3.2. Determination of the Parameters of the General Heat Conduction Model
It is also worthwhile to examine the operation of the No-Sway Threshold in the case of an inhomogeneous system. In our case, by an inhomogeneous system we mean a system in which the system is not composed solely of one type of identical material but is formed by at least two media with different material properties. In this example, among the three examined material elements, let the central element be simple rock salt, while the two boundary material elements are silver. (Silver was chosen as the boundary element because silver is known to be one of the chemical elements with the best heat conduction properties.) The physical parameters of rock salt used differ significantly from those of silver, which thus highlights more clearly the effects observed in inhomogeneity. The parameter values applied in the calculations are listed in
Table 1.
The resultant heat conduction of two elements with different thermal conductivities can be expressed according to Equation (
10), where
and
are, in this order, the thermal conductivity coefficients of one and the other material element.
In the heat conduction equation written for this case, the other parameters of the thermal diffusivity coefficient (
K)—the heat capacity and the density—were substituted by the physical parameters of the examined material element. See Equation (
11) written for the one-, two-, and three-dimensional cases.
In the examined example, the initial temperature of the two boundary silver material elements is 24 °C, while the temperature of the central rock salt element is 18 °C. The determination of the conduction number (
K) close to the No-Sway Threshold in this case is more complicated and differs from the calculation formula already presented. With the calculation given in Equation (
11), under the parameters of step size 0.010 m and differentiation time 8.500 s, the conduction number of the central material element reaches the No-Sway Threshold.
When calculating the temporal variation in the temperature values, it can be observed that the target temperature is reached within (3·) time, whereas the target temperature should be reached within (1·) time for the temperature of the central material element at the vicinity of the No-Sway Threshold. This phenomenon shows that either the differentiation time can be further increased or the differentiation distance can be decreased.
For the two boundary material elements, under the parameters of step size 0.010 m and differentiation time 9.150 s, the conduction number reaches the No-Sway Threshold. When calculating the temporal temperature variations, it can be observed that the system is indeed stable, but the temperature values reach the target value in an oscillatory manner. Based on the results, it can be stated that the optimal value of the differentiation time must lie somewhere between 8.500 s and 9.150 s. For its precise determination, a generalization of Equation (
11) is required, that is, taking into account the differing physical parameters of the adjacent elements in the determination of the conduction number, in the following manner (see system of Equation (
12)):
The system of Equation (
12) expresses a general three-element one-dimensional heat conduction model. In this case, each material element possesses different material or physical properties. For better simplification, the thermal conduction number K can be decomposed into the thermal conductivity coefficient
between two neighboring elements and the expression “
A.” Here, “
A” represents the differentiation time and the differentiation distance, as well as the heat capacity and the mass density, in accordance with Equation (
12). In the following derivation, the goal is to determine a general formula of the thermal conduction number
K.
Let us assume that our case is a one-dimensional heat conduction model with three material elements. Each material element is of different material quality (here, silver, rock salt, and High-Density Polyethylene = HDPE). By this definition, their heat conduction, heat capacity, and density are also different. Based on the system of Equation (
12), the heat conduction occurring among them can be written. In
Figure 4 and
Figure 5, with the differentiation length and time parameters
= 0.010 m,
= 14 s, and
= 10.5 s, the temperatures of the elements were calculated.
In
Figure 4, it is shown that the temperature of the material element with identifier
decreases strictly monotonically to the target temperature (curve marked in red in
Figure 4). In the monotonicity of the function, there is an anomaly between time steps
t = 1 and
t = 3. The function curve of the temperature variation in the central element with identifier
X (marked in green) is not monotonic. Between the mentioned time steps
t = 1 and
t = 3, the temperature reaches a local maximum, after which the temperatures decrease; then, the direction of monotonicity changes, that is, the function curve begins to increase strictly monotonically. A similar change characterizes the material element with identifier
(blue curve in
Figure 4), only there the temperature begins to decrease earlier. It can be stated that, with these
and
differentiation parameter settings, the system is indeed stable, but it does not meet the qualitative mathematical requirements imposed by the No-Sway Threshold in connection with temperature variations, in other words, the requirement that the function of temperature variation should be monotonic in all cases.
