Experimental and Numerical Study on the Insulation Performance of a Photo-Thermal Roof in Hot Summer and Cold Winter Areas

: The use of a solar architecture system is a feasible way to reduce the energy consumption of a building. The system also has important signiﬁcance to the “Dual-carbon” plan. In this study, the heat transfer characteristics of a photo-thermal roof were analyzed in hot summer and cold winter zones; a model to calculate insulation performance was established. In the summer climate, the thermal performances of the photo-thermal roof and an ordinary roof were explored through experiments and simulations. The results showed that the heat transfer and temperature of the photothermal roof were lower than those of the ordinary roof. Heat transfer through a photo-thermal roof can be changed by adjusting the water ﬂow of collectors. The water saturation of insulation materials is an important factor that affects the insulation performance of a roof. Compared with the ordinary roof, the change in water saturation was shown to have less impact on the insulation performance of the photo-thermal roof. The water saturation increased from 0 to 30%, while the heat transfer per unit area of the photo-thermal roof only increased by 0.9 W/m 2 ; 97.3% lower than that of the ordinary roof. The effect of reducing the insulation material thickness was less for the photo-thermal roof than for the ordinary roof. When the insulation material thickness was reduced from 100 mm to 0 mm, the average temperature in the indoor non-working area reached 38.5 ◦ C and 27.1 ◦ C in the ordinary roof and the photo-thermal roof, respectively. The insulation thickness of the photo-thermal roof had little effect on the indoor air temperature. The research results provide a reference for the roof energy-saving design of new buildings and the roof energy-saving transformation of existing buildings.


Introduction
In order to ensure the sustainable development of human society, the "Dual-carbon" plan was proposed. The "Dual-carbon" plan is a "carbon emission peak and carbon neutrality" plan. The main way to achieve the goals of the "Dual-carbon" plan is to reduce the consumption of fossil energy to reduce greenhouse gas emissions [1]. Energy consumption by buildings accounts for more than one-third of global energy consumption, and the carbon dioxide emissions of buildings account for 40% of the total emissions worldwide [2,3]. Moreover, with the continuous improvement of people's living standards, building energy consumption will continue to grow [4,5]. Therefore, it is important to achieve the goals of the "Dual-carbon" plan in the construction field as soon as possible, reduce the energy consumption of buildings and develop renewable energy utilization technology through building energy conservation technology research [6].

Experimental Measurements
In the experiment, temperature signals were collected by a k-type thermocouple with an accuracy level of 1 and a measurement error of less than 0.1%. The room studied under summer conditions was is an air-conditioned room, with the area 1 m from the inner surface of the roof being a non-working area. As shown in Figure 2, temperature detectors were placed on the roof surfaces, in the non-working area, and in the water inlet and outlet. The main temperature signals collected were: the internal and external roof surface temperature and the inlet and outlet water temperatures. Additionally, detectors were used to record the outdoor air temperature. The data acquisition unit (XSR-70A) is used to record the temperature data in real time. The radiation recorder (TBQ-2) was used to measure the solar irradiance of the test site. Test equipment and parameters are shown in Table 1.

Experimental Measurements
In the experiment, temperature signals were collected by a k-type thermocouple with an accuracy level of 1 and a measurement error of less than 0.1%. The room studied under summer conditions was is an air-conditioned room, with the area 1 m from the inner surface of the roof being a non-working area. As shown in Figure 2, temperature detectors were placed on the roof surfaces, in the non-working area, and in the water inlet and outlet. The main temperature signals collected were: the internal and external roof surface temperature and the inlet and outlet water temperatures. Additionally, detectors were used to record the outdoor air temperature. The data acquisition unit (XSR-70A) is used to record the temperature data in real time. The radiation recorder (TBQ-2) was used to measure the solar irradiance of the test site. Test equipment and parameters are shown in Table 1.    As shown in Figure 3a, solar rays reached the photo-thermal roof, and a small portion were reflected by the glass cover of the collector, while the rest were absorbed by the collector. The collector converted solar radiation into heat. Most of the heat was used to heat the heat-carrying fluid and was carried away by the heat-carrying fluid. Some heat caused the temperature of the collector to increase. The collector then dissipated heat to the surrounding environment through convection and radiation. During heat dissipation by the collector, some of the heat was transferred to the room through the roof. The heat transfer conducted by the ordinary roof is shown in Figure 3b. The solar radiation directly reached the outer surface of the roof and increased the temperature of the roof, and the heat directly entered the room through the roof.  As shown in Figure 3a, solar rays reached the photo-thermal roof, and a small portion were reflected by the glass cover of the collector, while the rest were absorbed by the collector. The collector converted solar radiation into heat. Most of the heat was used to heat the heat-carrying fluid and was carried away by the heat-carrying fluid. Some heat caused the temperature of the collector to increase. The collector then dissipated heat to the surrounding environment through convection and radiation. During heat dissipation by the collector, some of the heat was transferred to the room through the roof. The heat transfer conducted by the ordinary roof is shown in Figure 3b. The solar radiation directly reached the outer surface of the roof and increased the temperature of the roof, and the heat directly entered the room through the roof.  The energy balance equation of the heat transfer model can be expressed using Equation (1) [30].
Since the thicknesses of each solid material layer of the solar collectors and roofs were much smaller than their length and widths, their heat conduction can be regarded as onedimensional along the z-axis direction (height direction). Ignoring the diffusion component and viscosity dissipation, the above formula can be transformed into Equation (2).
The equation of energy balance was established with the collector as the research object as shown in Equation (3).

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In Equation (3), the left-hand side of the equation represents the internal energy of the collector, whereas the right-hand side of the equation represents the heat gain term, the heat conduction term, and the heat loss term. The heat loss of the collector includes two main parts. One part is the heat emitted by the collector and the external environment through radiation and convection, and the other part is the heat loss that results from heating the fluid in the collector. As the distance between the collector and the outer surface of the roof was very small, only 100 mm, and the coverage area of the collector was large, there was little natural wind between the collector and the roof. In the hot summer condition, the temperature of the rear cover plate of the normal working collector was higher than that of the outer surface of the roof, making it difficult for natural convection between them. Therefore, it was assumed that the air between the collector and the roof was almost stagnant. The convective heat transfer between the collector's rear cover and the roof was not considered. S h can be expressed using Equation (4).
Taking the outside surface of the photo-thermal roof as the research object, the heat balance equation can be expressed as shown in Equation (5).
Equation (6) is the energy balance equation for the photo-thermal roof.
where S h represents the heat gain of the photo-thermal roof, determined using (5). S h can be expressed using Equation (7).
Different from the photo-thermal roof, heat gain by the ordinary roof mainly came from direct solar irradiation. Taking the outer surface of the ordinary roof as the research object, the heat balance equation was established, as shown in Equation (8).
Equation (9) is the heat transfer energy balance equation for the ordinary roof.
where S h represents heat gain by the ordinary roof, determined using Equation (8). S h can be expressed using Equation (10).
Although the collectors performed strongly in terms of heat accumulation, most of this heat energy was used to produce domestic hot water. The heat gained by the photo-thermal roof mainly came from radiant heat transfer between the collectors and the roof. However, the ordinary roof directly absorbed solar irradiation, converted it into heat energy, and transferred it to the rooms.
According to Equations (6) and (9), when the heat received on the roof outer surface and the roof structure is constant, the heat entering the room through the roof is only related to the effective thermal conductivity of the roof's insulation materials, and the more effective the thermal conductivity is, the more heat that is transferred into the room through the roof.

