Solving the problem of pipeline freezing with respect to external heat exchange.
Parfentieva, Natalija ; Valancius, Kestutis ; Samarin, Oleg 等
1. Introduction
Engineering systems in buildings, in particular, heating, cold and
hot water supply systems, as well as the system supplying heat to air
heaters in air supply ventilation units and external utility lines, for
the most part, use water as operating fluid. However, there is a risk of
pipeline freezing during cold winter seasons due to sudden gradual drops
in temperature and in the event of replacing heating systems of heat
supply under emergency operating conditions. The volume naturally
increases in the freezing process, leading to increase in pressure
within the pipe and subsequent destruction thereof Gordon, J. [1] and
Gilpin, R. [2].
The freezing process is usually considered in cases where water
does not move in the pipe and the temperature decreases with time [3].
The solution of the aforementioned problem is directly related to
the solution of the Stefan J. [4]. In addition to using
theoretical-analytical and numerical methods, such as variation methods
of solving the problem of water freezing in pipes and freezing front
movement [5, 6] based on compiling a heat balance equation or solving a
heat conduction equation, experimental research in carried out [7, 8].
In addition to the above, various effects are taken into account,
including uneven distribution of ice in the cross-section of the pipe
[9], the flow of liquid along the pipe caused by natural convection
inevitably occurring during freezing. The latter has been found to have
little effect on the freezing process.
Despite the numerous studies mentioned above, of great practical
interest is the case where water moves inside the pipe, i.e. where
forced convection occurs. The water flow and the release of heat
naturally slow down the freezing process. However, practice shows that
pipelines may freeze at low temperatures.
Various engineering methods are used to prevent the process,
including laying external pipeline networks to an appropriate depth and
installing heat insulation; in certain cases intense forced water
circulation in pipes is created, resulting in the release of heat due to
internal friction.
However, the likelihood of accidents cannot be completely excluded
in any situation, and therefore, the issue pertaining to the rate of
water freezing in pipe-lines should be studied. It should be noted that
mathematical modelling of hydraulic and thermal modes of heating system
does not take the issue of freezing into account Gilpin R. [10].
The complexity of solving the aforementioned problem lies in size
of the areas that vary with time where the temperature field is
examined. Physical properties of this fluid, such as the thermal
conductivity coefficient, heat capacity, and density change sharply when
passing through the moving boundary; moreover, at the boundary, heat
release occurs due to fluid transitions, in our case, ice turning into
water, which complicates solving the problem even more. No exact
solution for the general case has yet been found. There are known
specific solutions, for example, a number of approximate solutions have
been obtained for temperature distribution in the case of plane
interface in a semi-infinite fluid,; it should be noted that the
McDonald A., at al [3] solves the problem for the pipeline, but for
simplification purposes it is assumed that external surface temperature
of the pipe is known and constant which corresponds to first-type
boundary conditions.
The purposes of this study are to 1) formulate the problem of
freezing of moving water in pipes under sharp temperature drops taking
into account the flowing of water in pipes; 2) determine the rate of
freezing, which is important in order to estimate the time required to
eliminate the damage inevitably done in the process; 3) study the ways
of reducing the likelihood of accidents.
2. Statement of the problem and mathematical model
In practice, the simplified solution where the temperature at the
pipe boundary is specified as the environment temperature can be
considered sufficiently ac-curate only in the case of underground,
particularly, channel-free laying, where pipes come in direct contact
with the soil, in which case the soil temperature at the pipeline laying
level can be considered to be the temperature at the pipe boundary.
At the same time, situations may emerge, primarily with respect to
internal networks, where pipelines are laid using open laying methods
(Fig. 1), and there-fore, the nature of heat exchange with the
environment on the surface thereof must be taken into account, which, in
turn, requires switching to third-type boundary conditions.
In this case, we will solve the problem of heat transfer in
zone-inhomogeneous medium.
