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Article

Comparative Analysis of Basic and Extended Power Models of Boreholes Expansion Dependence on Explosive Charge in Blasting in Clay Soil

1
Faculty of Geotechnical Engineering, University of Zagreb, Hallerova aleja 7, 42000 Varaždin, Croatia
2
Independent Researcher, Vidikovac 29, 43000 Bjelovar, Croatia
*
Author to whom correspondence should be addressed.
Geosciences 2020, 10(4), 151; https://doi.org/10.3390/geosciences10040151
Submission received: 16 March 2020 / Revised: 5 April 2020 / Accepted: 16 April 2020 / Published: 18 April 2020

Abstract

:
Spherical cavities made by explosive charge activation in a clay soils differ in size and shape. The mass of explosive charge lowered on the bottom of the borehole in a one-time blasting is typically relatively small and is calculated by a desired and planned performace. The effect of smaller explosive charge for spherical cavities is in principle different than continuously filled borehole in mining and blasting operations. Detonation of smaller explosive charge crushes the material in proximity of activated explosive charge. With the increase of distance from the explosive charge, the released energy in not enough for crushing of the materials, but instead compacts it. This paper is an extension of the previous research, which resulted in a smallest error of estimated in a model shown as the sum of square residuals (SS), largest value of determination coefficient (R2) and smallest loss of information through Akaike’s Information Criteria (AIC and AICc). This paper presents an extended power model of dependence of spherical cavity volume expansion on explosive charge. Extended model is a basic model with an additional parameter to ensure more precise mathematical description and further decrease of error of estimate for all efficiency indicators and for both types of explosive used.

1. Introduction

Spherical cavity blasting is one-time or multiple time blasting of small explosive charges at the bottom of the borehole with the purpose of expansion [1,2]. Detonation of the explosive charge at the bottom of the borehole results in a high value of pressure of detonation products [3,4]. The solid in the proximity of the explosive charge dislocates while more distant soil compreses [5], resulting in spherical cavity. The volume of the spherical cavity (Vrc) depends on the mass and type of explosive charge (Q) and geotechnical characteristics of the soil [6,7,8,9]. A diagram of relationship between the volume of spherical cavity and the mass of explosive charge has been made based on the results of spherical cavity blasting (Figure 1) [2].
Spherical volume increase made by spherical cavity blasting differ in shape and size, but in cohesive soils are typically spherical in shape [10]. The mass of explosive charge used in one-time spherical cavity blasting is usually small and determined by planned performace, typically between tens of grams to a couple of kilograms [11,12].
The research was carried out on the exploitation field Cukavec II, where exploitation of clay has been carried out for more than 50 years. The structure of the deposit is dominated by kaolinite, quartz, feldspar, and chlorite, and the granulometric composition shows that the mineral raw material contains about 75% of the clay component, while the rest is silt. The geotechnical properties of the clay soil were determined as part of the research. Cohesion c, internal friction angle φ and volume weight γ were determined. Cohesion is c = 23.4 KN/m2, internal friction angle φ = 19.8°, and volume weight γ = 18.7 KN/m3. Since the clay is hydroalumosilicate, which means that it absorbs water and therefore becomes brittle, the exploitation of the clay can only be carried out in dry months and when the air temperature is above 0 °C [13]. Spherical cavity blasting is rare in hard rocks. Namely, the effect of smaller explosive charge for spherical cavities is in principle different than continuously filled borehole in mining and blasting operations. Detonation of smaller explosive charge crushes the material in proximity of activated explosive charge. With the increase of distance from the explosive charge, the released energy is not enough for crushing materials, but instead compacts it [4,11,12,14].
Practical use of spherical cavity blasting in geotechnical works is in implementation of constructive elements for anchoring of foundation and retaining walls, permanent clay slope protection, and stabilization of different constructions such as transmission pole, tunnels, etc. [6,15].
Original data source, for the volume of spherical cavity (Vrc), horizontal (Lre), and vertical (Dre) borehole increase, were obtained in field research from 2014 to 2016 [6,15]. Težak D. et al., 2019 [1] introduced the initial values of spherical cavity volume, horizontal, and vertical borehole increase. The inclusion of these values in the database resulted in the reduction of the error of estimation of the dependence of the boreholes expansion on the explosive charge during spherical cavity blasting. Two types of explosive charge were used: ANFO explosives commercially known as Pakaex and the Ammonia Nitrogen Powder Explosive Permonex V19. Technical specifications from the manufacturer for Pakaex: density 0.87 g/cm3, VOD 2950 m/s, gas volume 984 l/kg, energy 3.7 kJ/kg and for Permonex V19: density 0.95 g/cm3, VOD 4500 m/s, gas volume 900 l/kg, energy 4.2 kJ/kg [14].
In all six cases, combinations of one of three efficiency indicators (Vrc, Lre and Dre) and type of explosive (Pakaex and Permonex V19), power model turned out to be the most efficient. Power model gives smallest estimation error values shown as the sum of square residuals (SS), largest values of determination coefficient (R2) and smallest loss of information shown by Akaike’s Information Criteria (AIC and AICc) [1].
This work gives an extended power model of spherical cavity expansion dependence on explosive charge. Extended model is essentially just a basic model with an additional parameter. The purpose of introduction of additional parameter is to ensure more precise mathematical description of already mentioned dependence and further decrease of estimation error. The decrease of estimation error is important in the determination of explosive mass used for spherical cavity blasting and coherent soil compaction. The smaller the estimation error, the more efficient and precise predicition of needed explosive mass can be made.
Based on existing analysis and an extended model, three analysis variants of a relationship between the volume of spherical cavity and explosive charge can be made:
  • Basic database—basic model
  • Extended database—basic model
  • Extended database—extended model
Obtained results are compared and justification of introduction of new parameters in the model was made.

