Method of preserving heat exchange surface and method of cooling moist air

Abstract

A method of cooling moist air through a heat exchange surface suppresses the formation of dew and frost on a heat exchange surface by preparing a carrier which has a heat conduction ratio higher than that of the moist air if the air temperature in a temperature boundary layer, is below the dew-point when the air temperature in the temperature boundary layer is above 0 C., or below the freezing-point when the air temperature in the temperature boundary layer is below 0 C., the carrier being arranged within the temperature boundary layer and on the heat exchange surface, which is in contact with moist air and is used for cooling; and removing moisture from the air by condensing or sublimating water vapor in the moist air on the surface of the carrier by arranging the carrier opposite of the heat exchange surface and within the temperature boundary layer.

Claims

1. A method of maintaining a heat exchange surface which is in contact with moist air and is used for cooling, by suppressing the formation of dew and frost on the heat exchange surface, comprising: arranging a carrier facing a heat exchange surface, within a temperature boundary layer which is determined in accordance with temperature and flow of moist air on the heat exchange surface, the carrier having a heat conduction ratio higher than that of the moist air in cases where the air temperature in the temperature boundary layer is either (i) below the dew-point and above 0 C., or (ii) below 0 C., and flowing the moist air along the heat exchange surface and the carrier, thereby removing moisture by condensing or sublimating water vapor in the moist air on a surface of the carrier, and replacing the carrier when dehumidifying performance of the carrier is deteriorated.

2. A method of cooling moist air through a heat exchange surface which is in contact with the moist air and is used for cooling, by suppressing the formation of dew and frost constituting a thermal resistant layer on a heat exchange surface, comprising: arranging a carrier facing a heat exchange surface, within a temperature boundary layer which is determined in accordance with temperature and flow of moist air on the heat exchange surface, the carrier having a heat conduction ratio higher than that of the moist air in cases where the air temperature in the temperature boundary layer is either (i) below the dew-point and above 0 C., or (ii) below 0 C., and flowing the moist air along the heat exchange surface and the carrier, thereby removing moisture by condensing or sublimating water vapor in the moist air on a surface of the carrier.

3. The method of cooling moist air through a heat exchange surface according to claim 1, wherein the surface of the carrier on which the water vapor is condensed or sublimated faces away from the heat exchange surface, wherein the carrier is configured such that condensed liquid flows down along the surface of the carrier facing away from the heat exchange surface, and wherein the temperature of the moist air within the temperature boundary layer is above 0 C.

4. The method of cooling moist air through a heat exchange surface according to claim 1, wherein the surface of the carrier on which the water vapor is condensed or sublimated faces away from the heat exchange surface, wherein a temperature on the surface of the carrier facing away from the heat exchange surface is below the dew point of the moist air, wherein the temperature of the moist air within the temperature boundary layer is between 0 C. and 40 C., and wherein the surface of the carrier facing away from the heat exchange surface undergoes condensation, super cooling, and loss of super-cooling.

5. The method of cooling moist air through a heat exchange surface according to claim 2, wherein the surface of the carrier on which the water vapor is condensed or sublimated faces away from the heat exchange surface, wherein a temperature on the surface of the carrier facing away from the heat exchange surface is below the dew point of the moist air, and wherein the temperature of the moist air within the temperature boundary layer is below 40 C.

6. The method of cooling moist air through a heat exchange surface according to claim 2, wherein the surface of the carrier on which the water vapor is condensed or sublimated faces away from the heat exchange surface, wherein a temperature on the surface of the carrier facing away from the heat exchange surface is above the dew point of the moist air and below 0 C., and wherein the temperature of the moist air within the temperature boundary layer is below 0 C.

7. The method of maintaining a heat exchange surface according to claim 1, wherein the carrier is a planar structure with a regular or irregular cross section having non-opening portions and openings arranged in an alternate manner, each of the non-opening portions including a predetermined width, and wherein the carrier is disposed away from the heat exchange surface by a predetermined distance.

8. The method of cooling moist air through a heat exchange surface according to claim 2, wherein the carrier is a planar structure with a regular or irregular cross section and having openings of a predetermined width arranged in an alternate manner, and wherein the carrier is disposed away from the heat exchange surface by a predetermined distance.

9. The method of maintaining a heat exchange surface according to claim 7, wherein the carrier is a mesh-form including openings with predetermined widths and wires with predetermined widths and thicknesses.

10. The method of cooling moist air through a heat exchange surface according to claim 8, wherein the carrier is a mesh-form including openings with predetermined widths and wires with predetermined widths and thicknesses.

11. The method of maintaining a heat exchange surface according to claim 7, wherein the width of the carrier is between 100 m and 2000 m, the width of the openings is between 100 m and 1000 m, and the depth of the carrier from the surface of the carrier on a temperature boundary layer side thereof to a heat exchange surface side thereof is greater than 100 m.

12. The method of cooling moist air through a heat exchange surface according to claim 8, wherein the width of the carrier is between 100 m and 2000 m, the width of the openings is between 100 m and 1000 m, and the depth of the carrier from the surface of the carrier on a temperature boundary layer side thereof to a heat exchange surface side thereof is greater than 100 m.

