has the least value (5.0 s). Based on the results of the investigation, it was found out that there is a great influence of strength properties on crushing time of rock types."
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I tried to find a site where I can buy a needle penetrometer for weak rocks/soft rocks. But my search was not successful. Does anybody where I can get a needle penetroemter? Links are welcome.
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Compared to the old-fashioned and currently used emulsion type explosives, the explosive filling of the tunnel face with bulk charging provides better and higher quality vibration values. if you are drilling in the tunnel face with the Mwd (measurement while drilling) featured jumbo. Because with the mwd-capable machine, heterogeneous drilling is performed in the formation whose face surface is uneven and the drilling lengths are different. Therefore, a homogeneous charge in a heterogeneous face with an emulsion-type explosive of constant kilogram will be difficult. Therefore, I think that more stable vibration data will be obtained with bulk charging. What is your opinion?
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I obtained an empirical formula with 95% accuracy rate with emulsion type explosive. Thank you very much for your esteemed reply. I think I can get more accurate results with bulk charging. Thank you very much for your interest, Mr. Signh.
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Are you interested in reservoir characterization? Want to learn about tools that can be applied to oil & gas, critical minerals, and CCUS? Then consider participating in the Premier-Corex short course at the 2023 Rocky Mountain Section AAPG meeting in Bismarck this June. Can't make it to North Dakota? No problem! There's a virtual option. See below for details and links to the meeting registration site:
What: RMS-AAPG Premier Corex Short Course
When: June 4 (Sunday) 2023, 8 am to 5 pm
Where: Radisson Hotel Bismarck (room TBD); virtual component*
Sponsoring Organization(s): Premier-Corex; AAPG Rocky Mountain Section
Title: Applications of Reservoir Characterization Workflows to a Range of Geologic Energy Resources in Sedimentary Basins
Instructors
Mike Dix (Premier Corex) - Geology and petrology
Jules Reed (Premier-Aberdeen) - Core analysis, special core analysis, flow studies in general
Sean Arrington (Premier-Houston) - Rock mechanics
Peter Johnson (Carbon Solutions) - Reactive transport and other modeling
Organizers
Mike Dix (Premier Corex), Bryan Guzman (Premier Corex), Bret Fossum (UND-EERC), Tim Nesheim (NDGS), and Justin Birdwell (USGS)
Description: This 1-day course will provide a review of reservoir characterization workflows for sedimentary basins relevant to development of variety of different resources. A variety of topics will be covered, including (for details, visit: https://www.rms-aapg2023-bismarck.com/short-courses):
Who Should Attend: Geoscientists and engineers interested in reservoir characterization using core, cuttings, and other data types to develop conventional and unconventional oil & gas resources, carbon sequestration prospects, and critical elements/minerals in sedimentary basins.
Morning Schedule
Unconventional Resources (2 hours)
Conventional Resources (2 hours)
Afternoon Schedule
Critical Elements/Minerals (1.5 hours)
CCUS (2.5 hours)
Register here
Fees (in-person and virtual options)
Professionals: $200
Students: $50
Virtual Attendees: $125
*Note, virtual attendees may not be able to view all content due to use of proprietary data in some modules.
Includes: Handouts, presentations, Q&A: light breakfast and boxed lunches provided for in-person attendees
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Interested
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If one is monitoring an underground rockmass structure (underground powerhouse currently producing electricity) using microseismic monitoring process and there is no occurrence of earthquake, blasting, micro-earthquakes, transportation of material etc. in that region.
We are getting about 150 microseismic event in six month and the deformation is low.
Can we say that we are doing dynamic stability analysis of that underground structure using Microseismic monitoring? If yes why?
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Micro-seismic investigation definitely pave the way for assesment of dynamic stability of caverns. However, the signals should be recorded and interpreted on daily basis and with due care & precision.
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In order to calculate the volume of an in situ block intersected by three joint sets, besides spacings between joints, we also need the intersection angle between joint sets. How can we calculate the intersection angle between joint sets using dip and dip direction data? Can you recommend any methods, software, or papers related to this subject?
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Dear Followers of the Question,
I asked my question to ChatGPT. Here is the answer:
To calculate the intersection angle between two joint sets using dip and dip direction data, we can use the following formula:
cos(θ) = cos(α1)*cos(α2) + sin(α1)*sin(α2)*cos(δ1-δ2)
where:
- θ is the intersection angle between the two joint sets
- α1 and α2 are the dips of the two joint sets
- δ1 and δ2 are the dip directions of the two joint sets
Once we have calculated the value of cos(θ), we can use the inverse cosine function (usually denoted as cos^-1 or acos) to obtain the value of θ.
Note that dip direction data is typically given in degrees clockwise from north, so we may need to convert this to azimuth (degrees clockwise from east) before using the formula. This can be done using the following formula:
azimuth = (450 - δ) mod 360
where:
- δ is the dip direction in degrees clockwise from north
- the "mod 360" ensures that the value of azimuth is always between 0 and 360 degrees.
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Rock Mechanic
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Dear Dr.RK.Naresh
Thank you so much Best Regard Jaffar
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Kindly suggest a recent review paper on developing landslide early warning system in Hard Rock Slopes? It would be great if papers are provided where role of rainfall is considered in rock slope. It is important to mention here that, I require papers where rainfall role in hard rock slopes is considered NOT soil slopes. Kindly suggest recent papers on this topic. Thanks
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Dear
N. Bar
Thanks for the referred paper.
Regards,
Raj
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I would like to know what the minimum strength of a rock has to be when I want to conduct a point load test. When rocks or indurated soils have a strength below a certain treshold they fail very fast and the result of the point load test is not evaluable.
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Hello
minimum value to of UCS to perform reliable PLT is accompanied by the deformation mode prior to failure. Progressive failure and large indentation with large "footprint" of the cone create problems in correlation. Quasi-brittle rock materials can be tested starting from UCS 15 MPa, while softer materials need at least about UCS 20 MPa. Take care that also coefficient for correlation between the test index and the UCS can vary: for most brittle rocks, the ratio is approximately 10, for soft sedimentary stones the ratio can be lower ( 5). As a consequence, PLT results might have to be interpreted differently.
