IJSDP Derbal
IJSDP Derbal
Planning
                                                                              Vol., No., Month, Year, pp. **-**
                                                                     Journal homepage: http://iieta.org/journals/ijsdp
https://doi.org/10.18280/jesa.xxxxxx ABSTRACT
 Received:                                       In this paper, we delve into the intricate challenge of fine-tuning fragmentation levels in
 Accepted:                                       mining operations. This adjustment is often hindered by a myriad of factors, including
                                                 natural fractures, those induced by previous blasts, cleavage, and the inherent
 Keywords:                                       approximations in geometric and load parameters utilized in blast design. While existing
 Fragmentation zones, fracturing, oversized      research has primarily concentrated on optimizing mining progress, considering the power
 blocks, detonics, digital mapping, blasting,    and grade distribution, we advocate for the critical necessity of integrating the dynamic
                                                 nature of fractures within the rock mass. This integration holds paramount significance, as
 advancement direction, block diagram.           fractures can profoundly affect the stability of the rock mass and influence the selection of
                                                 blasting techniques. By accounting for the evolution of these fractures, our aim is to gain
                                                 better control over the blasting process, subsequently yielding substantial implications for
                                                 the technical, economic, and safety aspects of mining operations. Our study systematically
                                                 examines the influence of these factors in the formulation of blasting plans. To initiate this
                                                 process, we employ geometric modeling techniques, leveraging digital cartography and
                                                 stereography tools. The ultimate objective of this research is to minimize the volume of
                                                 oversized materials in the mining process, contributing to more sustainable mining
                                                 practices. To illustrate these principles in a practical context, we present a case study that
                                                 entails the measurement of rock fragmentation resulting from blasts conducted at the
                                                 limestone quarry in Aïn El Kebira, located in the Setif province in northeastern Algeria.
                  Figure 2. Blast resulting in the fragmentation of large oversized blocks beyond the mid-range +400mm
   The estimated rate reaches a high limit of 40% in some areas, with a median value of 20% for the entire deposit, a confirmation
later validated through the use of photoplanimetry.
3. SUSTAINABLE METHOD FOR DETERMINING                                progression direction based on grade distribution, power
THE VOLUME OF OVERSIZED MATERIALS                                    (which is not an issue for us, given that we are dealing with a
                                                                     massive deposit in a mountainous terrain), and the
   The volume of oversized materials was determined                  requirements for effective fragmentation control.
through photogrammetry, as illustrated in Figure 3:
                                                                        For digital mapping, two topographic maps at a 1/50000
                                                                     scale were used to locate the site (See Figure 4), situated in
                                                                     the neighboring Algerian cities of Sétif and Kherrata. A
                                                                     digital terrain model from digital photos was also employed
                                                                     to digitize the discontinuities of the deposit, including
                                                                     fractures and bedding joints.
                                                                        The data was primarily processed using the ArcGIS and
                                                                     Rockworks software programs to calculate statistical
                                                                     parameters.
4. DIGITAL MAPPING
                                                                             Angle °
                                                               Angle °
Angle °
Angle °
Angle °
Angle °
Angle °
Angle °
Angle °
                                                                                                                                                             Angle °
       Google COLAB environment. This allowed for the
       calculation of the dip angle of the layers based on
       the geometric data of the lines digitized on the
       bedding joints, namely, the coordinates x1 y1 at the    8              5        32        20         0        21        32         0        25        21
       beginning of a line and the coordinates x2 y2 at the    16             5        34        20         0        21        32        16         1        21
       end of a line (See Figure 11).                          16             5        16        20         0        21        32        16        12         5
                                                               16             5        16        20        13        21        32         9        12        16
                                                               16             5        32        22        12         2        28        11        21        16
                                                               16            42        32        22        35         2        28        35        15        16
import math                                                    9             42        32        38         0        42        32        36        17        21
import matplotlib pyplot as plt                                9             42        32        38         0        42        21        36         3        21
# Function to calculate the dip angle for a single layer       9             42        5         38         1        42        21        36         7        21
def calculate_dip_angle(layer_depth, layer_thickness):         9             42        32        38         4        42        6         36         1        21
   dip_angle_radians = math.atan(layer_thickness /             65            21        32        38         4        42        6         36         0        21
layer_depth)                                                   29             5        32        38         4        26        6         16         0        21