13. The method of maintaining a heat exchange surface according to claim 1, wherein the carrier is a three-dimensional structure with voids, the carrier being constituted by fibers with predetermined lengths and a regular or irregular cross section being superimposed in a non-woven manner.

14. The method of cooling moist air through a heat exchange surface according to claim 2, wherein the carrier is a three-dimensional structure with voids, the carrier being constituted by fibers with predetermined lengths and a regular or irregular cross section being superimposed in a non-woven manner.

15. The method of maintaining a heat exchange surface according to claim 13, wherein the three-dimensional carriers are thickened in such a way that a portion of the carrier is disposed in a main air flow outside the temperature boundary layer, and wherein said method further includes a step of promoting heat transfer of the heat exchange surface by guiding the air flow inside openings of the carrier within the temperature boundary layer.

16. The method of cooling moist air through a heat exchange surface according to claim 14, wherein the three-dimensional carriers are thickened in such a way that a portion of the carrier is disposed in a main air flow outside the temperature boundary layer, and wherein said method further includes a step of promoting heat transfer of the heat exchange surface by guiding the air flow inside openings of the carrier within the temperature boundary layer.

17. The method of maintaining a heat exchange surface according to claim 7, further comprising a step of carrying out a water repellent treatment on the surface of the carrier to vary the surface condition of the carrier so as to improve the dehumidification performance by the sublimation, or the condensation of the water vapor on the surface of the carrier and so as not to block the openings under the liquid condition.

18. The method of cooling moist air through a heat exchange surface according to claim 8, further comprising a step of carrying out a water repellent treatment on the surface of the carrier to vary the surface condition of the carrier so as to improve the dehumidification performance by the sublimation, or the condensation of the water vapor on the surface of the carrier and so as not to block the openings under the liquid condition.

19. The method of maintaining a heat exchange surface according to claim 7, wherein the surface of the carrier is set to possess adsorption performance to vary the surface condition of the carrier so as to improve the dehumidification performance by the sublimation, or the condensation of the water vapor on the surface of the carrier.

20. The method of cooling moist air through a heat exchange surface according to claim 8, wherein the surface of the carrier is set to possess adsorption performance to vary the surface condition of the carrier so as to improve the dehumidification performance by the sublimation, or the condensation of the water vapor on the surface of the carrier.

21. The method of maintaining a heat exchange surface according to claim 7, wherein the carrier includes fibers which are made of a water absorptivity resin to enhance the water absorptivity, water retentivity, and capillary water absorptivity of the carrier to improve the dehumidification performance by the sublimation, or the condensation of the water vapor on the surface of the carrier.

22. The method of cooling moist air through a heat exchange surface according to claim 8, wherein the carrier includes fibers which are made of a water absorptivity resin to enhance the water absorptivity, water retentivity, and capillary water absorptivity of the carrier to improve the dehumidification performance by the sublimation, or the condensation of the water vapor on the surface of the carrier.

Description

BRIEF DESCRIPTION OF THE DRAWINGS

(1) FIG. 1 is a general side view illustrating a first embodiment of the present invention.

(2) FIG. 2 is a schematic view illustrating a temperature distribution in accordance with the situation in which the frost is formed on the carrier C, in the first embodiment of the present invention.

(3) FIG. 3 is a conceptual graph illustrating the occurrence of frost formation and the condensation phenomena using the water saturated and ice saturated curves.

(4) FIG. 4 is a schematic view illustrating a situation in which the frost is formed on the carrier C, in the first embodiment of the present invention.

(5) FIG. 5A is a schematic view illustrating an alternative of the carrier C in the first embodiment of the present invention.

(6) FIG. 5B is a schematic view illustrating an alternative of the carrier C in the first embodiment of the present invention.

(7) FIG. 6A is a schematic view illustrating a further alternative of the carrier C in the first embodiment of the present invention.

(8) FIG. 6B is a schematic view illustrating a further alternative of the carrier C in the first embodiment of the present invention.

(9) FIG. 6C is a schematic view illustrating an alternative of the carrier C in the first embodiment of the present invention.

(10) FIG. 7A is a schematic view illustrating an alternative of the carrier C in the first embodiment of the present invention.

(11) FIG. 7B is a schematic view illustrating an alternative of the carrier C in the first embodiment of the present invention.

(12) FIG. 8 is a conceptual view illustrating a condensation phenomenon on the surface of the carrier C and the heat exchange surface S in a second embodiment of the present invention.

(13) FIG. 9 is a planar photograph illustrating a metal net in the embodiment of the present invention.

(14) FIG. 10 is a three-dimensional image illustrating the metal net in the embodiment of the present invention.

(15) FIG. 11 is a plan view and a side view each illustrating the metal net in the embodiment of the present invention.

(16) FIG. 12 is a view illustrating the process in which the frost crystals P4 grow in a case where the heat exchange surface S is groove-machined.

(17) FIG. 13 is a view illustrating the observation result of the formation of the frost crystals P4 in a case where the metal net is disposed on the heat exchange surface S in FIG. 9, in the embodiment of the present invention.

(18) FIG. 14 is a sketch illustrating the formation of the frost crystals P4 and the mechanism of the growth of the frost in FIG. 13.

(19) FIG. 15 is a side view illustrating the observation result of the formation of the frost crystals P4 in a case where a gap is provided between the metal net in FIG. 9 and the heat exchange surface S, in the embodiment of the present invention.