2. Previous Research

Other than performed research from 2014 to 2016 [15], and researche in Težak, D. 2018 [6] and Težak, D. et al. 2019 [1], there are a couple of similar methods found in literature.
Literature review shows works that deal with improvements of geotechnical properties of soils using released energy in detonation of explosive charge. This is known as explosive compaction (EC). EC is a technique of soil modification that relies on explosive charge detonation to compact surrounding soft soil [16]. It should be noted, from the literature, that the explosive compaction method (EC) is used less frequently than other construction methods, primary vibrational methods, deep soil mixing (DSM), deep dynamic compaction (DDC), or jet grouting.
Literature review also showed the use of three-dimensional (3D) visualization method of natural discontinuities in a rock buring borehole drilling. This is very useful for easier and more predictable drilling plan and hydraulic fracture control [17]. Another work shows a combined interpretation of core images and acoustic images of the borehole wall for characterization of rock structure [18].
For the purpose of Težak, D. 2018 [6] doctoral thesis, application "Bušotine" was created which gives a detail 3D representation and volume of spherical cavity. Similar development of application was found in a literature review. For example, application “The BoreIs” was developed [19] as an extension to the ESRI Arcscenes three-dimensional (3D) GIS environments. It is mostly used by geologists to find spatial patterns in their data, beyond the limits of data tables and flat maps.

