Influence of Roof Windows Area Changes on the Classroom Indoor Climate in the Attic Space: A Case Study
Abstract
:1. Introduction
- ▪ Better utilization of daylight accompanied with proper management;
- ▪ Regular cleaning of windows and bulbs from dust; this can save energy in light;
- ▪ Incorrect lamp maintenance can absorb up to 50% of light through a thick layer of dust;
- ▪ When leaving the room, the last obligation is always to turn off the light.
2. Materials and Methods
- ▪ Measurement of daylight value, Daylight Factor;
- ▪ Prediction of summer overheating;
- ▪ Calculated on the basis of simulation tools based on measured or predicted data;
- ▪ Search for optimization of indoor light and thermal climate.
2.1. Daylight Metrics
- —is the global external horizontal illuminance [lx];
- —is the direct external illuminance, recalculated on the horizontal plane [lx];
- —is the diffuse external horizontal illuminance [lx].
- —is the extraterrestrial illuminance expressed on the horizontal plane [lx];
- —is the luminous extinction coefficient [-];
- —is the optical relative air mass of the atmosphere [-];
- —is the luminous turbidity factor (TV = 4 representing ISO/CIE Type 12 clear sky standard conditions and the environment in common cities areas).
- —is the factor of light transmission at angle from the window normal [-];
- —is the factor of light transmission in normal direction [-];
- —is the factor of dirt reduction for the outer side of the glass [-];
- —is the factor of dirt reduction for the inner side of the glass [-].
- —is luminous flux [lm];
- —is area [m2].
- Einternal—illuminance of internal horizontal plane (lx);
- Eexternal—illuminance of external horizontal plane (lx).
- DFmin—is minimum of daylight factor [%],
- DFaverage—is average value of daylight factor [%].
- AWINDOW—is area of windows [m2];
- AFLOOR—is area of floor [m2];
- AWALL—is area of walls [m2].
2.2. Summer Overheating
- In summer—from + 24 to 28 °C;
- In winter—from + 22 to 24 °C.
- —is the volume of infiltrated air [m3 /s];
- —is the effective area of the orifice through which air can flow [m2];
- ct and cv are the outflow factors for the pressure difference caused by gravity and wind.
- -
- The air temperature changes relatively slowly, rarely rising or falling by more than a few degrees in an hour;
- -
- In the case of sunlight, large and rapid changes in values can occur within a few minutes. This is due to the very sensitive connection to cloudy skies;
- -
- The wind speed can take on multiple values in a few minutes. The record of this quantity is very variable, although it is possible to notice a certain character of increase or decrease during the day. Simplifying such a course of climatic factors into hourly values requires aggregation, which must necessarily omit a large number of sometimes very different records.
- —is opening time of windows [h];
- —is outside air temperature [°C].
3. Case Study—Classroom in Attic of School Building
3.1. Context
3.2. Daylight Rating
3.3. Daylight Measurement and Daylight Simulation
3.4. Prediction of Indoor Climate in Summer Period
4. Discussion
5. Conclusions
Author Contributions
Funding
Acknowledgments
Conflicts of Interest
References
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Area (m2) Side Windows | Area (m2) Roof Lights | Area (m2) Windows (Side + Roof) | Area (m2) Wall | WWR (%) | WFR (%) | |
---|---|---|---|---|---|---|