   dip_angle_degrees                                     =     29            21        32        39         4        26        6         16         0        21
math.degrees(dip_angle_radians)                                29            21        11        39         4        26        7         16        22        21
   return dip_angle_degrees                                    29            21        32         0         4        26        7         16        25        21
# Sample data: depth and thickness of geological layers        32            23        4         26         8        11        32        22         4        26
layer_data = [                                                 7             16        32        22         4        26        7         16        32        26
                                                               16            26        16         7        35        25        16        26        16         7
   {"depth": 10, "thickness": 5},
                                                               35            26        23        26         9         6        32         1        28         7
   {"depth": 15, "thickness": 7},
                                                               9              1        32        26         5        15        9          2        32        26
   {"depth": 8, "thickness": 3},                               5             15        9          7        32        16        32        30        20        30
]                                                              32             1        4         26         2         5        32        25         4        26
# Calculate dip angles for each layer
dip_angles = []                                                  240 dip angles have been calculated and are listed in the
for layer in layer_data:                                      following table:
   depth = layer["depth"]
   thickness = layer["thickness"]
                                                                         •      Step 4: Using the Rockworks software for block
   dip_angle = calculate_dip_angle(depth, thickness)
                                                                                diagram drawing, a conceptual schema of the
   dip_angles.append(dip_angle)
                                                                                deposit was created based on geological surveys in
# Create a plot
                                                                                the "Medjounes II" part of the deposit. An Excel file
plt.figure(figsize=(8, 6))
                                                                                containing the coordinates of geological surveys,
plt.plot(range(1, len(layer_data) + 1), dip_angles,
                                                                                depth, and CaO content was imported using the
marker='o', linestyle='-', color='b')
                                                                                "Solid" function to proceed with the schematization
plt.title('Dip Angles of Geological Layers')
                                                                                of the 3D terrain model showing the distribution of
plt.xlabel('Layer')
                                                                                CaO content (See Figure 12).
plt.ylabel('Dip Angle (degrees)')
plt.grid(True)
# Show the plot
plt.show()
   The known methods for controlling the fragmentation of                         (a) Mechanical fragmentation
rock masses with explosives can be classified based on
various factors [21]:
   Adjustment through the influence of the explosion on the
rock mass can be achieved by varying:
   a) Specific explosive consumption calculated.
   b) Diameter of the charge.
   c) Type of explosive used.
   d) Charge construction.
   e) Orientation of the initiation of continuous charge.
   f) The order of initiation of parts of the discontinuous
                                                                              (b) Rock fragmentation by explosives
charge.
   g) Quality of stemming and its length, and more...
                                                                                     Figure 13. Force diagram
   During the change in the character of the charge's effect in
the regulated fragmentation zone, the part of the energy
                                                                     However, there are several distinguishing features
transmitted in the practically unregulated fragmentation zone
                                                                  between explosive fragmentation and mechanical
varies, resulting in changes in the dimensions of these zones
                                                                  fragmentation. Mechanical fragmentation has a two-sided
and the intensification of fragmentation in the mass.
                                                                  force pattern (Fig.13.a), whereas explosive fragmentation
   Adjustment of the explosive effect on the rock mass in the
                                                                  (except for oversize reduction and tight-space blasting)
unregulated fragmentation zone can be achieved by the
                                                                  exhibits a one-sided force pattern (Fig.13.b).
interaction of adjacent charges and groups of charges through
                                                                     In mechanical fragmentation, different pieces of rock are
the variation of:
                                                                  involved, while in blasting, fractured rock masses of
   a) Hole layout and the number of rows.
                                                                  significant dimensions are encountered. The fissures and
   b) Delay intervals and the sequence of charge firing, bench
                                                                  heterogeneity during blasting facilitate the division of large
height, hole layout patterns on the bench.
                                                                  rock pieces and reduce the specific energy capacity for
   Methods for controlling fragmentation can be divided into
                                                                  destruction. During blasting, fissures act as a barrier to the
two classes:
                                                                  expansion of energy, reducing the possibility of
   The first class relates to methods that ensure the desired
                                                                  fragmentation and often increasing the specific explosive
level of fragmentation: specific explosive consumption,
                                                                  consumption required to achieve the desired particle size
calculated diameter, and hole layout.
                                                                  [22].