[FIGURE 1 OMITTED]
Let's compile for the aforementioned case a relevant system of
differential and algebraic equations of heat balance, heat exchange, and
the heat flow released due to internal friction [11]:
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII] (1)
The boundary condition on the pipe surface takes the following
form:
[q.sub.l] = 2 [pi][r.sub.o] [alpha]([t.sub.e]-[t.sub.sur]). (2)
For the moving boundary inside the pipe, where r = [r.sub.F], it
can be expressed as t = 00:
[[rho].sub.2][r.sub.ps] d[r.sub.F]/d[tau] = [lambda][partial
derivative]t/[partial derivative]t, (3)
where [t.sub.1,2] are the temperatures in frozen and non-frozen
areas; [t.sub.e] is the outside air temperature; [t.sub.sur] is the pipe
surface temperature; [a.sub.1,2,] [m.sup.2]/s - the thermal diffusivity
in the said areas; [r.sub.0], m is the pipeline radius; [r.sub.F], m is
the freezing front radius changing with time; [[rho].sub.2] - water
density, kg/[m.sup.3]; [lambda] is the heat conductivity of ice, W/mK;
[alpha], W/[m.sup.2]K - heat transfer coefficient.
Solving the (1)-(3) equation system allows us to identify
temperature fields in both solid and liquid areas--the way it was done
by Parfentieva N.A. [12] and Poots G. [13].
However, our main task is to determine the rate of freezing,
therefore, we are not addressing the problem of identifying the
temperature fields. Still, if we know the position of the freezing front
and boundary conditions, we can determine the temperatures in the two
areas.
Let us consider the expression for linear density of heat flow
[q.sub.l], W/m, passing through the freezing front surface:
[q.sub.l] = 2[pi][lambda][t.sub.sur]/ln([r'.sub.F]) (4)
The expression includes [r'.sub.F] = [r.sub.F]/[r.sub.o] - the
freezing front dimensionless radius of the current relative to the
pipeline radius [r.sub.o], m.
The introduction of the dimensionless radius of the freezing front
will allow in the future doing the calculations for any radius of the
pipe.
We assume that the freezing point of water is zero degrees, and
ignore the difference between the outer and inner pipe diameters in this
case. Based on the Stefan condition, taking into account that the
specific surface area of the phase boundary per 1 metre of pipeline
equals 2[pi][r.sub.F], the same density value of the heat flow [q.sub.l]
can be written as:
[q.sub.l] = 2[pi][rho][r.sub.ps] [r.sub.F] d[r.sub.F]/d[tau] -
[q.sub.l.pf] = 2[pi][rho] [r.sub.ps][r.sup.2.sub.o] [r.sub.F]
d[r'.sub.F]/d[tau] - [q.sub.l.pf]. (5)
The value [q.sub.l.pf], W/m, represents the linear density of the
heat flow released in the process of water moving inside the pipeline
due to viscous friction.
It can easily be demonstrated that the said parameter can be
expressed as:
[q.sub.l.pf] = [pi]R[r.sup.2.sub.o][r'.sup.F.sub.2]w, (6)
where w is the speed of flowing water, m/s; and R are specific
friction pressure losses, Pa/m. The following expression holds true for
hydraulically smooth pipes [14]:
R = 3.2 x [10.sup.4] [w.sup.1.79]/[(2[r.sub.o][r'.sub.F] x
[10.sup.-3]).sup.1.29] (7)
And finally, on the outer surface of the pipeline, the surface heat
exchange condition holds true:
[q.sub.l] = 2[pi][r.sub.o][alpha]([t.sub.out] - [t.sub.sur]). (8)
The overall heat exchange coefficient a may, at the first
approximation, be considered constant along the pipe length, as, subject
to one and the same pipe diameter, it primarily depends on the
temperature difference ([t.sub.out] - [t.sub.sur]), and the said
difference should not significantly change, as, according to the
statement of the problem, [t.sub.out] = const, and at the beginning of
the freezing [t.sub.sur] will also be substantially constant and equal
to the temperature of the phase transition.
