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				<title level="a" type="main">Mathematical Modelling of Gas Admixtures Release, Dispersion and Explosion in Open Atmosphere</title>
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							<persName><forename type="first">Yurii</forename><surname>Skob</surname></persName>
							<email>y.skob@khai.edu</email>
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								<orgName type="institution">National Aerospace University &quot;Kharkiv Aviation Institute&quot;</orgName>
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									<addrLine>17, Chkalov st</addrLine>
									<postCode>61070</postCode>
									<settlement>Kharkiv</settlement>
									<country key="UA">Ukraine</country>
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							<persName><forename type="first">Sergiy</forename><surname>Yakovlev</surname></persName>
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								<orgName type="institution">National Aerospace University &quot;Kharkiv Aviation Institute&quot;</orgName>
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									<addrLine>17, Chkalov st</addrLine>
									<postCode>61070</postCode>
									<settlement>Kharkiv</settlement>
									<country key="UA">Ukraine</country>
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								<orgName type="department">Institute of Information Technology</orgName>
								<orgName type="institution">Lodz University of Technology</orgName>
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									<postCode>90-924</postCode>
									<settlement>Lodz, City</settlement>
									<country key="PL">Poland</country>
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							<persName><forename type="first">Oksana</forename><surname>Pichugina</surname></persName>
							<email>o.pichugina@khai.edu</email>
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								<orgName type="institution">National Aerospace University &quot;Kharkiv Aviation Institute&quot;</orgName>
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									<addrLine>17, Chkalov st</addrLine>
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									<country key="UA">Ukraine</country>
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							<persName><forename type="first">Mykola</forename><surname>Kalinichenko</surname></persName>
							<email>m.kalinichenko@khai.edu</email>
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								<orgName type="institution">National Aerospace University &quot;Kharkiv Aviation Institute&quot;</orgName>
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									<addrLine>17, Chkalov st</addrLine>
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									<country key="UA">Ukraine</country>
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							<persName><forename type="first">Kyryl</forename><surname>Korobchynskyi</surname></persName>
							<email>k.korobchinskiy@khai.edu</email>
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								<orgName type="institution">National Aerospace University &quot;Kharkiv Aviation Institute&quot;</orgName>
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									<addrLine>17, Chkalov st</addrLine>
									<postCode>61070</postCode>
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					<term>gas mixture, admixture release, evaporation, explosion pressure wave, overpressure, mass concentration, probit analysis, accident consequences 1 1707-843X (S. Yakovlev)</term>
					<term>0000-0002-7099-8967 (O. Pichugina)</term>
					<term>0000-0002-8685-065X (M. Kalinichenko)</term>
					<term>0000-0002-3676-6070 (K. Korobchynskyi)</term>
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<div xmlns="http://www.tei-c.org/ns/1.0"><p>The method of the numerical solution of a three-dimensional problem of atmospheric release, dispersion and explosion of gaseous admixtures is presented. It can be equally applied for gases of different densities, including hydrogen. The system of simplified Navier-Stocks equations received by truncation of viscous members (Euler equations with source members) is used to obtain a numerical solution. The algorithm is based on explicit finite-difference Godunov scheme of arbitrary parameters breakup disintegration. To validate the developed model and computer system comparisons of numerical calculations with the published experimental data on dispersion of methane and hydrocarbons explosions have been carried out. Computational experiments on evaporation and dispersion of spilled liquid hydrogen and released gaseous hydrogen at different wind speed values have been conducted. The largest mass concentrations of hydrogen between bottom and top limits of flame propagation and cloud borders have been determined. The problem of explosion of hydrogen-air cloud of the complex form generated by large-scale spillage of liquid hydrogen and instant release of gaseous hydrogen has been numerically solved at low wind speed. Shock-wave loadings affecting the buildings located on distance of 52 m from a hydrogen release place have been shown.</p></div>