The Effective Thermal Conductivity of the Roof's Insulation Material
Building thermal insulation materials are mostly porous media filled with air and moisture. The volume ratio of air and water changes depending on the environmental temperature and humidity. Therefore, building insulation materials are actually a mixture of solid-phase insulation materials, liquid-phase water, and air, which can be expressed using Equation (11).
Among these three substances, the volume of the solid-phase insulation material does not change, while the volume of air decreases as the liquid water content increases. The volume of liquid water can be expressed as water saturation using Equation (12).
The thermal conductivity of water is greater than that of air. When the liquid water content in the pores increases, the volume of air will reduce, and the effective thermal conductivity of the material will increase. When the pores are filled with air and water, due to the hydrophilicity of the solid surfaces of the pores, the volume of liquid water, and other factors, the distribution of liquid water varies widely. It is difficult to accurately calculate the effective thermal conductivity of the insulation material. If the heat conduction of the porous medium satisfies the requirements of the parallel heat conduction model, its effective thermal conductivity can be expressed using Equation (13) [31].
If the heat conduction of the porous medium satisfies the requirements of the serial heat conduction model, its effective thermal conductivity can be calculated using Equation (14) [31].
The above two methods of calculating the effective thermal conductivity represent the extreme conditions. In reality, the situation is somewhere in between.
In this study, stone wool board with a porosity of 95% was used as the roof insulation material. This material has a monofilament fiber thermal conductivity of about 1.25 W/(m·K) [32]. When the rock wool board was used as the roof insulation material, heat transfer was directed in the direction of its thickness. Some studies have pointed out that the interior part of the rock wool board was mainly composed of a large number of rock wool monofilament fibers and a small number of slag balls [32]. In the thickness direction, the inclined lapping of monofilament fibers of the rock wool board at different angles did not represent single horizontal or vertical placement, and a small number of slag balls were also randomly scattered inside, leading to the coexistence of serial heat conduction and parallel heat conduction in the rock wool board. In addition, the distribution of liquid water in the pores of the porous media was irregular. In order to simplify the analysis, the effective thermal conductivity was calculated by Equation (16).
The above calculation method shows the variation law of effective thermal conductivity for the roof insulation material used in this study, and this is also shown in Figure 4. the interior part of the rock wool board was mainly composed of a large number of rock wool monofilament fibers and a small number of slag balls [32]. In the thickness direction, the inclined lapping of monofilament fibers of the rock wool board at different angles did not represent single horizontal or vertical placement, and a small number of slag balls were also randomly scattered inside, leading to the coexistence of serial heat conduction and parallel heat conduction in the rock wool board. In addition, the distribution of liquid water in the pores of the porous media was irregular. In order to simplify the analysis, the effective thermal conductivity was calculated by Equation (16).
The above calculation method shows the variation law of effective thermal conductivity for the roof insulation material used in this study, and this is also shown in Figure  4.  As shown in Figure 4, the effective thermal conductivity calculated by the parallel heat conduction model changes linearly with the water saturation. In the serial heat conduction model, when the water saturation is less than 80%, the effective thermal conductivity increases slightly as the water saturation increases, from 0.025 W/(m·K) to 0.108 W/(m·K). When the water saturation is more than 80%, the change in the effective thermal conductivity relative to the water saturation increases sharply, from 0.108 W/(m·K) to 0.616 W/(m·K).
The varied relationship between the effective thermal conductivity and the water saturation calculated according to Equation (16) is shown in Figure 4. The water saturation can affect the effective thermal conductivity of rock wool board over a large range. With an increase in the water saturation, the effective thermal conductivity of rock wool board also increases. When the water saturation increases from 0% to 100%, the effective thermal conductivity increases by 933.3%, in theory. With an increase in water saturation from 0% to 30%, the effective thermal conductivity increases from 0.06 W/(m·K) to 0.14 W/(m·K), an increase of 60.7%.

Simulation Conditions
In order to determine the similarities and differences in thermal performance between the photo-thermal roof and the ordinary roof, a numerical simulation was used to create two physical models. One was a simplified three-dimensional model of an air-conditioned room with a photo-thermal roof, and the other was an ordinary air-conditioned room with the same bare roof structure and materials. The numerical model was calculated with FLUENT software. In order to simplify the model, a water pipe and its surrounding components in the center of the collector of the photo-thermal roof were considered to have the smallest width unit.
Considering the limited cooling capacity of the air conditioner, the air area of the top floor room was divided into two parts according to height. One part was the area of air 1000 mm below the roof, the non-working area, and the other part was the personnel working area. The air conditioner was able to maintain a constant temperature of 26°C in the working area. Due to close contact with the roof, the temperature of the non-working area was affected by heat transfer from the roof and the temperature of the working area. In order to further simplify the model, only 0.5 m of the indoor air-conditioned area and its upper space components were modeled. In order to further simplify the model, only the non-working area and the area 0.5 m below it were modeled. The minimum size of the numerical model was 134 mm × 2000 mm × (δ + 1906) mm, where δ is the thickness of the insulation layer of the roof, which represents the amount of change.
The size of the water pipes in the solar collector was 8 × 2000 × 8 mm, and the distance between the two water pipes was 126 mm. The components used in the model were all general materials with general dimensions, and the dimensions and materials are shown in Table 2. This simulation introduced the solar ray tracing model. The geographical location was set to 27.88 • N, 112.87 • E with a time zone of +8. Ideal weather conditions were set as clear and cloudless, and the time was adjusted to obtain different solar radiation conditions. The DO radiation model was chosen, and the value of angular discretization was increased appropriately to obtain a more accurate simulation result. For the turbulence model, k-ε equation models with high accuracy were used. The boundary conditions of the model are shown in Table 3. The simulated values of the meteorological parameters varied according to the purpose of the simulation. When using experimental data to verify the model, the meteorological parameters needed to be adjusted to be consistent with the experimental data. When using the model to explore practical problems, the meteorological parameters used were the typical meteorological parameters for Xiangtan City in summer [33], and the specific values are listed in Table 4. The air density is affected by temperature. Therefore, the Boussinesq hypothesis was set to represent air density to simplify the solution. The coefficient of thermal expansion of air was set to 0.0037/k. The SIMPLEC algorithm was used to calculate the incompressible flow field. In the solving process, when the variable residuals of the continuity equation, momentum equation, k equation, and e equation were less than 10 −3 and the variable residuals of energy equations and the radiation equation were less than 10 −6 , convergence of the calculation was considered to be achieved.