In
Figure 5, the function curve of temperature variation has no inflection point. For the two boundary elements (
(red),
(blue)), the threshold value of the conduction number (
K) calculated remains below 0.333 in this case. For the central element, two different values result for
K, depending on which neighboring material element’s heat conduction is taken into account. In one case, the value of
K is 0.119, while in the other case it is 0.413. In the general case, based on the calculated values, it cannot be established whether the model oscillates around the target value or not. Based on
Figure 5, it can be stated that in the temperature variations of the elements with identifiers
X and
there is no longer oscillatory-type behavior. Accordingly, in summary it can be stated that the threshold values defined in the system of Equation (
9) can also be used in the general case; however, they do not provide the optimal differentiation time and differentiation distance.
For the method of calculating the optimal differentiation time and distance, a function analysis is required. In the case of a thermally closed system, if there is no heat source within the system, then the monotonicity of the function of temperature variations will be determined by the first two sections of the function curves. As a first step, the temperature values corresponding to the time steps
t = 0,
t = 1, and
t = 2 must be determined. The initial temperatures are known. Into the system of Equation (
12), all the known temperatures can be substituted. For the sake of abbreviation of the equations, the element at position
1 was denoted by A and the element at position
by B, while the central element was denoted by the subscript 0.
The system of equations corresponding to the time instant
t = 2 is Equation (
15), in which the temperature values belonging to the time instant
t = 1 appear. From the combination of the systems of Equations (
14) and (
15), the system of Equation (
16) was obtained. (The physical meaning of the symbolic expressions of the unknowns appearing in the equations of systems (
14)–(
16) has already been defined earlier. See earlier.)
The slopes of the functions of the temperature variations are given by the differences of systems of Equations (
13), (
14), and (
16) as follows: the difference of the last terms of the systems of Equations (
13) and (
14), respectively, the difference of the last terms of the systems of Equations (
14) and (
16), gives the slope of the first two sections of the broken-line type function curve of the temperature variation in the central material element, in the above order. Similarly, the slopes for the other material elements are determined accordingly. Since the temperature of the central element appears in each of the heat conduction equations, it is sufficient to examine only the heat conduction equation written for the central material element.
The slope of the first section of the mentioned temperature variation function curve is (1) −(0); the slope of the second section is (2) −(1). The slope of the first section is greater than that of the second section, since the amount of heat transported decreases over time during the process. According to the construction, it is true that if the temperature of the central element increases during the temperature variation, then the slope will always have a positive value, while if the temperature certainly decreases, then the slope will be negative. In a stationary thermal state, the difference is 0.
Based on this, if the ratio of the slopes thus calculated is formed, then the function of temperature variation can be characterized by the following four cases:
- (a)
If it can be written for the slopes that
then the values of the terms of the sequence composed of the slopes corresponding to the individual sections of the broken-line type function increase in time. In this case, the function is considered or called unstable, since in the closed thermodynamic system the speed of the heat conduction transport process shows a decelerating character in time. In this case, the function values diverge to positive infinity.
- (b)
If it can be written for the slopes that
then the values of the terms of the sequence composed of the slopes corresponding to the individual sections of the broken-line type function decrease in time, but while retaining the decreasing character, they remain positive throughout. In this case, the function is considered and called stable, because in the closed thermodynamic system the stationary thermal state develops among the material elements.
- (c)
If it can be written for the slopes that
then the broken-line type function reaches the stationary-state function value already at the first time instant (i.e., time step;
t = 1). From the point of view of the model, this case is called the ideal case. This designation is justified because in this case this new—stationary—state can be determined with a single calculation.