(20) FIG. 16 is a sketch illustrating the formation of the frost crystals P4 and the mechanism of the growth of the frost in FIG. 15.

(21) FIG. 17 is a graph illustrating a relationship between the heat flux and the temperature of the heat exchange surface S, in a case where the metal net is disposed within the temperature boundary layer and in a case where the metal net is not disposed within the temperature boundary layer, in the embodiment of the present invention.

(22) FIG. 18 is a graph illustrating a temperature distribution within the temperature boundary layer BL based on the surface of the frost layer, in the embodiment of the present invention.

BEST MODE FOR CARRYING OUT THE INVENTION

(23) A first embodiment of the present invention is described in detail, with reference to the drawings.

(24) In the following embodiments, a size, a material, a specific numerical limitation, etc. are only examples for making it easy to grasp the present invention, so that these elements are not intended to limit the present invention, unless explicitly described otherwise, in particular.

(25) In the following description, with respect to the same elements as those in the following embodiments, an explanation thereabout is omitted by attaching the same reference numbers to those elements.

(26) With an example of a case where an air is cooled to below 0 C. by using coolant by means of a heat exchanger HX, the embodiment of the present invention is explained about, with reference to the drawings.

(27) As shown in FIG. 1, a planar carrier with openings is disposed in an atmosphere of a moist air outside of the heat exchanger HX.

(28) The heat exchanger HX includes the thickness t and an outer surface of the heat exchanger HX forms a heat exchange surface S by flowing coolant with temperature of Tc inside of the heat exchanger HX.

(29) Tin of the moist air flowing along the cooling surface constitutes a temperature distribution in which a slow slope is formed within a temperature boundary layer BL formed based on the surface of the heat exchange surface S to a low Tout of the cooling surface. The following explanation is under the condition that the temperature of the air is between 0 C. and 40 C.

(30) At this stage, in a case where the planar carrier C including openings in the temperature boundary layer BL is formed so as to secure a gap relative to the heat exchange surface S, water vapor in the moist air becomes a saturated state (the temperature of air becomes the dew point) at the opposite side of the heat exchange surface S in the carrier C, due to the lowering of its temperature, so that the condensation occurs in the condensation nuclei in the air.

(31) Such floating condensed droplets P1 fall down and accumulate to form a group of droplets on the surface of the carrier C.

(32) The group of droplets grows by a coalescence of the droplets P1 newly falling down and accumulating, or by water vapor being condensed in the atmosphere.

(33) The droplets are super-cooled in many cases, but when they grow up to 100 m, a super-cooled state is lost, so that a frozen ice surface is formed. At this stage, water vapor begins to sublimate to the frozen ice surface, so that frost crystals P4 are rapidly formed. Since the openings O are closed by the formation of the frost, the frost with air-passage characteristics grow thick. At this stage, the water vapor in the moist air grows into the frost crystals P4, so that the amount of the water vapor reaching the heat exchange surface S through the carrier C decreases due to the water vapor being caught by the frost crystals P4, whereby the growth of the frost on the heat exchange surface S is halted.

(34) In this state, a sensible heat exchange is stably conducted through the heat exchange surface S by the formation of the frost on the surface of the carrier C disposed within the temperature boundary layer BL.

(35) Although the amount of heat transfer is gradually decreased due to an increase of a thermal resistance of the frost layer, in a case where the frost crystals P4 grow on the heat exchange surface S, a stable heat exchange transfer is attained by such gradual decrease of the amount of the heat transfer being halted. In addition, since a latent heat transfer through the carrier C is conducted due to the fact that the formation of the frost occurs in the same manner as a case of that through the conventional heat exchange surface S, the total amount of heat exchange increases more than that under the growth of the frost only on the heat exchange surface S.

(36) Such being the case, a new heat exchange configuration in which the latent heat exchange through the surface of the carrier C and the conventional sensible heat exchange through the heat exchange surface S are separated from each other is attained by an innovative idea in which the carrier C including the openings S is formed within the temperature boundary layer BL of the heat exchange surface S.

(37) In this connection, with respect to the temperature boundary layer BL described above, the thickness of the temperature boundary layer BL varies in accordance with environmental conditions. Normally, the environmental conditions include the ambient temperature and the flow of fluid, however, an explanation about such conditions are omitted here. What is explained about here is a case how the frost layer grows on the surface of the carrier C within a temperature boundary layer BL in FIG. 1 within which nothing exists as shown in FIG. 2(A). As shown in FIG. 2(B), the thin temperature boundary layer BL in FIG. 2(A) becomes thick by the carrier C being disposed therewithin. In addition, as shown in FIG. 2(C), the more the frost grows, the thicker the temperature boundary layer BL becomes. Such being the case, although the frost may grow within a constant temperature boundary layer BL within which nothing exists by the carrier C being disposed therewithin, even if the thickness of the temperature boundary layer BL is very thin, the temperature boundary layer BL becomes thick under the condition that the heat conduction ratio of the carrier C is higher than that of air. This follows that it is considered to be feasible to vary and thicken the thickness of the temperature boundary layer BL by disposing at least a portion of the carrier C within the temperature boundary layer BL, so that there is considered to be much room for utilizing the above-described phenomenon.

