Blasting of Unstable Rock Elements on Steep Slopes
Abstract
:1. Introduction
2. Materials and Methods
2.1. Experimental Approach to Powder Factor (PF)
- A is a coefficient that varies according to the rock type;
- B depends on the employed explosive type;
- C is related to the blasting pattern adopted;
- S is the area of the excavation section.
- A coefficient characteristic of the rock to be blasted;
- A coefficient characteristic of the employed explosive;
- A coefficient of “effect” referring to the result to be obtained with the blasting (size distribution of the blasted material, width of the zone of influence of the charge);
- A characteristic dimension of the blasting pattern geometry (normally, the line of least resistance), eventually raised to a power, or a polynomial combination of several characteristic dimensions.
- C is the explosive charge;
- k′ represents a coefficient referring to the rock type;
- k″ depends on the employed explosive type;
- k‴ is the “effect” coefficient for fragmentation;
- I is the characteristic dimension of the rock block to be blasted;
- f(I) is a function of “I” raised to a power of a number varying from 2 to 3, with lower values associated with blasting along a defined failure surface and higher values referring to blasting volume.
2.2. General Constraints of Blasting Operations on Rock Slopes
- Assessment of the rock quality and lithological and strength properties of the rock formations to ensure effective drilling and blasting outcomes;
- Understanding the joints’ orientation (dip, dip direction) and characteristics of joints within the rock mass to optimize drilling angles and minimize potential instability;
- Implementation of measures to mitigate vibrations generated during drilling and blasting operations, reducing the risk of structural damage and instability of additional rock blocks or discomfort to nearby structures and communities;
- Determination of the required fragmentation size of the blasted rocks, in order to enable the required removal of the subsequent muck or material after blasting;
- Assessment of the accessibility of the drilling site to ensure efficient deployment of drilling equipment and personnel;
- Incorporation of time-sensitive requirements, such as the need to swiftly reopen roads or access routes, into the scheduling and execution of drilling and blasting operations.
2.3. Risks and Undesired Effects
2.4. Design Criteria
- Type of explosive.
- Drilling (Ød) and explosive (Øe) diameter (i.e., cartridge diameter).
- Length of hole (Lh).
- Explosive length (Le).
- Tensile strength of rock (T).
- is explosive volumetric mass;
- k is a coefficient that takes into account the effect of the alignment of the holes, which ranges from 0.5 (if the spacing between the holes is less than 10 * Ød) to 1 when the spacing is higher (more than 30–40 * Ød).
2.5. Analysis of Case Histories for Validation
- 1.
- The first one was presented in [18] and concerns the blasting of a large dangerous block (about 60,000 m3) overhanging the village of Meiringen, Switzerland (Figure 2).The initial intervention stemmed from the looming threat of a significant rockfall poised to engulf the town. Minor detachments from the limestone cliff, situated approximately 340 m above the town, had already been documented. The rock mass was Dogger limestone, exhibiting relatively robust resistance properties with a tensile strength of 5 MPa and a shear strength of 11 MPa. To ensure optimal safety measures, the blasting parameters were meticulously calibrated, employing a dense drill hole pattern to facilitate the fine fragmentation of the material. This is, on the other hand, an ever-present concern in this kind of blasting, as the uncontrolled fall down of large intact blocks can lead to substantial damage to infrastructure and does not allow forecasts of falling trajectories. Hence, the aim was to limit the size of blasted blocks to no more than 1 cubic meter. To protect the town, the construction of a sturdy stone embankment was performed along the forecast fall down path, capable of containing an estimated volume of around 60,000 m3. The blasting was carried out in four distinct rounds.
- 2.
- A second case on Quebec highway 155 (Figure 3) is described in [19], motivated by the danger represented by a potentially unstable rocky dihedral of a volume of about 800 m3 looming over the road, passing at an altitude of 30 m lower. The rock was andesitic gneiss of the Precambrian age. The analysis of stability indicated a very low safety factor, which was variable from 1.16 to 1.06 depending on the assumed friction angle.The PF adopted, decidedly enormous for European standards, was about 0.77 kg/m3, probably motivated by the need to achieve very fine fragmentation. Blasting has been implemented with micro-retarded electrical detonators. Before the blasting, the road below was protected with a sand bed 1 m thick.
- 3.