See also USING THE POINT LOAD TEST TO DETERMINE THE UNIAXIAL COMPRESSIVE STRENGTH OF COAL MEASURE ROCK by Rusnak and Mark.
Hope this can help
Regards
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Rock in chemical solution will appear chemical damage, this damage is a kind of water-rock interaction, so we can expect rock mechanical properties cracking, what else can we pay attention to?
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Thank you for your reply. In fact, I once studied the dissolution process of rock minerals in the process of acid leaching, and observed the rock morphology after the acid leaching process by scanning electron microscope. I'm actually curious about the formation of rock cracks https://www.researchgate.net/profile/Blessing-Taiwo-5during acid leaching.@
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Hello everyone. I'm working on reservoir rock mechanical properties. Do you know any conducted study on correlation between rock mechanichanal and thermal properties?
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Thank you Mehdi Razavifar jan.
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I want to get information about world-class universities, especially in the fields of geotechnical engineering and tunneling. Therefore, the following questions arise:
Which universities and in what research topics are the best at present?
What are the reasons for choosing them?
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Colorado School of Mines
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Please share the links in your comments.
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While I am not aware of any dataset related to what you are exactly looking for, but, you may consider exploring the following datasets:
1. Dataset of Country-Specific Interests Towards Fall Detection From 2004–2021 - https://dx.doi.org/10.21227/85jy-7m92
2. A Dataset on Online Learning-Based Web Behavior from Different Countries Before and After COVID-19 - https://dx.doi.org/10.21227/pa7d-nt11
3. Online Learning Global Queries Dataset: A Comprehensive Dataset of What People from Different Countries Ask Google About Online Learning - https://dx.doi.org/10.21227/xbvs-0198
4. Exoskeleton Twitter Dataset: A Comprehensive Dataset of Tweets Related to Exoskeletons - https://dx.doi.org/10.21227/r5mv-ax79
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I am currently focusing on 3D geomechanical modeling. And in the future, I want to extend it to a 4D model. During my recent studies, I realized that most of the 4D geomechanical modeling that has been done has not properly updated the elastic properties such as Young's modulus, bulk modulus, Poisson ratio, etc. If a 3D static model is extended to a dynamic model, or a two-way or one-way coupling is performed, it is necessary to consider all material behaviors in a time-dependent manner. Please share if you have useful information in this regard or if you have a suggestion, I would be grateful if you could comment.
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Hi Erfan Rahimi , in time-dependent 3D geomechanical simulation ("4D" coupled flow and geomechanical simulations) there a many interdependencies between material properties (e.g., elastic properties, strength properties, porosity/ permeability, fluid properties) and simulated fields (stress, strain, pore pressure).
You have to think carefully when including additional interdependencies (or vice versa NOT including these interdependencies), whether they add (i) a lot of additional complexity, (ii) create a lot of additional insight, (iii) create complexity without creating insight, (iv) the error incurred by failing to include the interdependency. As you correctly point out, updating elastic properties in the overburden is NOT commonly for coupled flow and geomechanical modelling. This is one of the cases where you make the simulations a lot more complex, without adding a lot of insight. Elastic properties due to stress/strain changes in the overburden change by less than a percent from their initial value - and updating the elastic properties will affect the simulated stress field by an amount which is insignificant compared to our ability to calibrate the stress field. In your picture, you show a loop which includes updating of velocities for 4D seismic attribute generation. Here updating the velocities (even by less than 1%) results in something we can observe in field data in the form of time-lapse timeshifts. In a similar manner, if permeabilities are stress dependent in a significant manner and neglecting to include this coupling will create a large error, it is customary to include this coupling. Another example of coupling which is sometimes, but not always, used is to use non-linear stress-strain relationships in the reservoir, if significant compaction occurs and the reservoir rock will experience irreversible compaction.
In summary, keep models as simple as possible, and add complexity if there is a good reason. Do not fall into the trap of making models "complex" for the sake of complexity. Complex models are harder to interpret, and don't necessarily provide more insight. There is an unfortunate tendency of assuming that "complex" models are "better" models. They sometimes are, and often are not.
Hope this makes sense, and addresses your question.
Cheers,
Jorg
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I have completed a Master of Engineering in Mining Engineering. I am currently exploring the possibility of pursuing a Ph.D. in the same domain in early 2022 or 2023.
My areas of interest are the following:
- Rock mechanics and ground control
- Backfilling the mined-out area
- Gemstones and their processing
- Open-pit optimization
Any other suggestion beyond this abovementioned is also welcome.
Thank you.
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Dear Jean,
Application of AI techniques, numerical and analytical methods for the investigation of discontinuous rock structural stability can be polite.
There are several papers that can be helpful:
Best regards,
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I am a master degree candidate in Mining Engineering. I am interested in rock mechanic and geotechnical area of study in mining, which will be highly in demand in the future. any suggestions would be appreciated.
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Dear Abdul Basit Abdullah,
Appllication of soft computing methods and artificial intelligence techniques for prediction of target parameters in rock mechanics would be useful, so it would be possible for you to work on up-to-date research topics by considering ML and DL.
Best wishes,
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Bit of background… Geotechnical engineering in mining focus on broader classification (RQD, Q, RMR etc). The makeup of rocks grouped in these classifications and other classes like lithology can vary significantly. For example, some data I’ve looked has a range of 40% iron content for an individual lithology. I would expect something like iron influence rock mass strength, an influence which would be masked if not lost, when relating the broader categories to excavation performance.
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All of the points listed above can be applied also to underground mining works with some adaptations to the individual stoping designs and types of mineral deposits
HGD
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I am a Ph.D. candidate in Mining Engineering. I was so confused in the selection of a suitable topic for my Ph.D. My areas of interest include Slope Stability, Rock Mechanics, Rock Blasting, Slope Stability, Waste Management, and Environmental Management in Mines. any suggestions would be appreciated.