(38) Here, conditions for the occurrence of frost formation, or the condensation phenomenon is explained about, with reference to FIG. 3. If a condition of water vapor in an atmosphere corresponds to a water-saturated atmosphere (including super-saturated state) under air temperature higher than 0 C. (zone A), water droplets are generated by water vapor being condensed to condensation nuclei in an atmosphere, and then, falls and accumulates on the cooling surface, whereby water vapor is condensed to such accumulated water droplets by a repetition of the above growth and combining into one process to form into big droplets. When a gravity force exerting on such big droplets exceeds an adhesion force between the big droplets and the cooling surface, the big droplets flows (falls) down on the cooling surface.

(39) If a condition of water vapor in an atmosphere corresponds to the water-saturated atmosphere (including super-saturated state) under air temperature between 0 C. and 40 C. (zone C), super-cooled water droplets are generated by the water vapor being condensed to condensation nuclei in an atmosphere, and then, fall and accumulate on the cooling surface, whereby the super-cooled water droplets grow to be joined to each other, and then, become frozen, and as a result, the water vapor sublimates to the frozen ice particles to cause the formation of frost.

(40) If a condition of water vapor in an atmosphere corresponds to an ice super-saturated atmosphere and does not correspond to the water-saturated atmosphere under air temperature between 0 C. and 40 C. (zone B), ice crystals are generated by water vapor being sublimated to sublimation nuclei in the atmosphere, and then, falls and accumulates on the cooling surface, whereby water vapor are sublimated to such accumulated ice crystals to cause the formation of frost.

(41) Now, the condensation or the sublimation phenomenon is explained about in more detail. When a moist air is cooled, water vapor in the atmosphere becomes a super-saturated state (refer to as a water super-saturated state) in which the water vapor cannot maintain its gas state any longer, so that the condensation phenomenon sets in. An air temperature at this state is referred to as dew point. In addition, in a case where an ambient temperature is below 0 C., the water vapor can become either an ice super-saturated state or a water super-saturated state. This is because the amount of super-saturated water vapor under the ice state is smaller than that under the water state, the ice super-saturated phenomenon precedes over the water super-saturated phenomenon, so that the water vapor over the amount of the super-saturated water vapor emerges as ice crystals (referred to as ice crystal hereinafter) by sublimating to the ice crystal nuclei in the atmosphere. An air temperature at the stage is referred to as a freezing point.

(42) In this connection, if the water vapor is further cooled under a low temperature to become a water super-saturated condition where a condensation phenomenon sets in, like the case of the air temperature above 0 C., however, under the condition of the air temperature is below 40 C., the condensed droplets immediately become the super-cooled droplets without being frozen. An air temperature at the stage is also referred to as dew point, like a case of the air temperature above 0 C. The super-cooled droplets stochastically become frozen with time. Since the water vapor pressure of the ice is lower than that of the surroundings, water vapor positively sublimates to such an icy surface, whereby frost crystals P4 rapidly start to grow.

(43) In addition, in a case where a condition of the water vapor in the atmosphere corresponds to the water-saturated atmosphere (including super-saturated state) under the condition that the air temperature is below 40 C. (zone D), the water vapor is caused to condensate to the condensation nuclei in the atmosphere to immediately form into frozen particles, and then, frozen particles having fallen and accumulated on the cooling surface to form frost in a powder form.

(44) In this connection, if the temperature of the cooling surface is below 40 C., but the air temperature in the atmosphere is above 40 C. warmer than the cooling surface, the accumulated powder frost gets thick, and if the temperature of the surface of the frost layer becomes above 40 C. due to that it is exposed to the atmosphere, water vapor sublimates to the frost to cause the formation and the growth of the frost.

(45) Further, in a case where a condition of the water vapor in the atmosphere correspond s to the ice super-saturated state and does not correspond to the water-saturated state under the condition that the air temperature is below 40 C. (zone E), the water vapor is caused to sublimate to sublimation nuclei in the atmosphere to immediately form into ice crystals, and then, the water vapor sublimates to ice crystals having fallen and accumulated on the cooling surface to form frost.

(46) In this connection, the above explanation is based on the assumption that the condensation nuclei or the sublimation nuclei exist in the atmosphere within the temperature boundary layer BL near the cooling surface. However, since the condensation nuclei or the sublimation nuclei also exist on the heat exchange surface S, the condensation or the sublimation phenomenon can directly occur on the heat exchange surface S. This follows that, even if the super-saturated phenomenon does not occur in the air, the condensation or the sublimation phenomenon can occur on the heat exchange surface S, only if the condition of the heat exchange surface S corresponds to the surroundings.

(47) That is to say, even if the surroundings of the heat exchange surface S does not correspond to the super-saturated state, the condensation or the sublimation phenomenon can occur only on the surface of the carrier C, so long as the surface of the carrier C corresponds to the super-saturated state.

(48) (2) As to Phenomenon in which Frost Forms on Carrier C within Temperature Boundary Layer BL and does not Grow on Heat Exchange Surface S

(49) The above phenomena has not been made clear yet, but is surmised as follows.

