2.2. Methods
A high-resolution scanning electron microscope (HR-SEM) was used with a voltage of 5.00 kV and a current of 0.1 nA. T2 and ETD detectors were used. The highest magnification at which clear images were obtained was 150,000×. The material was characterized by the x-ray photoelectron spectroscopy (instrument “PHOIBOS”, with software “SpecsLab Prodigy”, model “4.34.1-r66167”). Lens analyzer: MediumArea: 1.5 kV, analyzer slit: 5:7 × 20/B: open. Scanning program: FixedAnalzyerTransmission, retention time: 0.1, excitation energy 1486.61, binding energy 1400, pass energy 40, detector voltage: 2170. Specific surface and the pore-size distribution was measured by the Brunauer-Emmett-Teller (BET) method with 3P INSTRUMENTS Surface Area and Pore Size Analyzer, Sync 110A model. Samples were degassed at 200 °C for 2 h. The nitrogen was used as an adsorbate. Thermal analyses (Thermogravimetry—TG and Differential Scanning Calorimetry—DSC) of the AN prill were performed at 20–800 °C. All investigated materials were exposed to an airflow of 30 mL·min−1. Instead of inert gases like nitrogen, an airflow was selected due to the fact it could sustain the similar conditions in the both the furnace and balance chamber like in the case of the typical explosive detonation. Directly prior to each measurement, the explosive sample (20 mg) was placed in the DSC aluminum pan using a spatula. The TG baseline was determined using a heating profile for the empty pan. The TG drift was ca. 5 μg, which constituted 0.02 mass%.
Thermodynamic calculations were made in the ZMWCyw software. The software was developed by the Military University of Technology in Warsaw. Calculations relay on the physico-chemical properties of each component. If component is not present in the ZMWCyw database, it can be defined and added by the user. ZMWCyw software allows for the calculation of parameters like the explosion pressure and temperature heat of the explosion, the post-blast volume, etc. The oxygen balance of each individual explosive material was calculated according to the standard [
23].
Measurements of the heat of explosives were performed in a detonation calorimeter. The 50 g non-ideal explosive sample was initiated with an Erg electric detonator and a 5 g RDX booster. The obtained results took into account the characteristic temperatures of the cycles (T
1–T
4), the duration of the main period of the cycle (n), and the total heat effect (Q) calculated for the preset heat capacity of the assembly (K), which were read after completing the measurement. The total heat effect was calculated using (1).
where
K indicates the heat capacity of the assembly, cal °C; Δ
T– the differentiation of the temperature during the main period of the cycle; Δ
T =
T3 −
T2, °C;
T1,
T2,
T3,
T4—the distinguished temperatures in characteristic points of the measurement cycles, °C;
k—the coefficient which is responsible for making a correction on losses of the assembly, °C, computed based on Equation (2):
where
n denotes the duration of the main period of the cycle, min.
A detailed description of measurements of the heat of the explosion is provided in [
24].
Post-blast oxide analysis was performed according to the standard [
25], which is in accordance with the council directive [
26]. Non-ideal explosive charges of a mass of 600 g were placed inside the steel mortar which was inside the blasting chamber (
Figure 1). After the blasting chamber was sealed, explosive charges were detonated.
After decomposition reaction, the fan system was activated in order to achieve the homogenization of the post-blast fumes. The homogenization process lasted 3 min. Subsequently, post-blast gases samples were collected for 20 min in the ventilation system. The amounts of CO and CO2 were determined by IR (MIR 25e) and NOx by chemiluminescent (TOPAZE 32M) analyzers.
The velocity of detonation (VOD) was measured based on the standard [
28] by blasting 600 g of non-ideal explosive charge in a glass pipe. The pipe’s inner diameter was 46 mm. VOD was measured by placing two short-circuit probes close to the top and bottom of the tube. The distance between the probes was 150 mm. The VOD was established by the division of the time difference which was derived by the progressing detonation with a distance between probes (Equation (3)):
where
l denotes the distance between two probes and
t is the time difference [
29].
All non-ideal explosives were initiated by the 14 g RDX (Royal Demolition Explosive)-based charge.