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<div xmlns="http://www.tei-c.org/ns/1.0"><head n="1.">Introduction</head><p>Hydrogen is widely applied in the different industries. Particular danger of its application is conditioned by the large energy of combustion, fast transition from burning to detonation, and, as a consequence, powerful explosion of the cloud in the atmosphere after release. Hydrogen differs essentially from other explosive compressed gases and liquids, firstly, by very small density, and, secondly, by very low liquid stage temperature. The quantity of hydrogen participating in explosion is defined by conditions of its evaporation (in case of release and spillage in liquefied form), dispersion and mixing with air. These processes will be influenced by specified above properties of liquefied and compressed hydrogen <ref type="bibr" target="#b0">[1]</ref>. Spilled liquids evaporate from spillage surface mixing with fresh air and forming dangerous mixtures. These physical processes substantially depend on shape of the spill spot <ref type="bibr" target="#b1">[2]</ref>, environment conditions, especially, wind speed <ref type="bibr" target="#b2">[3]</ref>, earth surface relief <ref type="bibr" target="#b3">[4]</ref>.</p><p>Usually, accidental release of dangerous liquids takes place after malfunction of storage or transportation equipment (Figure <ref type="figure" target="#fig_0">1Figure</ref> 1Figure 1Figure 1). Released admixture mixes with fresh air and creates air-gas cloud with some gas concentration, and the mixture could explode. Accidental gas releases and could explosions cause significant damage to the environment and create such dangerous factors as shock-impulse loads on humans and building constructions <ref type="bibr" target="#b4">[5]</ref> in hazard zones, toxic inhalation dozes (if admixtures are toxic) <ref type="bibr" target="#b1">[2]</ref>, and thermal radiation dozes from high-temperature combustion products <ref type="bibr" target="#b5">[6]</ref> and fire flame fluxes <ref type="bibr" target="#b6">[7]</ref>. Safety experts need all the information about distribution of dangerous factors around accident epicenter in order to assess the consequences for environment and provide protection measures to mitigate them <ref type="bibr" target="#b7">[8]</ref> reaching acceptable risk levels and check if protection construction could withstand explosion loads without destruction <ref type="bibr" target="#b8">[9]</ref>. Mathematical modeling of physical processes during accidental release and explosion of combustible gases (Figure <ref type="figure" target="#fig_1">2</ref>), instead of full experiment, could significantly reduce the costs of risk assessment work. Atmospheric dispersion of gaseous admixtures is traditionally modeled under the assumption of Gaussian distribution of the admixture concentration and on the basis of corresponding analytical functional dependences <ref type="bibr" target="#b9">[10]</ref>. But for neutral, heavy and light gases only the partial solutions are obtained, and such important factors as relief and gas compressibility under explosion condition can not be taken into account. The most adequate description of the physical processes of dispersion of chemically reacting gases is possible only using the Navier-Stokes system of non-stationary equations for compressible gas <ref type="bibr" target="#b10">[11]</ref>. Currently, numerical simulation of turbulent flows is carried out by solving the Reynolds-Favreaveraged Navier-Stokes equations, supplemented by a model of turbulence <ref type="bibr" target="#b11">[12]</ref>. However, most turbulence models do not describe with an equal degree of adequacy the various types of flows that can appear <ref type="bibr">[13]</ref>. This is especially true for flows with intense flow breaks and/or large pressure and temperature gradients. That is why, more simple than Navier-Stokes equations model but sophisticated enough in order to take into account relief, flow compressibility, and to avoid difficulties to select adequate turbulence model is needed aiming to extract mass concentration admixture and overpressure distributions as hazardous risk factors.