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Set some topics that you interested
Read some new papers on the subject
Find a theoretical basis about the subject
Look for some aspects that you can make a difference
Don't limit yourself to special subjects
Try to find a subject related to new ideas ( Smart Mine, Robots and drones in mining, Sustainability and environmentalism, deep-sea mining)
Also, this paper will be useful:
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I am looking for the data from the completed Tunneling projects located all over the Nepal if possible. Data can be geological mapping, Physical features, rock mechanical data if any, tunnel convergence or any deformation related values, etc.
Can anyone direct me to the places or person that can help me in this process.
Thank you!!
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Thank you Nick! Being in Kathmandu, Bikram has better overview about it I assume. The major sources from where tunneling data can be collected are DoED, NEA, NTA and IPPAN. It is good that you have started to update the data record on tunneling status in Nepal.
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What are the parameters required for designing open pit mines?
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Bench height.
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Hi everyone!
How we can calculate the stress intensity factor (KI and KII) in numerical software such as FLAC, UDEC or any software except Abacus (I mean Integral J)?
There are some equations for determining KI and KII based on stress in crack tip, but it cannot be calculate the KI and KII because of teta angle in these equations. Does any relationship between KI and KII based on stress in crack tip (for inclined crack)?
Thanks in advance for answering.
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Im interested too , if u can help me sir
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we have some experimental data of mechanical strength of rock material. We compare this data with the estimated strength (calculated using several existing criteria) and also determined the error percentage for each criteria. 
So i want to know that
what is the maximum percentage of error, that is acceptable for rock mechanics purposes, specially when we compare the experimental data with the estimated ones.
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the error for my study (prediction of unconfined compressive strength - 1120 data points) is about 30%
do you have any reference regarding your answer that may help me
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dear friends from the rock mechanics field
Good day. I have what may seem a minor problem, but I cannot crack it somehow.
I have attached a page from Hoek & Brown (1997) paper, which gives elaborate spreadsheet formulas for simulation of triaxial data and conversion to Mohr-Coulomb parameters, in absence of actual triaxial tests. All the formulas are explained and mutually connected except one.
What is the formula for signt??
It is the normal stress which must be specified in order to calculate the tangent to the Mohr envelope. There is a myriad of formulas involved with the problem and I just don't see the answer. I would greatly appreciate assistance.
Cheers, Hrvoje Vučemilovič
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Hoek Brown criteria helps in determining rock failure conditions, while Mohr Coulomb criteria is related to plasticity of rocks and strength.
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I did my PhD research on slaking rocks or soft sedimentary rocks, respectively. During my literature research in the beginning of my PhD project it was pretty obvious that there is no general defintion of the terms "soft rock", "weak rock" etc.
There are two fundamental views. On the one hand there are the (classic) defintions with respect to the strength of the rocks on the other hand there are defintions relating to the slaking behaviour of rock.
Even in the very recent book "Soft Rock Mechanics and Engineering" most of the reseachers find it necessary to define the term "soft rock" and how it is used in the following chapters indicating that there are still lots of open questions regarding a general definition of this/these group of geomaterial.
What is your opinion on the definition on the term "soft rock", "weak rock", "slaking rock" etc.?
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Building on some of the previous posts, in my mind "weak rock" refers to the rock's strength. Typically, a boundary strength value will be specified to separate "weak" from "strong" for a given context.
"Soft rock" refers to how a rock responds to weathering, or how abradable the rock is (there tends to be a correlation, but they are different processes). A rock that quickly weathers is "soft." Likewise, a rock that is readily abraded, for example when it forms a stream bed, is "soft." Often, but not always, these "soft" rocks will exhibit slaking behavior when they are cycled through wetting and drying. It is a specific form of disintegration in response to weathering and is associated with clay minerals. Slaking can also result from freezing and thawing or the growth of precipitates, like salt.
Low strength, readily weathered/abraded, and prone to slaking are often attributes that are found together (e.g. a claystone). Likewise, high strength, slow to weather, and not being prone to slaking are often found together (e.g. a quartzite). However, there are exceptions. For example, some sandstones can be relatively strong, but weather relatively quickly without exhibiting slaking behavior.
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Dear colleagues!
What is the best method to determine In SItu Block Size Distribution if I have orientation, spacing and persistence data collected from 3D Point Cloud?
I considered using 3DEC but I am not very fluent in the software.
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Hi Friend
I think you use the Rmi classified to detemine Vb.
Thanks
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Hello everyone!
I'm looking for the most recent developments in analytical, numerical and experimental micromechanical modelling of mechanical and flow response of Jointed Rocks.
I would like this space to be open and free also to suggestions of materials, articles and so on.
Thanks a lot!
Augusto Borges
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Hi
What's your project subject? What do you like do?
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I am planning of furthering my career by doing a PhD in Mining engineering, most likely in 2021 or early 2022. My areas of interest are Rock Mechanics and mining geotechnical. I am not too sure about the topic that I chose. Is this topic still interesting enough for now?
or are there any suggestions for other topics that are more interesting?
as well as university recommendations for me to take my doctoral programe ?
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In underground mines the stability aspect of the infrastructure and of the mining process itself will always be relevant. Obtaining methods or techniques of self-support or support through external elements under a minimum cost scheme is one of the fundamental aspects for the technical and economic viability of the exploitation of an underground mining deposit. Mines that have suffered collapse in some of their areas have experienced great losses due to stoppage of their operations, loss of equipment and in some cases of people, therefore it is an issue that continues to be valid. Something similar happens in open pit or surface mines. The equilibrium slope must be maintained to ensure that the slope is stable. A steep slope allows for greater stability, but is too expensive. On the other hand, a slope with a steeper incline is more economical but reduces its safety factor. It is necessary to find the optimal inclination that allows the company to generate maximum profitability without affecting safety. Finally I could tell you that it is a very good topic for your thesis. Cheers
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There are three primary areas of ground movement towards a pressurised TBM: at the face, along the shield skin and at the tail void -(In the attached figure).
Can the maximum surface Settelment of the tunnel Longitudinal Cross section due to the displacement of the tunnel face can be added with the Transverse cross-section surface Settelment and introduced as the final surface Settelment? in 2D model-numerical method.?