(50) Explaining about a case where temperature is above 40 C. at which the super-cooled state occurs, since many condensation or sublimation nuclei exists at the initial stage in the atmosphere including the carrier C, as shown in FIG. 4(A), a super-saturated state occurs, so that condensed droplets P1 in the atmosphere begin to float. Thereafter, as shown in FIG. 4(B), the condensed droplets P1 accumulate on the surface of the carrier C and the heat exchange surface S, and then, they grow on the heat exchange surface S due to the condensation or the sublimation of newly fed water vapor.

(51) Then, as shown in FIG. 4(C), the condensed droplets P1 grow into big super-cooled water droplets P3 by a repetition of the above joint, and the big super-cooled water droplets P3 becomes frozen particles. At this stage, as shown in FIG. 4 (D), water vapor in the air sublimates to the frozen particles, so that the frost begins to grow. Since a rapid growth of the frost on the surface of the carrier C begins, water vapor is caught by the surface of the carrier C, so that the amount of water vapor flowing into the atmosphere on the heat exchange surface S decreases, whereby the super-saturated phenomenon is mitigated.

(52) Then, as shown in FIG. 4(E), since the frost grows at an upper area between the carriers C, a large amount of water vapor becomes unable to flow into an space between the carrier C and the heat exchange surface S, and as a result, water vapor forms into the frost on the surface of the carrier C, while, water vapor does not form into the frost on the heat exchange surface S. In this connection, since the sensible heat exchange without the formation of the frost can be maintained on the heat exchange surface S due to the fact that the convection current still exists, the amount of the sensible heat exchange can be maintained at the same level as that at the initial stage. A best heat exchange configuration can be achieved by a combination of this sensible heat exchange through the heat exchange surface S and the latent heat exchange through the surface of the carrier C.

(53) In this connection, although the above phenomenon occurred by arranging the surface of the carrier C parallel to the heat exchange surface S was explained about, the above phenomenon is attributed to the mechanism in which the formation of the frost on the heat exchange surface S can be prevented due to the fact that the water vapor does not form the super-saturated state on the heat exchange surface S. Accordingly, even if a heat transfer promoter N for promoting the heat transfer through the heat exchange surface S constituting a flow for destroying the temperature boundary layer is utilized, the sensible heat transfer can be promoted by removing water vapor by means of the carrier C at last, since the heat transfer by the convection current can be increased.

(54) For example, as shown in FIG. 5(A), if the heat transfer promoter N in a plate form is disposed outside the carrier C, a portion of a flow of the fluid is guided to the side of the carrier C to promote the flow of the fluid passing thorough the openings O of the carrier C, whereby the formation of the frost on the heat exchange surface S and the heat transfer through the heat exchange surface S can be promoted. In FIG. 5(B), the structure of the carrier C and the heat transfer promoter N in FIG. 5(A) is constituted only by the carrier C. A plurality of the normal planar carriers C are separated from each other in the flow direction in such a way that only a portion at the upstream side is disposed outside of the temperature boundary layer.

(55) (3) Relationship Between Shape, Size and Opening O of Carrier C, and Heat Exchange Surface S Under Growing Phenomena of Frost

(56) The relationship between the shape, the size and the opening O of the carrier C, and the heat exchange surface S is now explained about, with reference to FIGS. 6(A) to 6(C).

(57) In a case where the growth of the frost in the atmosphere the temperature of which is between 0 C. and 40 C., the carrier C may be sized in such a way that condensed water droplets accumulates to form a group of the super-cooled water droplets P3 and may have any cross section shape. The opening O may be sized in such a way that the frost layer having grown on the carrier C closes the opening O at the growing stage.

(58) The opening O between the adjacent carriers C may be blocked by the growth of the frost on the adjacent carriers C.

(59) In addition, the depth of the carrier C may be any, so long as a space between the carrier C and the heat exchange surface S is kept.

(60) In a case where the carrier C is provided on the heat exchange surface S, since an area for the sensible heat exchange through the heat exchange surface S decreases, it is considered to be important that the carrier C is kept away from the heat exchange surface S in a case where the latent heat exchange and the sensible heat exchange are intended to be separated from each other by means of the carrier C.

(61) In this connection, it was explained that the provision of the space between the heat exchange surface S and the carrier C matters for the water vapor passing through the opening O, and this is assumed that an invasion of the water vapor into the illustrated space from the right and the left side thereof does not occur.

(62) Since there are various kinds of configurations of the heat exchange surface S depending on the heat exchanger HX, the concrete explanation of the heat exchange surface S is omitted here, but, needless to say, the configuration of the heat exchanger HX is selected so as to prevent such an invasion of the water vapor.

(63) Examples of the cross sectional shapes of the carrier C is shown in FIGS. 6(A), 6(B), and 6(C). Any cross sectional shape of the carrier C can be adopted, as shown in FIGS. 6A, 6B, and 6C. Since the carrier C includes the openings O, the openings O can be formed by a mechanical cutting operation, an electric discharge machining, a sandblasting method, an etching method, etc., or by a pressing machining. Any method can be adopted. In addition, a wire in a meshed form such as a metal mesh, or a punching metal, a metal lath (expand metal) can be utilized.

