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Modeling of Hydrogen Blending on the Leakage and Diffusion of Urban Buried Hydrogen-Enriched Natural Gas Pipeline

Yue Su1, Jingfa Li2,*, Bo Yu2, Yanlin Zhao1, Dongxu Han2, Dongliang Sun2

1 Beijing Key Laboratory of Process Fluid Filtration and Separation, College of Mechanical and Transportation Engineering, China University of Petroleum (Beijing), Beijing, 102249, China
2 School of Mechanical Engineering & Hydrogen Energy Research Centre, Beijing Institute of Petrochemical Technology, Beijing, 102617, China

* Corresponding Author: Jingfa Li. Email: email

Computer Modeling in Engineering & Sciences 2023, 136(2), 1315-1337. https://doi.org/10.32604/cmes.2023.026035

Abstract

With the introduction of various carbon reduction policies around the world, hydrogen energy, as a kind of clean energy with zero carbon emission, has attracted much attention. The safe and economical transportation of hydrogen is of great significance to the development of hydrogen energy industries. Utilizing natural gas pipelines to transport hydrogen is considered to be an efficient and economical way. However, hydrogen has a higher risk of leakage due to its strong diffusion capacity and lower explosive limit than conventional natural gas. Therefore, it is of great significance to study the leakage and diffusion law of hydrogen-enriched natural gas (HENG) pipelines for the safe transportation of hydrogen energy. In this study, the leakage and diffusion characteristics of urban buried HENG pipelines are investigated numerically, and the dangerous degree of leakage is analyzed based on the time and area when the gas concentration reaches the lower explosive limit. The influences of hydrogen blending ratio (HBR), operating pressure, leakage hole size and direction, as well as soil type on the leakage and diffusion law of HENG are analyzed. Results show that the hydrogen mixing is not the key factor in increasing the degree of risk after gas leakage for urban buried HENG pipelines. When the HBR is 5%, 10%, 15% and 20%, the corresponding first dangerous time is 1053, 1041, 1019 and 998 s, respectively. This work is expected to provide a valuable reference for the safe operation and risk prevention of HENG pipelines in the future.

Graphical Abstract

Modeling of Hydrogen Blending on the Leakage and Diffusion of Urban Buried Hydrogen-Enriched Natural Gas Pipeline

Keywords


1  Introduction

As global warming is becoming serious, many countries have begun to introduce relevant policies to limit the emission of greenhouse gas. The development of clean energy has become an important issue facing the world’s energy industry [1,2]. As a kind of clean energy with zero carbon emission, hydrogen has attracted much attention in recent years [35]. However, the transportation of hydrogen seriously restricts its wide utilization. At present, the main delivery methods of hydrogen include road, rail, pipelines and ocean transportation in the form of gaseous hydrogen, cryogenic liquid hydrogen, and solid or liquid hydrogen carriers [611]. Among these methods, pipeline transportation is generally viewed as an effective way to achieve the large-scale and long-distance delivery of hydrogen. However, due to the flammable and explosive properties of hydrogen, some safety issues of hydrogen pipeline transportation must be considered.

There are two common ways for hydrogen delivery through pipelines, one is the pure hydrogen pipelines, and the other is mixing hydrogen into natural gas pipelines [12,13]. Considering the cost of the above two methods, the latter one that is blending a certain proportion of hydrogen into natural gas is a good choice in the transition period of hydrogen energy industry [14]. Transporting the hydrogen-enriched natural gas (HENG) to downstream users through existing natural gas pipelines can save the cost of new pipelines and related equipment [15,16]. However, the mixing of hydrogen can affect the mechanical properties of pipeline steels. For example, the welds can be subjected to hydrogen degradation and the various pipeline defects can be places of hydrogen accumulation which leads to hydrogen embrittlement of the pipe wall [1725]. Compared with natural gas, hydrogen has a wider explosive limit, larger diffusion coefficient and lower ignition energy, which is more prone to explosion accidents once leakage occurs. Therefore, attention must be paid to the safe operation of HENG pipelines.

