Pengjin Liua,
Hongwei Mub,
Jiafa Dua,
Xianwei Dongc,
Jianfei Sun*bd and
Yongliang Zhang*b
aQinghai Shanjin Mining Co., Ltd., Qinghai Haixi, China
bSchool of Mechanical and Automotive Engineering, Qingdao University of Technology, Qingdao, China. E-mail: sunjianfei@qut.edu.cn; zhangyongliang@qut.edu.cn; Fax: +86-532-68052755; Tel: +86-532-68052755
cSchool of Emergency Management and Safety Engineering, North China University of Science and Technology, Tang Shan, China
dKey Lab of Industrial Fluid Energy Conservation and Pollution Control (Ministry of Education), Qingdao University of Technology, Qingdao 266520, P. R. China
First published on 3rd April 2025
Coal spontaneous combustion fires not only waste coal resources, but also restrict underground safety production. Therefore, research on natural prevention and control of coal fires is particularly important for ensuring coal mine safety production. Based on the theory of coal spontaneous combustion and the mechanism of inhibition, the inhibition performance of sodium hypophosphite inhibitors in the process of coal spontaneous combustion oxidation was studied. Firstly, the CO release and inhibition rates of coal samples and inhibited coal samples during the heating and oxidation process were calculated using a programmed heating method. Then, combined with infrared spectroscopy, the influence of hypophosphite on its surface functional groups during coal spontaneous combustion oxidation was studied from a microscopic perspective. Subsequently, thermogravimetric experiments were conducted to analyze the changes in the thermal characteristic curves of inhibited coal samples at different heating rates and particle sizes. Finally, a kinetic model was proposed to analyze the activation energy of the inhibition reaction. Results indicated that the addition of sodium hypophosphite has a natural inhibitory effect on the oxygen absorption and thermal decomposition stages of coal samples.
The spontaneous combustion and oxidation of coal is a complex physical and chemical process, and the oxidation rate increases continuously with the oxidation process. It can be roughly divided into three stages: preparation period, natural period, and combustion period.3 The natural period coal begins to accelerate oxidation, and the combustion period is the most intense stage of coal oxidation. Coal will release different gases at different oxidation stages, manifested macroscopically as varying gas concentrations with temperature. As is well known, the main functional groups that undergo combustion in coal include active groups such as oxygen-containing groups, alkyl side chains, sulfur-containing groups, and nitrogen-containing groups.4 Due to the fact that most of the structure of coal contains oxygen-containing functional groups, this component undergoes major losses during the stage of coal oxidation and spontaneous combustion.5 In addition, clean coal can be pyrolyzed at high temperatures to remove volatiles and prepare coal coke, which can be used as low-impurity amorphous carbon raw materials for the preparation of carbon nanomaterials, and undergo nitric acid oxidation to prepare coal-based graphene oxide (GO) materials. At present, coal-based GO materials have potential applications in biosensors, drug delivery systems, energy storage devices, adsorbents, and catalysts.36,37
In general, the indicator gases for predicting coal spontaneous combustion are mainly classified into three categories:6–11 the first category comprises carbon oxides (CO and CO2). Due to the early appearance of CO gas, it appears in all stages of coal spontaneous combustion, and the release amount shows a strong regularity with temperature increase, which is more common in predicting coal natural fires. The second category comprises saturated hydrocarbons (C2H6, C3H8, and C4H8) and alkane ratios (C2H6/CH4, C3H8/CH4, C4H10/CH4, C3H8/C2H8, and C4H10/C2H8). The amount of gas released is greatly affected by the coal structure, and the detection of such gases during coal spontaneous combustion usually indicates that oxidation has entered an accelerated stage.12,13 The third category of indicator gas comprises mainly unsaturated hydrocarbons, including C2–C4 olefins and C2H2 alkynes, which are affected by the degree of coal metamorphism and have different critical temperatures during the oxidation and spontaneous combustion process.14
At present, flame retardants are widely used in coal mine production fire prevention and extinguishing practices, and have achieved significant results.15 Moreover, they have the advantages of convenient use and wide application ranges, and are one of the commonly used fire prevention and extinguishing technologies in coal mines at home and abroad. At present, commonly used inhibitors include halogen salt inhibitors (MgCl2, CaCl2, NaCl, sodium hypophosphite, aluminum hypophosphite, etc.), ammonium salt inhibitors (NH4Cl, (NH4)2HPO5, etc.), ionic liquid inhibitors ([Bmim][OTf], [Bmim][AC], etc.), and antioxidant inhibitors (tea polyphenols, citric acid, catechins, etc.).16,17 However, ammonium salt inhibitors are prone to producing harmful gases such as ammonia during use. Ionic liquids and antioxidant inhibitors have good inhibition performance, but their prices are too expensive. Compared to other flame retardants, halogen salt flame retardants are inexpensive, easy to produce, and safe to use. They are widely used in coal mines and have strong water absorption properties. The absorbed water can form a thin film on the surface of the coal, reducing the probability of coal coming into contact with oxygen. They mainly prevent and extinguish fires by exerting their physical flame retardant effect of absorbing water and isolating oxygen, so they are called physical flame retardants.18–20 The research overview of different inhibitors for suppressing coal spontaneous combustion process is shown in Table 1.