(64) With respect to the size of the carrier C, the width of the carrier C is between 100 m and 2000 m, the width L of the opening O is between 100 m and 1000 m, and the depth between the surface of the carrier C and the heat exchange surface S is above 100 m. In addition, since the carriers C do not have to be arranged in a planar manner, the carrier C in a non-woven form can be adopted, as shown in FIG. 7A. According to such a non-woven carrier C, it is technically advantageous to attain a sufficient function without providing gaps on the heat exchange surface S.

(65) In addition, as shown in FIG. 7B in which the carrier C is disposed outside the temperature boundary layer BL, a portion of the carrier C outside the temperature boundary layer BL can be functioned as the heat transfer promoter N.

(66) (4) Treatment of Frost Having Grown on Surface of Carrier C

(67) It is fundamentally crucial that by the dehumidification of the carrier C by means of the condensation or the sublimation, to suppress the condensation or the sublimation on the heat exchange surface S, and one more important matter is how to treat the frost having grown on the surface of the carrier C under the condition of the temperature below 0 C. Since the frost grows thick to form into a thermal resistance layer with time, whereby the growth of the frost decreases while the air-passage is hindered, and as a result, the heat transfer is deteriorated, the treatment of the frost is needed to maintain the heat transfer.

(68) The treatment of the frost differs in accordance with the preservation of the heat exchange surface S, the utilization of the frost and the separation of the latent heat exchange and the sensible heat exchange

(69) The target of each of the preservation of the heat exchange surface S and the separation of the latent heat exchange and the sensible heat exchange is the heat exchange surface S itself or to exchange heat through the heat exchange surface S and the surface of the carrier C, and has nothing to do with the treatment of the frost itself.

(70) Accordingly, there are various kinds of methods for attaining the above target, since any treatment of the frost does not matter.

(71) That is to say, conventional defrosting methods (hot gas, water sprinkling, off-cycle defrosting, an electrical heater, brine sprinkling, etc.) can be adopted. A new idea of a utilization of jet flow by an air nozzle, or a mechanical process by using a brush can be adopted. The technique of vibrating the carrier C also can be adopted.

(72) In case of the utilization of the frost, a secondary utilization of the frost is needed under a concept that the frost is deemed a heat storing body. More specifically, the carrier C on which the frost has grown with time is replaced by a new carrier C on which no frost is formed, and the replaced carrier C with frost is utilized on the spot, or moved to a place where the frost is peeled off from the surface of the carrier C by the physical method such as the jet flow, the vibration, or the mechanical method such as the brush to be utilized for a certain application. In addition, in a case where the frost is utilized for the heat storing body, the carrier C with frost can be utilized as it is, in accordance with applications.

(73) In case of the separation of the latent heat exchange and the sensible heat exchange, the carrier C may be replaced, since the frost needs to be treated highly efficiently due to the formation of the frost on the surface of the carrier C in order to maintain the high efficiency of the latent heat exchange.

(74) A second embodiment of the present invention is now explained about, with reference to FIG. 8. The technical feature of this embodiment lies in the fact that the relationship between the carrier C and the heat exchange surface S under the dropwise condensation state is specified.

(75) With respect to the relationship between the carrier C and the heat exchange surface S under the dropwise condensation phenomenon occurring at the temperature above 0 C., the heat exchange surface S is oriented to be vertical. This vertical orientation is needed in order for the condensed droplets P1 to drop by gravity. As shown in FIG. 8, a general technical problem of the condensation phenomena on the heat exchange surface S is the decrease of the heat transfer through the heat exchange surface S due to the formation of a water membrane on the heat exchange surface S caused by a surface tension of the condensed droplets P1. In this embodiment, a good heat exchange can be maintained without the formation of such a water membrane by disposing the carrier C within the temperature boundary layer BL of the heat exchange surface S so as to treat the condensed droplets P1 on the surface of the carrier C to drop them by gravity.

(76) Since the latent heat exchange due to the condensation phenomena on the surface of the carrier C is added, the heat exchange can be improved, as compared with a case of the heat exchange only on the heat exchange surface S. In this connection, the generation of dew can be caused to improve the heat transfer based on the condensation by effecting the water repellent finishing on the surface of the carrier C, while at the same time, a good condensation phenomena can be caused, since the condensed droplets with small diameters can drop by gravity. In addition, the plugging of the opening O by the condensed droplets can be prevented.

(77) With respect to the relationship among the width W of the carrier C, the width L of the opening O, and the depth, it is considered that the size of the opening O needs to be smaller than that is needed for the formation of the frost, since a secondary growth of the frost so as to plug the opening O is not expected to occur, unlike the first embodiment, so that the water droplets tend to easily reach the heat exchange surface S through the opening O. In this connection, it is surmised that the positive generation of dew on the heat exchange surface S is halted, since the condensation on the surface of the carrier C decreases the water vapor in the atmosphere, so that the water droplets having passed through the opening O in the atmosphere of the space between the heat exchange surface S and the carrier C are reduced.

(78) Embodiment

(79) The inventors confirmed the effectiveness of the present invention by carrying out an experiment concerning the suppression of the frost crystals P4 in which a micro object is disposed within the temperature boundary layer to utilize the condensation and the solidification occurring within the temperature boundary layer to grow the frost crystals P4 within temperature boundary layer to control their growth, with a view to realizing a phenomenon in which the frost crystals P4 is not adhered on the heat exchange surface S.