In recent years, there have been many studies on the risk assessment of oil and gas pipelines [26,27], among which pipeline leakage is one of the most critical research hotspots. Many scholars have carried out experimental studies on the leakage and diffusion of natural gas pipelines [2830], in which the high-pressure gas cylinders were used to mimic the leakage process of natural gas pipelines and the sensors were placed in the soil to detect the leakage gas concentration. For example, Hideki et al. [28] conducted a full-scale experiment on buried natural gas pipeline leakage, it was found the molecular diffusion caused by the difference of gas density and concentration has a great influence on the gas leakage and diffusion, and the experimental results were in accord with Darcy’s law and Fick’s law. Bonnaud et al. [29] experimentally studied the influence of pipeline gas leakage on soil properties, and the effects of leakage surface, gas pressure, pipeline buried depth and water content on soil migration and crater formation were analyzed. Yan et al. [30] carried out leakage experiments with a mixture of 2.5% (volume fraction) of methane and 97.5% of air, and installed multiple combustible gas sensors around the leakage hole to monitor the variation of gas concentration around the soil over time.

With the development of computer technology, many scholars used numerical simulation methods to investigate the leakage law of buried natural gas pipelines and obtained abundant research results [3134]. Compared with experimental study, the numerical simulation possesses the advantages of safety, high efficiency and flexible variable control, which is easier to analyze the law of gas leakage and diffusion under different working conditions. For instance, Wang et al. [31] adopted ANSYS Fluent to simulate the leakage process of buried natural gas pipelines, and analyzed the influence of different pipeline internal pressures, leakage hole sizes, leakage direction, soil properties and pipelines buried depth on the leakage characteristics. Results showed that the leakage hole size, leakage direction and internal pressure are the key factors affecting the leakage and diffusion processes. Amir et al. [32] established an accurate formula for calculation of leakage flow according to simulation results, which illustrated that the relationship between gas leakage flow and pipeline pressure, leakage hole size and the ratio of leakage hole size to pipeline diameter was linear, second-order and fourth-order, respectively, and the error between mathematical model and simulation results was within 7%. Javad et al. [33] adopted finite element methods to simulate the leakage process of buried natural gas pipelines, in which the soil anisotropy was taken into account and the water content of each soil layer was supposed to be variable. The influence of soil mechanical and hydraulic properties on gas diffusion was analyzed, and the relationship between leakage flow rate and pipeline pressure and leakage hole diameter was derived. Liu et al. [34] established a mathematical model to estimate the leakage rate of buried natural gas leakage through experiments and CFD simulation. From the above analysis, it can be seen that scholars have used different numerical methods or established a series of models to describe and study the leakage process of natural gas, including the detection and positioning of leakage points [35,36] and the calculation of leakage flow [37,38], etc.

Although there are a lot of studies focusing on the leakage of buried natural gas pipelines, the research on the leakage of HENG pipelines is still rarely reported in the literature. Compared with traditional natural gas pipelines, HENG pipelines are more prone to leakage risk due to the embrittlement effect of hydrogen on pipeline steels. In addition, hydrogen has the characteristics of low explosive limit, high flame temperature and fast flame propagation speed, so once an explosion occurs, its destructive power will be far more than that of traditional natural gas. Therefore, it is of great significance to study the leakage and diffusion of HENG to ensure the safe transportation of hydrogen energy. In this study, the risk increase caused by the blending of hydrogen was quantitatively analyzed by using parameters, such as dangerous time and dangerous distance, which makes up the gap in the safety of hydrogen transportation in pipelines at present. As urban gas pipelines are usually located in areas with high population density, once the leakage occurs, it will cause more serious consequences. Thus, in this study, the urban buried HENG pipelines are taken as the research object. Compared with long-distance pipelines, urban natural gas pipelines are usually characterized by small diameters and low pressure.