</p><p>In presented work an attempt to solve numerically a three-dimensional problem of the admixture dispersion in the atmosphere and explosion equally applied for different density gases (including hydrogen) have been made.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="2.">Mathematical model</head></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="2.1.">Model brief description</head><p>A mathematical model of the physical process of the emergency release and dispersion of a gas impurity into the atmosphere, its dispersion in the surface layer of the atmosphere with the formation of a gas-air mixture and its explosion allows us to obtain non-stationary fields of the mass concentration of the impurity and pressure in the accident zone. These distributions of hazardous parameters can be further used to calculate the fields of hazardous factors (excess pressure and impulse of the compression phase in the shock wave front) to assess the consequences of their impact on the environment (operating personnel and man-made facility structures) in order to develop recommendations for reducing the operation risks of high danger enterprises.</p><p>To evaluate the spacious distribution of hazardous admixture mass concentration during the release and dispersion processes the basic equations system of air-gas mixture movement in the near-Earth atmosphere layer is used based on Euler approach supplemented with admixture conservation equation. An instant explosion model is used to define overpressure fields and asses explosion consequences. Admixture mass concentration is controlled during the calculation process to localize the area where admixture concentration is within flammability limits, and in the moment of explosion air-gas mixture flow parameters are replaced on detonation parameters. After that explosion products concentration and pressure distributions are controlled to evaluate overpressure and impulse at the explosion wave front. This useful information can be used in future versions of the model to calculate human damage probability using probit analysis model.</p><p>The computational domain is a parallelepiped located in the right Cartesian coordinate system (Figure <ref type="figure" target="#fig_3">3</ref>). It is divided into spatial cells which dimensions are determined by the scale of the characteristic features of the area (surface roughness, objects dimensions).</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="2.2.">Basic equations</head><p>An adequate description of physical processes of nonreactive gas mixture with air and further admixture dissipation in the atmosphere (or enclosed ventilated premise) is possible only with the use of time-dependent Navier-Stocks equations for compressible gas. The limited resources of modern computers do not allow obtaining effectively the direct numerical solution of these equations. As a rule, numerical modeling of large space turbulent flows is carried out by solving of Reynolds-averaged Navier-Stocks equations <ref type="bibr" target="#b13">[14]</ref> added by turbulence model <ref type="bibr" target="#b14">[15]</ref>. However the majority of turbulence models do not describe with an identical degree of adequacy all various types of flows. It especially relates to flows with intensive stream separation and large-scale gradients of pressure and temperature. As a result of the flow structural analysis and decomposition of the full gas-dynamic mathematical model it is assumed that the convective mass exchange mainly influences on the process considered. Thus, for the description of processes of two-component gas mixture and dissipation it is enough to use the simplified Navier-Stocks equations received by the truncation of viscous members (Euler approach with source members).</p><p>The calculated space Ω is a parallelepiped located in the right-hand Cartesian system of coordinates (X, Y, Z) with the basis in plane XOZ (axis Y is directed opposite to the Earth's gravity). The calculated space is broken into spatial cells. The full system of the time-dependent equations describing three-dimensional two-component gas mixture flow looks like <ref type="bibr" target="#b15">[16]</ref>, <ref type="bibr" target="#b16">[17]</ref>, <ref type="bibr" target="#b17">[18]</ref>:</p><formula xml:id="formula_0">𝜕𝑎 ⃗ 𝜕𝑡 + 𝜕𝑏 ⃗⃗ 𝜕𝑥 + 𝜕𝑐 ⃗ 𝜕𝑦 + 𝜕𝑑 ⃗ 𝜕𝑧 = 𝜌𝑓 ⃗ ,<label>(1)</label></formula><p>where a, b, c, d, f represent the following vector-columns:</p><formula xml:id="formula_1">𝑎 ⃗ = [𝜌, 𝜌𝑢, 𝜌𝑣, 𝜌𝑤, 𝐸] 𝑇 ,<label>(2)</label></formula><formula xml:id="formula_2">𝑏 ⃗⃗ = [𝜌𝑢, 𝑃 + 𝜌𝑢 2 , 𝜌𝑢𝑣, 𝜌𝑢𝑤, (𝐸 + 𝑃)𝑢] 𝑇 , (<label>3</label></formula><formula xml:id="formula_3">) 