From (8) and (4) we can receive:
[t.sub.sur] = [t.sub.out]/1-1/[Bi ln ([r'.sub.F])], (9)
then the result substitutes into (4) and after that into (5) as a
left part, and into the right part (5)--the expression (6) taking into
account (7), and then we get:
[q.sub.l] = -2[pi][lambda][t.sub.out]/ln([r'.sub.F])-1/Bi =
[pi][r.sup.2.sub.o][r'.sub.F][2[rho][r.sub.ps]d[r'.sub.F]/d[tau] - A [w.sup.3][r'.sup.F]/[r'.sup.1.28.sub.F]], (10)
where A is cited in (11). This expression follows from (7). Value B
shows the impact of the liquid friction on heat flow [q.sub.l]. It can
be shown that, subject to (6)-(7):
B = A[w.sup.2.79] [r.sup.2.o] /[lambda][t.sub.out], where A = 3.3 x
[10.sup.4]/[(2[r.sub.o] x [10.sup.-3]).sup.1.29]. (11)
Then it is possible to get in a non-dimensional form:
1/Bi - ln ([r'.sub.F]) = [r'.sub.F] d[r'.sub.F]/dFo
- B [r'.sup.5.28.sub.F], (12)
when one may express d[r'.sub.F] and finally obtain the final
solution as an integral (13).
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII] (13)
Parameter Fo' represents a modified Fourier criterion
(non-dimensional time), and Bi complex represents a non-dimensional Biot
criterion characterising the ratio between the external heat exchange
and internal heat conduction. They are defined in this case by the
following expression:
Fo' = [lambda][t.sub.out][tau]/[rho][r.sub.ps][r.sup.2.sub.o];
Bi = [alpha][r.sub.o]/[lambda], (14)
where [tau] is time, s, calculating from the beginning of freezing.
The integral (13), with certain simplifications, can provide the
approximate dependence of moving boundary on time, but we find it
reasonable to use numerical methods to obtain such dependence.
[FIGURE 2 OMITTED]
3. Results and discussion
From the Fig. 2 shows calculation results--the value of Bi was
considered to be equal to 0.67, which corresponds to real-life heat
exchange conditions for the pipe with an outer diameter of 325 mm.
Dependence diagrams of the freezing radius at various values of B are
shown in Fig. 2 in solid lines.
The increase in value of B leads to the increase in Fo' with
the given value of freezing front radius, which is physically quite
obvious, as the heat released due to friction should slow down the
process.
The dashed line shows the dependence of Fo' on [r.sub.F] at Bi
[right arrow] [infinity] and B = 0, i.e. not taking into account the
heat released due to friction and under first-type boundary conditions
for the purposes of comparison with the analytical solution contained.
Under the first-type boundary conditions, as we can see, we get a
significantly lower freezing time value, although the nature of the
dependence remains the same.
It is obvious that when solving similar problems to obtain
numerical time values for practical use, third-type boundary conditions
should be taken for the outer pipe surface.
4. Conclusions
It is easily seen that at Bi < [infinity] the freezing occurs
more slowly due to the presence of additional resistance to heat
exchange on the outer pipeline surface. At the same time, for each Bi a
certain limit value of B is maintained, at which Fo' [right arrow]
[infinity], meaning physical termination of further freezing as a
consequence of external heat loss compensation with internal heat
release occurring due to friction: the heat released due to friction is
equal to the heat transferred to the air by time unit. Therefore, to
obtain correct calculations, friction should by all means be taken into
account. Obviously, as the value of Bi goes down with decreasing
[r.sub.o], pipes of smaller diameter are in a better position than
larger ones, and considering that the value of B also increases, the
effect is enhanced. Therefore, we conclude that to ensure additional
protection against freezing, it is advisable to use reduced diameter
pipelines, thus increasing the resistance to external heat exchange and
share of frictional heat.
This conclusion is not obvious--large pipe diameter must protect
the fluid from the complete freezing but from our calculations, we can
conclude that the friction plays an important role in this process, so
the flow of the fluid in the tube should be Puazeil flow, wherein the
heat release is going around the pipe section. It is important for the
above numerical calculations and comparison the results with Bi [right
arrow] [infinity] when heat release is ignored by the internal friction,
causes an error significantly greater than 100%.
The simplified formulation of the problem leads to the qualitative
conclusions, but the solution cannot be used for specific engineering
calculations. The introduction of generalized variables allows to use
obtained solutions for any parameters: tube diameter, volume flow rate,
surface properties, etc. Additionally solution can be used when driving
a liquid with non-water properties.
Thus, the problem of pipeline freezing at temperatures lower than
temperatures of phase transition in the presence of moving liquid inside
them has been solved. The obtained solution can be used in calculations
not only with respect to pipeline freezing, but also for axially
symmetric structures made of moisture permeable materials.