Coal | Inhibitors | Preparation method | Influence factors | Resistance rate (%) | Ref |
---|---|---|---|---|---|
Yangquan coal 15 # | 30% calcium chloride, 20% sodium silicate | Solvent mixture | Inhibition temperature and solvent concentration | 55 | 31 |
Dongshan coal | 20% ammonium dihydrogen phosphate | — | 95–105 °C | 88 | 33 |
Lignite, gas coal, and fat coal | — | — | 3–18% O2 | — | 34 |
Huainan coal | 0–10 wt% BMIM BF4 | Impregnation method | 0–22% O2 IL concentration | — | 35 |
Based on the above-mentioned self-ignition mechanism of coal, the self-ignition conditions of coal can be divided into two categories: physical conditions and chemical conditions. Therefore, the self-ignition inhibition mechanism of coal can also be divided into physical inhibition and chemical inhibition.21 Physical inhibition mainly aims to prevent coal spontaneous combustion by changing the environmental conditions or physical conditions of the coal itself, so that it does not have the conditions for spontaneous combustion.22 The inhibition mechanism of chemical inhibitors is to destroy or reduce the active groups in coal molecules with low activation energy that are easily oxidized through chemical action, capture and reduce the free radicals generated during the coal oxidation reaction process, thereby interrupting the chain reaction of coal spontaneous combustion, improving the oxidation reaction conditions of coal at low temperatures, and making it difficult for coal to achieve spontaneous combustion.23,24 Usually, physical inhibition is relatively simple, by covering and isolating oxygen to form a membrane film, reducing the probability of coal coming into contact with oxygen, thus achieving fire prevention and extinguishing.25
A. C. Smith et al.26 added inorganic salt inhibitors to coal to suppress spontaneous combustion, and the research results showed that sodium nitrate, sodium chloride, and calcium carbonate had the best effect on inhibiting coal spontaneous combustion, while ammonium dihydrogen phosphate, calcium chloride, and ammonium chloride had slightly lower effects. Yukihiro Adachi et al.27 found that mixing amino cationic surfactants and nonionic surfactants in a certain ratio and covering the surface of coal is very effective in preventing coal from heating up. Alkaline inhibitors can effectively reduce the contact between surface active groups of coal and oxygen, and have a good inhibitory effect on coal spontaneous combustion. Acidic inhibitors (such as sodium persulfate, citric acid and other acidic compounds) mainly remove inherent metals from coal, suppress the catalytic effect of some inherent metals on coal spontaneous combustion, and achieve the effect of suppressing coal spontaneous combustion.28 Previous studies have shown that halogen salt inhibitors have a higher contribution to coal seam inhibition, and further research is needed on the thermal characteristics of coal oxidation inhibition processes.