𝑐 ⃗ = [𝜌𝑣, 𝜌𝑢𝑣, 𝑃 + 𝜌𝑣 2 , 𝜌𝑣𝑤, (𝐸 + 𝑃)𝑣] 𝑇 , (<label>4</label></formula><formula xml:id="formula_4">) 𝑑 ⃗ = [𝜌𝑤, 𝜌𝑢𝑤, 𝜌𝑣𝑤, 𝑃 + 𝜌𝑤 2 , (𝐸 + 𝑃)𝑤] 𝑇 , (<label>5</label></formula><formula xml:id="formula_5">) 𝑎 ⃗ = [0, 0, −𝑔, 0, −𝑔𝑣 + 𝑒 𝑠 𝜌 ⁄ ] 𝑇 ,<label>(6)</label></formula><p>where t represents time, u, v, w are the components of air speed vector, P,  -pressure and density, and E is full energy of a volume unit of gas mixture:</p><formula xml:id="formula_6">𝐸 = 𝜌 (𝑒 + 1 2 ⁄ (𝑢 2 + 𝑣 2 + 𝑤 2 )),<label>(7)</label></formula><p>where e -internal energy of gas mass unit; components of the vector 𝑓 ⃗ -projections of the distributed volumetric sources; g -gravitational acceleration; 𝑒 𝑠 -intensity of a thermal emission in gas volume unit as a result of chemical reaction.</p><p>If consider leaked and evaporated explosive admixture <ref type="bibr" target="#b18">[19]</ref> and combustion products as separate gases <ref type="bibr" target="#b19">[20]</ref>, the law of each admixture component transfer, taking into account a diffusion speed, looks like <ref type="bibr" target="#b20">[21]</ref>:</p><formula xml:id="formula_7">𝜕(𝜌𝑄) 𝜕𝑡 + 𝜕(𝜌𝑢𝑄) 𝜕𝑥 + 𝜕(𝜌𝑣𝑄) 𝜕𝑦 + 𝜕(𝜌𝑤𝑄) 𝜕𝑧 = 𝜌 𝑄 𝑡 + 𝜌 𝑄 𝑠 ,<label>(8)</label></formula><p>where Q -relative mass density of an admixture (the ratio of gaseous admixture substance density to the mixture density); 𝜌 𝑄 𝑡 -an admixture density change rate as a result of diffusion (according to Fick law <ref type="bibr" target="#b21">[22]</ref>, 𝜌 𝑄 𝑡 = 𝑑𝑖𝑣(𝜌𝑄 𝐷 𝑔𝑟𝑎𝑑𝑄), and the factor of diffusion 𝑄 𝐷 is defined according to Berljand <ref type="bibr" target="#b22">[23]</ref>); 𝜌 𝑄 𝑠 -an admixture density change rate as a result of chemical reaction.</p><p>The system of the equations (1, 8) is completed by the mixture component heat-transfer</p><p>properties equations <ref type="bibr" target="#b23">[24]</ref>. For ideal gas the value of e is related to the values of P and  of the mixture by the following dependence 𝑒 = 𝑃 ((𝑘 − 1)𝜌) ⁄ .</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="2.3.">Boundary conditions</head><p>It is assumed that the air flow quantity component of velocity does not surpass sound speed. Entry boundary conditions are set on the finite-difference cells surfaces through which atmospheric air enters. The approaching flow is defined by values of total enthalpy</p><formula xml:id="formula_8">𝐼 0 = 𝑘 𝑘 − 1 𝑃 𝜌 + + 1 2 ⁄ (𝑢 2 + 𝑣 2 + 𝑤 2 ),<label>(9)</label></formula><p>entropy function</p><formula xml:id="formula_9">𝑆 0 = 𝑃 𝜌 𝑘 ,<label>(10)</label></formula><p>flow velocity vector (angles 𝛼 𝑥 , 𝛼 𝑧 ), and relative admixture mass density Q (Q  1 if the gaseous admixture flows in). The entry flow parameters are defined by equations (3, 4) (if angles 𝛼 𝑥 , 𝛼 𝑧 are set) using "left" Riemannian invariant correlation <ref type="bibr" target="#b23">[24]</ref>. On impermeable computational cells' surfaces the "no passing" conditions are satisfied: 𝑞 𝑛 = 0 where 𝑛 ⃗⃗ is a vector of normal to considered surface. Exit boundary conditions are set on the computational cells surfaces through which the mixture flows out (except for the atmospheric pressure 𝑃 𝐴 , the "right" Riemannian invariant correlation <ref type="bibr" target="#b23">[24]</ref> is used).</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="2.4.">Initial conditions</head><p>At start time in all "gaseous" cells of the computational space the parameters of an ambient air are assigned. In cells, where the admixture cloud takes place, relative mass concentration of an admixture equals 1 (100%). In cells with hydrogen evaporation (or outflow) the law of admixture consumption variation is set.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="2.5.">Algorithm of the numerical solution</head><p>The vector equation ( <ref type="formula" target="#formula_0">1</ref>) is a consequence of the mass, impulse and energy conservation laws which can be presented in the integrated form for each calculated cell</p><formula xml:id="formula_10">𝜕 𝜕𝑡 ∭ 𝑎𝑑𝑉 𝑉 + ∯ 𝐴 ̂𝑑𝜎 𝜎 = ∭ 𝜌𝑓𝑑𝑉 𝑉 , (<label>11</label></formula><formula xml:id="formula_11">)</formula><p>where V is a volume of an elementary computational cell, 𝜎 ⃗-a limiting surface of the given cell which has an external normal vector 𝑛 ⃗⃗ (𝜎 ⃗ = 𝜎 𝑛 ⃗⃗)</p><formula xml:id="formula_12">) n σ (   = </formula><p>, 𝐴 ̂ -a tensor of the flow density of conservative variables 𝑎 ⃗ which columns are vectors b, c and d, accordingly.