References
[1.] Gordon, J. 2006. An Investigation into freezing and bursting
water pipes in residential construction, Research Report No. 96-1,
Building Research Council, School of Architecture, University of
Illinois at Urbana-Champaign, p.1-51. http://hdl.handle.net/2142/54757.
[2.] Gilpin, R. 1977. The effects of dendritic ice formation in
water pipes, International Journal of Heat Mass Transfer 20: 693-699.
http://dx.doi.org/10.1016/0017-9310(77)90057-6.
[3.] McDonald, A.; Bschaden, B.; Sullivan, E.; Marsden, R. 2014.
Mathematical simulation of the freezing time of water in small diameter
pipes, Applied Thermal Engineering 73: 140-151.
http://dx.doi.org/10.1016/j.applthermaleng.2014.07.046
[4.] Stefan, J. 1981. Uber die Theorie der Eisbildung, insbesondere
uber die Eisbildung im Polarmeere, Annalen der Physik 42: 269-286 (in
German).
[5.] Parfentieva, N.A.; Samarin, O.D. 2007. Solving the stefan
problem with respect to pipeline freezing, Vestnik MGSU 1: 67-70 (in
Russian).
[6.] Churchill, S.; Chu, H. 1975. Correlating equations for laminar
and turbulent free convection from a horizontal cylinder, International
Journal of Heat Mass Transfer 18: 1049-1053.
http://dx.doi.org/10.1016/0017-9310(75)90222-7.
[7.] Cho, S.H.; Sunderland, J. 2011. Heat-conduction problems with
melting or freezing, Journal of Heat Transfer 91(3): 421-426.
http://dx.doi.org/10.1115/1.3580205.
[8.] Lapina, N.N.; Pushkin, V.N. 2010. Numerical solution of
one-dimensional plane stefan problem, Vestnik DGTU 10(1): 16-21 (in
Russian).
[9.] Muehlbauer, J.; Sunderland, J. 1965. Heat conduction with
freezing or melting, Applied Mechanics Review 18: 951-959.
[10.] Gilpin, R. 1976. The influence of natural convection on
dendritic ice growth, Journal of Crystal Growth 36: 101-108.
http://dx.doi.org/10.1016/0022-0248(76)90220-7.
[11.] Gabrielaitiene, I. 2011. Numerical simulation of a district
heating system with emphases on transient temperature behavior,
Proceedings of the 8th International Conference "Environmental
Engineering", 2: 747-754. http://dspace1.vgtu.lt/handle/1/1274.
[12.] Parfentieva, N.A. 2011. Mathematical modeling of thermal
behaviour of structures in phase transition conditions, Vestnik MGSU 4:
320-322(in Russian).
[13.] Poots, G. 1962. On the application of integral methods to the
solution of problems involving the solidification of liquids initially
at the fusion temperature, International Journal of Heat Mass Transfer
5: 525-531. http://dx.doi.org/10.1016/0017-9310(62)90163-1.
[14.] Samarin, O.D. 2014. Calculation of pressure losses in polymer
pipes, Santekhnika 1: 22-23 (in Russian).
Received April 02, 2015
Accepted June 23, 2015
Natalija Parfentieva, Moscow State University of Civil Engineering,
Yaroslavskoye 26, Moscow, Russia, E-mail: nparfentyeva@gmail.com
Kestutis Valancius, Vilnius Gediminas Technical University,
Sauletekio al. 11, Vilnius, Lithuania, E-mail:
kestutis.valancius@vgtu.lt
Oleg Samarin, Moscow State University of Civil Engineering,
Yaroslavskoye 26, Moscow, Russia, E-mail: samarin1@mtu-net.ru
Sabina Paulauskaite, Vilnius Gediminas Technical University,
Sauletekio al. 11, Vilnius, Lithuania, E-mail: spaul@vgtu.lt
Jolanta Ciuprinskine, Vilnius Gediminas Technical University,
Sauletekio al. 11, Vilnius, Lithuania, E-mail:
jolanta.ciuprinskiene@vgtu.lt
http://dx.doi.org/10.5755/j01.mech.21.5.11411