- (d)
Finally, if it can be written for the slopes that
then the signs of the terms of the sequence composed of the slopes corresponding to the individual sections of the broken-line type function change in time. In this case as well, the function is considered and called unstable because in this closed thermodynamic system the nature of the temperature variation cannot be oscillatory monotonic (that is, the temperature cannot sometimes decrease and at other times increase).
To further aid the understanding of the four cases above, the following explanation is given: If the ratio of the slopes is greater than 1, that is, if the absolute value of the slope of the second section is greater than that of the first, then the temperature variation accelerates. In other words, in this case the temperature of the material element tends toward positive or negative infinity depending on whether the differences in the numerator and denominator of the fraction formed from the slopes are positive or negative in sign. The related limiting case is when the ratio is exactly 1. In this case the rise in the temperature does not accelerate, but its value tends toward positive or negative infinity.
If the value of the ratio formed from the slopes is less than 0, then the slopes of the examined sections of the temperature variation change sign. In the example shown in
Figure 4, the denominator of the fraction is positive, since the temperature of the central material element increases compared to the zeroth time instant. However, the temperature will subsequently decrease, so the difference of the temperatures calculated for the second and first time instants (time steps) will be negative. Thus, in this case the settling will be oscillatory. In inequality (
20) it is not indicated, but its limiting case is when the ratio becomes
. In this limiting case, the temperature changes periodically with constant amplitude.
If the ratio of our fraction is less than
, then the amplitude of the periodic variation oscillates between positive and negative infinity, changing constantly in time. If the value of the ratio formed from the slopes falls between 1 and 0, then the temperature reaches the stationary state according to a monotonic function with gradually decreasing slope, as shown in
Figure 5. Its limiting case is the case when the value of the numerator of the fraction is 0. Then, naturally, the mathematical value of the entire ratio is also 0. This case occurs when
In other words, when in the closed thermodynamic system there exists a locally stationary state (meaning a stable state from which, if the system is perturbed, it can only move toward a lower-energy but still stable state), in which case the change in the internal energy of the central material element per time instant (time step) will be zero.
By understanding the above, the next step in the optimization of the model is that among the above cases list in
Section 3.2, we shall use case lists (c) in
Section 3.2 in the following because it was established that from the point of view of model construction it is the ideal case. Thus, considering case list (c) in
Section 3.2, into Equation (
19) the values of the temperature of the central, i.e., zeroth, material element determined by the systems of Equations (
13), (
14), and (
16) can be substituted. From the variables
,
, and
appearing in these equations, the ratio of the time duration (
) and the square of the step length (
2), i.e., [
/
2], can be factored out. The
st power of the product of mass density and heat capacity is denoted by
,
,
. After factoring out the multiplier [
/
2] and rearranging the equation, the following equality (
21) results:
By applying the Method of Equating Coefficients, from Equation (
21) the system of inequalities (
22), consisting of three identical inequalities, can be derived:
In the identical inequalities (
22), on the left-hand sides stands the ratio of the parameters determining the run of the model [
/
2], and on the right-hand sides stand the physical parameters characterizing the material elements. All this therefore means that we are able to determine the optimal values of our model parameters with the help of the physical parameters characteristic of the material elements.
For the verification of the obtained result, the necessary physical parameters of silver, rock salt, and HDPE were substituted into the system of identical inequalities (
22). While, similarly to the previous two examples, a
= 0.010 m differentiation distance was set, the system of equations yielded
= 13.871 s, 13.385 s, and 21.192 s. Checking the validity of these results, we obtained that the value given by the first identical inequality of (
22) is the ideal one, since at the time instants (time steps)
and
the temperature of the central material element turns out to be nearly identical. The result (
) obtained from the second identical inequality is smaller compared to the value obtained in the first, i.e., ideal case. At the time instant (time step)
, the temperature is higher than the value obtained at the previous time instant
. With this described differentiation time setting, the operation of the model is sufficient (that is, not optimal, but corresponding to the real temperature variation function).