</p><p>The mixture component transfer law ( <ref type="formula" target="#formula_7">8</ref>) can be presented also in the integrated form for each computational cell:</p><formula xml:id="formula_13">𝜕 𝜕𝑡 ∭ 𝜌𝑄𝑑𝑉 𝑉 + ∯ 𝜌𝑄𝑞𝑑𝜎 𝜎 = ∭(𝜌 𝑄 𝑡 + 𝜌 𝑄 𝑠 )𝑑𝑉 𝑉 ,<label>(12)</label></formula><p>The equations <ref type="bibr" target="#b10">(11,</ref><ref type="bibr" target="#b11">12)</ref> suppose occurrence and existence of parameters break surfaces of two types: shock waves and tangential breaks. The functions, satisfying to the equations <ref type="bibr" target="#b10">(11,</ref><ref type="bibr" target="#b11">12)</ref>, can be considered as the gas dynamics equations generalized solutions. The use of integrated conservation laws as initial for construction of finite-difference equations provides the formation of breakup solutions without isolation of breaks.</p><p>The set of gas-dynamic parameters in all computational cells at the moment of time n t represents the known solution. Gas-dynamic parameters at the moment of time</p><formula xml:id="formula_14"> + = + n 1 n t t</formula><p>are calculated by means of explicit finite-difference approximations for equations <ref type="bibr" target="#b4">(5)</ref> according to Godunov method <ref type="bibr" target="#b23">[24]</ref>. At first stage continuous distribution of parameters is replaced with piecewise constant integral-averaged values in each computational cell. At the same time the borders of a cell represent unstable surfaces of arbitrary breakup which disintegrate to steady wave elements: a shock wave, a contact surface and a wave of rarefaction. For each such breakup the streams of mass, impulse and energy through sides of gas cells are defined. The stability of the finite-difference scheme is provided due to a choice of time step size.</p><p>On the basis of mathematical model the computer system of the engineering analysis of the gas-dynamic processes of release, mixture and dispersion was developed which is used in the research computer information system. It allows predicting an admixture concentration change in time and space in the calculated area and computing shock-wave parameters formed after detonation in the atmosphere during fuel-air mixture dispersion process with the use of personal computers for practically reasonable time.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="3.">Mathematical model validation</head><p>Since we did not possess hydrogen experimental data, we have used propane and methane experimental data to verify mathematical model and developed computer system.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="3.1.">Propane evaporation from a water surface</head><p>In order to verify the developed model for gaseous admixture dispersion in the atmosphere the comparison of the computation results with experimental data <ref type="bibr" target="#b24">[25]</ref> was conducted (Figure <ref type="figure" target="#fig_4">4Figure 4Figure 4</ref>). </p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="3.2.">Gas cloud explosions in the atmosphere</head><p>For validation of calculation model of atmospheric gas cloud explosions a comparison of calculated results with experimental data <ref type="bibr" target="#b25">[26]</ref> іs conducted (Figure <ref type="figure" target="#fig_6">5</ref>).</p><p>An explosion of a stoichiometric propane-air mix cloud was calculated at conditions of experiment: volume of the gas mixture cloud -1495 m 3 ; energy of explosion -4940 МJ. On the basis of these data initial conditions for calculation, pressure and temperature of combustion products in the cloud, have been defined: </p><formula xml:id="formula_15">𝑃 = 𝐸(𝑘 − 1) 𝑉 + 𝑃 𝐴 = 4940𝑒 6 (1.</formula><p>where V -volume of the gas mixture cloud; E -energy of explosion; k -adiabatic coefficient; PA -atmospheric pressure; mix -molar mass of the mixture; mix -mixture density; R -universal gas constant.</p><p>For obtaining parameters of gas detonation, more sophisticated models <ref type="bibr" target="#b26">[27]</ref> can be used to assess explosion hazards <ref type="bibr" target="#b27">[28]</ref>. In work <ref type="bibr" target="#b25">[26]</ref> on the basis of experiments of explosion of clouds of acetylene, propane and methane with air and propane and methane with oxygen the correlation dependence was received that allows to define the overpressure   <ref type="bibr" target="#b25">[26]</ref> and analitical correlation dependance <ref type="bibr" target="#b25">[26]</ref> In Figure <ref type="figure" target="#fig_6">5</ref> the results of numerical calculations are presented which well enough coincide with experimental data and with correlation dependence <ref type="bibr" target="#b25">[26]</ref>.