2  Numerical Models

2.1 Physical Model

This study mainly focuses on the common small hole leakage of buried pipelines, in which the leakage and diffusion processes of HENG in the soil are considered, and the leakage and diffusion of gas in the air after spilling from the soil are ignored. The reason is that the urban natural gas pipelines are generally laid under roads. As roads are generally covered with asphalt, the leakage gas is usually hard to escape from the ground surface in large quantities. Moreover, due to the strong diffusion effect of hydrogen, the leakage gas generally diffuses into the atmosphere quickly, and it is difficult to be accumulated in air. Therefore, the diffusion process of HENG in air is not the focus in this work. As shown in Fig. 1, the leakage area is simplified into a rectangular area of 4 m × 4 m × 2.5 m. The pipeline is located in the center of the area, the diameter and depth of the pipeline are 100 and 1.5 m, respectively, and the leakage hole is a circular hole located in the center of the pipeline.

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Figure 1: Schematic diagram of the physical model

2.2 Mathematical Model

The following hypotheses are made to simplify the model and calculation: (1) The leakage gas mixture is an ideal gas, the heat transfer between gas and soil is ignored and only the mass transfer is considered; (2) The soil is isotropic and evenly distributed, and the soil structure does not change during the gas leakage process; (3) The operating pressure of the pipeline is constant during the gas leakage process; (4) There is no moisture in the soil, and the soil pore is fully filled with air.

Based on above assumptions, the leakage mathematical model of urban buried HENG pipelines includes mass conservation equation, momentum conservation equation, species transport equation and turbulence model.

(1)   Mass conservation equation,

ϕρt+(ρu)=0(1)

where ϕ is the soil porosity; ρ is the mixed gas density, kg/m3; u is the gas flow velocity, m/s; t is the time, s.

(2)   Momentum conservation equation [39],

ϕρuit+ρϕ2(ui)ui=p+μϕ2ui+ϕρg+Si(2)

where p is the pressure, Pa; μ is the dynamic viscosity, Pas; g is the gravitational acceleration, m/s2; Si is the source term, which can be expressed by below formula in porous media,

Si=(j=13Dijμuj+j=13Cij12ρ|u|uj)(3)

where the first term at the right-hand side of the equation is the viscous loss term, and the second term denotes the inertia loss term. Dij and Cij are the specified matrices.

For simple and uniform porous media, Eq. (3) can be simplified as,

Si=(1aμui+C212ρ|u|ui)(4)

where 1/a is the viscous resistance coefficient, 1/m2; C2 is the inertial resistance coefficient, 1/m.

To obtain the 1/a and the C2 in Eq. (4), the Ergun equation should be solved simultaneously [40]. Ergun equation is a semi-empirical formula applicable to a wide range of Reynolds number and a variety of filler, which can be written as,

|Δp|L=150μDp2(1ϕ)2ϕ3u+1.75ρDp(1ϕ)ϕ3u2(5)

where Dp is the average diameter of porous medium particles, mm; The formulas for calculating the resistance coefficient and the inertial resistance coefficient are described by,

1a=150Dp2(1ϕ)2ϕ3(6)

C2=3.5DP(1ϕ)ϕ3(7)

The leakage and diffusion of HENG is a multi-component fluid flow process, for the mass transfer process, it can be described by the species transport equation.

(3)   Species transport equation,

ϕt(ρc)+(ρuc)=(ρDc)(8)

where c is the mass concentration of gas; D is the diffusion coefficient, m2/s.

The process of gas leakage from the pipeline at a certain pressure can be regarded as a high-speed jet. Thus, the k-ε model is used to describe the turbulence process in this study.

(4)   The k-ε turbulence model,

t(ρk)+xi(ρkui)=xj[(μ+μtσk)kxj]+GK+GbρεYM+Sk(9)

t(ρε)+xi(ρεui)=xj[(μ+μtσε)εxj]+C1εεk(GK+C3εGb)C2ερε2k+Sε(10)

where GK, Gb and YM are turbulence parameters; the constants C1ε = 1.44, C2ε = 1.92, σk = 1.0 and σε = 1.3.

3  Numerical Methods

3.1 Mesh Generation

In this study, the ICEM 2020R1 is used to discretize the computational domain of the buried pipeline. The structured grid is adopted in this study, which has better computational efficiency and grid quality than unstructured grids. In addition, an O-grid mesh is used in the area of leakage hole and the pipeline cross section to better deal with the irregular geometry [41], and the fine mesh is adopted at the leakage hole, as shown in Fig. 2.