In this study, the different particle sizes of raw coal samples were first selected, and sodium hypophosphite was chosen as the inhibitor. Different concentrations of inhibitor solutions were added to the raw coal samples to prepare composite coal samples. The coal samples were heated in a temperature oxidation test furnace to analyze the exhaust gas composition of the coal. The chemical structure changes and thermal characteristics of the coal samples before and after oxidation were analyzed to identify the changes in the coal samples before and after oxidation. This study using characterization methods to obtain dynamic monitoring and intelligent warning for suppressing coal oxygen composite reaction and coal spontaneous combustion, as well as active, graded, and collaborative prevention and control of coal spontaneous combustion, and obtain the formation, evolution, and inhibition mechanism of coal spontaneous combustion, and also provide reference and guidance for the development of other types of flame retardants for on-site fire prevention and extinguishing work, as well as theoretical research on fire prevention and extinguishing technology.
Number | Name | N% | C% | S% | H% | O% |
---|---|---|---|---|---|---|
1 | Lin Nancang 1184 | 1.371 | 75.91 | 1.151 | 4.724 | 16.844 |
Coal sample | Content of each component | Mad% | 5.285 | |||
Vdaf% | 38.485 | |||||
Aad% | 17.27 | |||||
Spontaneous combustion tendency level | II |
The elements and characteristics of different types of coals are different. Industrial analysis of coal can clearly understand the coal quality of various types of coal. The industrial analysis and testing of coal are based on the national standard “Methods for industrial analysis of coal”,30 and the main measurement contents through industrial analysis include moisture, ash content, volatile matter, and fixed carbon, as shown in Table 1. The industrial analysis of spontaneous combustion tendency is divided into three levels: Class I is prone to natural combustion, Class II has a certain tendency towards spontaneous combustion, and Class III is not prone to spontaneous combustion. Based on the results in Table 2, it was classified into Class II. Among them, the ash content of coal is 17.27%, the higher the ash content, the more heat is carried away by the slag, and the lower the utilization rate of coal. The moisture content of raw coal is the highest and the ash content of raw coal is the lowest through experiments. After pre-oxidation treatment, the moisture content of coal decreases, which is conducive to combustion, and the ash content increases, indicating that some organic carbon and water are consumed together.
![]() | (1) |
In the formula: E is the resistance rate (%), A is the total amount of carbon monoxide released from the raw coal sample (ppm), and B is the total amount of carbon monoxide released from the coal sample that has been inhibited (ppm). The higher the inhibition rate of the inhibitor, the stronger its ability to prevent coal oxidation.
Oxygen A (g) + coal B (s) = oxidation product C (s) + generated gas D (s) | (2) |
Coal underwent a series of complex chemical reactions when heated and in contact with oxygen, producing oxidation products and some volatile gases. This process was generally considered irreversible. There are two forms of describing dynamics:
Differential form:
![]() | (3) |
Integral form:
G(α) = kt | (4) |
In the formula: T is the reaction time (min), α is the conversion rate, i.e. the conversion rate of B at time t (%), and k is the reaction rate constant.
It is the mechanism function of oxidation kinetics in differential form. It is the integral form of the dynamic mechanism function, and it is generally believed that the relationship between the rate constant k and the thermodynamic temperature T follows the Arrhenius equation, which states:
k = A![]() | (5) |
In this equation, A refers to the pre factor, E is the activation energy (kJ mol−1−1), and R is the universal gas constant (8.314 J mol−1 K−1).
![]() | ||
Fig. 1 CO concentration versus temperature curve for coal samples with different levels of added sodium hypophosphite. |
The results show that the detection time of CO gas in coal samples is basically similar when different concentrations of hypophosphite are added, and it is generally around 50 °C. Before 100 °C, due to the presence of moisture in the coal sample, the CO release of the coal sample with sodium hypophosphite added did not change significantly compared to the original coal sample. After 100 °C, the vaporization of moisture in the coal sample intensified, and the moisture was removed with the airflow. At this time, the temperature difference between the inside and outside of the coal sample tank increased. As the moisture decreased, the CO concentration of the coal sample with added hypophosphite began to decrease compared to the original coal sample, and this is because raising the temperature promoted the volatilization of free water inside the coal, while the inhibitor played a certain role in preventing coal oxidation, thereby reducing the concentration of CO. When the coal oxidation temperature was increased to 300 °C, as the concentration of sodium hypochlorite increased to 17%, the release rate of CO increased. When the concentration of sodium hypochlorite continued to increase to 20%, the release rate of CO decreased. This result indicates that suitable inhibitors under high-temperature conditions are beneficial for the inhibitory effect of hypophosphite on coal samples.