(80) Experiment Equipment and Method

(81) In this research, the suppression of the formation of the frost on the heat exchange surface S was studied by a metal mesh being disposed within the temperature boundary layer BL to cause the frost crystals P4 to grow on the metal mesh.

(82) An experimental small chamber, a thermostatic system for maintaining the temperature and the humidity in the experimental small chamber constant, a measurement system, an observation system, and a heat transfer section are provided. The temperature and the humidity in the experimental small chamber are controlled by an air conditioner, a humidifier, a dehumidifier and a heater, while the temperature and the humidity in the experimental chamber are measured by an Asman wet-and-dry bulb thermometer disposed in the experimental small chamber.

(83) (1-1) Observation of Frost Crystals P4

(84) FIGS. 9 and 10 show a photograph and a three-dimensional image of the metal mesh used in this research. The metal mesh is planar-woven with 100 m diameter made of steel (SUS304) wires and has an aperture of 150 m.

(85) The heat exchange surface S is made of oxygen-free cupper and polished into a mirror surface (angle of contact by static droplet, =62), and the metal mesh in FIG. 10 is rested and fixed on the heat exchange surface S. In addition, a space is provided between the heat exchange surface S and the metal mesh and the micro object is disposed within the temperature boundary layer.

(86) The observations of the formation and the growth of the frost crystals P4 were made with a digital microscope, focusing both on the heat exchange surface S and the metal mesh, and digitally recording the images. Analytical software was then used to analyze the recorded images.

(87) The observation experiments were carried out under the following conditions: heat exchange surface temperature tw=25 C., the heat exchange surface S (upward-facing) orientation =0.

(88) (1-2) Heat Flux

(89) The frosting phenomenon is a transient process because the frost layer changes with time. It should be noted that the present experiments were conducted under the condition that the heat exchange surface temperature changed with time. The heat flux of [W/m2] on the surface was obtained by using the recorded temperature and the lumped-thermal-mass approximation, which is possible because the heat exchange surface is made of oxygen-free copper.

(90) FIG. 11 shows a schematic diagram of the heat exchange surface. The heat exchange surface consists of 5 oxygen-free cupper plates, each 40 mm wide, 18 mm long, and 10 mm thick. The heat exchange surface is flat and has been polished sufficiently. The sides and the rear of these plates have been insulted with fabric-laminated Bakelite. Further, the rear side of the plates have been thermally insulated with Isowool (having a heat conduction ratio k=0.07 W/m/K at 400 C.). In order to reduce heat transfer from Bakelite into the cooling surface as much as possible, oxygen-free copper plates have been embedded into the heat exchange surface. Note that care has been taken to prevent frost formation on the cooling surface during its initial cooling to a predetermined temperature and before the start of the experiment by covering the heat exchange surface with a polyethylene sheet. To cool the heat transfer section to a predetermined temperature, it was dipped in a Dewar filled with liquid ethanol, which is cooled by liquid nitrogen to a desired temperature. Next, the heat exchange surface was maintained at the predetermined temperature for 10 minutes, and was placed to be oriented vertically in the experimental small chamber to start the experiment. Additional experiments have been carried under each experimental condition with the heat transfer section covered by an insulating member to evaluate the heat loss, which is necessary for the accurate evaluation of the heat flux.

(91) The heat-flux experiments were carried out under the following conditions: moist air temperature, to =25 C.; initial heat exchange surface temperature tw=40 C.; wettability of heat exchange surface or angle of contact, =62; and at distance from the leading edge of the heat exchange surface, y=41, 61, 81 and 101 mm.

(92) (2) Experimental Result and Study

(93) (2-1) Mechanism of Formation and Growth of Frost Crystals P4

(94) The inventors paid attention to the size of the super-cooled water droplets P3 to vary the configuration of the heat exchange surface S by artificially providing fine concave and convex surfaces with several hundred m on the heat exchange surface S, and as a result, succeeded in preventing the frost crystals P4 from growing on the heat exchange surface S (a portion of the heat exchange surface S).

(95) At present, the area in which the frost crystals P4 are not formed amounts to 75% of the entire heat exchange surface S. FIG. 12 shows a typical example of an observation result of the process of the formation and the growth of the frost crystals P4, in a case where fine grooves in a mesh form are machined on the cooling surface.

(96) In a case where the fine grooves in a mesh form are machined, although the convex portion is shaped to be a square, the super-cooled water droplets P3 are generated on the convex surface to be coalesced into big droplets with time after the start of the experiment. The super-cooled water droplets P3 having repeatedly coalesced becomes a single droplet on the square convex surface to form into a protruded plateau ice after the super-cooled state is lost.

(97) The super-cooled state lasts up to fifteen minutes after the start of the experiment, based on the fact that a white ring by a light is confirmed on the central portion.

(98) Next, a plurality of the frost crystals P4 are generated from the protruded plateau ice. In this connection, during the growth of the frost crystals P4, the existence of the frost crystals P4 was not confirmed on the groove portion.

(99) Based on the above observation result, we investigated to form the frost crystals P4 within the temperature boundary layer.