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Figure 2: Schematic diagram of meshing

3.2 Boundary Conditions and Solution Methods

In ANSYS Fluent software, the setting of boundary conditions is shown in Table 1. At the initial moment, the soil pore is considered to be fully filled with air, and the initial leakage rate and concentration of HENG are both set as 0 in soil, and the initial pressure is set as the atmospheric pressure.

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The finite volume method is used to discretize the governing equations, and the pressure and velocity coupling is handled with SIMPLE algorithm (Semi-Implicit Method for Pressure-Linked Equation). The selected models and discrete schemes are shown in Table 2.

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3.3 Monitoring Points

To quantitatively analyze the concentration variation of leaked HENG around the soil in the leakage and diffusion processes of pipeline, 10 monitoring points are set around the leakage hole. The coordinate origin is located in the center of the whole computational domain, and the location and the distribution of monitoring points (red points) are presented in Table 3 and Fig. 3, respectively.

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Figure 3: Distribution of monitoring points

3.4 Case Parameter Setting

To analyze the effects of influencing factors such as pipeline operating pressure, HBR, soil type, leakage hole diameter and leakage direction on the leakage and diffusion law of HENG, 13 groups of numerical cases are designed and presented in Table 4.

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4  Model Validation

4.1 Validation of Grid-Independent Solution

The grid number has an important influence on calculation results. Generally sparse meshes cannot guarantee high numerical accuracy, while too fine meshes can increase the computational burden. To obtain grid-independent solutions, the leakage gas concentration at P1 point is monitored in four grid numbers of 132060, 180435, 261030 and 321694, as shown in Fig. 4. It can be seen that with the increase of grid number, the curves of monitored gas concentration with leakage time are getting closer with each other. When the grid number of 261030 is used, the calculation result is almost the same as that of 321694, thus 261030 grids are adopted in this study.

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Figure 4: Validation of grid-independent solution

4.2 Validation of Mathematical Model

Yan et al. [30] conducted a concentration detection experiment of gas leakage from a buried pipeline in 2015, which was carried out in a 5 m × 5 m × 3 m earthen tank. Gas concentration sensors were installed in multiple positions inside the earthen tank to detect the concentration of leakage gas. To validate the mathematical model established in this study, the numerical simulation is conducted to mimic the experiment. The comparison between experimental data and simulation results under the same condition is shown in Fig. 5.

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Figure 5: Model validation by experiment

It is worth noting that in this experiment, 2.5% (volume fraction) methane and 97.5% air were mixed to ensure experimental safety, and only methane concentration was detected. As the volume fraction of methane is low, the concentration variation can only be observed after a relatively long experiment time, as shown in Fig. 5 that the methane concentration is only about 0.8% at t = 6000 s. It is also obvious to see that the predicted methane concentration by the established model in this study agrees well with the methane concentration measured in Yan’s experiment, indicating that the established mathematical model is reliable.

5  Analysis of Leakage and Diffusion Processes

5.1 Leakage and Diffusion Processes

In this part, firstly the case 2 is taken as an example to show the variation of HENG concentration over time in leakage and diffusion processes through 2D slices, as shown in Fig. 6. The slice is located at the center of the computational domain and is parallel to the x and y axes, respectively. As can be seen from Fig. 6, at the beginning of leakage process, the leakage gas diffuses into soil under the influence of pressure and concentration difference, and the concentration of leakage gas around the leakage point increases rapidly, and the whole leakage and diffusion area shows a spherical distribution. It can also be noted that there exists a high concentration area (red area with volume fraction > 0.95) around the leakage hole. The size of high concentration area increases significantly within t = 40 min after the leakage occurs, and changes slightly after 40 min. There is also risk in the periphery of the spill area (the light blue part with volume fraction > 0.05), the leakage gas concentration in this area is larger than the lower explosive limit (LEL) of pure methane, and thus it is also larger than the LEL of HENG. The area continues to increase with the leakage time and the dangerous area spreads to the surface at t = 20 min, and the whole computational domain reaches the dangerous concentration at t = 80 min.