In Fig. 1, it can be seen that the coal sample with 20% concentration of sodium hypophosphite has the lowest CO release, and after 280 °C, the CO release exceeds that of 15% concentration of sodium hypophosphite. Comparing the coal samples with three different concentrations of sodium hypophosphite, the trend of CO release is basically consistent with that of the original coal sample, and it is lower than that of the original coal sample during the heating process. Among them, the best effect is achieved with 20% concentration of sodium hypophosphite.
Inhibitor concentration% | Resistance rate of sodium hypophosphite E/% |
---|---|
15 | 32.1304 |
17 | 17.2003 |
20 | 33.1778 |
As shown in Table 3, the best inhibitory effect is achieved when the concentration of sodium hypophosphite is 20%, mainly because the sodium hypophosphite inhibitor not only has strong moisture absorption and retention properties, but also forms a liquid film on the surface of the coal, greatly reducing the contact area between the coal sample and oxygen, lowering the temperature, and reducing the rate of coal oxidation reaction, achieving the goal of preventing coal oxidation. In the later stage, as the coal temperature rises, the evaporation of water exceeds the limit, and the liquid film formed in the coal body ruptures due to water loss, losing the function of oxygen isolation and inhibition cooling. Sodium hypophosphite also has strong reducibility, which can chemically react with active molecules and free radicals generated by coal at low temperatures, thereby interrupting the free radical reaction chain of coal oxidation reaction and preventing further oxidation and spontaneous combustion of coal.
Spectral peak number | Spectral peak position (cm−1) | Corresponding functional groups | Belong |
---|---|---|---|
1 | 694 | Out of plane deformation vibration of C–H substituted in benzene ring | Methylene plane vibration |
2 | 810–749 | C–H | Out of plane deformation vibration of C–H substituted in benzene ring |
3 | 1034–918 | — | Minerals and ash content |
4 | 1120 | C–O | C–O of phenols, alcohols, ethers, and esters |
5 | 1370 | –CH3 | Methyl shear vibration |
6 | 1438 | –CH2– | Methylene shear vibration |
7 | 1599 | C![]() |
C![]() |
8 | 1740 | C![]() |
Stretching vibration of fatty acid anhydride C![]() |
9 | 2852 | –CH2–CH3 | Symmetric stretching vibration of methylene and methyl groups |
10 | 2917 | –CH2–CH3 | Asymmetric stretching vibration of methylene and methyl groups in cyclic or aliphatic compounds |
11 | 3500 | –OH | The stretching vibration of OH bound hydroxyl groups |
12 | 3690–3618 | –OH | Alcohols, phenols – OH stretching vibration |
According to Fig. 2 and Table 4, the absorption peaks in the coal sample can be classified into three types: oxygen-containing functional groups, fatty hydrocarbons, and aromatic hydrocarbons. Peaks 4, 8, 11, and 12 in Table 4 belong to oxygen-containing functional groups. Peaks 11 and 12 are caused by the bending and stretching vibrations of free and bound hydroxyl groups in alcohols and phenols, which can be used to determine the presence of alcohols, phenols, and organic acids. The 8th absorption peak belongs to the fatty acid anhydride and is a unique absorption peak in coal, manifested as the stretching vibration of CO. The C–O vibration of phenols, alcohols, ethers, and esters in coal is manifested as the 4th absorption peak, while the absorbance of absorption peak 4 in the spectrum is only 0.012, indicating a high degree of coal metamorphism and easy oxidation of active functional groups.