In the third case, the temporal variation in the temperatures gives a periodically changing, oscillatory character; therefore, this solution, according to the earlier justification list (d) in
Section 3.2, is incorrect. The result of 18.751 s obtained for the ideal case falls between the differentiation times applied in the examples shown in
Figure 4 and
Figure 5.
By calculating the first five iterations of the ideal case and representing the results visually, the broken lines shown in
Figure 6 are obtained, as the temperatures depend on the time steps.
In
Figure 6 the optimal solution is shown, that is, the case in which, by applying a given differentiation distance (
), the stationary state can be determined with the least amount of computation, while the temperature variation does not have the previously detailed periodically oscillating character and closely follows the heat conduction process observable in nature.
In
Figure 6 it can also be seen that the temperature change continues, since the heat capacity of the material element identified as
(the result curve drawn with red line color in
Figure 6) is greater than that of the other two material elements (i.e., the central and the other outer material elements). The target temperature, that is, the system temperature taken in the stationary state from the point of view of heat conduction, will be 22.222 °C, which the entire thermodynamic system reaches at the 64th time instant (time step), that is, after 887.750 s.
The system of identical inequalities (
22) can be extended to two and three spatial dimensions. In both of these cases it is assumed that the differentiation distance is identical in every direction of the coordinate system, that is,
. Due to the extent of the derivations, we present here only the final result. We note that the derivation of this general case is identical to that already presented for the one-dimensional case using the systems of equalities and inequalities (
13) and (
22). The only difference is that in the case of the systems of Equations (
13)–(
16), they consist not of three but of seven equations, since in three dimensions the central material element is bordered not by two but by six neighboring material elements. From the results of the derivations for one-, two-, and three-dimensional cases, the following general dimension-independent formula can be deduced:
(In the (
23) identical inequalities,
O (origo) is the middle element,
n is the dimension number, and
i is the neighboring element.)
With the system of identical inequalities (
23), the optimal or near-optimal differentiation time (
) and differentiation distance (
, since
) can be determined both for the one spatial dimension and even for the three general spatial dimension cases. It can be applied to every model where the size of the differentiation distance is identical for all material elements making up the model, and this condition is fulfilled for every spatial dimension (
).
In cases when the element sizes of the material elements constituting the heat conduction model are not identical per dimension (that is,
), then the system of identical inequalities (
23) is no longer applicable. In the generalization of model construction, the use of material elements of non-identical sizes may also be necessary. In order to be able to interpret different magnitudes of element sizes within the model, we must return to the derivation of the two- and three-dimensional cases. In the general two- and three-dimensional cases, and in the general formula given in (
23) derived from them, we always applied the assumption
.
In the earlier part of this publication, between (
22) and (
23), the complete derivation for one spatial dimension was presented. A similar derivation for the two- and three-dimensional cases was not included due to its length, but we note here that the course of that derivation is identical with the one applied in the already presented one-dimensional case.
The system of Equation (
24) describes two-dimensional heat conduction, in which notations similar in meaning to those used in the previous examples are applied, taking into account that in two spatial dimensions the central material element (denoted with lower index 0) has four neighboring material elements (the number of rectangles touching the four sides of a rectangle is four), whose notations are in turn lower-indexed
.
The system of Equation (
24) gives the temperatures
,
,
,
of the four material elements neighboring a fixed central material element as functions of time in the
n-th time step.