Simulation Verification
Simulation verification was carried out using experimental data collected on July 12. Figure 5 shows that the solar radiation intensity was basically stable at about 930 W/m 2 , and the air temperature was stable at about 37.8 • C during the period from 10:00 to 14:30. When the solar radiation intensity and air temperature remained constant, roof heat transfer reached a steady state. The outside surface temperature of the ordinary roof continued to rise from 10:00 to 14:00, and the temperature did not rise after reaching the maximum value of 53.0 • C at 14:30. At this time, the outside surface temperature of the ordinary roof reached the corresponding steady-state value. Compared with the ordinary roof, the rise in the outside surface temperature of the photo-thermal roof was slightly delayed. The total phase delay can be calculated using Equation (17), and the delay time of the outside surface of the photo-thermal roof was 2 h. Therefore, the outside surface temperature of the photo-thermal roof reached a steady-state value of 37.0 • C at 16:30. According to Equation (17) [34], the delay time of the inner surface of the roof was 5.5 h. Therefore, under a stable external thermal environment, the inner surface temperature of the ordinary roof reached its corresponding steady-state value of 43.2 • C at 20:00, and the inner surface temperature of the photo-thermal roof reached its corresponding steady-state value of 36.8 • C at 23:00.
Buildings 2022, 12, x FOR PEER REVIEW 10 of 24 When the solar radiation intensity and air temperature remained constant, roof heat transfer reached a steady state. The outside surface temperature of the ordinary roof continued to rise from 10:00 to 14:00, and the temperature did not rise after reaching the maximum value of 53.0 °C at 14:30. At this time, the outside surface temperature of the ordinary roof reached the corresponding steady-state value. Compared with the ordinary roof, the rise in the outside surface temperature of the photo-thermal roof was slightly delayed. The total phase delay can be calculated using Equation (17), and the delay time of the outside surface of the photo-thermal roof was 2 h. Therefore, the outside surface temperature of the photo-thermal roof reached a steady-state value of 37.0 °C at 16:30. According to Equation (17) [34], the delay time of the inner surface of the roof was 5.5 h. Therefore, under a stable external thermal environment, the inner surface temperature of the ordinary roof reached its corresponding steady-state value of 43.2 °C at 20:00, and the inner surface temperature of the photo-thermal roof reached its corresponding steady-state value of 36.8 °C at 23:00.
Under the experimental conditions, the solar radiation intensity was 930 W/m 2 , the air temperature was 37.8 °C , the thickness of the roof insulation layer was 100 mm, and the average water temperature in the collector was 50 °C . These values were substituted into the numerical calculation model. Considering that the experimental building was a new building, the roof had an excellent waterproofing performance. Therefore, the saturation rate was set to 0. It was calculated that the outer and inner surface temperatures of the ordinary roof were 54.3 °C and 38.7 °C , respectively, and the outer and inner surface temperatures of the photo-thermal roof were 30.7 °C and 28.1 °C , respectively. In general, the values simulated by the photo-thermal system were slightly smaller than the experimental values. This is because the radiation heat transfer between the wall and roof was not considered in the simulation calculation. In order to analyze the error between the experimental value and the simulated value, the relative error calculation results are shown in Table 5.  The photo-thermal roof outer surface temperature The photo-thermal roof inner surface temperature Air temperature The ordinary roof outer surface temperature The ordinary roof inner surface temperature Solar radiation intensity Under the experimental conditions, the solar radiation intensity was 930 W/m 2 , the air temperature was 37.8 • C, the thickness of the roof insulation layer was 100 mm, and the average water temperature in the collector was 50 • C. These values were substituted into the numerical calculation model. Considering that the experimental building was a new building, the roof had an excellent waterproofing performance. Therefore, the saturation rate was set to 0. It was calculated that the outer and inner surface temperatures of the ordinary roof were 54.3 • C and 38.7 • C, respectively, and the outer and inner surface temperatures of the photo-thermal roof were 30.7 • C and 28.1 • C, respectively. In general, the values simulated by the photo-thermal system were slightly smaller than the experimental values. This is because the radiation heat transfer between the wall and roof was not considered in the simulation calculation. In order to analyze the error between the experimental value and the simulated value, the relative error calculation results are shown in Table 5.  Table 5 shows that the simulated value for the ordinary roof was relatively close to the experimental value, and the maximum value of relative error (RE) was 8.1%. The simulated value for the photo-thermal roof was slightly different from the experimental value, and the maximum RE was 11.1%. The root-mean-squared error (RMSE) was 3.3. This suggests that the experimental values are in good agreement with the simulated values.