(100) Firstly, a metal mesh with a size substantially same as the convex portion in FIG. 12 is selected as the micro object disposed within the temperature boundary layer and is rested on the heat exchange surface S. FIG. 13 shows an observation result of the formation of the frost crystals P4 in a case where the metal mesh in FIG. 10 is rested on the flat heat exchange surface S. In this connection, the observation was carried out from above. According to the observation, it was confirmed that the super-cooled water droplets P3 are generated on the heat exchange surface S and the surface of the metal mesh, and that a plurality of the frost crystals P4 were generated from the protruded plateau ice on the metal mesh after the loss of the super-cooled state. On the other hand, the frost crystals P4 were not confirmed on the heat exchange surface S.

(101) In addition, when the metal mesh is removed from the heat exchange surface S, the frost formed on the metal mesh immediately melted. Further, the growth of the frost crystals P4 on the heat exchange surface S contacting the metal mesh was not confirmed. FIG. 14 is a sketch illustrating the mechanism of the formation and the growth of the frost crystals P4. The growing speed of the frost crystals P4 is the fastest at the convex portion of the metal mesh, while spherical ice is adhered on the heat exchange surface S after the loss of the super-cooled state, however, the frost crystals P4 was not formed due to the size of the ice being below 150 m.

(102) Next, the experiment was carried out on the condition that a space between the metal mesh used in the observation with respect to FIG. 13 and the heat exchange surface S was provided.

(103) FIG. 15 shows an observation result from side, and FIG. 16 is a sketch drafted based on the observation result. As shown in FIGS. 15 and 16, it was confirmed that the frost crystals P4 are formed to grow on the surface of the metal mesh, but that the frost crystals P4 are not formed to grow on the heat exchange surface S.

(104) Base on the above results, it is considered that we confirmed the effectiveness of the method of controlling the mechanism of the formation and the growth of the frost crystals P4 proposed by this research. In addition, it is considered that the prevention of the formation of the frost on the heat exchange surface S was accomplished, since the frost layer did not grow on the heat exchange surface S at the time when the metal mesh was removed.

(105) (2-2) Heat Transfer Involving Formation of Frost

(106) The comparison of the experimental result between the case where the metal mesh is disposed within the temperature boundary layer BL and the case where the metal mesh is not disposed within the temperature boundary layer BL (the smooth surface) is carried out. FIG. 17 shows a relationship between a heat flux and a temperature of the heat exchange surface S. In this connection, the temperature of the heat exchange surface S in a case where the metal mesh is attached is not a temperature of the surface of the metal mesh, but that of the surface of the heat transfer portion made of oxygen-free copper. As clearly shown in FIG. 17, it was confirmed that the metal mesh does not influence much on the heat flux, since there is not a peculiar difference of the heat flux between the two cases.

(107) FIG. 18 shows a temperature distribution within the temperature boundary layer on the basis of the position of the surface of the frost layer. In this connection, the thickness of the frost layer was measured based on the surface of the frost layer. The heat exchange surface S on which the frost crystals P4 are adhered is oriented to be horizontally upward.

(108) The heat exchange surface S is an end face of a square pillar made of oxygen-free copper with 50 mm wide, 50 mm long, and a copper plate with the thickness of 1 mm is adhered to the end face by epoxy adhesion to form the heat exchange surface. The temperature of the surface of the heat exchange surface S is measured by adhering CA thermocouple (diameter: 100 m) to the underside of the copper plate. The temperature of the surface of frost layer is measured by a thermocouple. The thermocouple is attached in an arc form to a support portion made of Bakelite with a thermal insulating effect to be mounted on a traverse device horizontally and vertically movable relative to the heat exchange surface S through a metal supporting rod. The measurement was conducted in such a way that the temperature within the temperature boundary layer BL is measured by a digital scope, while the temperature of the moist air portion at the position where the thickness of the frost layer is measured is measured as a frost layer surface temperature. The heat transfer portion the side of which is thermally insulated by adhesive made of foamed urethane and silicone was disposed in the experimental small chamber made of Dan puller. It was confirmed that the frost layer surface temperature was below 0 C., so that the frost crystals P4 grew, in a case where the metal mesh is provided.

(109) The embodiments of the present invention are described in detail above. A person skilled in the art may make various modifications and changes insofar as they are not out of the scope of the present invention.

(110) For example, in this embodiment, although dehumidification was carried out within the temperature boundary layer BL by disposing the planar carrier C or the mesh carrier C within the temperature boundary layer BL determined in accordance with the temperature of the exchange surface S, the planar carrier C or the mesh does not need to be disposed, so long as dehumidification is secured within the temperature boundary layer BL.

(111) For example, in this embodiment, although the mesh carrier C is disposed within the temperature boundary layer BL determined in accordance with the temperature of the exchange surface S, and then, is replaced, other physical object by which the formation of the frost is promoted may be disposed, so long as the formation of the frost or the dew on the heat exchange surface S can be prevented.

DESCRIPTION OF REFERENCE SIGNS

(112) HX heat exchanger C carrier S surface of heat exchanger O opening N heat transfer promoter BL temperature boundary layer Tc coolant temperature Tin temperature at inner surface of heat exchanger Tout temperature at outer surface of heat exchanger Tair temperature of moist air Tm temperature of main air flow W width of mesh L width of opening t thickness of heat exchanger Y gap P1 condensation liquid droplet P3 super-cooled water droplet P4 frost