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="4.">Numerical computations of hydrogen releases</head></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="4.1.">Release conditions</head><p>Processes of gaseous hydrogen release (spilled liquid hydrogen evaporation), hydrogen-air mixture formation, explosion and further dispersion of hydrogen-air cloud in the atmosphere (taking into account the movement of the air, gravity, presence of buildings, and thermodynamic gas properties) are considered. Usually, the evaluation of safety measures of a hydrogen fueling station is provided using physical modeling <ref type="bibr" target="#b29">[30]</ref>, and then quantitative risk assessment can be done <ref type="bibr" target="#b30">[31]</ref> to satisfy safety regulation documents <ref type="bibr" target="#b31">[32]</ref>.</p><p>Some possible scenarios at hydrogen dispensing station are modeled <ref type="bibr" target="#b28">[29]</ref>. The station has the large cryogenic hydrogen tank (5.7 m 3 ) that feeds three 12-cylinder packages in total amount 799.2 m 3 in which gaseous hydrogen is stored at ambient temperature. The hydrogen under pressure is dispensed to vehicles' tanks. The station is separated from residential area by three zones.</p><p>• The region in the immediate vicinity of the equipment to protect the personnel from small leaks.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head>•</head><p>An exclusion zone in the immediate area of the facility (23 m) to provide protection against unplanned minor releases of hydrogen.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head>•</head><p>An additional margin, as large as 53 m is necessary to protect against large potentially catastrophic release of hydrogen. The most dangerous scenarios from the potential catastrophe point of view have been numerically simulated using the created mathematical model and developed computer system.</p><p>1. Spillage from the tank of all volume of liquid hydrogen, consecutive evaporation of cold liquid, mixture of gaseous hydrogen with moving air and the further dispersion of a mix towards residential area.</p><p>2. Release of all volume of the gaseous hydrogen compressed under a high pressure from cylinders of distribution with formation of a cloud and its further dispersion in a stream of air.</p><p>3. Explosion of a hydrogen-air cloud that is formed as a result of evaporation of spilled liquid hydrogen or instant gaseous hydrogen release.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="4.2.">Spillage of liquid hydrogen</head><p>According to the scenario 1, numerical computations of an instant spillage of all volume of liquid hydrogen from the cryogenic tank of dispensing station with formation of a spillage pond with total area of 65.7 m 2 were conducted. Liquid hydrogen evaporation productivity was evaluated of 11.56 kg/sec <ref type="bibr" target="#b28">[29]</ref>. The wind blew with speeds of 1, 3 and 10 m/sec, and its direction was towards residential area. The calculation space has the following dimensions: the length along OZ axis -70 m, width (OX) -22 m, and height (OY) -20 m.</p><p>Hydrogen mass concentration distributions near the surface of the ground are presented on Figure <ref type="figure" target="#fig_7">6</ref>. With an increase in wind speed the rate of dispersion increased too (Figure <ref type="figure" target="#fig_8">7</ref>). According to comparison of hydrogen time-space concentration distributions at different wind conditions in the case of spilled liquid hydrogen its buoyancy is insignificant because of low vapor temperature and, as a consequence, small difference between densities of hydrogen and air. Mass concentration fields are very important data for safety experts to carry out following risk assessment. They can evaluate the total amount of hydrogen mass that potentially could explode (mass concentration has to be between flammability limits). This parameter characterizes the power of the explosion and the hazardous area where overpressure exceeds acceptable safe levels. </p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="4.3.">Dispersion of gaseous hydrogen cloud</head><p>An instant release of all gaseous hydrogen from a package of dispensing high-pressure cylinders with the formation of a cloud in volume 799.2 m 3 have been numerically simulated according to the scenario 2. According to results of numerical experiments, buoyancy of hydrogen is essential only at low wind speeds (Figure <ref type="figure" target="#fig_9">8</ref>). It should be noted that the fields of mass concentration of flammable impurities significantly depend not only on wind speed, but also on the presence of obstacles in the form of buildings in the actual space, which distort the flow velocity fields, which will subsequently affect the distribution of pressures in the zone of emergency release and With an increase of wind