Experimental Results and Analysis
The thermal insulation performance of the roofs was tested during the hot season in 2021. Experimental data from seven consecutive sunny days from 8 to 14 July 2021 were used. The first three days were cloudy, and the influence of clouds on the solar radiation intensity value was greater on those three days than on the next four days. The relationships between the roofs' internal and external surface temperatures and the solar radiation intensity and air temperature are shown in Figure 5.
As can be seen from Figure 5, the temperature and solar radiation intensity values measured in the experiment showed periodic changes. The solar radiation intensity began to rise from about 6:00, reaching a maximum of about 900 W/m 2 from 10:00 to 14:30, and then gradually decreasing before dropping to 0 W/m 2 after 19:00. The outdoor air temperature fluctuated between 31.1 and 38.6 • C and reached its maximum value at 14:00-15:30 every day.
The roof temperature changed periodically under the influences of the solar radiation intensity and air temperature. However, the peaks of different temperature curves occurred at different times and the magnitude of the temperature fluctuation differed. The outer surface temperature of the ordinary roof reached a maximum value of about 53.3 • C from 13:00 to 14:30 and then gradually decreased until the next wave cycle began at 7:30 the next day. There was a delay in the inner surface temperature fluctuations of the ordinary roof, whereby a maximum temperature of about 42.3 • C occurred between 18:00 and 19:30 every day, before gradually decreasing and reaching a minimum value at about 10:30 the next day. The temperature fluctuations were roughly similar, but the peaks and peak times differed slightly over different periods due to fluctuations in the solar radiation intensity and air temperature during the day. The solar radiation intensity fluctuated greatly in the first three days of the experiment, the air temperature was lower, the peak of each temperature was slightly lower, and the peak appeared slightly earlier than on the last four days.
As can be seen from Figure 5, on July 12, the weather was fine with few solar rays shielded by clouds, and the meteorological conditions were in line with the typical local summer climate. Therefore, July 12 was selected as a typical day and used to analyze the relationships among various temperatures. To cover the full cycle of each curve, the timeline for typical days to 0:30 on July 12 until 12:30 on July 13. Figure 6 shows the experimental data for the typical day. During the typical day, the outdoor air temperature was 31.7-38.2 °C , the solar radiation intensity increased from 6:00 to a maximum of 930 W/m 2 from 11:00 to 14:30 and then gradually decreased to 0 W/m 2 after 19:00.
As shown in Figure 6, the outer and inner surface temperatures of the photo-thermal roof were significantly lower than those of the ordinary roof for most of the study period. On the typical day, the outer and inner surface temperature peaks of the ordinary roof were 53.0 °C and 43.3 °C , while those of the photo-thermal were 37.0 °C and 36.8 °C , respectively. Under the same thermal disturbance conditions, the outer and inner surface temperature peaks of the photo-thermal roof reduced by 30.2% and 15.0%, respectively, compared with those of the ordinary roof. The heat gain of the roofs was composed of solar radiation and heat transfer from the surrounding air. The decrease in the outer surface temperature peak of the photo-thermal roof indicates a decrease in heat gain on the roof surface and a decrease in the amount of heat transferred to the inner surface of the roof through the roof structure.
This occurred because the solar irradiation on the photo-thermal roof was partly used to heat the water flow in the collector and partly used to increase the temperature of the collector, and then the heat from the collector was transferred to the outer surface of the roof. The air layer between the collector and the roof also weakened the amount of heat transfer. However, the ordinary roof was exposed directly to solar rays. When the outdoor air temperature was the same, the temperature peak of the outer surface of the ordinary roof was higher than that of the photo-thermal roof. Figure 6 also shows that, for the ordinary roof, the outer surface temperature peak time was 14:30, the inner surface temperature peak time was 19:50, and the temperature wave delay time was 5 h and 20 min. The outer surface temperature of the photo-thermal During the typical day, the outdoor air temperature was 31.7-38.2 • C, the solar radiation intensity increased from 6:00 to a maximum of 930 W/m 2 from 11:00 to 14:30 and then gradually decreased to 0 W/m 2 after 19:00.
As shown in Figure 6, the outer and inner surface temperatures of the photo-thermal roof were significantly lower than those of the ordinary roof for most of the study period. On the typical day, the outer and inner surface temperature peaks of the ordinary roof were 53.0 • C and 43.3 • C, while those of the photo-thermal were 37.0 • C and 36.8 • C, respectively. Under the same thermal disturbance conditions, the outer and inner surface temperature peaks of the photo-thermal roof reduced by 30.2% and 15.0%, respectively, compared with those of the ordinary roof. The heat gain of the roofs was composed of solar radiation and heat transfer from the surrounding air. The decrease in the outer surface temperature peak of the photo-thermal roof indicates a decrease in heat gain on the roof surface and a decrease in the amount of heat transferred to the inner surface of the roof through the roof structure.
This occurred because the solar irradiation on the photo-thermal roof was partly used to heat the water flow in the collector and partly used to increase the temperature of the collector, and then the heat from the collector was transferred to the outer surface of the roof. The air layer between the collector and the roof also weakened the amount of heat transfer. However, the ordinary roof was exposed directly to solar rays. When the outdoor air temperature was the same, the temperature peak of the outer surface of the ordinary roof was higher than that of the photo-thermal roof. Figure 6 also shows that, for the ordinary roof, the outer surface temperature peak time was 14:30, the inner surface temperature peak time was 19:50, and the temperature wave delay time was 5 h and 20 min. The outer surface temperature of the photo-thermal roof reached its maximum value at 16:30 and the inner surface temperature reached its maximum value at 22:00. Compared to the ordinary roof, the temperature wave on the outer surface of the photo-thermal roof was delayed by 2 h and the inner surface temperature wave was delayed by 4 h.
In terms of the amplitude of the roof surface temperature, the order, from small to large, was as follows: the inner surface of the photo-thermal roof, the outer surface of the photo-thermal roof, the inner surface of the ordinary roof, the outer surface of the ordinary roof. On the typical day, the amplitudes were 2.0 • C, 4.5 • C, 7.3 • C, and 20.5 • C, respectively.
The outer surface temperature amplitude of the photo-thermal roof was 78.0% lower than that of the ordinary roof, and the amplitude of the surface temperature inside the photo-thermal roof was reduced by 72.6%. Thus, the photo-thermal roof was shown to have better thermal stability.
As shown in Figure 7, the change trend for the interior and exterior surface temperature difference between the ordinary roof and the photo-thermal roof was similar to that observed for solar radiation intensity. Although there was a delay in the increase in the inner surface temperature of the roofs, the time which the maximum temperature difference between the roof interior and exterior surface occurred was basically the same as that of the solar radiation intensity. When the solar radiation intensity was maximal, the roof outer surface received the most heat, while the inner surface released heat to the room at a low level, so the roof heat storage was maximal, as was the inner and outer surface temperature difference. photo-thermal roof was reduced by 72.6%. Thus, the photo-thermal roof was shown to have better thermal stability. As shown in Figure 7, the change trend for the interior and exterior surface temperature difference between the ordinary roof and the photo-thermal roof was similar to that observed for solar radiation intensity. Although there was a delay in the increase in the inner surface temperature of the roofs, the time which the maximum temperature difference between the roof interior and exterior surface occurred was basically the same as that of the solar radiation intensity. When the solar radiation intensity was maximal, the roof outer surface received the most heat, while the inner surface released heat to the room at a low level, so the roof heat storage was maximal, as was the inner and outer surface temperature difference. The maximum temperature difference between the inner and outer surfaces was 14.2 °C for the ordinary roof and 1.5 °C for the photo-thermal roof, as shown in Figure 7. Thus, in the photo-thermal roof, heat transfer was only one-ninth that in the ordinary roof under the experimental conditions. This shows that the photo-thermal roof has better insulating properties than the ordinary roof.

Effect of Water Saturation
In order to explore the influence of changes in the water saturation of insulation materials on the insulation performance of the photo-thermal roof, simulation studies were carried out when the water saturation level was 0, 10%, 20%, and 30%. The solar radiation intensity was set to 1000 W/m 2 , the air temperature to 35.8 °C , the roof insulation thickness was set to 100 mm, and the water flow was adjusted to keep the pipe wall temperature constant at 50 °C to determine the relationship between the temperature, heat flux, and water saturation for the top room model with the photo-thermal roof and the ordinary The maximum temperature difference between the inner and outer surfaces was 14.2 • C for the ordinary roof and 1.5 • C for the photo-thermal roof, as shown in Figure 7. Thus, in the photo-thermal roof, heat transfer was only one-ninth that in the ordinary roof under the experimental conditions. This shows that the photo-thermal roof has better insulating properties than the ordinary roof.