   The second class includes methods that allow for changing
                                                                     The smaller the diameter of the charge, the less likely the
the level of fragmentation in limited zones and do not exclude
                                                                  energy expansion screen effect is between the charge and the
the flow of oversized fractions. This encompasses various
                                                                  free surface of the bench.
methods that may reduce the volume of oversized material by
                                                                     With an increase in specific explosive consumption, the
10-20%, including the use of discontinuous charges (solid,
                                                                  degree of fragmentation in the rock mass increases more
air, water stemming), charges with empty or water-filled
                                                                  intensively over the output (Fig.14). Then comes the so-
intervals in sub-drilling or between the charge and stemming,
                                                                  called state of saturation of the rock mass with blast energy,
sequential initiation of different parts, reverse initiation of
                                                                  where it can't absorb a large amount of energy spent
continuous charges, different types of explosives with
                                                                  unnecessarily on rock dispersion. In this case, the change in
varying detonation velocities, densities, and volumetric
                                                                  fragmentation intensity remains insignificant, and the curve
energy concentrations, paired hole blasting, block blasting
                                                                  roughly parallels the x-axis. The curve's smoothness is also
from high benches, combination of charges with different
                                                                  influenced by the direction of practically unregulated
diameters and lengths, micro-delay blasting patterns, blasting
                                                                  fragmentation [14,15].
in confined spaces, pre-splitting, and more.
                                                                     For a small charge diameter (d < 150mm), the curve passes
                                                                  lower, and in some cases, it can even reach the x-axis (in this
5.2 Calculation of the blasting plan parameters
                                                                  case, the oversize output is zero). With a large charge
5.2.1 Theory for calculating specific explosive
                                                                  diameter (d > 250mm), the curve passes higher, and
consumption
                                                                  practically, for any specific explosive consumption (q), it's
                                                                  impossible to achieve a zero-oversize output; in other words,
  For the destruction of rock masses down to a specific
                                                                  there are minimum values for the oversize output, denoted as
particle size, a certain amount of energy needs to be expended
                                                                  Vct and Vtc [21].
  The curve intersects the y-axis at a point that represents the       With increasing fragment sizes, all the lines shift
content of oversize material in the rock mass before blasting.      downward, meaning the specific explosive consumption
                                                                    decreases. To determine its value, if you know the content of
                                                                    the large fraction in the mass (the point on the line on the
                                                                    ordinate axis), it is necessary to carry out one or, preferably,
                                                                    two experimental blasts with selected different specific
                                                                    consumptions, plot the large fraction flow rate obtained on
                                                                    the graph, and connect the point on the ordinate axis to the
                                                                    point obtained using a straight line. By extending this line to
                                                                    its intersection with the line representing the minimum
                                                                    oversize flow rate, you can find the threshold value of q.
                                                                    Beyond this threshold, it is not rational to go because, in this
                                                                    zone, the curve of the large fractions' flow rate with varying
                                                                    specific consumption already levels off [20].
                                                                       Most often, it is not practical to apply the specific
                                                                    consumptions determined in this way because they result in
                                                                    a broad rock pile and mining operations that are not feasible
                                                                    according to the technology. When carrying out experimental
     Figure 14. Dependence of the oversize output on q for          blasts, you should select rock blocks with similar properties
 different charge diameters and their rock breakability. 1-2:       based on hardness and fissuring and use a method for
 Oversize output from the unregulated fragmentation zone,           conducting experimental blasts developed by researchers
                   1_for d1, 2_for d2. [4]                          from the Moscow Mining Institute [22].
                                                                       The practical method for determining specific explosive
   Depending on the rock's fissure category and the                 consumptions for 234 mm diameter holes, taking into
permissible fragment size in the operations, this value can         account the fissuring of the rock mass and the strength
vary from 100% to 0.                                                properties of its components, is based on the fundamental
   When calculating explosive consumption, it is practical to       work of Academician Rjevsky, V. V.[6]. The dependence of
replace the curves on the graph with straight lines. In this        q on rock strength properties (hardness coefficient f) during
case, the precision of the results obtained falls within the        the blasting of divisions to fragment sizes less than 100 mm
range of 15-20%, which is generally acceptable. The                 is as follows:
selection of a rational specific consumption is a techno-
economic issue that is resolved based on the cost of                             𝑞 = 𝑓. 𝑒. 𝑏. 𝜎𝑐2 0,73.102 . 0,349                 (1)
extracting valuable minerals for all processes. However, in
most cases during blasting, efforts are made to minimize the          Where:
oversize output, aiming for a value close to 0%.                      This formula is analogous to the theoretical formula by
   In the graph (Fig.15) showing the variation of q for a given     Academician Rebinder, P.A., encompassing the laws of
charge diameter and different rocks based on their                  Patinger, P.R., and Kirpitchev, V.L.[6].