The heat conduction model from this point on already assumes that the central material element’s lengths per dimension are not equal, that is,
. We assume that there exists another system, similar to the above heat conduction system, which has physical parameters different from the heat conduction parameters appearing in the system of Equation (
24), and in which the lengths per dimension of the material elements constituting the two-dimensional system are identical (that is,
), but the temporal change in heat conduction between the elements occurs in an identical manner and magnitude in both systems. In this case, we correspond the model to another model with a uniform lattice spacing as follows (see the system of Equation (
25)):
In this system, let the size of each element be
, where
. Then, the system of Equation (
24) can be made equivalent to the system of Equation (
25), in which the factor
t/R appearing in front of the square bracket has been factored out. In this case,
. We obtained this value by bringing the expressions
and
, which stand before the terms inside the bracket, to a common denominator. After the factoring, inside the bracket each term includes, in accordance with the earlier multiplier, the proportionality factor
, respectively,
.
The system of Equation (
25) assumes a system composed of cube-shaped material elements of identical edge length, starting from the system of Equation (
24). Since from this point the steps of the derivation are identical to those applied for Equations (
13) and (
22) and the corresponding systems of equalities and inequalities, we do not provide the further derivation in full detail, but only present the final result. The steps of the derivation that are not explicitly written out were as follows: determination of the first two sections of the function of temperature change, examination of the monotonicity of these sections, description of the second section of the function of temperature change for zero slope, that is,
, and determination of the extreme values of the model parameters using the Method of Equating Coefficients in a form identical to that carried out for the system of equalities (
22). At the end of the derivation, for two-dimensional heat conduction with material elements of variable edge length, the following system of equalities was obtained:
(In the (
26) identical inequalities,
O (origo) is the middle element,
n is the dimension number, and
i is the neighboring element.)
The full derivation of the three-dimensional case is likewise not presented here due to its length. The methodology of the derivation is identical to that listed for the two-dimensional case and to that already presented for the one-dimensional, equal-edge-length case by the systems of equations and equalities–inequalities (
13)–(
22). As before, the model can then be brought into the general form given in (
27) for the expression in three spatial dimensions. All the notations used here correspond in logic to the notation technique applied earlier.
(In the (
27) identical inequalities,
O (origo) is the middle element,
n is the dimension number, and
i is the neighboring element.)
3.4. Grid Optimization
Using the data from the previous examples, let us examine as an example the heat conduction between silver and table salt, for now in one spatial dimension. Let a one-dimensional model be given for our case, in which there are six material elements, of which three elements are silver and three are rock salt. The material elements in the model are arranged relative to each other as shown in
Figure 8, that is, three rock salt elements are next to each other (the blue hatched areas in the figure) and three silver material elements (the black cross-hatched areas in
Figure 8) also next to each other, and the contact between the two different types of material occurs between the third and fourth element pieces, thus modeling the contact boundary surface of the different types of materials.
Let the temperature of material elements 1–3 (NaCl) be
H, and that of material elements 4–6 (Ag) be
L. In the case of a model with uniform grid division, that is, when the discretization distance (
) is the same everywhere, the discretization time (
) can be determined based on the system of equal inequalities (
21). Substituting into the (
21) system of equal inequalities the given parameters of the two materials and the discretization distance, which in this example we take as
= 1 mm, the following discretization times are obtained as solutions, in order, for the six consecutive material elements:
= 16.78 s, 16.78 s, 11.54 s, 0.29 s, 0.19 s, and 0.19 s. Since in our heat conduction model different discretization times cannot be defined for a series of material elements participating in the heat conduction, the (
21) equal inequalities are satisfied only if, among the different discretization times, the smallest value is taken as valid—in our case this is 0.19 s. We note that since this value was obtained for the fifth and sixth material elements, that is, for those having only silver material neighbors, the discretization time could also have been determined based on the first inequality of the system of equal inequalities (
9), i.e., by observing the No-Sway Threshold.