Effect of Water Saturation
In order to explore the influence of changes in the water saturation of insulation materials on the insulation performance of the photo-thermal roof, simulation studies were carried out when the water saturation level was 0, 10%, 20%, and 30%. The solar radiation intensity was set to 1000 W/m 2 , the air temperature to 35.8 • C, the roof insulation thickness was set to 100 mm, and the water flow was adjusted to keep the pipe wall temperature constant at 50 • C to determine the relationship between the temperature, heat flux, and water saturation for the top room model with the photo-thermal roof and the ordinary room, as shown in Figures 8 and 9.  An increase in water saturation led to an increase in the effective thermal conductivity of the roof, which enhances the heat transfer of the roof. The data presented in Figures  8 and 9 show that when the water saturation rose from 0 to 30%, the heat flux per unit area of the ordinary roof rose from 65.9 W/m 2 to 99.1 W/m 2 , an increase of 50.4%; the inner surface temperature of the ordinary roof rose from 39.4 °C to 45.6 °C , an increase of 15.7%; and the air temperature 400 mm below the roof increased from 33.1 °C to 36.8 °C , an increase of 11.1%. Owing to the enhanced heat transfer, the outer surface temperature of the roofs decreased. When the water saturation rose from 0 to 30%, the outer surface temperature of the ordinary roof dropped from 55.1 °C to 53.2 °C , and the temperature gradient of the roof in the vertical direction dropped from 52.3 °C /m to 25.3 °C /m. Thus, as the water saturation of the roof insulation material increased, the heat transfer of the roof increased and the inner surface temperature and indoor air temperature increased, even though the temperature difference between the inner and outer surfaces of the roof may have reduced. The heat radiation from the inner surface of the roofs to the rooms was enhanced.  An increase in water saturation led to an increase in the effective thermal conductivity of the roof, which enhances the heat transfer of the roof. The data presented in Figures  8 and 9 show that when the water saturation rose from 0 to 30%, the heat flux per unit area of the ordinary roof rose from 65.9 W/m 2 to 99.1 W/m 2 , an increase of 50.4%; the inner surface temperature of the ordinary roof rose from 39.4 °C to 45.6 °C , an increase of 15.7%; and the air temperature 400 mm below the roof increased from 33.1 °C to 36.8 °C , an increase of 11.1%. Owing to the enhanced heat transfer, the outer surface temperature of the roofs decreased. When the water saturation rose from 0 to 30%, the outer surface temperature of the ordinary roof dropped from 55.1 °C to 53.2 °C , and the temperature gradient of the roof in the vertical direction dropped from 52.3 °C /m to 25.3 °C /m. Thus, as the water saturation of the roof insulation material increased, the heat transfer of the roof increased and the inner surface temperature and indoor air temperature increased, even though the temperature difference between the inner and outer surfaces of the roof may have reduced. The heat radiation from the inner surface of the roofs to the rooms was enhanced. An increase in water saturation led to an increase in the effective thermal conductivity of the roof, which enhances the heat transfer of the roof. The data presented in Figures 8  and 9 show that when the water saturation rose from 0 to 30%, the heat flux per unit area of the ordinary roof rose from 65.9 W/m 2 to 99.1 W/m 2 , an increase of 50.4%; the inner surface temperature of the ordinary roof rose from 39.4 • C to 45.6 • C, an increase of 15.7%; and the air temperature 400 mm below the roof increased from 33.1 • C to 36.8 • C, an increase of 11.1%. Owing to the enhanced heat transfer, the outer surface temperature of the roofs decreased. When the water saturation rose from 0 to 30%, the outer surface temperature of the ordinary roof dropped from 55.1 • C to 53.2 • C, and the temperature gradient of the roof in the vertical direction dropped from 52.3 • C/m to 25.3 • C/m. Thus, as the water saturation of the roof insulation material increased, the heat transfer of the roof increased and the inner surface temperature and indoor air temperature increased, even though the temperature difference between the inner and outer surfaces of the roof may have reduced. The heat radiation from the inner surface of the roofs to the rooms was enhanced.
When the water saturation increased from 0 to 10%, the inner surface temperature and heat transfer of the roofs changed sharply. The inner surface temperature of the ordinary roof increased by 4 • C, and the heat flux per unit area increased by 21.0 W/m 2 . However, the inner surface temperature of the photo-thermal roof only increased by 0.1 • C, and the heat flux of the roof only increased by 0.6 W/m 2 .
With an increase in the water saturation, the change pattern of the photo-thermal roof temperature was similar to that of the ordinary roof. However, the photo-thermal roof showed a smaller temperature fluctuation. When the water saturation increased from 0 to 30%, the inner surface temperature of the photo-thermal roof rose from 28.4 • C to 28.6 • C, an increase of 0.2 • C. Compared with the ordinary roof, the temperature rise was 96.8% lower. The heat flux per unit area of the photo-thermal roof increased from 11.5 W/m 2 to 12.4 W/m 2 , an increase of 0.9 W/m 2 . Compared with the ordinary roof, the increase was 97.3% lower. As the water saturation increased, the temperature of the non-working area in the photo-thermal room did not show obvious fluctuations, and the indoor air temperature distribution was more uniform.
In summary, compared with the ordinary roof, the photo-thermal roof has smaller heat transfer, lower roof temperature and indoor non-air-conditioned area temperature. An increase in water saturation of insulation materials will enhance the heat transfer of roofs. However, an increase in water saturation has less negative impact on photo-thermal buildings than on ordinary buildings.

Effect of the Thickness of Roof Insulation Materials
In order to obtain an excellent thermal insulation performance, roof materials with low thermal conductivity are usually used. There are certain requirements regarding the thickness of thermal insulation materials. In hot summer and cold winter zones, 100 mm thick rock wool boards are usually used as roof insulation materials.
To determine the relationships among the temperature, heat flux, and roof insulation material thickness with the photo-thermal roof and the ordinary roof, the solar radiation intensity was set to 1000 W/m 2 , the air temperature was set to 35.8 • C, the water saturation level was set to 0, and the water flow was adjusted to keep the pipe wall temperature constant at 50 • C, as shown in the Figures 10 and 11. With an increase in the water saturation, the change pattern of the photo-thermal roof temperature was similar to that of the ordinary roof. However, the photo-thermal roof showed a smaller temperature fluctuation. When the water saturation increased from 0 to 30%, the inner surface temperature of the photo-thermal roof rose from 28.4 °C to 28.6 °C , an increase of 0.2 °C . Compared with the ordinary roof, the temperature rise was 96.8% lower. The heat flux per unit area of the photo-thermal roof increased from 11.5 W/m 2 to 12.4 W/m 2 , an increase of 0.9 W/m 2 . Compared with the ordinary roof, the increase was 97.3% lower. As the water saturation increased, the temperature of the non-working area in the photo-thermal room did not show obvious fluctuations, and the indoor air temperature distribution was more uniform.
In summary, compared with the ordinary roof, the photo-thermal roof has smaller heat transfer, lower roof temperature and indoor non-air-conditioned area temperature. An increase in water saturation of insulation materials will enhance the heat transfer of roofs. However, an increase in water saturation has less negative impact on photo-thermal buildings than on ordinary buildings.