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Figure 6: Distribution of leakage gas concentration around soil at different leakage time

Fig. 7 demonstrates the streamline of the leakage gas flow at t = 80 min. Due to the isotropy of soil, the streamline of the leakage gas is uniform and stable, and the leakage gas flows out perpendicular to the boundary. After the pipeline leakage, the HENG will spread evenly around. At the boundary, the gas flows freely and the streamlines are almost perpendicular to the soil boundary.

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Figure 7: Streamlines distribution of leakage gas on the slices

5.2 Variation of Leakage Gas Concentration at Different Positions

Fig. 8 shows the concentration change of leakage gas measured at 10 monitoring points in case 2 with time. It can be seen that the location closer to the leakage hole has a higher gas concentration, and the time for the leakage gas concentration to reach equilibrium is much shorter. It takes about 2000 s for the concentration of leakage gas measured at P1 to reach equilibrium and stabilize at about 98%, and the other monitoring points will take much longer time to reach an equilibrium state. Because the diffusion of leakage gas is uniform, the variation trend of leakage gas concentration along x, y, and z directions is basically the same.

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Figure 8: Variation of leakage gas concentration at monitoring points over time

6  Analysis of Leakage Consequence

To quantitatively describe the degree of risk of flammable gas leakage and diffusion in soil, Bu et al. [42] defined three parameters: the first dangerous time (FDT), the farthest dangerous range (FDR) and the ground dangerous range (GDR). Wherein, FDT represents the time required for the gas concentration at the ground surface directly above the leakage hole to reach the LEL. At this time, once there is an ignition source at the ground surface, the leakage gas will be ignited and cause explosion risk. FDR denotes the farthest distance that the gas cloud with a concentration above the LEL can diffuse along the pipeline. GDR stands for the maximum extent that the gas cloud at the ground surface can diffuse. It is obvious that both FDR and GDR are time-dependent parameters.

6.1 Analysis of Leakage Consequence under Different HBRs

Hydrogen blending ratio (HBR) has significant impacts on the leakage and diffusion of HENG. However, the determination of HBR is restricted by many factors and the upper limit of HBR is different in various countries [43]. In this study, the volume fraction (also mole fraction) of 20% is taken as the upper limit of HBR. Taking cases 1∼4 as examples, the leakage and diffusion of pipeline when HBR is 5%, 10%, 15% and 20% is studied, respectively.

To analyze the influence of HBR on leakage risk, the Le Chatelier law [44,45] expressed by Eq. (11) is applied to calculate the explosive limit of HENG under different HBRs. The calculation results are shown in Table 5.

1LELmix=yiLELi(11)

where LELmix is the LEL of mixed gas; LELi is the LEL of gas component i; yi is the volume fraction of gas component i.

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Since the monitoring point P4 is at the ground surface and directly above the leakage hole of the pipeline, the leakage time of P4 when the concentration of mixed gas reaches the LEL is FDT. Fig. 9 shows the concentration variation of methane, hydrogen and mixed gas with time under different HBRs. It can be seen that when the HBR is 5%, 10%, 15% and 20%, the corresponding FDT is 1053, 1041, 1019 and 998 s, respectively. The reason can be attributed to that the increase of HBR leads to the decrease of LEL of mixed gas, and the mixed gas concentration at P4 remains unchanged under the same pipeline pressure, thus the FDT is shortened. Therefore, the increase of HBR will lead to the increase of explosion risk after leakage diffusion, which is another key factor limiting HBR after the embrittlement of pipelines and the deterioration of ignition performance of the terminal stove.

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Figure 9: Variation of mixed gas concentration at P4 under different HBRs

Tables 6 and 7 display the FDR and GDR at different HBRs and leakage time. It can be clearly seen that the FDR and GDR increase with the rise of the HBR and leakage time. There are two main reasons for this phenomenon. First, the increase of HBR leads to the decrease of LEL, and the dangerous concentration can be reached at a relatively low concentration of mixed gas. Second, the diffusion of hydrogen in the soil is stronger, and its diffusion range is larger at the same time. These two reasons aggravate the development of combustible gas cloud, resulting in the increase of FDR and GDR.