Now, let us examine the same case, but with the discretization time given initially (known) as
= 1 s. In this case, with the (
21) equal inequalities, after substituting the parameters, the optimal discretization distances can be determined for the individual material elements. Performing the calculations, the following values are obtained for the discretization distances of the individual material elements: 2.44 mm, 2.44 mm, 2.94 mm, 18.4 mm, 22.6 mm, and 22.6 mm. If the model’s grid division is uniform everywhere (which initially was not assumed here), then the discretization distance of the model must be 22.6 mm according to the (
21) equal inequalities. (In this case, from the series of obtained results, the largest value will be the appropriate one, since with a larger denominator, the value of the ratios is smaller.) In this case, i.e., if we were to choose a uniform grid division, the solution would remain suboptimal. In the case of the above example, the optimal heat conduction model can be achieved if the calculated discretization distance is applied as the size of the individual elements of the grid. If in the example model we do not change the number of material elements, then compared to
Figure 8, the structure of the model changes as follows:
In
Figure 9, the material elements are shown in linearly scaled distances, taking into account the discretization distances. The figure shows that the linear dimensions of the NaCl material elements are smaller, while the linear dimensions of the Ag material elements are larger. The linear length of the third material element in the sequence does not coincide with that of the first and second material elements, and likewise, the linear length of the fourth material element does not coincide with the linear dimensions of the fifth and sixth material elements. Where the model is homogeneous in material, the discretization distances—and thus the sizes of the elements—are identical. Differences arise only at the boundary surfaces. It can be said about the heat conduction model thus constructed with variable grid division (but constant in time) that it is optimized based on its parameters; that is, at certain points of the model, the temperature change function reaches the stationary state with fewer calculations, while the shape of the temperature change function develops according to real heat conduction. Using the previously introduced expression, the calculated temperature change follows a natural function.
The above solution, as also appears in the (
21) system of identical inequalities, can be applied to two- or three-dimensional space. Let us examine such a multidimensional but real dissipative example. The next example is a proof-of-concept, which primarily compares the constant grid spacing solution resulting from our earlier derivations with the variable grid spacing solution that we have defined as ideal. Our goal with this is primarily to highlight the difference between the two models with different grid spacing, and it is not our aim to provide an exact solution to the posed engineering problem. For an exact engineering solution, in addition to heat conduction, flow and thermal radiation phenomena would also have to be modeled, which lies beyond the scope of the present paper. The comparison of the grid configurations is still a preliminary result and does not contain accuracy metrics relating to the results determined by the models. We plan to carry out the investigation of model accuracy in a later study, which according to our plans would already compare the simulated results derived from the mathematical model with real measurement data. In the present example—as will become clear from its description—we examine the model of a designed but not realized system, which therefore does not even provide an opportunity to perform comparative measurements.
The Flexblue® French-designed Small Modular Reactor (SMR) was planned as a cylindrical body, more precisely: 150 m in length and 14 m in diameter [
35,
51]. The project was to be realized through the joint cooperation of several organizations and companies, but following the 2008 concept, the project was nevertheless halted in 2016. The reasons for this included, among others, that based on the experience gained from the Fukushima Daiichi nuclear power plant disaster, the International Atomic Energy Agency (IAEA) tightened its regulations. An SMR placed beneath the sea surface carries a higher risk of terrorist attack. In the event of a malfunction, the isolation of radioisotopes and the decommissioning of the facility would be complicated by ocean currents. Moreover, during reactor operation, the waste heat released would considerably warm the surrounding water, and with this warming, the marine biome in the vicinity of the nuclear unit would change.
For the heat conduction analysis of Flexblue®, let us simplify the example itself. As a result of the simplification, suppose that we examine only the heat conduction between seawater and a steel pipe, while disregarding convection and other flows in the water. Since the detailed designs of the equipment are not public and thus not known, we also stimulate as assumptions of our model that we disregard the internal details and structural composition, and within the tank of 20 cm wall thickness we assume only air.
To compute the heat conduction of the outer wall of Flexblue®, we constructed both the uniform-grid model and the variable-grid model detailed previously.