speed the air flow prevents the cloud movement up pressing it to the ground. Calculation results are similar to the results of the physical experiment <ref type="bibr" target="#b32">[33]</ref> provided in the photographs of the hydrogen cloud plume, which arises as a result of evaporation from the liquid hydrogen spill spot under different wind conditions (Figure <ref type="figure" target="#fig_10">9</ref>). Obviously, if wind speed is greater then hydrogen buoyancy, hydrogen behaves as a neutral gas. Both in the case of spilled hydrogen dispersion and dispersion of instantly released gaseous hydrogen, the presence of construction facilities and residential buildings essentially affect flow symmetry decreasing transfer and mixing processes in the space before the buildings and accelerating these processes between constructions.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="4.4.">Explosion of hydrogen cloud</head><p>In computations on dispersion the dependence of hydrogen mass in the cloud between top and bottom concentration limits of flammability was determined (Figure <ref type="figure" target="#fig_11">10</ref>). The largest mass of hydrogen and, consequently, maximal explosion energy will be under low wind speed conditions. But, as evident from Figure <ref type="figure" target="#fig_11">10</ref>, a, an explosive cloud with less hydrogen mass and larger energy of explosion can be located closer to residential constructions. In case of instant release of compressed gaseous hydrogen, the cloud is compact enough (Fig. <ref type="figure" target="#fig_11">10, b</ref>) and it can be considered as spherical cloud. But, in case of presence of constant source of assigned productivity (hydrogen spillage evaporation), the hydrogen mixture that explodes according to the mathematical model occupies the space of complex shape (Figure <ref type="figure" target="#fig_12">11</ref>) in the calculated area. The air-gas mixture with mass concentration that is lower than bottom flammability limit does not explode because of lack of fuel component. If mass concentration is greater than top flammability limit, the mixture will not explode too because of lack of oxidant.  An increase of pressure takes place between residential constructions, as it would be expected. Overpressure affecting the walls of buildings (on the right side of the Figure <ref type="figure" target="#fig_13">12, a</ref>) is about 28 kPa that allows suggesting the possibility of serious destructions of residential buildings and industrial facilities threatening to health or even life of industrial object personnel and residential area inhabitants.</p></div>
<div xmlns="http://www.tei-c.org/ns/1.0"><head n="5.">Conclusions</head><p>The three-dimensional model of the release and explosion of gaseous admixtures in the atmosphere has been developed. The validation of the numerical results shows acceptable accuracy in comparison with known experimental data.</p><p>Numerical computations for dispersion of evaporated spilled liquid and instantly released gaseous hydrogen and for explosion of the hydrogen-air cloud generated during dispersion have been carried out.</p><p>Obtained results can be usually predicted at qualitative level but presented numerical computations have allowed making quantitative forecasting with no contradictory physical picture.</p><p>Numerical modelling of the harmful admixture dispersion in the atmosphere generated as a result of air-fuel mixture distribution in three-dimensional space with the use of developed computer information system is applicable to engineering calculations for different technological systems, including ones which work on liquefied and gaseous hydrogen.</p><p>Presented mathematical model can be used in more complex information system as a predictor of distribution of such a hazardous flow parameter as pressure during an accidental gas explosions. Calculated pressure field is an origin of such hazardous factors values as maximum overpressure and impulse of pressure phase at the front of the explosion wave which moves away from an accident epicenter and influences harmfully on humans and buildings. This information about the explosion wave can be used to evaluate distribution of damage probability and to assess the risks of dangerous industrial objects by safety experts.