workability, the percentage of oversize blocks (dhg >
700mm) in the rock mass before blasting is plotted on the y-                                      𝜎𝑐2 𝑆𝑝 𝑃𝑛
axis.                                                                                  𝐾𝑤 2 =        +                             (2)
                                                                                                  2𝐸   𝑉
VII 0,88-1,10 0,990 1,20-1,50 100 25-47 1450-2050 2,95-3,20 II-I XVI-XVIII
Compressi
                                                                                                                                  Displacement resistance
                                                                                                                resistance
                                                                                                                   σcomp
                                                                                                                                                             Tensile strength σt
                                                                                                                    on
                                                                                                                                        σdépl kgf/cm2
                                                                                      Ps (g/cm3)
                                                                                                                                                                  Kgf/cm2
                                                                                                                       Kgf/cm2
                                                                                                        (Mpa)
                                  (b)
 Figure 17. Initiation direction of charges: a) From bottom         Rock drillability                 Qét          Classes               Categories
       to top, b) From top to bottom, and c) Mixed                         level
                                                                   Very easy drillability             ≤10             I              1, 2,3,4,5
                   (recommended). [8:10]
                                                                   Average drillability             10,1÷20           II           6, 7, 8, 9,10
                                                                   Difficult drillability           20,1÷30          III         11, 12, 13, 14,15
7. PROPOSED SCHEME                                                    Very difficult                30,1÷40          IV          16, 17, 18, 19,20
                                                                        drillability
    1. Determination of drillability (standard q): The             Exclusively difficult            40,1÷50           V          21, 22, 23, 24,25
resistance of rocks to blasting is characterized by the specific        drillability
standard consumption of explosives. It is determined by the
following formula:                                                   Medjounes I → Difficult tirability, Class III, Category 14.
                                                                     Medjounes II → Very difficult tirability, Class IV,
          𝑞é𝑡 = 0,02(𝜎𝑐𝑜𝑚𝑝 + 𝜎𝑑é𝑝 + 𝜎𝑡𝑟 )2𝛾                 (11)   Category 17.
   The permissible particle size of large blocks after blasting            The length of the subdrilling is determined by the
is limited by the following conditions:                                 following formula:
                                                                              √16,072+4×0,95×0,44×16,07×15×17,55 −16,07
   Based on the obtained results, the acceptable block size is          𝑊=                                                = 5,54𝑚
                                                                                           2×0,95×0,44×15
set at 1.04 m. Any block not meeting this dimension will be
                                                                        (Medjounes I)
considered an oversized rock and will require a secondary
fragmentation operation (secondary blasting) to reduce its
                                                                              √16,072+4×0,95×0,49×16,07×15×17,62 −16,07
size.                                                                   𝑊=                                                = 5,32𝑚
                                                                                           2×0,95×0,49×15
                                                                        (Medjounes II)
   3.    Hole Diameter Determination: We choose a hole
         diameter based on the initial recommendations                    Calculation of W according to safety conditions:
         proposed in our analytical summary, considering
         both quantitative and qualitative criteria (based on                               𝑊 ≥ 𝐻𝑡𝑔𝛼 + 𝑐                            (25)
         the categories of fissuring and drillability). For our
         case, we adopt: D = 150 mm.                                       This sentence means: "Htgα+c=15 . tg85°+3=4.13m
                                                                        Htgα+c=15×tg85°+3=4.13m; therefore, the conditions are
                           q = q’. K ex                          (18)   met."
                                                                           It's confirming that the calculated value of 4.13 meters
  q' is chosen from the table of q selection in this article,           satisfies the specified conditions.
equal to 0.45 kg/m3.