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6.2 Analysis of Leakage Consequence under Different Operating Pressures

In this part, the consequences of HENG leakage under different pipeline operating pressures are analyzed by cases 2 (0.1 MPa), 5 (0.2 MPa) and 6 (0.3 MPa). Fig. 10 shows the change of leakage gas concentration with time under different pipeline operating pressures, and depicts the FDT under different pressures. As can be seen from Fig. 10, when the operating pressure is 0.1, 0.2 and 0.3 MPa, the corresponding FDT is 1041, 498 and 361 s, respectively. The increase in pipeline operating pressure will increase the gas leakage rate, and the gas diffusion rate in the soil will also be faster, so the LEL is reached in a shorter time. Tables 8 and 9 respectively present the FDR and GDR in the leakage process under different pipeline operating pressures and leakage time. As the simulated computational domain is limited, the value larger than 4 m is marked as “> 4 m” in these two tables. It can be observed that both FDR and GDR increase with the rise of pipeline operating pressure at any time. The main reason lies in that with the increase of pipeline operating pressure, the gas leakage rate will increase significantly, resulting in the increase of gas cloud diffusion area at the same time.

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Figure 10: Variation of mixed gas concentration at P4 under different pipeline operating pressures

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6.3 Analysis of Leakage Consequence under Different Leakage Hole Diameters

Taking cases 2, 7, 8 and 9 as examples, the leakage consequences of HENG with leakage hole diameters of 10, 20, 30 and 40 mm respectively are analyzed and discussed in this part. Fig. 11 shows the change of mixed gas concentration with time under different diameters of leakage hole. It can be seen that when the diameter of leakage hole is 10, 20, 30 and 40 mm, the corresponding FDT is 4981, 1876, 1041 and 618 s, respectively. Under the same pipeline pressure, the increase of leakage hole size will increase the leakage flow rate, which leads to the decrease of FDT at P4. Tables 10 and 11 respectively present the FDR and GDR values in the leakage process. It is found that both the FDR and GDR increase with the rise of the leakage hole diameter and leakage time. This is because that the increase of the leakage hole diameter can lead to the increase of the leakage flow, thus the gas cloud of the leakage gas increases at the same time, and both FDR and GDR increase.

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Figure 11: Variation of mixed gas concentration at P4 under different leakage hole diameters

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6.4 Analysis of Leakage Consequence under Different Leakage Directions

In this part, the influence of leakage direction on the leakage consequence of HENG is analyzed by cases 2, 10 and 11, where the leakage hole is located directly above, on the horizontal side and directly below the pipeline, respectively. Fig. 12 shows the distribution of mixed gas concentration in x-z plane of the three cases at the leakage time 30 min.

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Figure 12: Distribution of mixed gas concentration under different leakage directions

Fig. 13 demonstrates the change of leakage gas concentration detected at monitoring point P4 in cases 2, 10 and 11 with time. It is found that when the leakage hole is located directly above, horizontally and directly below the pipeline, the corresponding FDT is 1041, 1442 and 1558 s, respectively. Tables 12 and 13 present the FDR and GDR values under different leakage directions. It indicates that the FDR value is the largest when the leakage hole is located on the horizontal side of pipeline. Because when the leakage hole is located on the horizontal side, the diffusion of leakage gas along the pipeline will be intensified. For GDR, the value is the largest when the leakage hole is vertically upward, this is because the leakage gas can diffuse quickly to the ground surface to form gas clouds.

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Figure 13: Variation of mixed gas concentration at P4 under different leakage directions

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6.5 Analysis of Leakage Consequence under Different Soil Types

Taking cases 2, 12 and 13 as examples, the influence of soil type on the consequences of HENG leakage is analyzed. First, according to the particle diameter and porosity of soil, the viscous resistance coefficient and inertial resistance coefficient are calculated by using Eqs. (6) and (7), as shown in Table 14.

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Fig. 14 shows the change of leakage gas concentration monitored at P4 point in cases 12 and 13 with time. The analysis shows the corresponding FDT of sand, loam and clay is 157, 1041 and 69062 s, respectively. The soil type has great influences on gas leakage and diffusion processes. There exists remarkable difference in FDT between different soil types, for instance, the difference between the FDT of sand and clay is up to two orders of magnitude.