</p></div><figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_0"><head>Figure 1 :</head><label>1</label><figDesc>Figure 1: Typical accidental process development scheme</figDesc></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_1"><head>Figure 2 :</head><label>2</label><figDesc>Figure 2: Typical consequences assessment procedures scheme</figDesc></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_3"><head>Figure 3 :</head><label>3</label><figDesc>Figure 3: Calculation scheme: 1 -spill spot; 2 -ground surface; 3 -air wind vector; 4evaporation process; 5 -total evaporation rate; 6 -mixture; 7 -explosion products; 8overpressure explosion wave</figDesc><graphic coords="3,93.50,433.47,407.40,227.40" type="bitmap" /></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_4"><head>Figure 4 :</head><label>4</label><figDesc>Figure 4: The maximal propane concentrations: 1, 2 and 3 -computations, 4, 5 and 6 -experimental data [25] at heights 0.8, 1.4 and 2.3 m, accordingly The evaporation process of liquid propane from a spillage pond occupying the area of 256 m 2 was modeled at ambient air parameters: pressure 101325 Pa, temperature 291 K, wind speed 8.1 m/s. The propane evaporated with the consumption of 27.6 kg/sec and had the temperature 230 K in a gaseous stage. The calculated propane concentration distributions at heights 0.8, 1.4 and 2.3 m at the moment of time 450 sec from the evaporation start time in comparison with experimental gauging [25] are well enough conformed to experimental data.</figDesc><graphic coords="6,165.50,137.26,264.00,212.40" type="bitmap" /></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_5"><head>⁄</head><label></label><figDesc>f P  in the shock wave front from distance from an epicenter for the assigned energy of explosion: -dynamic radius; R -distance from an explosion epicenter; E -energy of explosion.</figDesc></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_6"><head>Figure 5 :</head><label>5</label><figDesc>Figure 5: Explosion waves parameters in comparison with experimental data<ref type="bibr" target="#b25">[26]</ref> and analitical correlation dependance<ref type="bibr" target="#b25">[26]</ref> </figDesc><graphic coords="7,105.20,160.99,384.60,255.60" type="bitmap" /></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_7"><head>Figure 6 :</head><label>6</label><figDesc>Figure 6: Numerical computations of spilled liquid hydrogen dispersion (wind speed 1 m/sec: a -the plane XOZ near the ground; b -the plane YOZ view</figDesc><graphic coords="8,103.10,421.18,388.80,320.40" type="bitmap" /></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_8"><head>Figure 7 :</head><label>7</label><figDesc>Figure 7: The maximum hydrogen concentration distribution along the OZ-direction for different wind speed conditions: a -evaporation from spill spot ; b -instant release of all the hydrogen amount</figDesc><graphic coords="9,80.00,149.38,435.00,164.40" type="bitmap" /></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_9"><head>Figure 8 :</head><label>8</label><figDesc>Figure 8: Hydrogen concentration distribution in 5 sec after release in planes XOZ and YOZ for different wind speed conditions: a, d -1 m/sec; b, e -3 m/sec; c, f -10 m/sec</figDesc><graphic coords="9,81.50,443.72,431.40,293.40" type="bitmap" /></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_10"><head>Figure 9 :</head><label>9</label><figDesc>Figure 9: Liquid hydrogen evaporation from the spill spot surface (physical experiment [33]) for different wind speed: a -1.6 m/sec; b -3.8 m/sec; c -6.3 m/sec</figDesc><graphic coords="10,107.00,188.06,380.40,112.20" type="bitmap" /></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_11"><head>Figure 10 :</head><label>10</label><figDesc>Figure 10: The history of total mass of gasious hydrogen which mass concentration is within flammability limits (the air-hydrogen mixture could explode) during the dispersion process for different wind speed conditions : a -evaporation after spillage; b -after instant gas release</figDesc><graphic coords="10,72.00,507.28,451.00,152.70" type="bitmap" /></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_12"><head>Figure 11 :</head><label>11</label><figDesc>Figure 11: Mass concentration distribution of hydrogen within flammability boundaries in YOZ plane (wind speed makes up 1 m/sec)The numerical results of blast wave parameters for the wind speed option 1 m/sec at detonation of the cloud generated after an instant gaseous hydrogen release are presented in Figure12. The mass of hydrogen in the cloud equals 63 kg at the moment of explosion.</figDesc><graphic coords="11,113.60,110.69,367.80,171.60" type="bitmap" /></figure>
<figure xmlns="http://www.tei-c.org/ns/1.0" xml:id="fig_13"><head>Figure 12 :</head><label>12</label><figDesc>Figure 12: Pressure distribution after hydrogen explosion: a -near the ground; b -in YOZ plane</figDesc><graphic coords="11,91.25,359.66,412.20,331.80" type="bitmap" /></figure>
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