                                                                          The distance between the holes in the first row:
                          K ex = 𝐴é𝑡 /𝐴𝑢                         (19)
                                                                                                 𝑎 = 𝑚. 𝑊                           (26)
  Kex = 1.1
  Aét: Standard Explosive - Ammonite N6GV
  𝑎 = 𝑚. 𝑊 = 0,95 × 5,54 = 5,26𝑚 (Medjounes I)
  𝑎 = 𝑚. 𝑊 = 0,95 × 5,32 = 5,05𝑚(Medjounes II)                     𝑙𝑏2 = 𝐿 − 𝑙𝑐ℎ2 = 17,55 − 9,66 = 7,89𝑚 (Medjounes I)
                                                                   𝑙𝑏2 = 𝐿 − 𝑙𝑐ℎ1 = 17,62 − 9,91 = 7,71𝑚 (Medjounes II).
   The distance between rows of holes: staggered pattern due
to the shape of the blocks.                                        -    Mining mass flow:
                                                          (29)
                         𝑄𝑐ℎ2 = 𝑞. 𝑊. 𝐻. 𝑏                         ∑𝐿 =
                                                                           𝑉           11988,5
                                                                                =                = 532,82𝑚 (Medjounes I)
                                                                           𝐽𝑚           22,50
                                                                            𝑉          14969
          𝑄𝑐ℎ2 = 𝑞. 𝑊. 𝐻. 𝑏 = 0,44 × 15 × 5,26 × 4,47              ∑𝐿 =         =               = 724,25𝑚 (Medjounes II)
                                                                           𝐽𝑚          20,66
               = 155,18 𝑘𝑔/𝑡𝑟 (Medjounes I)
          𝑄𝑐ℎ2 = 𝑞. 𝑊. 𝐻. 𝑏 = 0,49 × 15 × 5,05 × 4,29              -    Number of holes drilled:
               = 159,23 𝑘𝑔/𝑡𝑟 (Medjounes II)
                                                                                                           ∑𝐿                      (34)
                                                                                                   𝑁𝑡𝑟 =
  -       Load length:                                                                                      𝐿
                                                                           ∑𝐿          532
      •     1st row:                                               𝑁𝑡𝑟 =        =              = 30,36 ≅ 30 ℎ𝑜𝑙𝑒𝑠 (Medjounes I)
                                                                            𝐿          17,55
                                                                           ∑𝐿          724,25
                                         𝑄𝑐ℎ1             (30)     𝑁𝑡𝑟 =        =               = 41,1 ≅ 41 ℎ𝑜𝑙𝑒𝑠 (Medjounes II)
                                                                           𝐿           17,62
                                𝑙𝑐ℎ1 =
                                          𝑃
                                                                   -    Number of sounders:
            𝑄𝑐ℎ1       192,33
  𝑙𝑐ℎ1 =           =            = 11,97𝑚 (Medjounes I)
             𝑃         16,07
            𝑄𝑐ℎ1       197,46                                                                   𝑁𝑠 =
                                                                                                           ∑𝐿                      (35)
  𝑙𝑐ℎ1 =           =            = 12,29𝑚 (Medjounes II)                                                𝑅𝑠 .𝑛𝑝𝑠 .𝑁𝑗
              𝑃        16,07
                                                                                 532
      •     2nd row:                                                      𝑁𝑠 =            = 2,357 ≅ 03 sounders
                                                                             224 × 1 × 1
                                         𝑄𝑐ℎ2             (31)     𝑓𝑢𝑟𝑢𝑘𝑎𝑤𝑎 (Medjounes I)
                                𝑙𝑐ℎ2 =                                           532
                                          𝑃
                                                                        𝑁𝑠 =              = 3,325 ≅ 04 sounders
                                                                             160 × 1 × 1
            𝑄𝑐ℎ2       155,18
  𝑙𝑐ℎ2 =           =            = 9,66𝑚 (Medjounes I)              𝐴𝑡𝑙𝑎𝑠 𝑐𝑜𝑝𝑐𝑜 (Medjounes I)
              𝑃        16,07                                                    724,25
            𝑄𝑐ℎ2       159,23                                            𝑁𝑠 =             = 3,23 ≅ 04 sounders
  𝑙𝑐ℎ2 =           =            = 9,91𝑚 (Medjounes II)                        224 × 1 × 1
              𝑃        16,07
                                                                   𝑓𝑢𝑟𝑢𝑘𝑎𝑤𝑎 (Medjounes II)
  -       Jam length:                                                           724,25
                                                                         𝑁𝑠 =             = 4,53 ≅ 05 sounders
                                                                              160 × 1 × 1
      •     1st row:                                               𝐴𝑡𝑙𝑎𝑠 𝑐𝑜𝑝𝑐𝑜 (Medjounes II)