But in the transverse two-dimensional method, we cannot get Settlements dou to face pressure induced by tunnel advanc.
I was going to get the Settlements dou to face pressure from the longitudinal 2D model and add it to the other Settlements Caused by other factors
In the longitudinal section of the tunnel, details and geometries and conditions have been implemented so that only the displacement caused by the face pressure is created and that the shield cone and mortar injection and consolidation are not modeled.
so only max surface settelment in longitudinal cross cestion is occurred due to face pressure It is capable of adding with max surface settelment in transverse cross sestion due to injection pressure and shield cone?
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I simulated the shield driven-tunnel by FLAC 2D, in which step of numerical model must be applying the traffic loads of ground surface (20 Kpa)? the traffic loads of ground surface change along day and night
@steps:
1. elastic initial equilibrium.
2. elastic-plastic initial equilibrium.
3. Simultaneous with excavation and pre-installation lining.
*in which step influence the traffic loads is real? (interaction with ground above tunnel)
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I need a large model say 100 x100 m with a mesh size of 0.05m. such a large model cannot be made in version 7. before upgrading to version 8, I need to confirm whether it is working in version 8 or not?
I have also tried trail version 8. it is also not working
if anyone has version 8, I can send you a file to check.
Thanks
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When conducting analysis of foundation on rocks, and the triaxial test results of the rock material is found as c=3 MPa and ϕ= 44 degrees. In analysis, this cohesion value has to be reduced to account for the rock mass, to a value of maybe 50-300 kPa. Is this assumption correct? Or are there some correlations in the literature?
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This is one of the toughest questions in rock mechanics. Many 'answers' may be far from the truth - which we will never know anyway. But here goes: what if 2D UDEC-MC or UDEC-BB are allowed/available. Represent the jointing as sketched by an engineering geologist, digitize, and apply scaled JRC, JCS values using block size scaling. Convert the non-linear BB to MC for the joints if UDEC-BB not available. Try to model with some discontinuous jointing, and use numerically glued joints. Can estimate a lower-bound c for the intact bridges/glued joints from a linear tangent to the tensile and UCS Mohr circles, c =1/2(sigma c x sigma t)E0.5: construct and check, also estimate phi. If a continuum analysis is to be performed with linear MC or non-linear HB be aware that degrading c and mobilizing phi is more correct than the usual addition. If the building is very high and you are under higher stress, the more correct curved envelope for the critical intact bridges is found by moving 1 x UCS along the normal stress axis and drawing the critical state max. shear strength Mohr circle, with radius = UCS, therefore max possible shear strength numerically similar to UCS (Singh et al 2011). Sigma 1 (max) = 3 x UCS for stronger more correct curvature than HB. Note also stress-dependent deformation moduli might be relevant for a high building.
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For saving money, petroleum industry prefer poroelastic equation to calculate minimum horizontal stress rather than direct measurement (e.g. via Leak-off tests). Still, by comparing the value of calculation and measurement, it is showed that the value from calculation always underestimate the one from measurement. This phenomena has been interpreted to be caused by tectonic strain. I determine the tectonic strain. And, I'm trying to find some implication of tectonic strain on petroleum processes, for instance, wellbore stability or sanding production potential.  
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Hi, Uy Vo! The tectonic strain strongly affects the well construction process, including causes such complications as walls collapse, stuck pipe, loss circulation fluid, mobile formations, unconsolidate formations. These are very unpleasant and expensive types accidents and complications and cause great economic damage to oil companies.
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Residual soil is the product of the weathering processes for rocks.
What are the main characteristics of this residual soil?
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Dear Dr. Al-Obaidi:
Residual means it formed in place or in-situ. It is commonly used for ore mineralization be it created by mechanical or chemical weathering on top of a fertile bedrock (parent rock). It can be a placer or a kaolin deposit. In soil sciences it makes little sense because soil is an autochthonous cover on top of different types of parent material from almost organic free oxisols to organic rich ones with well – defined horizons. You should not use this technical term anymore. There is something similar called paleosol which is a soil intercalated into a stratigraphic sequence with all hallmarks of a special modern soil type but subjected to soil-diagenesis so that it comes closer a chemical sediment like silcretes or ferricretes. In this case the transition into sediments is not sharp. There is another type of soil called soil-sediment. It is a former soil which was reworked by water and shows the features of clastic sediments.
For examples and distinction see:
DILL, H.G. (2020) A geological and mineralogical review of clay mineral deposits and phyllosilicate ore guides in Central Europe - A function of geodynamics and climate change.- Ore Geology Reviews 119 (in print)
DILL, H.G. (2017) Residual clay deposits on basement rocks: The impact of climate and the geological setting on supergene argillitization in the Bohemian Massif (Central Europe) and across the globe.- Earth Sciences Reviews 165: 1-58.
DILL, H.G., BUZATU A., and MAFTEI A.E. (2017) Capturing digital data with handheld devices to determine the redox regime, lithology and provenance of siliciclasticsediments and residual deposits - A review and field manual.- Arabian Journal of Geosciences 10: 188-217 (plus supplementary data).
DILL, H.G. (2016) Kaolin: soil, rock and ore From the mineral to the magmatic, sedimentary, and metamorphic environments.- Earth Sciences Reviews 161: 16-129.
Kind regards
H.G.Dill
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Dear colleagues!
What is the best method to determine the spacing of the discontinuities on a digital 3D model of a rock slope obtained with TLS? I am only looking for a manual method since the aim of the Master thesis is to compare manual and semi-automatic methods.
Semi-automatic mapping results were obtained using DSE.
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If you are specifically thinking about fractures, there is a lot of literature on observational methods to quantify spatial attributes, well beyond "spacing". Here are just a few references to get started. These are generic but contain concepts that could be applied to TLS data.