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Figure 14: Variation of mixed gas concentration at P4 under different soil types

Table 15 presents FDR values in the leakage process under different soil types. It can be observed that FDR value meets the relationship of sand > loam > clay at different times. At t = 5 min the FDR of sand is larger than the size of computational domain. Table 16 shows GDR values in the leakage process under different soil types. It can be found that the HENG concentration at the ground surface of clay still fails to reach the LEL at t = 50 min. For sand, the GDR value exceeds the size of computational domain at t = 20 min.

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6.6 Comparison of Different Influencing Factors

Fig. 15 displays the comparison of FDT, FDR and GDR in the leakage process under different cases, in which the presented FDR and GDR values correspond to the values measured at t = 20 min. It is clearly seen among the influencing factors discussed in this study, the soil type has the greatest influence on the leakage and diffusion processes for urban buried HENG pipeline. The FDT value of clay is about 440 times larger than that of sand. In addition, the leakage hole diameter and pipeline operating pressure also have great influence on leakage and diffusion processes of urban buried HENG pipeline. The influence of leakage direction and HBR are relatively small. Especially the HBR has the weakest influence, and the differences of FDT, FDR and GDR at different HBRs are subtle.

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Figure 15: Analysis of leakage consequences under different calculation conditions

In summary, hydrogen has a wider explosive limit and is easier to diffuse than natural gas, which requires additional safety measures, including leakage monitoring equipment and upgraded ventilation systems to prevent explosions which may occur after gas leakage.

7  Conclusions

In this study, the leakage of urban buried HENG pipelines is investigated numerically, and the influences of HBR, pipeline operating pressure, the diameter of leakage hole, leakage direction and soil type on the leakage consequences are analyzed and discussed in detail. The concluding remarks of this work can be summarized as follows:

(1)   The HENG presents a spherical diffusion process when it leaks from urban buried pipelines. The gas concentration field around the leakage hole changes rapidly at the initial stage of the leakage, and then gradually becomes stable. The whole leakage area basically conforms to the fact that the closer to the leakage hole, the higher the leakage gas concentration is and the more stable it tends to be. Because of the strong diffusion effect of hydrogen, the increase of HBR will enlarge the whole gas cloud.

(2)   The severity of the leakage consequences for urban buried HENG pipeline is affected by multiple influencing factors, among which the soil type is the most critical factor. For clay and sand, the FDT difference is up to two orders of magnitude. The pipeline operating pressure and leakage hole diameter also influence leakage consequences obviously, but the leakage direction and HBR exert slight effects on the leakage and diffusion of urban buried HENG pipeline.

(3)   For natural gas pipelines, if the influence of hydrogen on pipeline mechanical properties is not considered, the analysis of FDT, FDR and GDR show the hydrogen blending is not the key factor in increasing the risk after urban buried pipeline leakage.

Funding Statement: This study is supported by the National Key R&D Program of China (No. 2021YFB4001602), the National Natural Science Foundation of China (No. 51904031) and the Award Cultivation Foundation from Beijing Institute of Petrochemical Technology (No. BIPTACF-002).

Conflicts of Interest: The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

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Cite This Article

APA Style
Su, Y., Li, J., Yu, B., Zhao, Y., Han, D. et al. (2023). Modeling of hydrogen blending on the leakage and diffusion of urban buried hydrogen-enriched natural gas pipeline. Computer Modeling in Engineering & Sciences, 136(2), 1315-1337. https://doi.org/10.32604/cmes.2023.026035
Vancouver Style
Su Y, Li J, Yu B, Zhao Y, Han D, Sun D. Modeling of hydrogen blending on the leakage and diffusion of urban buried hydrogen-enriched natural gas pipeline. Comput Model Eng Sci. 2023;136(2):1315-1337 https://doi.org/10.32604/cmes.2023.026035
IEEE Style
Y. Su, J. Li, B. Yu, Y. Zhao, D. Han, and D. Sun "Modeling of Hydrogen Blending on the Leakage and Diffusion of Urban Buried Hydrogen-Enriched Natural Gas Pipeline," Comput. Model. Eng. Sci., vol. 136, no. 2, pp. 1315-1337. 2023. https://doi.org/10.32604/cmes.2023.026035


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