Usually, the higher the absorbance of oxygen-containing functional groups in coal, the higher the content. The nature of oxygen-containing functional groups is active, and when they come into contact with oxygen in the air, they are easily attacked by oxygen and oxidized. The bridge bonds in coal molecules break to form unstable peroxides while releasing heat to further promote the decomposition reaction, leading to an increase in coal temperature and the occurrence of coal spontaneous combustion. The higher the degree of coal metamorphism, the lower the content of oxygen-containing functional groups on the coal surface, and the less likely oxidation reactions occur.
The absorption peaks of fatty hydrocarbons are represented by peaks 1, 5, 6, 9, and 10. Peak 10 belongs to the asymmetric stretching of methylene (–CH2) and methyl (–CH3), peak 9 belongs to the symmetric stretching vibration of methylene (–CH2) and methyl (–CH3), peak 6 belongs to the shear vibration of methylene (–CH2), peak 5 is the shear vibration of methyl (–CH3), and peak 1 is generated by the planar vibration of methylene.
Peaks 2 and 7 belong to the category of aromatic hydrocarbons, and the stretching vibration of the CC double bond in the skeleton structure of mononuclear aromatic hydrocarbons is shown as peak 7 in the spectrum. The absorption peak 2 comes from the deformation vibration of the C–H bond on the surface of aromatic hydrocarbons, and peak 3 does not correspond to any functional groups and belongs to minerals. Its absorbance is 0.016, indicating that the mineral content is not very high, that is, the ash content of kaolinite minerals and sulfur-containing substances in the coal sample is relatively low.
The comparison results of characteristic functional groups between the raw coal sample and the deactivated coal sample after constant temperature oxidation at 90–300 °C are shown in Fig. 3 and 4. For oxygen-containing functional groups, the peaks 11 and 12 attributed to –OH were significantly enhanced in the coal sample treated with inhibition at 90 °C compared to the original coal sample. The absorbance of the coal sample with added sodium hypophosphite increased by about two times, mainly due to the hydrophilicity of hypophosphite. During the low-temperature stage, hypophosphite absorbs water from the surrounding environment, and water molecules are polar molecules with larger dipole moment vibration amplitudes. Therefore, the intensity of the –OH spectrum peak was enhanced, and sodium hypophosphite exhibited a stronger intensity due to its presence of crystalline water. As the temperature increased to 300 °C, the absorption rate of water by hypophosphite became lower than the evaporation rate, and the water content began to decrease. At the same time, some highly active hydroxyl groups detach from the coal body and generate water after heating. Therefore, the intensity of the –OH spectrum peak gradually approaches consistency with the original coal sample as the temperature increased.
![]() | ||
Fig. 3 Fourier transform infrared spectra of coal sample oxidation in the low temperature range: 90 °C, 120 °C, and 150 °C. |
![]() | ||
Fig. 4 Fourier transform infrared spectra of coal sample oxidation in the high temperature range: 200 °C, 250 °C, and 300 °C. |
The peak intensity of peak 8 in the raw coal sample gradually increased with temperature, and the absorbance degree increased from 0.016 at 90 °C to 0.138 at 300 °C, indicating that more functional groups decompose to form CO. After adding sodium hypophosphite, the absorbance of C
O decreased. The reason may be that at high temperatures, sodium hypophosphite decomposes to produce hypophosphite ions, which have strong reducibility, resulting in a decrease in the peak intensity of some carbonyl groups in coal molecules.
Peak 4 belongs to C–O of phenols, alcohols, ethers, and esters, and the absorbance shows a trend of first increasing and then decreasing. At 150 °C, the absorbance reaches its maximum value of 0.322, indicating that some functional groups undergo cleavage to produce C–O. After adding sodium hypophosphite, peak 4 shows a similar trend to the original coal sample, and there is not much difference in C–O absorbance, indicating that the inhibitory effect of sodium hypophosphite on C–O bonds is not significant.
Peaks 5, 6, 9, and 10 belong to fatty hydrocarbons, mainly the stretching vibration of methyl and methylene groups. The spectral peak intensity in the raw coal sample is relatively low, and it shows a decreasing trend with increasing temperature, indicating that these functional groups easily undergo oxidation–reduction. After adding sodium hypophosphite, the intensity of spectral peaks in the coal sample decreased, with peaks 9 and 10, showing the most obvious. This is mainly due to the decomposition of hypophosphite, which prevents the oxidation process of methyl and methylene groups.