Andrews, B. J., Roberts, J. J., Shipton, Z. K., Bigi, S., Tartarello, M. C., and Johnson, G.: How do we see fractures? Quantifying subjective bias in fracture data collection, Solid Earth, 10, 487–516, https://doi.org/10.5194/se-10-487-2019, 2019
Watkins, H., Bond, C. E., Healy, D., & Butler, R. W. H. (2015). Appraisal of fracture sampling methods and a new workflow to characterise heterogeneous fracture networks at outcrop. Journal of Structural Geology, 72, 67-82. 10.1016/j.jsg.2015.02.001
Sanderson, D. J., & Nixon, C. W. (2015). The use of topology in fracture network characterization. Journal of Structural Geology, 72, 55-66. 10.1016/j.jsg.2015.01.005
Roy, A., Perfect, E., Dunne, W. M., & McKay, L. D. (2014). A technique for revealing scale-dependent patterns in fracture spacing data. Journal of Geophysical Research: Solid Earth, n/a-n/a. 10.1002/2013jb010647
Randall Marrett, Julia F.W. Gale, Leonel A. Gómez, Stephen E. Laubach,
Correlation analysis of fracture arrangement in space, Journal of Structural Geology, Volume 108, 2018, Pages 16-33,
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I want to measure the hardness of particles that are smaller than 120 micrometers. Do you think we can use depth sensing nano indentation method to measure the hardness of this material?
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You can certainly use nano-indentation to measure the hardness of a particle less than 120 um in diameter. First, minimize the mismatch between the modulus of elasticity and yield strength associated with the particle and the modulus and yield strength associated with the mounting resin. Once the material is mounted, use standard polishing and grinding procedures to minimize the surface roughness, achieve a mirror finish, and expose the cross-section of the particle. Once you've calibrated your nanoindenter frame stiffness, compliance, and tip's contact area function using a reference material such as fused silica, determine the particle-dominated depth limit using the criteria proposed by Yan et al. such that indentation depth is less than or equal to 0.02 * R, where R is the radius of a given particle. Otherwise, David Mercier et al. appear to have had success when using the guiding principal established by Constantinides et al., which advocates for a depth limit of 10% of the particle size. From my own experience, when the mismatch between a particle's stiffness and the stiffness of a given mounting material is very large, then Constantinides 10% rule no longer holds and the 2% particle radius rule from Yan et al. remains reasonable.
With the aforementioned in mind you will still face a significant challenge in so far as the indentation size effect is concerned. Depending upon the radius of your particle, when you abide by Yan et al.'s approach then you may not obtain enough values of hardness as a function of indentation depth to apply the Nix-Gao relation before surpassing the particle-dominated depth limit. Therefore, care needs to be taken in interpreting the results. In other words, the hardness will not be the "true" hardness without the Nix-Gao analysis unless your particle is 120 um in diameter, then you could potentially solve for the true hardness by fitting the hardness vs. depth data between depths of 100 nm and 1200 nm. Such a range would likely be sufficient for indentation size effect analysis.
Lastly, one could take an alternative approach. You could acquire a flat-punch indenter tip and compress the micro-particles using an indenter. See Assadi et al. for more information surrounding this alternative approach.
Best,
Bryer C. Sousa
Materials Science and Eng.
Worcester Polytechnic Institute
Assadi et al.
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Can someone provide a manual or a guide of geotechnical investigation procedures for different types of constructions in English? I mean a guide of methodology and standard procedures for transmission towers, bridges, regular houses, etc?
I am interested in a manual which is compatible with Eurocodes or ASTM standards.
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There are so many tunnel excavations, and so many who use either 'observational' (maybe double-shell) NATM or single-shell B + S(fr) selection from Q, or RMR, or less frequently RMi. Many then ask their younger (?) numerical modellers 'in the office' to check for 'plastic zone' size (often using the RocScience Hoek-Brown, GSI, Phase 2 / RS 2 software). We can alternatively use UDEC-MC or UDEC-BB to check for bolt and shotcrete loading. There are no 'plastic zones', just modelled joint adjustments: some joint shearing, joint aperture changes, and deformations. An altogether clearer idea of rock mechanics mechanisms. We can make improvements in bolt spacing or length or shotcrete thickness/strength if needed. Unfortunately it has been known for a long time that one should not add 'c' and sigma n tan(phi), either in linear Mohr-Coulomb or non-linear Hoek-Brown. This applies to the FEM continuum models. The nested equations involving a crudely estimated GSI (from a diagram, not from characterization) and the following opaque equations of c and phi need software as they are so complex. There is also a disturbance number D giving great freedom for the result, and a deformation modulus equation without depth or stress adjustment. Unfortunately the 'plastic zones' that the young modellers produce, though very colourful, may be grossly exaggerated, as found in a formal court case concerning a stable tunnel excavated without the need for shotcrete support. Is it not time to re-think the numerical modelling we are often doing in rock engineering? It is often based on so many a priori assumptions with even the input needing software. Mostly, the empirical methods, though with some inevitable weakness like subjectivity, are at least based on a posteriori principles.
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I believe that the condition of the inner and outer layers of the rock should be taken into account in the discussion of plastic dependence.
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I'm searching for open access and peer reviewed international journal (obviously of high quality and with Impact Factor) to publish research on geology, geomorphology, landslides, geotechnics, soil and rock mechanics.
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I would say Applied Sciences or Geosciences journals by mdpi
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For RMR and SMR classifications, field work is required to obtain information about discontinuity dip, strike and ,.... Are are aware of any resource to learn this field work?
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Please contact Dr. R.V.K.Singh, Liasion Officer, CIMFR, Dhanbad and its branches at Nagpur, Roorkee etc.
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From Wikipedia
”In engineering, a foundation is the element of a structure which connects it to the ground, and transfers loads from the structure to the ground. Foundations are generally considered either shallow or deep. Foundation engineering is the application of soil mechanics and rock mechanics(Geotechnical engineering) in the design of foundation elements of structures.
How future Materials and development of smart structures and new technologies in construction Will Shape the Future of buildings foundations?
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Good question Azm Shaher Al-Homoud .
Type of foundation should be a function of soil conditions and applied load. Recently, we observe also other factors influencing the geotechnical design.