2.3. Microstructured Charcoal Characteristics
Figure 2 shows the comparative images of the two classes of carbon materials which were used in this research. The preliminary comment which can be made is that the carbon of −90 μm class had a visibly smoother surface, while the carbon of −1.18 mm class had highly developed surface morphology with many uneven features over the surface. It can even be clearly concluded from the image taken at 100,000× magnification that a number of pores and rainures below 100 nm were present. The smoother surface of the −90 μm class sample can be explained by the mechanochemical reactions which probably took place during the intensive ball milling of the sample when the graphene layers overlapped, forming an apparent multilayered smooth-carbon structure with very few pores or irregularities visible. In the case of the −1.18 mm carbon, much less force was used since carbon was crushed to a granular size with a small mechanochemical action. Therefore, original structures which evolved in the process of the destructive wood distillation were more present. Since the process is very similar to the pyrolysis used in the activated carbon production, many pores and irregularities such as rainures formed on the surface with the process of the evaporation of liquid contents from the wood and under pressure of evolving vapors.
A collection of the XPS scans is shown in
Figure 3. A wide scan
, Figure 3a, in the region from 100 to 1400 eV, revealed that the carbon and the oxygen were the dominant elements, while some traces of calcium, nitrogen, and chlorine were also revealed. These last three elements were present probably as the remains of the nutrients used by the tree used for the production of carbon and are expected in negligible quantities. More detailed information is needed on the nature of the chemical relations in which carbon and oxygen are involved and, therefore, the XPS narrow spectra of these elements were performed and shown.
Carbon C1s narrow spectra,
Figure 3b, curve fitting showed three prevalent chemical relations in which carbon was involved. These are visible as the peaks shown by dashed lines. The peak at 284.5 eV was expected to be dominant since this binding energy belongs to the graphitic C-C bond and it is clearly visible and in place. The fitted peak at 285.7 eV can belong to the liaison of carbon with S, Cl, or N. Similarly, the fitted peak at 287.7 eV can correspond to the carbon bonded with S, Cl, or N, but can also be a sign of the functional groups forming on the edges of carbon layers, such as alcohols, ethers, and kethons. To resolve this, an O1s narrow spectra (c) was also fitted and it showed only one dominant peak at 532.7 eV. This peak may represent the metal carbonates or the carboxylic group bonding with carbon. Since there was no carboxylic peak visible in the vicinity of 288.5 eV during the carbon 1 s narrow scan (b), it can be concluded that it is probable that the oxygen present represents traces of the calcium carbonate which is naturally present after wood pyrolysis. Calcium as an element is present since the trees are absorbing it as a nutrient from the soil. The presence of the calcium from metal carbonate was confirmed by typical peaks at the Ca 2p scans (d), although some charging occurred in this narrow scan. Clear presence for chlorine was also confirmed in the narrow scan of Cl 2p electron (e), with the position at 198.5 eV, which corresponds to the metal chlorides. Again, this is probably the nutritive chlorine which was bound to the sodium chloride or other chloride salts absorbed by the tree during its development. However, this presence can be used for the discussion since chloride ions could influence the blasting properties. The narrow spectra of the N 1s (f) was quite difficult to analyze and, due to a lot of noise, it was not very conclusive. It can be said with certainty that the quantity is small and that the peak at 400 eV perfectly corresponds to the C-NH2 bond which is quite common on the edges of the carbon species produced by pyrolytic methods in general.
An adsorption analysis of the N
2 as well as pore size distribution is presented in
Figure 4 and
Figure 5. The aim of these analyses was to make preliminary research of the possible influence of these MC-enhancer characteristics on the post-blast oxides generated during the detonation of non-ideal explosives.