Peak 7 comes from the skeletal vibration of CC in the aromatic nucleus. With the increase in temperature of the raw coal sample, the absorbance of C–H in the periphery of aromatic hydrocarbons changes significantly, which may be due to the small bond energy of C–H, which is not strong and easy to break. After adding sodium hypophosphite, sodium hypophosphite gradually electrolyzes with the increase in temperature to produce hypophosphite ions, which take over the position of H in C–H of the benzene ring periphery and maintain the relatively stable structure of the benzene ring.
Peak 3 attributed to minerals has remained stable, with no significant difference in peak intensity between the original coal sample and the blocked coal sample.
In general, the low-temperature oxidation reaction of coal mainly goes through the following processes:32,38
(i) Coal is damaged by external forces, generating a large amount of free radicals that react with oxygen in the air, as shown in the following reaction equation:
![]() | (6) |
![]() | (7) |
![]() | (8) |
In the reaction equation, R is the alkyl group, R˙ – with electronic functional groups and ˙ – unpaired electrons.
(ii) The oxidation reaction of free radicals is an exothermic reaction, providing conditions for further reaction of peroxide free radicals. Different free radical peroxides have different reactions, as shown in the following reaction equation:
![]() | (9) |
![]() | (10) |
![]() | (11) |
![]() | (12) |
(iii) As the free radical peroxide reaction proceeds, CO2 gas is generated, as shown in the following reaction equation:
![]() | (13) |
Fig. 5 shows the relationship curve between the absorption peak area intensity of oxygen-containing functional groups (–C–O) and fatty hydrocarbons (RCH3 and R2CH2) after peak fitting and temperature changes.
The content of RCH3 groups in the raw coal sample began to increase with the increase in temperature and showed a decreasing trend after 150 °C. After adding sodium hypophosphite, the content of RCH3 groups in the coal sample decreased to a certain extent. After 150 °C, the content of RCH3 groups in the coal sample with sodium hypophosphite added was similar to that of the original coal sample, but lower than that of the original coal sample. After 220 °C, the content of RCH3 groups in the coal sample with sodium hypophosphite added exceeded that of the original coal sample, indicating that the inhibitory effect of sodium hypophosphite on RCH3 groups has ended.
The content of R2CH2 groups in raw coal samples decreases with the increase in temperature, while the content of R2CH2 groups in coal samples with sodium hypophosphite added between 90 °C and 120 °C increases and is lower than that in raw coal samples. As the temperature increases, the difference in the R2CH2 group content between coal samples with added sodium hypophosphite and raw coal gradually decreases, indicating that the inhibitory effect of sodium hypophosphite on the R2CH2 group content gradually weakens with the increase in temperature. When the temperature approaches 250 °C, the R2CH2 group content of coal samples with added sodium hypophosphite exceeds that of raw coal samples, and the inhibitory effect of sodium hypophosphite on R2CH2 groups ends.
The content of –C–O in the raw coal sample shows an approximate trend of first increasing and then decreasing with the increase in temperature, reaching its peak at around 200 °C. After adding sodium hypophosphite, the content of –C–O in the coal sample shows a similar trend of change. At 150–200 °C, sodium hypophosphite is added to the coal sample. The content of C–O significantly decreased, and sodium hypophosphite had a certain inhibitory effect on C–O throughout the entire heating process.