Effect of the Thickness of Roof Insulation Materials
In order to obtain an excellent thermal insulation performance, roof materials with low thermal conductivity are usually used. There are certain requirements regarding the thickness of thermal insulation materials. In hot summer and cold winter zones, 100 mm thick rock wool boards are usually used as roof insulation materials.
To determine the relationships among the temperature, heat flux, and roof insulation material thickness with the photo-thermal roof and the ordinary roof, the solar radiation intensity was set to 1000 W/m 2 , the air temperature was set to 35.8 °C , the water saturation level was set to 0, and the water flow was adjusted to keep the pipe wall temperature constant at 50 °C , as shown in the Figures 10 and 11.  As shown in Figures 10 and 11, the inner surface temperature and the indoor nonworking area temperature of the roofs increased as the thickness of the insulation material decreased, while the temperature of the roof outer surface decreased. The heat flux of the roofs increased as the thickness of the insulation material decreased. When the thickness of insulation material was 100 mm, in contrast with the high temperature of 55.1 °C measured on the outside surface of the ordinary roof, the temperature of the photo-thermal roof was only 31.1 °C , a decrease of 43.2%. The inner surface temperature of the photothermal roof was 28.4 °C , which is 27.9% lower than that of the ordinary roof. The heat transfer per unit area of the photo-thermal roof also decreased from 65.9 W/m 2 to 11.5 W/m 2 , a decrease of 82.5%.
When the insulation material thickness was reduced to 0, the inner surface temperature of the ordinary roof was 50.2 °C and the heat flux was 181.1 W/m 2 . Under the same conditions, the inner surface temperature of the photo-thermal roof was 28.6 °C , a reduction of 38.0% compared with that of the ordinary roof, and the heat flux was 19.2 W/m 2 , a reduction of 89.4% compared with the ordinary roof.
As shown in Figures 10 and 11, the indoor non-working area temperature of the ordinary roof reached to 40.1 °C when the thickness of the insulation material was reduced from 100 mm to 0 mm. In the same situation, the maximum temperature of the indoor non-working area of the photo-thermal room was only 28.1 °C , slightly higher than the temperature of the working area. Therefore, even when the thickness of the insulation layer was 0 mm, the photo-thermal roof still had an excellent thermal insulation performance.
Under actual conditions, the water saturation of the roof insulation materials may change periodically and cannot always be maintained in a completely dry state. If the thickness and water saturation of the roof insulation material changes, the inner surface temperature and heat flux will change under the above environmental conditions. Changes are shown in Figures 12 and 13. As shown in Figures 10 and 11, the inner surface temperature and the indoor nonworking area temperature of the roofs increased as the thickness of the insulation material decreased, while the temperature of the roof outer surface decreased. The heat flux of the roofs increased as the thickness of the insulation material decreased. When the thickness of insulation material was 100 mm, in contrast with the high temperature of 55.1 • C measured on the outside surface of the ordinary roof, the temperature of the photo-thermal roof was only 31.1 • C, a decrease of 43.2%. The inner surface temperature of the photo-thermal roof was 28.4 • C, which is 27.9% lower than that of the ordinary roof. The heat transfer per unit area of the photo-thermal roof also decreased from 65.9 W/m 2 to 11.5 W/m 2 , a decrease of 82.5%.
When the insulation material thickness was reduced to 0, the inner surface temperature of the ordinary roof was 50.2 • C and the heat flux was 181.1 W/m 2 . Under the same conditions, the inner surface temperature of the photo-thermal roof was 28.6 • C, a reduction of 38.0% compared with that of the ordinary roof, and the heat flux was 19.2 W/m 2 , a reduction of 89.4% compared with the ordinary roof.
As shown in Figures 10 and 11, the indoor non-working area temperature of the ordinary roof reached to 40.1 • C when the thickness of the insulation material was reduced from 100 mm to 0 mm. In the same situation, the maximum temperature of the indoor non-working area of the photo-thermal room was only 28.1 • C, slightly higher than the temperature of the working area. Therefore, even when the thickness of the insulation layer was 0 mm, the photo-thermal roof still had an excellent thermal insulation performance.
Under actual conditions, the water saturation of the roof insulation materials may change periodically and cannot always be maintained in a completely dry state. If the thickness and water saturation of the roof insulation material changes, the inner surface temperature and heat flux will change under the above environmental conditions. Changes are shown in Figures 12 and 13.
A change in water saturation affects the effective thermal conductivity of the roof: the greater the water saturation, the greater the heat transfer of the roof, the lower the outer surface temperature of the roof, and the higher the inner surface temperature.
As shown in Figures 12 and 13, a decrease in the thickness of the roof insulation material or an increase in water saturation will promote heat transfer in the roof. When the thickness of the insulation material was constant, the heat transfer of the two roofs continuously increased, and the inner surface temperature of the roofs increased constantly as the water saturation level increased. When the water saturation level was 30% and the thickness of the roof insulation material was 100 mm, the inner surface temperature of the ordinary roof was 45.6 • C and the heat flux was 99.1 W/m 2 . The inner surface temperature of the photo-thermal roof was 28.6 • C, 41.5% lower than that of the ordinary roof. The heat flux of the photo-thermal roof was 12.4 W/m 2 , 87.5% lower than that of the ordinary roof. When the water saturation level was 30% and the thickness of the roof insulation material was 25 mm, the inner surface temperature of the ordinary roof was 48.9 • C and the heat flux was 155.6 W/m 2 . The inner surface temperature of the photo-thermal roof was 28.5 • C, 41.7% lower than that of the ordinary roof. The heat flux of the photo-thermal roof was 16.9 W/m 2 , 89.1% lower than that of the ordinary roof. It can also be seen from Figures 11 and 12 that the inner surface temperature of the photothermal roof was about 28.5 • C, which is only about 2.5 • C higher than the working area temperature as the thickness of the roof insulation layer changed from 100 mm to 25 mm and the water saturation of the insulation material increased from 0 to 30%. Thus, even when the insulation layer thickness was 25 mm and the water saturation level was high, the insulation performance of the photo-thermal roof was still good.  A change in water saturation affects the effective thermal conductivity of the roof: the greater the water saturation, the greater the heat transfer of the roof, the lower the outer surface temperature of the roof, and the higher the inner surface temperature.
As shown in Figures 12 and 13, a decrease in the thickness of the roof insulation material or an increase in water saturation will promote heat transfer in the roof. When the thickness of the insulation material was constant, the heat transfer of the two roofs continuously increased, and the inner surface temperature of the roofs increased constantly as the water saturation level increased. When the water saturation level was 30% and the thickness of the roof insulation material was 100 mm, the inner surface temperature of the ordinary roof was 45.6 °C and the heat flux was 99.1 W/m 2 . The inner surface temperature of the photo-thermal roof was 28.6 °C , 41.5% lower than that of the ordinary roof. The heat flux of the photo-thermal roof was 12.4 W/m 2 , 87.5% lower than that of the ordinary roof. When the water saturation level was 30% and the thickness of the roof insulation material  A change in water saturation affects the effective thermal conductivity of the roof: the greater the water saturation, the greater the heat transfer of the roof, the lower the outer surface temperature of the roof, and the higher the inner surface temperature.
As shown in Figures 12 and 13, a decrease in the thickness of the roof insulation material or an increase in water saturation will promote heat transfer in the roof. When the thickness of the insulation material was constant, the heat transfer of the two roofs continuously increased, and the inner surface temperature of the roofs increased constantly as the water saturation level increased. When the water saturation level was 30% and the thickness of the roof insulation material was 100 mm, the inner surface temperature of the ordinary roof was 45.6 °C and the heat flux was 99.1 W/m 2 . The inner surface temperature of the photo-thermal roof was 28.6 °C , 41.5% lower than that of the ordinary roof. The heat flux of the photo-thermal roof was 12.4 W/m 2 , 87.5% lower than that of the ordinary roof. When the water saturation level was 30% and the thickness of the roof insulation material In summary, a decrease in the thickness of insulation material will lead to an increase in cooling load. In order to reduce the energy consumption of an air conditioner, the thickness of insulation material should be appropriately increased. The roof insulation layer is often made of porous materials. Water entering the pores of porous materials will weaken the thermal insulation performance of the roof. With high water saturation and thin thickness of the insulation layer, the photo-thermal roof can still maintain a good thermal insulation performance.