3. Extended Power Model

The research was conducted on an exploitation field Cukovec II, near the city of Varaždin. During the research from 2014 to 2016, obtained field data were used to broaden the knowledge of effects of explosive charge in clay soils and of possible usage of certain types of explosives in geotechnical practice [15]. The area of interest was blasted in soft rock in order to create spherical volume cavities using different types and masses of explosive. Collection of all the field data and the innovative approach in data processing were published in Težak D. et al., 2019 [1].
Plan and methods of field research, as well as data processing, are shown in Mesec J. et al., 2015 [15], Težak D., 2018 [6]. Data used in data processing are shown in Table 1. Every spherical increase of a borehole has initial value of spherical volume (Vrc0), horizontal (Lre0), and vertical (Dre0) borehole increase, all shown in blue in Table 1 [1].
Data was processed using a power model. Basic power model is given as:
y = a · x b ,
This basic model is also shown in a Figure 2 and it can be clearly seen that the curve passes through the coordinate system origin point. Initial values of spherical volume increase (Vrc), horizontal (Lre), and vertical (Dre) borehole increase are shown as point data on the ordinate. Basic power model was extended with addition of a new parameter (c):
y = a · x b + c ,
The curve of extended power model passes through some point on the ordinate of the coordinatey system. Values of model parameters are determined by least square method in program package Statistica V 13.5 [20].
Different models are compared on the basis of determination coeficients values (R2) shown in Table 2 and Table 3. However, that value increases with the increase of number of parameters in the model and can only be used to compare the models with the same number of parameters. Since there is a difference between the basic and extended models, it is necessary to compare both on the basis of Akaike’s Information Criteria (AIC) which also takes into account the number of parameters [21,22,23,24]:
A I C = N · l n S S N + 2 · K ,
where: K—the number of paramters in the model and SS—sum of square residuals:
S S = i = 1 N ( y i y ^ i ) 2 ,
where: y i   - measured value and y ^ i —estimated value of the model.
Furthermore, when N is not much larger than K, corrected AIC is applied:
A I C c = A I C + 2 · K · ( K + 1 ) N K + 1 ,
It can be noticed that with the increase between the values of N and K, the second term in the equation decreases:
N K ,
The value of the second term can be neglected. However, it should be noted that the criteria “much larger” is not clearly defined in the literature (as far as known to the authors). Due to that fact, results for both criteria are shown in the paper. Obtainted values for SS, R2, AIC, and AICc are determined and shown for both types of explosive charge seperately (Table 2 and Table 3). Between the two models, the one that gives lesser values of AIC and AICc is considered superior.

4. Results and Discussion

In Težak D. et al., 2019 [1] for the purpose of analysing the effects of spherical cavity blasting, a mathematical model was made that describes the relationship between volume increase of a borehole and mass of the explosive charge. The aim of this paper was to establish a relationship between the increase volume of a spherical volume and mass of explosive charge, type of explosive used and its detonation and mining-technical parameters. In all the calculated models, the lowest value of AICc was for the extended model. That result justifies the addition of constant to the function argument as a new model parameter.
Introduction of the new parameter had an impact on the error of estimate value. The error is smaller in value in extended models, compared to the basic models, which can be seen from the sum of square residuals (column SS, Table 2 and Table 3). In Table 2 and Table 3, the yellow colour emphasizes the best values of sums of square residuals (SS), values of determination coefficient (R2), and values of Akaike’s Information Criteria (AIC and AICc).
The reason behind the decrease is obvious while estimating the initial value. Namely, in the basic model, the graph of the model traces through the coordinate system origin point (Figure 2), and the error of estimate for Q = 0 is the initial value. In the extended model, the graph traces through some point on the ordinate and that is the value of parameter c (Figure 2).
In five out of six presented cases, the difference between the initial value and its estimation is lower than the initial value itself (column c of Table 3, Figure 3 and Figure 4). The only exception is the extended model of spherical volume increase of a borehole for Permonex V19. In that case, the negative value of initial parameters was obtained (column c, Table 3, Figure 4a). Consequently, the estimation for Q = 0 is larger than the initial value. However, the sum of square residuals is still lower in the extended model, which confirmes the justification of introducing the new parameter.
Introduction of the new parameter in the power model also resulted in higher values of determination coefficient in extended models, compared to the basic models (column R2, Table 2 and Table 3). This difference was expected, since the value of the coefficient increases with the increase of numbers of parameters in the model. This is the reason behind using AIC and AICc for comparison.
The extension of the model caused the decrease in error of estimate, but also the increase in the number of the parameters. It is clear from the AIC and AICc expressions that their values are proportional to the error of estimate value and the number of the parameters. For that reason, it is necessary to establish whether reduction of error of estimated value is sufficient to justify the implementation of the new parameter.
The values of AIC and AICc are listed in Table 2 and Table 3 in separate columns. Lower AIC values were obtained for extended models for spherical volume increase for both explosive charges and horizontal borehole increase for Pakaex. However, AICc lower values for basic models were obtained for all cases.