The N
2 adsorption,
Figure 4, showed that the specific BET surface of the −1.18 mm granulated charcoal had a lower value of ca. 10.2 m
2·g
−1. This result is in contrast to the HRSEM images of the present sample (
Figure 2, left) and by the similar samples used in a previous study [
22] where it was established that some structures of high porosity and complex surfaces are developed and visible. However, based on
Figure 5, it was established that the dominant pore size in this sample was 2.9 nm and all of the pores were in the region below 20 nm diameter. Consultations with the experts from the industry revealed that it can be assumed that the actual specific surface is much higher; however, the pores were clogged due to the process itself, i.e., the exhaust gasses were turned back to the furnace in order to prevent the self-incineration of the material during the process of the pyrolysis. Therefore, it is probable that gas molecules such as SO
x, NO
x, CO
x, as well as some larger molecules which were believed to have evaporated in the process were actually adsorbed and clogged the pores. This should be considered especially during post-blast fume analysis. On the other hand, the carbon of –90 μm granulation had a somewhat higher specific surface of 16.9 m
2·g
−1. On the contrary, its most dominant pore sizes are 8.4 and 16.9 nm, as can be verified in
Figure 6. One explanation can be that the collapse of the structure under intensive milling crushed some of the smallest pores while some new, though larger pores opened along the structure, probably at some harder or even calcified regions (calcium carbonate was confirmed and already verified in the XPS spectra above).
2.4. Explosive’s Theoretical Properties
Calculated blasting properties, summarized in
Table 2, indicated the potential influence of MC on the tested explosive properties. However, the change of the oxygen balance influences the velocity of detonation in non-ideal explosives (peak VOD when oxygen balance is close to zero and release of the energy is almost complete). Moreover, a decrease of energy with increased content of MC should be followed by the decrease of enthalpy which in the end may affect the explosives sensitivity and critical diameter. In other words, with increased MC content, an explosive material will require higher heat of explosion from the primer, which means that this explosive will be less sensitive than the explosive which was theoretically calculated. Moreover, theoretical calculation indicated that the enthalpy decreases with the addition of MC. However, despite this fact, and by taking into consideration the non-ideal model of the detonation process, the MC should combust behind the reaction front [
30]. Under normal conditions, when the inert component which is characterized by the high-standard enthalpy of formation is provided to the explosive composition, an increase in blasting parameters like detonation temperature and pressure takes place. This increase of the detonation temperature will be present until the component which was added to the explosive composition is completely burnt near the Chapman-Jouguet plain. A subsequent change of temperature and pressure (both should decrease) will be accompanied by a drop in the VOD. This effect can be simply explained by the size of the reaction zone. Added MC results with an increase of the active surface. This caused both heat transfer and raised a chemical reaction surface. On the other hand, the addition of MC resulted with a decrease in the induction time of the initiation. Hence, the detonation pressure and temperature both decreased (
Table 1). This decrease could be explained by the increase of the surface of the chemical reaction which, in the end, affects both the chemical reaction surface (increases) and the induction time for the initiation (decreases). Moreover, MC addition will result with the shifting of the oxygen balance towards negative values. This can be explained by the replacement of hydrogen atoms from AN by carbon atoms from fuel oil. In other words, adding MC to the explosive chemical composition results in shifting the oxygen balance toward more negative values which, in the end, may result in additional content of carbon monoxide and soot appearing in gaseous products. These products of the detonation process can make a further impact on the afterburning effect as secondary reactions. The presence of secondary reactions, which are the result of the afterburning, may lead to an increase in the detonation pressure [
31]. Salzano and Basco in their afterburning research concluded that black powder afterburning generated a level of the energy which was comparable to the afterburning energy of TNT [
31]. The afterburning effect was not included in the ZMWCyw software. Moreover, due to the specific properties of the MC surface, it is expected that the MC content will influence the volume of the CO
x and NO
x in the post-blast fumes, which may hamper the afterburning effect.
Moreover, based on the potential blasting properties presented in
Table 2, it can be observed that the decrease in detonation temperature and the increase in pressure was generally followed by a drop in the explosion heat, in the post-blast volume, and the strength of the explosive. This influence can be explained by the conversion of mass and momentum equations that represent relationships between the detonation pressure, the velocity of detonation, and the post-blast volume that further affects the Chapman-Jouguet plain [
32]. Furthermore, Hugoniot’s equations indicate an equilibrium state being independent of the explosive density or the density of the post-blast fumes, confirming the potential drop in the velocity of detonation.
2.5. Explosive’s Properties
TG data (
Figure 6 and
Figure 7) indicated that in all cases, a small mass loss (below 200 °C) was due to the evaporation of FO from the surface of crystalline AN. A further increase in the temperature resulted in a total decrease in the mass of all studied samples, which can be explained by the decomposition of AN according to the following equation [
33]:
The susceptibility of AN-based explosives to decomposition depended weakly on either the size of MC grains or the chemical composition of the prepared samples. The explosives with lower FO (2.5 wt%.) and containing a higher amount of MC (3 wt%.) underwent decomposition in the first place. In turn, the samples containing 1 wt%. of MC and 4.5 wt%. of FO seemed to be most thermally stable.