Variation in the Average Water Temperature of the Collectors
In practical projects, a certain level of moisture exists in a building's thermal insulation materials, and the thermal conductivity is corrected. Generally, the corrected effective thermal conductivity of rock wool board is 0.07 W/(m·K). Figure 14 shows the influence of the water temperature in the collector on the temperature distribution of the room when the solar radiation intensity was 1000 W/m 2 , the air temperature was 35.8 • C, and the thickness of the rock wool board was 100 mm.
in cooling load. In order to reduce the energy consumption of an air conditioner, the thickness of insulation material should be appropriately increased. The roof insulation layer is often made of porous materials. Water entering the pores of porous materials will weaken the thermal insulation performance of the roof. With high water saturation and thin thickness of the insulation layer, the photo-thermal roof can still maintain a good thermal insulation performance.

Variation in the Average Water Temperature of the Collectors
In practical projects, a certain level of moisture exists in a building's thermal insulation materials, and the thermal conductivity is corrected. Generally, the corrected effective thermal conductivity of rock wool board is 0.07 W/(m·K). Figure 14 shows the influence of the water temperature in the collector on the temperature distribution of the room when the solar radiation intensity was 1000 W/m 2 , the air temperature was 35.8 °C , and the thickness of the rock wool board was 100 mm. As shown in Figure 14, the temperature of the photo-thermal roof and the non-working area increased as the average water temperature in the collectors increased. When the average water temperature rose from 50 °C to 90 °C , the outer surface temperature of the photo-thermal roof rose from 29.9 °C to 36.5 °C , an increase of 6.6%. The inner surface temperature of the photo-thermal roof increased from 28.4 °C to 32.4 °C , an increase of 14.1%. The average temperature of the indoor non-working area increased from 26.9 °C to 29.1 °C , an increase of 8.2%. However, compared with the temperature of the ordinary roof, the photo-thermal roof still showed an excellent insulation effect. Even when the average water temperature in the collectors was 90 °C , compared with the temperature of the ordinary roof, the outer surface temperature of the photothermal roof decreased by 32.7%, the inner surface temperature decreased by 23.9%, and the average temperature in the indoor non-working area decreased by 15.2%. The increase of the average water temperature also increases the roof temperature gradient. When the average water temperature rose from 50 °C to 90 °C , the vertical temperature gradient of the photo-thermal roof rose from 5.0 W/m to 13.6 W/m. However, when the average water temperature was 90 °C , the temperature gradient of the photo-thermal roof was still 64.8% lower than that of the ordinary roof. As shown in Figure 14, the temperature of the photo-thermal roof and the non-working area increased as the average water temperature in the collectors increased. When the average water temperature rose from 50 • C to 90 • C, the outer surface temperature of the photo-thermal roof rose from 29.9 • C to 36.5 • C, an increase of 6.6%. The inner surface temperature of the photo-thermal roof increased from 28.4 • C to 32.4 • C, an increase of 14.1%. The average temperature of the indoor non-working area increased from 26.9 • C to 29.1 • C, an increase of 8.2%. However, compared with the temperature of the ordinary roof, the photo-thermal roof still showed an excellent insulation effect. Even when the average water temperature in the collectors was 90 • C, compared with the temperature of the ordinary roof, the outer surface temperature of the photothermal roof decreased by 32.7%, the inner surface temperature decreased by 23.9%, and the average temperature in the indoor non-working area decreased by 15.2%. The increase of the average water temperature also increases the roof temperature gradient. When the average water temperature rose from 50 • C to 90 • C, the vertical temperature gradient of the photo-thermal roof rose from 5.0 W/m to 13.6 W/m. However, when the average water temperature was 90 • C, the temperature gradient of the photo-thermal roof was still 64.8% lower than that of the ordinary roof.
When the solar radiation intensity was 1000 W/m 2 , the air temperature was 35.8 • C, the thickness of the rock wool board was 100 mm, and the effective thermal conductivity was 0.07 W/(m·K), the heat transfer of the photo-thermal roof was affected by the change in the average water temperature in the collectors, as shown in Figure 15.
It can be seen from Figure 15 that an increase in the average water temperature in the collectors led to an increase in the photothermal roof heat transfer. When the water temperature increased from 50 • C to 90 • C, the roof heat transfer increased from 11.4 W/m 2 to 29.7 W/m 2 , an increase of 160.5%. This occurred because the radiant heat transfer between the collector's rear cover and the roof is the main source of heat received by the photo-thermal roof. The increase in the average water temperature also increased the temperature of the collector's rear cover and enhanced the radiant heat transfer of the collector to the photo-thermal roof. When the solar radiation intensity was 1000 W/m 2 , the air temperature was 35.8 °C , the thickness of the rock wool board was 100 mm, and the effective thermal conductivity was 0.07 W/(m·K), the heat transfer of the photo-thermal roof was affected by the change in the average water temperature in the collectors, as shown in Figure 15. It can be seen from Figure 15 that an increase in the average water temperature in the collectors led to an increase in the photothermal roof heat transfer. When the water temperature increased from 50 °C to 90 °C , the roof heat transfer increased from 11.4 W/m 2 to 29.7 W/m 2 , an increase of 160.5%. This occurred because the radiant heat transfer between the collector's rear cover and the roof is the main source of heat received by the photothermal roof. The increase in the average water temperature also increased the temperature of the collector's rear cover and enhanced the radiant heat transfer of the collector to the photo-thermal roof.