Concerning soil conditions, we may assume that best locations are already occupied and we move our development to "unsuitable places". That is why we should expect further development of deep foundations. It refers also to reinvested lots with remaining of older (demolished) structures. In that case, the reuse of old foundations or debris from demolition works may be an issue imposed by "eco" regulations. I guess that due to political reason (in relatively reach countries, that seem not to have other problems) the last mentioned aspect may also comprise a pressure to develop "low-emission" technologies e.g. substitution of cementous binders with some kind of fly-ash or other materials with neutral carbon footprint. That also imposes a discussion over sustainability of geotechnical technologies and their adequacy for a desired life time of the structure. For now, I have an impression that we tend to provide "immortal" foundations for temporary or short service structures.
Speaking about applied loads, I'd underline the aspect of seismic and climatic impact on tall buildings and structures. That imposes some measures in design of buildings and their foundations, adopted to those conditions. One may notice that the growth of the economy provokes irrational behavior of many investors and designing "original" (tall, deep, shaped in not natural way) structures just for show and fame. That is why so complicated foundation systems must be designed.
Finally, I'd like to point again on the importance of testing. Whenever we observe a progress, we are touching the unknown. In the case of foundations all the risks are multiplied by the consequence factor for the supported structure and the difficulties related to any strengthening or repair methods under the existing structure.
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I was simulated 500 kg TNT on the ground surface to explosion, soil is clayey sand with young modulus E=100 MPa, dimensions of ground crater due to detonation is 70 cm in depth and 200 cm length!!(according to figure)
Are the results of the sizes correct??
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As i see your result is to inaccurate. Check your model based-on an authentic paper and or verify a paper or case study model.
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I simulated one tunnel in the soil medium, I going to study on the ground surface settelment due to excavation tunnels
Which Constitutive model of the soils (SC-GC) is better? and why?
1. Mohr coulumb (MC)
2. Soft soil
3. Softening strain (SS)
4. Hardening soil (HS)
5.Hardening soil small-stiffness (HS-SS)
6. CY-Soil
7.CH-Soil
8. Druker-prager
9. cam-clay
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Difficult to say. I would suggest that you start with an elastic model, and then move your way down your suggested ladder until you meet a good match. However, ideally, your stress strain curve from lab results should be able to help in deciding your final selection.
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I have a rock specimen and a soil specimen. During my mechanical measurements I observed that the rock reacts much faster on stress rate changes (observable by a sharp kink in the deformation curve) than a soil (no such kink). What is the explanation? Where can I find a publication dealing with this phenomenon?
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The first thought is that elastic waves propagation takes place. Corresponding velocities are proportional to sqrt of elastic moduli. See, for example, https://petrowiki.org/Compressional_and_shear_velocities
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What is the uniaxial compressive strength of westerly granite?
References would be appreciated.
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The conventional triaxial compression for Westerly granite test indicates: CP = 100 MPa, USC = 201 MPa, reference: Haimson and Chang (2000).
you can find more in the following reference:
Strength criterion for rocks under compressive-tensile stresses and its application, Journal of Rock Mechanics and Geotechnical Engineering, Volume 7, Issue 4, August 2015, Pages 434-439, https://doi.org/10.1016/j.jrmge.2015.05.002
You can find it from the following link:
I hope it is helpful for you.
All the best.
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dilemmas in rock mechanics..
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Many sophsticated suggestions already. We could also return simply to 'the shear strength of rock masses' (a 50-60 years-old dilemma since Muller-Brace) - and ask why progressive failure (and the possibility of monitoring prior to eventual failure) often occurs. This should tell us to be aware that Mohr Coulomb and Hoek Brown - if used as 'intended' to add 'c' and 'sigma n tan phi' - need to be used sparingly to say the least. It is not just 'c' then 'sigma n tan phi' (degrading cohesion and mobilizing friction, and then post peak) but actually several components: CCSS - 'crack, crunch, scrape, swoosh' as intact rock bridges (if present) fail, then the new fractures are immediately sheared, then 'capable' joints (the 'scrape') then the clay-filled discontinuities/faults (the 'swoosh'). How can we put this together - degrading strength at successively larger shear strains/shear displacements?
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Dear RG users,
I am wondering if there are good research topics related with industries need on “Wastewater threatment facilities” and “Solid waste landfills” considering only Geotechnical aspects.
I am looking forward for your messages.
Best Regards
Bekir S.F.
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It is very important topic and really we and our planet is in need of such importance researches
Best Regards
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The most important current and future research to tackle problems related to industrial application in the field in soil and rock mechanics?
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One must distinguish between "hottest" and "most important" topics.
As for “hot” topics – look at the Universities. New tools (powerful hardware and software) make it possible for developing more and more sophisticated geotechnical research (calculations). Scientists publish more and more “indexed” but “unread” research papers without any influence on contemporary world. There are some key words in this “parallel universe” (sponsored by public institutions) like: green, eco-, sustainability that replaced former leaders: risk, reliability etc. The scientific world does even not pretend to address their findings to the current needs.
As for “important” topics – just look at the current situation in the developing countries. There is a big need for “infrastructure”, “food” and “energy” for the growing populations. The clue point is that development of Asian, African and South American countries does not demand for high-tech technologies or methods. The real world needs simple, cheap and robust geotechnical technologies to be applied in large infrastructural projects (roads, railways, dams, hydro-energy, flood protection, water supply for people and agriculture. �.
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I am trying to model the strain-softening behavior of rock mass using UMAT subroutine. And, I am applying the 'static Riks method'. My model is running fine in abaqus under small loading. However, when comparatively large loading is applied the analysis is being aborted after 18% load application with an error msg, 'THE SOLUTION APPEARS TO BE DIVERGING. CONVERGENCE IS JUDGED UNLIKELY'.
I have checked the .msg file, .log file and the UMAT subroutine file, but could not find any thing helpful.
Kindly give me some suggestions for solving this problem.
Regards, Dipaloke
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Can you select arc length method in ABAQUS?