Figure 8 and
Figure 9 illustrate DSC curves at 20–800 °C, obtained for the AN-based explosives containing both FO and MC. In all cases, the DSC profiles indicated four endothermic peaks at 61, 136, 176, and 272–292 °C. Two peaks at ca. 61 and ca. 136 °C were due to the crystallographic transformation of AN III→II and AN II→I, respectively. A third signal at ca. 176 °C originated from the melting point of the AN [
24].
The increase in temperature led to thermal decomposition of AN, for which the temperature of the fourth DSC peak depended on both the size of the MC grains and the chemical composition of the prepared samples. It was shown that the lowest temperature of decomposition of the investigated explosives was found for the samples containing 2.5 wt%. of FO and 3% wt%. of MC (272 °C for both samples containing MC grains of −1.18 mm and −90 μm). The highest temperature of the decomposition of the studied materials was found for the samples containing 4.5 wt%. of FO and 1 wt%. of MC (292 °C and 282 °C for the samples modified with microstructure charcoal grains of −1.18 mm and −90 μm, respectively).
Furthermore, it may be concluded from the obtained data that the size of MC influenced the decomposition reaction. For the samples containing MC, grains of −1.18 mm, DSC endothermic peaks occurred at 272–292 °C, while for counterparts modified with smaller MC particles of −90 μm, the DSC peaks were found at 272–282 °C. This shows that smaller MC grains enable the decomposition of materials prepared in such a way. The DCS data correlates with the TG profiles.
Results of blasting tests of non-ideal explosives where −1.18 mm and −90 μm MC powders were used are presented in
Table 3 and
Table 4. The obtained results verified some explosive properties which were established based on the thermodynamic models,
Table 2.
Obtained VOD values,
Table 3 and
Table 4, indicated the non-ideal character of tested explosives and confirms the research in [
9,
13]. Depending on the microstructure grain size, measured VODs were in the range of 1500–2050 m⋅s
−1. The measured velocities were lower than predicted from the theoretical calculation (in the range of ca. 2200–2400 m⋅s
−1). This derived from the properties of the non-ideal explosives (a decrease of explosive density plays a major role due to the explosive density-VOD relation). Regardless of the grain size, it was observed that MC addition resulted in an increase of the CO
2 content (in the case of MC addition of the grain size of −1.18 mm an increase volume of CO
X and NO
X from ca. of 94 dm
3⋅kg
−1 to 116 dm
3⋅kg
−1, in the case of MC addition of the grain size of −90 μm an increase volume of CO
X and NO
X from ca. of 94 dm
3⋅kg
−1 to 127 dm
3⋅kg
−1), and a decrease in CO content (except sample 4) in post-blast,
Table 3 and
Table 4. This change was followed by an increase in the volume of NO
x in post-blast fumes (except sample 4),
Table 3 and
Table 4. This relationship is likely explained by the shifting oxygen balance toward positive values (in the case of samples 1–3), as well as composition change. In the case of samples 1–3, the addition of the MC was followed with a decrease in the fuel component (the total wt. of fuel component is always 6.0% of total non-explosive wt.). This shift can be explained by the presence of oxygen in the microstructure charcoal chemical compositions. This was confirmed by the results of XPS analysis,
Figure 3c. Moreover, Muzyka and Topolnicka, as well as Radovic, indicated that the total oxygen content in hard coals is influenced by the degree of the metamorphism [
34,
35]. In other words, oxygen content decreases with the rank of coal. In the case of hard ranks (flame coal, coking coal, and anthracites), the oxygen content was in the range from 17% up to 2%. In brown coals, the oxygen content can vary between 15–35%. Due to this additional content of oxygen, as well as the fact that the individual share of the fuel component has lower negative oxygen balance in comparison with diesel fuel oil, it can be assumed that the oxygen balance of the explosive composition will have a higher positive oxygen balance than presented in
Table 2. This additional oxygen, based on Kistiakowski-Wilson’s work, will allow oxidation of CO to CO
2, which causes an increase in the carbon dioxide content and a decrease in the carbon monoxide content. However, higher oxygen balance results in an increase of the NO
x content. In the case of sample 4, the addition of MC was followed by a decrease in the AN-PP. The additional content of oxygen in MC was not equal to the content which was present in AN-PP. This resulted in obtaining a more negative oxygen balance than calculated (−10.34%), as shown in
Table 4. As a result, this will increase the CO
2 volume due to the higher carbon content in the non-ideal explosive chemical composition, as well as an increased volume of CO as the result of oxide deficient and the non-complete oxidation process. The decrease in the grain size influenced both the VOD and total-post-blast volume. It was observed that with a decrease in MC content, the post-blast volume and VOD increased; this can be explained by the detonation mechanism. Added MC reacts outside the shockwave front, which increases both the chemical reaction zone and heat exchange. This results from Hugoniot’s equation with an influence on pressure and volume and in shifting the Chapman-Jouguet point.