The TG-DTG-DSC curve of the raw coal sample is shown in Fig. 6, and the corresponding characteristic temperature points of the coal sample are shown in Table 5. In the initial stage, as the temperature increases, the TG curve shows a slight but not very obvious increase, which ends at 43.2 °C. During this stage, the coal sample is mainly subjected to physical adsorption, and the increase in temperature increases the internal energy of the coal, accelerating the physical desorption process. Chemistry gradually dominates, and the pre-existing gases and gases produced by chemical reactions in the coal escape, resulting in a decrease in the weight of the coal. When the temperature increases to 59.1 °C, the lowest point appears on the DTG curve, which is the point of maximum weight loss rate. When the temperature increases to 191.2 °C, due to the high temperature, the amount of oxygen absorbed by the coal increases sharply. When the temperature reaches 206.3 °C, the cracking of large molecules in coal molecules accelerates, and the active groups require more oxygen. The oxygen adsorption rate reaches its maximum. When the coal temperature reaches 430.5 °C, the internal energy between coal molecules reaches the bond energy for breaking the benzene and aromatic ring structures, making it difficult to oxidize and break the relatively stable cyclic molecules in the low-temperature stage. The reaction between coal and oxygen is most intense at 480.8 °C. After 570.7 °C, the TG curve gradually slows down, indicating that the organic compounds composed of carbon, hydrogen, etc. in coal molecules are completely burned.
T1/°C | T2/°C | T3/°C | T4/°C | T5/°C | T6/°C | T7/°C |
---|---|---|---|---|---|---|
a T1: high adsorption temperature; T2: critical temperature; T3: dry cracking temperature; T4: growth rate temperature; T5: ignition temperature; T6: maximum weight loss rate temperature; T7: Burning temperature. | ||||||
43.2 | 59.1 | 191.2 | 226.3 | 430.5 | 520.8 | 570.7 |
Within the temperature range of 43.2–570.7 °C, sodium hypochlorite covers the surface of coal, preventing contact between coal and oxygen, thereby inhibiting the coal oxygen reaction. When the amount of flame retardant additives increases, the quality loss increases, even exceeding the quality loss of raw coal.39 When the temperature exceeds 430.5 °C, the coal sample enters the rapid combustion stage, leading to the decomposition and formation of gaseous products. The formation of gaseous products may dilute the oxygen concentration on the coal surface.40 Continuing to increase the temperature, when the temperature exceeds the decomposition temperature of the flame retardant, a small amount of heat energy will be released, and the mass loss will slightly increase. In addition, the released gas dilutes the oxygen concentration.41,42
Sample | Heating rate/(°C min−1) | Weight gain range/°C | Range of weightlessness/°C | Maximum weight loss/°C | Maximum weightlessness rate/(%/min) | Maximum hot spot/°C | Maximum heat loss/(mW mg−1) |
---|---|---|---|---|---|---|---|
Raw coal | 10 | 194–291 | 195–610 | 520 | 3.7863 | 543.29 | 14.28 |
20 | 217–305 | 209–675 | 597 | 5.896 | 608 | 22.26 | |
Add sodium hypophosphite coal sample | 10 | 224–279 | 213–680 | 593 | 6.858 | 569.52 | 14.01 |
20 | 242–288 | 234–693 | 580 | 3.7804 | 635.67 | 17.74 | |
Sample | Particle size/mesh | Weight gain range/°C | Weight loss range/°C | Maximum weight loss point/°C | Maximum weight loss rate/(%/min) | Maximum heat release point/°C | Maximum heat loss/(mW mg−1) |
Raw coal | 40–80 | 194–291 | 291–610 | 520 | 3.7863 | 543.29 | 14.28 |
150–200 | 156–287 | 287–688 | 458 | 5.4578 | 456.83 | 14.59 | |
Add sodium hypophosphite coal sample | 40–80 | 224–279 | 279–680 | 593 | 6.858 | 569.52 | 14.01 |
150–200 | 174–290 | 290–692 | 493 | 7.821 | 498.51 | 18.29 |
According to Fig. 7 and Table 6, it can be seen that different heating rates have a significant impact on the oxidation process of coal samples. After changing the heating rate, both the raw coal sample and the blocked coal sample show varying degrees of backward shift in the TG curve. When adding sodium hypophosphite to the coal sample, the maximum heat loss of the coal sample at a heating rate of 10 °C min−1 was basically the same as that of the original coal sample. However, the maximum heat loss at a heating rate of 20 °C min−1 decreased significantly. The maximum heat loss difference between the original coal sample at a heating rate of 10 °C min−1 and 20 °C min−1 was 7.98 mW mg−1. After adding sodium hypophosphite, the maximum heat loss difference of the coal sample at different heating rates was 3.71 mW mg−1.