5. Conclusions

Previous papers showed different dependency models on spherical volume increase in boreholes for two different types of explosives, and the power model turned out to be the most successful. Justification of introduction of intial values in a database was also analysed. Each of those values are presented as a point data on an ordinate in a dispersion diagram. Obtained results show that introduction of a new parameter was justified.
The curve representing the basic power model runs through the coordinate system origin point. Due to this fact, there is a difference between the estimated values using the basic model and the initial value. In order to decrease that difference, a new parameter was introduced in the basic model, resulting in an extended power model whose cure runs through some point on the ordinate of the coordinate system.
Introduction of the new parameter into the model resulted in error of estimate reduction in five out of six cases and in an increase of determination coefficient in all cases. This confirms the main purpose of this paper: improved mathematical description of dependence of expansion of a borehole to explosive charge. This gives the possibility of better estimation of mass of explosive needed in an explosive charge in geotechnical practice, as well as faster and more efficient spherical cavity blasting.
For all shown effects of blasting for both types of explosive charge, Pakaex and Permonex V19, higher values of determination coefficient were obtained. This confirms the successful achievement of a mathematically better description of the relationship between spherical cavity blasting and explosive charge.
Comparison of obtained AIC values for basic and extended models shows that introduction of a new parameter was at least partly justified. In three out of six models, lower values of AIC for the extrended models were obtained. However, in all six cases, lower values of AICc were obtained for the basic models, making the basic model superior and the introduction of the new parameter not completely justifiable.
In conclusion, it is necessary to build a model that demonstrates the relationship between spherical cavity blasting and explosive charge that will result in the smallest value of error of estimate and also in the lowest AIC and AICc values.

Author Contributions

Conceptualization, I.K.; Data curation, J.M.; Formal analysis, I.K.; Investigation, D.T.; Methodology, I.K.; Project administration, J.M.; Resources, D.T.; Software, D.T.; Supervision, J.M.; Validation, I.M.; Visualization, I.M.; Writing—original draft, I.K. and D.T.; Writing—review and editing, I.M. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Acknowledgments

Publication process is supported by the Faculty of Geotechnical Engineering, University of Zagreb.

Conflicts of Interest

The authors declare no conflict of interest.