The afterburning effect is a result of the secondary reaction between unreacted FO or partially oxidized post-blast fumes which were derived from the primary reactions with the surrounding air. Based on the exemplary record of CO
x, shown in
Figure 10 and
Figure 11, it can be observed that afterburning appeared in the first minute after the detonation reaction. The first peak of CO (ca. of 370 ppm) and CO
2 (ca. of 6700 ppm) appears to be the direct effect of detonation. Subsequently, afterburning and homogenization appeared, which resulted in the stable volume of the oxides. With a decrease in the oxygen balance, the content of CO will increase (sample 4). The change of the MC diameter did not affect the characteristic of the CO
x volume. It only affected the content of CO
x, and thus the presented records can be treated as model ones. When shifting the oxygen balance toward positive values (sample 2 and sample 3), the content of CO
2 in the primary reaction increased due to the presence of additional oxygen. The products of the decomposition reaction should further influence the afterburning, which results in an increase in the detonation pressure and a shift in the Chapman-Jouguet plain [
27]. Moreover, the change of the oxygen balance the secondary reaction which appears from the NO
x should be included (
Table 5 and
Table 6, and
Figure 12).
The general record of the NO
x, Figure 12, shows that the first peak is derived from a detonation reaction. The subsequent decrease of NO
x is a result of both homogenization and the decomposition reaction. The small amount of nitrous acid may be an effect of the secondary reaction. However, in contrast to CO
x, it can be observed that the stabilization of the NO
x content takes much longer.
Table 5 and
Table 6 indicate the concentration of NO
x after 10 min from the detonation. The post-blast analysis indicated that oxygen balance affects the content of each individual oxide. In general, based on
Table 3,
Table 4,
Table 5 and
Table 6, it can be observed that the general ratio between NO/NO
x and NO
2/NO
x decreased with time and stabilized, which suggests the occurrence of secondary reactions and homogenization of the atmosphere in the blasting chamber.
The influence of the MC addition as well as MC grain diameter on the heat of the explosion is presented in
Table 7.
Based on
Table 7, it can be concluded that MC addition slightly increased the average heat of the explosion from 3940 J⋅g
−1 to within the range of 4050–4130 J⋅g
−1 and this depended on the non-explosive composition and grain size. Comparison of the MC grain size led to the conclusion that higher heat explosion values were obtained in the case of non-ideal explosives, where MC powder of the 90 μm grain was added. This can be explained by a typical detonation mechanism for the non-ideal explosive with the addition of metal. As stated previously, MC grains undergo a chemical reaction before the shockwave front, which progresses throughout the non-ideal explosive charge. This increases the chemical reaction zone. Moreover, the application of the MC of smaller grain size improves charge density. In the case of explosive charges of higher density, the distance between prills decreases. This has a direct impact on the appearance of hot appearance (smaller gaps between neighboring hot spots), which finally causes lower heat loss [
4,
36]. In other words, higher charge density improves the chemical reaction zone, the surface of the heat exchange, and reduces heat loss, resulting in an improved detonation temperature and a higher heat of explosion. It can be assumed that the application of the MC powder of smaller grain size could further improve the heat of explosion to a certain point (press point). After reaching the dead-pressed point, the non-ideal explosive should not detonate.