Under the same environmental conditions, the heat transfer of the ordinary roof was 82.1 W/m 2 . Even when the average water temperature was 90 °C , the heat transfer of the photo-thermal roof was 65.0% lower than that of the ordinary roof.
In order to explore the possibility of reducing the thickness of the thermal insulation layer of the photo-thermal roof under high water temperature, this paper also simulated a photo-thermal roof without insulation materials.
When the solar radiation intensity was 1000 W/m 2 , the air temperature was 35.8 °C and the average water temperature in the collectors was 90 °C , and the thickness of the insulation layer was adjusted; the temperature distribution in the photo-thermal room is shown in Figure 16. Under the same environmental conditions, the heat transfer of the ordinary roof was 82.1 W/m 2 . Even when the average water temperature was 90 • C, the heat transfer of the photo-thermal roof was 65.0% lower than that of the ordinary roof.
In order to explore the possibility of reducing the thickness of the thermal insulation layer of the photo-thermal roof under high water temperature, this paper also simulated a photo-thermal roof without insulation materials.
When the solar radiation intensity was 1000 W/m 2 , the air temperature was 35.8 • C and the average water temperature in the collectors was 90 • C, and the thickness of the insulation layer was adjusted; the temperature distribution in the photo-thermal room is shown in Figure 16. As shown in Figure 16, when the thickness of the insulation layer decreased from 100 mm to 0 mm, the vertical temperature gradient of the roof decreased from 13.7 °C /m to 1.3 °C /m, the outer surface temperature of the roof decreased from 36.5 °C to 3.2 °C , the inner surface temperature increased from 32.4 °C to 32.8 °C , and the average temperature of the indoor non-working area increased from 29.1 °C to 29.3 °C . Under the above simulated conditions, when the thickness of the insulation layer changed from 100 mm to 0 As shown in Figure 16, when the thickness of the insulation layer decreased from 100 mm to 0 mm, the vertical temperature gradient of the roof decreased from 13.7 • C/m to 1.3 • C/m, the outer surface temperature of the roof decreased from 36.5 • C to 3.2 • C, the inner surface temperature increased from 32.4 • C to 32.8 • C, and the average temperature of the indoor non-working area increased from 29.1 • C to 29.3 • C. Under the above simulated conditions, when the thickness of the insulation layer changed from 100 mm to 0 mm, the roof heat transfer increased from 29.7 W/m 2 to 31.5 W/m 2 . Therefore, the vertical temperature gradient of the photo-thermal roof is greatly reduced without insulation materials, but the increase of roof heat transfer is small. The roof insulation layer is not set, which increases the heat transfer coefficient and enhances the heat transfer of the photo-thermal roof. However, most of the heat by solar irradiation is absorbed by the water flow in the collector, and the heat transmitted to the roof is small. Increasing the heat transfer coefficient of the roof can increase the heat transfer less. From the above data, the heat transfer of the photo-thermal roof without the insulation layer is only increased by 0.8 W/m 2 , the inner surface temperature is increased by 0.4 • C, and the average temperature of the indoor non-working area is increased by 0.2 • C. When the water temperature is 90 • C, the cancellation of the insulation layer of the photo-thermal roof has little impact on the thermal insulation performance of the roof.
In summary, since the water flow in the collector takes away the heat energy converted by solar energy, the thermal insulation performance of photo-thermal roof is better. An increase in the average water temperature of the collector will lead to an increase in the heat transfer of the photo-thermal roof, the roof temperature, and the indoor non-working area temperature. However, when the average water temperature is 90 • C, compared with ordinary roofs, the photo-thermal roof still has smaller heat transfer, lower roof temperature, and indoor non-working area temperature. At this time, even if the insulation material thickness was reduced to 0 mm, the photo-thermal roof still has good thermal insulation performance.

Conclusions
This paper studies the thermal insulation performance of a building roof combined with photothermal technology. In the summer climate of a hot summer and cold winter area, the thermal performance of the photo-thermal roof and the ordinary roof is simulated, and the following conclusions are obtained: (1) Compared with the ordinary roof, the photo-thermal roof has smaller heat transfer, and lower roof temperature and indoor non-working area temperature. Adjusting the water flow of collectors can change the heat transfer through the roof. The photo-thermal roof has better insulation performance than the ordinary roof. Under the action of outdoor calculated temperature of air conditioning in summer, when the solar radiation intensity is 1000 W/m 2 , the heat transfer per unit area of the photo-thermal roof is 82.5% lower than that of the ordinary roof.
(2) The water saturation of roof insulation materials is an important factor affecting insulation performance, and the influence of water saturation on the insulation performance of the ordinary roof is greater than that of the photo-thermal roof. Under the simulated conditions, the water saturation increases from 0 to 30%, the inner surface temperature of the ordinary roof rise is 6.2 • C, the photo-thermal roof temperature rise is only 0.2 • C, a decrease of 96.8%; the heat transfer per unit area of the ordinary roof increases by 33.2 W/m 2 , and the photo-thermal roof increases by 0.9 W/m 2 , a decrease of 97.3%.
(3) The influence of the insulation material thickness change on the insulation performance of the photo-thermal roof is less than the ordinary roof. When the thickness is very small, the photo-thermal roof still has excellent insulation performance. When the roof insulation layer is cancelled, the inner surface temperatures of the ordinary roof and the photo-thermal roof are 50.2 • C and 28.6 • C, respectively, and the average temperature of the indoor non-working area can reach 38.5 • C and 27.1°C, respectively. The insulation thickness of the photo-thermal roof can be reduced or even cancelled.