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I am currently working on the effects of rock boulders upon a structure and I would like to simulate the dynamic impact force using Plaxis 2D. Since the duration of the impact is between 0-0,2 sec , how could I calibrate precisely a table of Impact Dynamic Force avoiding excessive Globar Error, and Log Info ''Accuracy condition not reached in last step''? Briefly, I'd like to mention that I tried to perform the analysis defining as accurately as possible a figure of Force domain.
Thank you in advance,
Paschalis M.
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You could design your impact load with very small time step in table load. then the PLAXIS will select an appropriate time step automatically or you could change the time step of the analysis to manual type and insert a very small time step by using number of steps close to 400 steps according to your case.
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We are trying to decipher origin of magnetite-apatite ores from Evate deposit, Mozambique. I would like to know if someone observed textures like that illustrated in the attached figure, showing oval baddeleyite crystal decorated by euhedral spinels, all enclosed in magnetite with geikielite exsolution lamellae. Note that smaller euhedral spinels are regularly distributed in the magnetite, except for spinel free-zone around the baddeleyite grain. In our opinion, this may indicate the spinel growth controlled by the Ostwald ripening, i.e. dissolution of small crystals and their redeposition on the surfaces of larger crystals and nucleation centers. This interpretation is supported by the intersection of some spinel grains by geikielite exsolution lamellae, thus suggesting the spinel growth taking place in Fe-oxide melt. I would be grateful for some alternative interpretations (solid state diffusion?), including references to published works describing similar phenomenon.
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In order to classify a rock mass foundation of a gravity dam to obtain its strength and deformability parameters using the Geological Strength Index (GSI), is the Ground Penetrating Radar (GPR) an adequate geophysical method to do it?
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The answer depends on the depth of target. As you know very well depth penetration of GPR method is very limited. Besides, deriving the fractures within rocks based on GPS is very hard. Therefore, classification of rock type beneath a site have to be done using other geophysical methods.
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Hello everyone,
  • What type of failure mechanism do you expect to occur in a slope composed of fissured clays?
  • Does the fissure properties influence the overall behavior?
  • Can you expect it to act similar to a disintegrated rock mass?
  • What type of numerical method would you choose to simulate the behavior?
I am particularly interested in fissures in the soil mass and not on the surface such as shrinkage or tension cracks. Also, you can see an example photograph attached.
Thank you for your interest.
Regards,
Bekir SF
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Thank you for your interest Samuel J. Abbey , Which constitutive model do you recommend?
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The current attention in improving the efficiency of mining energy minerals from the earth has encouraged concern in advances, difficulties and likely forthcoming development directions in numerical modeling for rock mechanics and rock engineering. Such modeling is necessary for studying the essential methods occurring in rock, for considering the anticipated and actual performance of structures built on and in rock masses, and hence for supporting rock engineering design. 
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Mr. Niaz, first thing you should keep in mind before starting to learn either FLAC3D or 3DEC that it not practically possible to learn the entire software at one go. Therefore, the beginning of learning of software should be problem specific. For example, if you have to design a pillar, knowledge of brick mesh generation would be sufficient, and you should control one’s temptation to learn not waste you time on other types. Furthermore, if you have griddle or Kubrix available with you, you should learn designing of shape using Rhino, meshing using Kubrix or Griddle and not invest your time on manual meshing; thereby, you can skip ‘Grid Generation’ section given in manual.
You may start with getting started section of the manual. Examples are given to make you comfortable with interface; you copy and paste the examples in text (or data) file to run the commands interactively through file driven mode. Command and plot windows can be opened simultaneously and text files can be called to develop an understanding of each keyword. If you want to see the how a keyword functions, you can insert comma before other lines to make them read as comments. Even after this if you are confident with any keyword, you may search it in command reference which describes every keyword in detail. After developing confidence with software interface, you may read ‘Problem Solving with FLAC3D or 3DEC’ section to develop an understanding on selection of material, meshing, stress initialization etc. After all these you will have a solid foundation to take up any problem for simulation. For project specific case, you may find a similar example in ‘Example Applications’ or ‘Verification Problems’ section.
After following above steps, you will have sufficient understanding and confidence to play with the commands or keywords to get any desired outcome.
I hope you find above suggestions helpful. Best of luck with your project.
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Would be reliable computing a finite element analysis of a dam-foundation system, using the rock mass parameters obtained through the GSI system, in order to evaluate the displacements in the rock mass, if you are using a software that not allow include information about the characteristics of discontinuities, only the rock mass stiffness?
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No certainly it is not reliable, rock discontinuities is a major item in determine both structural and seepage behavior of rock mass. if you don't have a detailed geological study, you may use geological maps to get the main faults locations and widths and from the RMR ( you may assume the worst for safety) you can estimate the width and spacing of minor discontinuities.
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Hey, I'm looking for a FEM analysis software to evaluate the displacements in a rock mass due to a presence of a specific gravity dam. I already have the strength and deformation properties of the rock mass and the dam.
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Dear Konstantinos,
The best software for analysing the stability of your problem is PLAXIS or FLAC..these two software is well established software for geotechnical engineering problem..among these two software PLAXIS is finite element based and FLAC is finite difference based software.. You will find lot of literature related to your topics ..the simulation of material properties in the analysis is very important..you will find rock joint rock model based Hoek and Brown method is available in PLAXIS..ABAQUS is basically developed for mechanical engineering and now civil engineers also using this software for various analysis..you choose the software as per your requirements and limitations of the software..ok all the best in your research..
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Hello to all RG users,
I am currently searching for softwares to anaylze the behavior of discontinuous media such as rock masses. It would be a lot better if they are especially developed for Geotechnical Engineering applications. I am also aware that discrete element solutions such as UDEC and 3DEC would do the work. Are there any other softwares for the particular field? I am interested in Discrete Element Method (DEM) and Discontinuous Deformation Analysis (DDA) but I am also open to any other methodologies and softwares. Please keep in mind that they should be used on Geotechniques.