- A further example related to the blasting of an overhanging block is shown in Figure 4 [20]: a local mountainside road in the northwest of Italy (the provincial road of Val Mastallone in Cravagliana, Vercelli province), which was periodically closed due to minor rockfalls after rainfall events and thawing periods.The object of the blasting is a spur in unstable conditions with a volume of about 2500 m3, as made clear by a previous collapse. The slope is made of weathered gabbric rock with a uniaxial compressive strength of 90 MPa and tensile strength of 8.5 MPa. This stretch of road was subjected to a systematic collapse of rock blocks of various sizes. Particularly critical was the earlier collapse of 1000 m3, from just below the blasted rock induced by a planar slide. The blasting design, provided by the authors, requested a preliminary careful geostructural survey to clearly define the persistence and location of main joints at the rear of the potential unstable volume. Both drilling and charging have been prepared by using both a hydraulic long-arm platform and the experience of skilled climbers along the slope. Non-electric ignition has been adopted.
- 4.
- The case of the demolition of an unstable monolithic slab (Figure 5) [20] of porphyry rock about 10 m wide, 33 m high, and 2–6 m thick, with a global size of about 1300 m3, that threatened a road with a high traffic density of more than 1 car/min: the provincial road Gattinara-Borgosesia in Serravalle Sesia (Vercelli province—Italy). The monolith was totally isolated from the rock mass of the slope by two open joints and its base was an irregularly and highly fractured rock portion. The authors carried out a local geostructural survey to help with the design of the blast round. The probability of occurrence of a sudden collapse of the slab was very high.
- 5.
- The demolition of a set of mutually bound blocks above provincial road 169 of Val Germanasca (Turin province) in Northern Italy (Figure 6). The rock was in this case a minute gneiss of mediocre quality and the total volume of the blocks was about 640 m3. In this case, which was known for decades for the inherent hazard it posed to road traffic, the greatest risk during the blasting was represented by the possibility of shearing the explosion line, following the beginning of the round, for the induced movement of the individual blocks. This phase did not stand alone, but after an arranged detailed local geostructural survey, a blasting design was carried out by the authors; after blasting, manual scaling and a strong and wide reinforcing of the rock slope was carried out (bolting, draperies, cable securing, net fences to intercept fragments fall along the slope). Before and after demolition, scaling operated by climbers was carried out to achieve better safety for work along the slope.
- 6.
- This case considers the demolition of a highly unstable monolithic block (Figure 7) of about 6000 m3 within a quarry area in Northern Italy, overlooking the quarry square. The rock was represented, in this case, by a gneiss of excellent quality (orthogneiss), with a compressive strength of 185 MPa, mainly used for ornamental purposes. The firing plan was studied by the authors to obtain a fragmentation between 0.5 and 2.0 m3 in order to allow the subsequent reuse of the blasted rock as by-products.Obviously, the main purpose of the blasting demolition was to improve the safety conditions of the site; however, when it is possible to recover and recycle blasted rocks, it is a good practice to do so in order to obtain new products/by-products for civil, building, road, and environmental applications.In a similar vein, when a rock slide occurs along a mountainside where road or infrastructures are present, it becomes urgent and necessary to remove the collapsed material, and its possible reuse (as aggregate, for backfilling, for embankments) depends also on the blocks’ fragment size distribution, especially to fulfill technical requirements concerning compaction and consistency.
3. Results
- K is a numerical coefficient depending on the rock behavior at failure;
- S is the spacing between two holes of the same row;
- Ød is the drilling hole diameter;
- R is a coefficient referring to rock type;
- E is a coefficient referring to explosive features;
- F is the desired fragmentation effect;
- D is the desired displacement of the blasted material.
4. Discussion
5. Conclusions
- (a)
- The relationship between row spacing, spacing, and detonation sequence is embedded within the PF formula, where these parameters influence fragmentation and displacement outcomes. Empirical correlations derived from case studies (Table 6) highlight how adjustments in spacing and sequencing can optimize energy distribution, reducing overbreak and enhancing safety. Future research will aim to quantify these interdependencies further, potentially integrating numerical simulations for greater predictive accuracy.
- (b)
- Developments and data collection should prioritize the investigation of additional real-world cases to bolster the robustness of the proposed formula for calculating the powder factor. Researchers can refine and validate the formula by analyzing a wider range of scenarios, ensuring its applicability across diverse geological and operational contexts. This expanded dataset will provide a more comprehensive understanding of the factors influencing blasting efficiency and allow for the identification of any additional variables that may impact the accuracy of the formula. Additionally, incorporating data from a variety of case studies will enhance the reliability and generalizability of the findings, ultimately contributing to more effective and precise blasting practices along rock slopes.