Figure 10 shows a single-line depiction representing one spatial-dimension direction for a 50.003 mm × 50.003 mm surface patch of the tank for these two models. The value of the 50.003 mm linear dimension resulted for the air material element at the air–steel media interface based on the solution of the (
22) identical inequalities. In the above-mentioned uniform-grid model, every material element has dimensions 50.003 mm × 50.003 mm × 50.003 mm along the three principal spatial directions. In the variable-grid model, the surface size is 50.003 mm × 50.003 mm, but then the thickness of the material elements was determined with the equation expressing the R of the (
27) identical inequality system, based on the optimal size for the given material element. Here, the optimal size was determined with the (
22) identical inequalities.
In the spatial Cartesian (Descartes) frame of reference, the (
22) identical inequality system can determine a differentiation distance only for a material element with equal edge lengths—i.e., cubes. We created material elements whose size differs in one spatial dimension by using the equation containing R from the (
27) identical inequalities to scale the
×
×
element to
× 50.003 mm × 50.003 mm, where
denotes the unknown thickness of the material element. By repeating this procedure for every material element, we obtain element b) of
Figure 10.
In both heat conduction models used, we examined cases with the same initial conditions and parameters. The case is an emergency shutdown in the Flexblue® SMR, as a result of which the air temperature inside the tank instantly became 200 °C. An additional initial condition was that the temperatures of the water and the steel were both 24 °C, and the leftmost and rightmost material elements of the single-line model expressing the linear dimension shown in
Figure 10 remained at constant temperature, that is, the temperature of the leftmost air material element was constantly 200 °C and the temperature of the rightmost seawater material element was constantly 24 °C for the entire simulated duration. The computational results, scaled up to the full surface, are shown in
Figure 11.
As was mentioned above, only renderings of Flexblue® are available to the authors; therefore, in determining the total external surface, we assumed that the two ends of the pressure vessel with cylindrical spatial geometry are not hemispheres, but would have been made with two end terminations having half-ellipsoid surfaces. Taking all this into account in the calculations, we determined, for the total surface, a surface-area value of 6714.39 m2.
In
Figure 11, we denoted the uniform-grid model by M1 (blue-colored domain), while the variable-grid model was denoted by M2 (orange-colored domain). The domains are bounded from above by the power–time curves of power taken up from the air and from below by the power–time curves of power delivered to the seawater. In
Figure 11 it can be seen that, in the two cases, the outer wall of Flexblue® stores the heat power to different extents. In the case of the uniform-grid model, comparing the solid blue curve with the solid orange curve of the variable-grid model shows that, according to the M1 model, the wall of the tank takes up more heat power from the air than is seen in the result obtained by the M2 model. If we compare the blue and orange dashed-line curves, it can be seen that, in the case of the uniform-grid model (M1), the function of heat power delivered to the seawater increases faster than the similar function obtained in the variable-grid model (M2). These results show that, in the case of the M2 model, the taken-up heat power heats the metal to a greater extent than in the M1 model.
The difference between the heat-power uptake of the steel tank modeled in the two models is also demonstrated by the two graphs shown in
Figure 12, which plot the temperature gradient at the 3000th min as a function of linear distance within the tank wall. Taking into account that the initial temperature of the steel tank was 24 °C, in the case of the uniform-grid model (M1) the temperature of the steel develops only between 26.229 °C and 25.835 °C. By contrast, the temperature gradient in the case of the variable-grid model (M2) varies between 34.648 °C and 30.041 °C within the wall. On this basis, in the case of the variable-grid model (M2), over the examined time domain a significant portion of the heat power was expended on the heating of the tank wall.
As a closing remark to the chapter, we consider it important to note that in this chapter we presented preliminary results that were produced by a sequence of calculations and are not yet simulation results run with our own, fully finished CHeTMoS target software. The sequence of calculations means using and computing, one after another, the equations and identical inequalities presented above—that is, precisely this series of recursive computations. The current version of our CHeTMoS software operates with uniform grid spacing. The possibility of applying variable grid spacing will be incorporated into our self-developed software following the present publication.