Как выбрать гостиницу для кошек
14 декабря, 2021
The results of ParaSol and Rayfront simulations will be described in this section. Figure 1 shows the annual heating demand as an average value for all four directions for each glazing type and climate. For the Stockholm climate the energy demand decreases from 78.2 kWh/m2,yr to 68.4 kWh/m2,yr for the low-e DG and 67.6 kWh/m2,yr for the AR low-e DG window. The low-e AR DG decrease the energy demand with 2.1% compared to the low-e DG. For all climates, replacing one of the panes in a double-glazed window from a clear to a low-e coated pane reduces the heating demand by 12-14%. Applying an AR-coated low-e pane reduces the heating demand somewhat further, approximately with 1-2%. The total energy saving for this room is about 160-240 kWh/year.
Summertime, the indoor temperature is not extremely high. The most common way to reduce overheating in multi-family houses in Nordic climates is to use cross ventilation by opening windows. The highest temperature without this extra ventilation is 340C for the standard glazing, however just for a couple of hours per year. For the
(h) Figure 2 Duration diagram for Stockholm in the south direction. |
Applying an AR-coating on a low-e window increases the light transmittance by 13% and the transmissivity by 14%. The calculated solar and light transmittance and the transmissivity Tr for the three glazing combinations are displayed in Table 4.
t-value (%) Figure 3 Average values of Tsol in all four directioi for May for each window and climate. |
g-value (%) 70.0 60.0 50.0 40.0 |
30.0 |
20.0 |
10.0 |
Figure 4 The g-values are average monthly values for May in all four directions for each window and place. |
Table 5 The midpoint daylight factors for the different windows.
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energy demand, about 2 percentage points. The calculated daylight factor for the midpoint of the room is shown in table 5. By applying an AR-coating on a low-e coating, the midpoint daylight factor in the room increases from 1.16 to 1.32 or approximately 12%. The difference in Tvis between low-e DG and AR low-e DG is 13% (see table 4) almost the same as the difference in daylight factor. |
low-e windows there are almost 1000h with temperatures over 30oC. Figure 2 describes this as a duration diagram i. e. for Stockholm in the south direction. The Copenhagen and Helsinki climates (not shown here) have very similar results. Figure 3 shows Tsol (average values of all four directions for May) for each window and climate. The difference of the low-e and the AR low-e DG is about 3%. The g-values are shown in figure 4 (average monthly values for May in all four directions) for each window and climate. The difference between g — values of the low-e DG and AR low-e DG is approximately the same as for the