Variant 0 | 9.3 | 9.20 | 18.5 | 171 | 11 | 39 |
Variant 1 | 9.3 | - | 9.3 | 171 | 5 | 20 |
Variant 2 | 9.3 | 5.50 | 14.8 | 171 | 9 | 32 |
Variant 3 | 9.3 | 11.0 | 20.3 | 171 | 12 | 43 |
Daylight Factor (%)—Measured Values in the Points | ||||
Point | 1 | 2 | 3 | U0 (-) |
A | 12.2 | 5.4 | 2.3 | |
B | 12.7 | 5.0 | 2.8 | |
C | 10.6 | 3.1 | 1.8 | |
0.29 | ||||
Daylight Factor (%)—Simulated Values in the Points Validation—According to Boundary Conditions Obtained from the Measurement | ||||
1 | 2 | 3 | U0 (-) | |
A | 12.3 | 4.9 | 2.0 | |
B | 12.1 | 4.7 | 2.5 | |
C | 9.7 | 2.8 | 1.5 | |
0.26 |
DF | DFmin (%) | DFmax (%) | DFaverage (%) | U0 (-) |
---|---|---|---|---|
Variant 0 | 50 | 47 | 64 | −67 |
Variant 1 | primary | primary | primary | primary |
Variant 2 | 38 | 41 | 51 | −25 |
Variant 3 | 58 | 48 | 68 | −25 |
Nr | Material/Layer (from Outside to Inside) | ρ (kg/m³) | c (J/kgK) | λ (W/mK) | Thickness (m) |
---|---|---|---|---|---|
1 | Cement lime Plaster | 2000 | 850 | 1.2 | 0.02 |
2 | Solid Brick Masonry | 1900 | 850 | 0.6 | 0.45 |
3 | Mineral Insulation Board | 115 | 850 | 0.043 | 0.1 |
4 | Air Layer 50 mm | 1.3 | 1000 | 0.28 | 0.05 |
5 | Gypsum Board | 850 | 850 | 0.2 | 0.013 |
Nr | Material/Layer (from Outside to Inside) | ρ (kg/m³) | c (J/kgK) | λ (W/mK) | Thickness (m) |
---|---|---|---|---|---|
1 | Roofing | 2400 | 1000 | 0.5 | 0.0001 |
2 | Air Layer 100 mm Low ventilated | 1.3 | 1000 | 0.59 | 0.1 |
3 | Mineral Insulation Board | 113 | 850 | 0.040 | 0.18 |
4 | Vapour retarder | 130 | 2300 | 2.3 | 0.0001 |
5 | Air Layer 50 mm | 1.3 | 1000 | 0.28 | 0.05 |
6 | Gypsum Board | 850 | 850 | 0.2 | 0.013 |
Nr | Material/Layer (from Outside to Inside) | ρ (kg/m³) | c (J/kgK) | λ (W/mK) | Thickness (m) |
---|---|---|---|---|---|
1 | Cement lime Plaster | 2000 | 850 | 1.2 | 0.01 |
2 | Steel-Concrete slab | 2300 | 850 | 1.6 | 0.25 |
3 | Mineral Insulation Board | 115 | 850 | 0.043 | 0.06 |
4 | Air Layer 70 mm | 1.3 | 1000 | 0.4 | 0.07 |
5 | Oriented Strand Board | 630 | 1400 | 0.13 | 0.02 |
6 | Oriented Strand Board | 630 | 1400 | 0.13 | 0.02 |
Nr | Material/Layer (from Outside to Inside) | ρ (kg/m³) | c (J/kgK) | λ (W/mK) | Thickness (m) |
---|---|---|---|---|---|
1 | Gypsum Board | 850 | 850 | 0.2 | 0.013 |
2 | Air Layer 120 mm | 1.3 | 1000 | 0.723 | 0.12 |
3 | Mineral Insulation Board | 115 | 850 | 0.043 | 0.04 |
4 | Gypsum Board | 850 | 850 | 0.2 | 0.013 |
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Dolnikova, E.; Katunsky, D.; Vertal, M.; Zozulak, M. Influence of Roof Windows Area Changes on the Classroom Indoor Climate in the Attic Space: A Case Study. Sustainability 2020, 12, 5046. https://doi.org/10.3390/su12125046
Dolnikova E, Katunsky D, Vertal M, Zozulak M. Influence of Roof Windows Area Changes on the Classroom Indoor Climate in the Attic Space: A Case Study. Sustainability. 2020; 12(12):5046. https://doi.org/10.3390/su12125046
Chicago/Turabian StyleDolnikova, Erika, Dusan Katunsky, Marian Vertal, and Marek Zozulak. 2020. "Influence of Roof Windows Area Changes on the Classroom Indoor Climate in the Attic Space: A Case Study" Sustainability 12, no. 12: 5046. https://doi.org/10.3390/su12125046
APA StyleDolnikova, E., Katunsky, D., Vertal, M., & Zozulak, M. (2020). Influence of Roof Windows Area Changes on the Classroom Indoor Climate in the Attic Space: A Case Study. Sustainability, 12(12), 5046. https://doi.org/10.3390/su12125046