Thank you
Regards
Bekir SF
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I recommend the ITASCA software such as (UDEC, PFC, 3DEC). They are designed specifically to anaylze the behavior of discontinuous media such as rock masses Bekir Salih Firincioglu
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Hello RG users,
The rocks are recrystallized limestones and dolomites and physically in various conditions such as in some areas the outcrop is fresh and intact, in some areas it is lightly or highly decomposed and weathered, even somewhere there are residual soils. Also, some areas contain discontinuities and some not.
Assume that I have the plain 3D geometry. I simply cannot assume that the whole area is homogeneous and has same characteristics.
My question is How can I efficiently represent such varying conditions (heterogeneity) in a 3D model based on FEM, DEM, FDEM etc. ? Is there any software capable of doing it?
Thank you!
Best Regards,
Bekir SF
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Dear Bakir,
You have distinct weathering zones in your bench slope. So, you can define these zones in your model as a starting point. You can use GSI for estimating material properties of these zones. Since you do not have any defined joint sets, as you said, you can apply RS2 or RS3, both are FEM analysis program. Your slope dimension seems greather than REV size of your rock mass. Therefore, you can model your slope using continuum approach. Your bench slope is more prone to circular or non-circular failure mechanisms rather than discontunity controlled slip failures, such as plane, wedge or toppling.
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Hello RG users,
I was wondering how can I determine the exact location of expected wedge, planar or toppling falures in rock slopes. Assume that I have already done kinematical analyses and results indicate such possible failure mechanisms. In this case, How can I possible know the location of the wedges etc. to prevent such an instability?
Thank you
Best Regards
Bekir SF
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I don't think using a probabilistic approach is the right thing to do. The most dangerous and statistically processed direction of cracks is not the same. The safety factor is very sensitive to the orientation of the cracks and changing the orientation by 5-10 degrees can change the safety factor several times. Enough odnogo adverse combination that basically the ledge collapsed. The analysis of field measurements of cracks and the choice of the most critical combinations is necessary. Also, it is possible to analyze already accomplished collapses (on what systems of cracks they occurred).
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I am looking for some references or general comments that I can use for granular material, incorporating geologic conditions (i.e alluvium material, colluvium,or igneous, metamorphic and sedimentary lithology).
Additionally, I would like to ask for you opinion in earthdam construction what measures I need to take to avoid an excessive particle breakage under compaction and hydraulic load.
Regards
Johnatan
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I feel you can use Drucker - Prager model to simulate the granular material response under different loading conditions..you will find more literature based on this model to simulate the granular material..ok all the best..with regards..
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Dear All,
I would like to learn if the cut and cover tunnels have special joints between their segments such as immersed tunnels. For example, immersed tunnels have special gasket joints (gina, horn ,stirn, etc.), omega seals and shear keys. Is there any kind of joints for cut and cover tunnels? And anyone has longitudinal sketch of these tunnels showing connection details?
Thank you very much in advance.
Best regards,
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Based on earthquake data, how we can define the type of rocks and minerals within the earth?
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Lots of earthquake stations today, therefore, lots of data to study using the velocity of the waves. Scientists know a lot more information than previously and there is more to study. The data displayed in the lecture suggested by Dr. @ Borko Bulajic are amazing!
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Hello,
I would appreciate it, if someone explain to me how I could estimate parameters of stoneley waves (such as arrival time, corresponding to the stoneley waves frequency or range of frequencies, velocity and so on...) that propagate in rock sample - limestone.
I've used ultrasonic pulser/receiver and oscilloscope for measurements and got this results ( please find attached ), but not sure what should be the next steps.
How I could differentiate where are P-wave, S-wave or Stoneley-wave moment of arrival and if there are any at all?
Never deal with this topic before, therefore would be grateful for guidance or advice on literature that I should read first.
Thank you.
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Some how you don't get my reply
Ori Yeheskel
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I am working on roughness influence on shear strength of rock. I am facing problems regarding roughness of the upper block as I asked in the question. I am looking forward to the answer. 
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I do not remember such a phenomenon from our 130 natural joint samples. On the contrary, JRC reduced due to highly-stressed damage 'islands'.
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Dear fellow researchers
In rock mechanics there are several methods to up-scale lab results to the field results (especially for Young's modulus) as it most of the times make a significant difference in analysis of tunnels, caverns, etc. However, in petroleum geomechanics the structure in question is a wellbore with a very small diameter (mostly less than 10 in.). I was wondering how much scale effect may be inflict in such a problem? Since the opening is almost as the size of the plugged core samples, is there any significant difference between lab mechanical properties and in-situ properties?
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Many good answers - but back to the scale of Abolfazl's question. Already the surrounding diameter(s) around the wellbore have increased the scale by an order of magnitude in relation to the cored plugs, and it is in the early phase of scaling that we see the biggest scale effects. The P-wave velocity, with appropriate stress-dependence in relation to depth, will show a reduced magnitude from plug size to 2-3 wellbore diameter sizes, due e.g. to JCS and JRC scale effects, if/because, jointing/bedding may be involved (i.e. down-hole velocity relative to lab plug). Modulus can be scaled via Vp, using the increased Vp at depth, which however brings the surround rock mass (20-30 inches scale?) closer to the confined plug modulus. So maybe strength falls faster than modulus with plug-to-surrounds scaling, due to the effect of confinement. UDEC-BB can give some indicators of the scaling using the Ln/Lo (small) block-size scaling. But suggest JCS replaced by confined strength due to the depth and absence of weathering.
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Problem with 10 node tetrahedral on RS3.
Results from using 4 node tetrahedral are similar to 6 node triangle on RS2 (and to analitical calculations) , but results with 10 node tetrahedral are very different, and not logical. Time calculation for 3d model of tunnel with 4 node tetrahedral is 20 minutes, and for 10 node tetrahedral is 16 hours.
What could be the problem with my model?
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Hi
I do not understand how i should change the data in the metric quality to improve my mesh. Please explain?
what would happen if i change either values in the tables
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Sawai et al., 2012 summarized in the appendix the different approaches in these cases like the intercept method. What do you think is the best way to approach this experimental problem?
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Dear Stefano
Teflon can be an expensive matter with time.