References

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Figure 1. Diagram of relationship between the volume of spherical cavity Vrc (m3) and the mass of explosive charge Q (kg) [2].
Figure 1. Diagram of relationship between the volume of spherical cavity Vrc (m3) and the mass of explosive charge Q (kg) [2].
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Figure 2. Schematic of basic and extended power model for spherical cavity volume increase Vrc (m3) in dependence on the mass of explosive charge Q (kg).
Figure 2. Schematic of basic and extended power model for spherical cavity volume increase Vrc (m3) in dependence on the mass of explosive charge Q (kg).
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Figure 3. Basic and extended power model for Pakaex: (a) Spherical volume increase; (b) Borehole horizontal increase; (c) Borehole vertical increase.
Figure 3. Basic and extended power model for Pakaex: (a) Spherical volume increase; (b) Borehole horizontal increase; (c) Borehole vertical increase.
Geosciences 10 00151 g003aGeosciences 10 00151 g003b
Figure 4. Basic and extended power model for Permonex V19: (a) Spherical volume increase; (b) Borehole horizontal increase; (c) Borehole vertical increase.
Figure 4. Basic and extended power model for Permonex V19: (a) Spherical volume increase; (b) Borehole horizontal increase; (c) Borehole vertical increase.
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Table 1. The results of spherical cavity blasting for explosives Pakaex and Permonex V19 [1].
Table 1. The results of spherical cavity blasting for explosives Pakaex and Permonex V19 [1].
PakaexPermonex V19
BoreholeExplosive Charge MassVolume of the Resulting CavityResulting Expansion of the BoreholeDeepening of the Resulting ExpansionBoreholeExplosive Charge MassVolume of the Resulting CavityResulting Expansion of the BoreholeDeepening of the Resulting Expansion
Q
(kg)
Vrc
(m3)
Lre
(m)
Dre
(m)
Q
(kg)
Vrc
(m3)
Lre
(m)
Dre
(m)
MB201.000.71001.15700.5200MB240.800.61841.19000.3100
MB411.000.80951.11100.6000MB260.800.56901.13100.3600
MB340.800.39350.95300.3300MB450.800.74051.07000.4000
MB180.800.34400.87700.4600PMB50.800.72271.07100.4200
MB190.800.36260.87500.4800MB230.600.52761.10400.3500
MB400.800.51901.06000.4000MB250.600.63301.08500.2900
MB350.600.25550.78300.2500PMB60.600.61511.15200.3500
MB170.600.61601.04300.3400MB360.400.11350.69300.2300
MB390.600.37851.08800.4000MB210.400.29250.93600.2600
MB150.400.24450.69800.3100MB270.400.21600.58500.3200
MB160.400.19450.78700.3000MB430.400.28150.86600.3000
MB380.400.29800.84800.4000MB220.200.08250.55700.2600
MB130.200.10050.57600.1800MB280.200.07000.50500.2200
MB140.200.06450.57700.2200MB420.200.14800.66200.2000
MB290.200.09800.68700.2400-0.000.00050.13100.0390
MB370.200.11750.60100.2500
-0.000.00070.13100.0390
Table 2. Parameter values and results of the power model analysis for explosive charge Pakaex.
Table 2. Parameter values and results of the power model analysis for explosive charge Pakaex.
Pakaex
(N = 17)
abcKSSR2AICAICc
Vrc10.660.66-20.1700.770−68.700−67.900
20.661.20-20.1700.800−74.278−73.528
30.641.320.0230.1690.804−74.358−72.758
Lre11.090.35-20.1300.780−72.920−72.120
21.090.35-20.1480.863−76.667−75.917
30.960.420.1330.1310.878−76.718−75.118
Dre10.500.53-20.0600.720−85.920−85.120
20.500.53-20.0600.804−92.130−91.380
30.450.640.0530.0570.812−90.894−89.294
Vrc, made spherical volume; Lre, horizontal borehole increase; Dre, vertical borehole increase.
Table 3. Parameter values and results of the power model analysis for explosive charge Permonex V19.
Table 3. Parameter values and results of the power model analysis for explosive charge Permonex V19.
Permonex V19
(N = 15)
abcKSSR2AICAICc
Vrc10.940.21-20.1100.870−64.260−63.340
20.941.32-20.1100.891−70.173−69.316
30.961.22−0.0330.1050.893−70.399−68.553
Lre11.300.51-20.1600.810−59.010−58.090
21.300.51-20.1700.870−62.972−62.115
31.180.590.1230.1570.885−62.384−60.538
Dre10.400.37-20.0200.710−90.320−89.410
20.400.37-20.0180.853−96.798−95.941
30.360.430.0430.0170.866−96.187−94.472
Vrc, made spherical volume; Lre, horizontal borehole increase; Dre, vertical borehole increase.

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MDPI and ACS Style

Kovač, I.; Težak, D.; Mesec, J.; Markovinović, I. Comparative Analysis of Basic and Extended Power Models of Boreholes Expansion Dependence on Explosive Charge in Blasting in Clay Soil. Geosciences 2020, 10, 151. https://doi.org/10.3390/geosciences10040151

AMA Style

Kovač I, Težak D, Mesec J, Markovinović I. Comparative Analysis of Basic and Extended Power Models of Boreholes Expansion Dependence on Explosive Charge in Blasting in Clay Soil. Geosciences. 2020; 10(4):151. https://doi.org/10.3390/geosciences10040151

Chicago/Turabian Style

Kovač, Ivan, Denis Težak, Josip Mesec, and Ivica Markovinović. 2020. "Comparative Analysis of Basic and Extended Power Models of Boreholes Expansion Dependence on Explosive Charge in Blasting in Clay Soil" Geosciences 10, no. 4: 151. https://doi.org/10.3390/geosciences10040151

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