- (c)
- The prospects for possible applications in excavation works or in geomechanical cases are related to the refinement of blasting scheme parameters according to a more reliable approach balancing and prioritizing the various involved factors: lab or site rapid testing, care regarding spacing and aperture estimation for joint structures, and the assessment of physical connections between rock volumes (rock bridges) for determining a progressive and complete kinematic evolution. Also, remote surface acquisition (photogrammetry or laser scanning) helps to build up the geometrical model and direct inspection with climbers and with unmanned vehicles (drones) is fundamental to detect possible persistent and hidden joints at the rear of slopes. Civil work (excavation or reclamation of impervious slopes), mining and quarrying bench profiling, and reinforcing work in mountain areas represent possible fields of application.
Case Study | K Coefficient | Rock Coefficient “R” | Explosive Coefficient “E” | Fragmentation Coefficient “F” | Additional Displacement Coefficient “D” | PF Real (kg/m3) PFr | Estimated PF (kg/m3) PFe |
---|---|---|---|---|---|---|---|
Meiringen (Switzerland) | 0.0059 | 0.50 | 1.10 | 1.20 | 1.20 | 0.30 | 0.30 |
Québec motorway (Canada) | 0.0059 | 1.00 | 1.10 | 1.40 | 1.00 | 0.77 | 0.22 |
Cravagliana (VC), Italy | 0.0059 | 1.00 | 1.00 | 1.40 | 1.00 | 0.24 | 0.25 |
Le Cave (VC), Italy—Slab | 0.0059 | 1.30 | 1.00 | 1.20 | 1.00 | 0.24 | 0.25 |
Perrero (TO), Italy—Catasta | 0.0059 | 1.00 | 0.95 | 1.00 | 1.00 | 0.16 | 0.16 |
Balmoreglio quarry (VB), Italy | 0.0059 | 1.00 | 1.00 | 1.00 | 1.00 | 0.23 | 0.23 |
Author Contributions
Funding
Institutional Review Board Statement
Informed Consent Statement
Data Availability Statement
Conflicts of Interest
References
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Case Studies | Rock Type | Total Volume (m3) | Fragmentation | Prevalent Explosive Type | Drilling Diameter (mm) | Spacing in Row (m) |
---|---|---|---|---|---|---|
Meiringen (Switzerland) | Limestone | 60,000 | high | ANFO | 85 | 3.0 |
Québec motorway (Canada) | Precambrian andesitic gneiss | 800 | very high | ANFO | 63 | 1.5 |
Cravagliana (VC), Italy | Weathered gabbro rock | 2500 | very high | slurry | 41 | 1.25 |
Le Cave (VC), Italy—Slab | Porphyry rock | 1300 | high | slurry | 41 | 1.1 |
Perrero (TO), Italy—Catasta | Minute gneiss | 640 | normal | dynamite | 34 | 1.0 |
Balmoreglio quarry (VB), Italy | Serizzo (gneiss) | 6000 | normal | watergel | 51 | 2.0 |
Class | Rock Type | R |
---|---|---|
1 | quartzites and compact porphyries | 1.30 |
2 | sound granitoid rocks, gneisses, basalts, gabbro rock | 1.00 |
3 | compact limestone and dolomite, grés, highly cemented sandstone | 0.90 |
4 | phyllites, hard shale clay, serpentine | 0.80 |
5 | marl and soft limestone, gypsum, poorly cemented sandstone | 0.50 |
Class | Explosive Type | E |
---|---|---|
1 | nitroglycerine, dynamite | 0.95 |
2 | slurries, watergel | 1.00 |
3 | ammonium nitrate (ANFO) | 1.10 |
Class | Fragmentation | F |
---|---|---|
1 | normal (several blocks bigger than 1 m3) | 1.00 |
2 | high (maximum size up to 1 m3) | 1.20 |
3 | very high (maximum size up to 0.5 m3) | 1.40 |
Class | Displacement | D |
---|---|---|
1 | no additional displacement in addition to the action of gravity | 1.00 |
2 | additional displacement required (few meters) | 1.20 |
3 | high additional displacement required (10 m or more) | 1.60 |
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Casale, M.; Dino, G.A.; Oggeri, C. Blasting of Unstable Rock Elements on Steep Slopes. Appl. Sci. 2025, 15, 712. https://doi.org/10.3390/app15020712
Casale M, Dino GA, Oggeri C. Blasting of Unstable Rock Elements on Steep Slopes. Applied Sciences. 2025; 15(2):712. https://doi.org/10.3390/app15020712
Chicago/Turabian StyleCasale, Marco, Giovanna Antonella Dino, and Claudio Oggeri. 2025. "Blasting of Unstable Rock Elements on Steep Slopes" Applied Sciences 15, no. 2: 712. https://doi.org/10.3390/app15020712
APA StyleCasale, M., Dino, G. A., & Oggeri, C. (2025). Blasting of Unstable Rock Elements on Steep Slopes. Applied Sciences, 15(2), 712. https://doi.org/10.3390/app15020712