In Fig. 8(a), 1 and 3 represent the TG curve and DTG curve of coal samples with a particle size of 40–80 mesh, and 2 and 4 represent the TG curve and DTG curve of coal samples with a particle size of 150–200 mesh, respectively. In Fig. 8(b), 1 and 2 represent the DSC curve and DDSC curve of coal samples with a particle size of 40–80 mesh, and 2 and 4 represent the DSC curve and DDSC curve of coal samples with a particle size of 150–200 mesh, respectively.
Fig. 8(c) and (d) intuitively reflect the trend of particle size variation with temperature. At the same heating rate, as the particle size increases, the thermal characteristic curves of both the raw coal sample and the coal sample with added hypophosphite shift backward, and the weight gain range decreases while the weight loss range expands. Under the same particle size, the maximum weight loss rate of coal samples with added sodium hypophosphite changed most significantly. With the increase in particle size, the maximum weight loss point in the raw coal sample shifted backward by 62 °C, and the maximum heat release point shifted backward by 86.46 °C. Compared with the same conditions of 150–200 mesh coal samples, the maximum heat loss is significantly increased. The main reason is that the increase in coal particle size greatly reduces the specific surface area of coal, resulting in a significant decrease in the contact area between coal and oxygen, reducing the oxidation reaction rate. The inhibitor reacts with the functional groups on the coal surface, further preventing coal oxidation, and the thermogravimetric curve shifts significantly backwards.
From Fig. 9, it can be seen that the activation energy of coal samples varies at different stages of the oxidation process. The activation energy increases continuously with the progress of the reaction. The activation energy of coal samples in the thermal decomposition stage is about twice that of the oxygen absorption weight gain stage. In the initial oxygen absorption weight gain stage, the addition of sodium hypophosphite increases the activation energy of coal samples by 6.72 kJ mol−1−1. As the reaction continues, the addition of sodium hypophosphite in the thermal decomposition stage increases the activation energy of coal samples by 12.07 kJ mol−1−1 compared to the original coal sample. At this stage, the inhibitory effect of sodium hypophosphite is most significant.
(1) The best inhibitory effect is achieved with a concentration of 20% sodium hypophosphite, and the higher the temperature, the more favorable the inhibition effect of hypophosphite.
(2) Sodium hypophosphite absorbs water from the surrounding environment during the low-temperature stage, and the intensity of the –OH spectrum peak increases. As the temperature increases, the water evaporates and the spectrum peak gradually decreases. The content of methyl and methylene groups in fatty hydrocarbons is relatively low. With the increase in temperature, the addition of sodium hypophosphite decomposes to produce H2PO2−, which combines with H+ in methyl and methylene to form weak acid hypophosphite. Preventing and delaying the oxidation process of methyl and methylene groups. The structure of CC in aromatic nuclei is relatively stable, and sodium hypophosphite has a significant early inhibition effect on the RCH3 and R2CH2 groups, and is effective throughout the inhibition of the oxygen-containing functional group C–O.
(3) As the heating rate and coal particle size increase, both the thermal characteristic curve and characteristic temperature show a backward shift. After adding sodium hypophosphite, the maximum heat loss of the coal sample at a heating rate of 10 °C min−1 was basically the same as that of the original coal sample. However, the maximum heat loss at a heating rate of 20 °C min−1 decreased significantly. The difference in maximum heat loss between the original coal samples at a heating rate of 10 °C min−1 and 20 °C min−1 was 7.98 mW mg−1.
(4) After adding sodium hypophosphite, the maximum heat loss of coal samples with a mesh size of 40–80 was not significantly different from that of the original coal sample, but significantly increased compared to coal samples with a mesh size of 150–200 under the same conditions.
(5) The activation energy during the oxidation process of coal samples was calculated, and the addition of sodium hypophosphite increased the activation energy of coal samples by 6.72 kJ mol−1.
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