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24-Bld-A5 Building Science · May 2017

Question 3 of 6

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

07-Bld-A5 Building Science — National Exam, May 2017. Six questions of 20 marks each were printed; per the paper's own NOTES only the first five in the answer book are graded, but all six are answered below as a complete study resource.

Reference texts: ASHRAE Handbook — Fundamentals (Chapters 1 Psychrometrics, 14 Climatic Design Information, 16 Ventilation and Infiltration, 25 Thermal and Water Vapor Transmission Data, 26 Heat, Air, and Moisture Control in Building Assemblies); McQuiston, Parker & Spitler, Heating, Ventilating, and Air Conditioning: Analysis and Design; National Building Code of Canada (NBCC).

Question 3 (20 marks)

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Given.

Location, date, time and collector geometry
ParameterValue
Latitude L44° N
Longitude80° W
DateJuly 21 (day 202 of the year)
Time1:00 PM
Collector surface azimuthEast
Collector tilt from horizontal, Σ45°
Check: two inputs are assumed since they were not in the printed data — (1) clock time is taken as solar time (no equation-of-time/longitude correction, the standard simplification at this exam level); (2) ground reflectance ρᵣ = 0.2, the ASHRAE default for ordinary (non-snow) ground.

Find. Total solar irradiation (direct + diffuse + ground-reflected) on the tilted, east-facing collector at the stated time, using the ASHRAE clear-sky model.

S (horizon) N collector tilt 45°, faces East sun, 1:00 PM β=63.3° alt φ=32.7° W of S θ=62.6° (angle of incidence) Sun-collector geometry, Toronto 44°N, July 21, 1:00 PM
A steeper (45°) tilt than a 60° collector turns the surface further toward the zenith, cutting the angle of incidence to the afternoon sun.

Approach. Find the solar position (declination, hour angle, altitude, azimuth) for the stated place/date/time, resolve the angle of incidence on the tilted east-facing surface, then evaluate the ASHRAE clear-sky direct, diffuse and ground-reflected components and sum them.

  1. Solar declination for day n = 202 (July 21): $$\delta = 23.45\sin\left(\frac{360(284+n)}{365}\right) = 23.45\sin(479.3^\circ) = 20.44^\circ$$
  2. Hour angle at 1:00 PM, one hour past solar noon (15°/hour): H = 15°.
  3. Solar altitude β, from sinβ = cosL·cosδ·cosH + sinL·sinδ: $$\sin\beta = \cos(44^\circ)\cos(20.44^\circ)\cos(15^\circ) + \sin(44^\circ)\sin(20.44^\circ) = 0.8937 \Rightarrow \boxed{\beta = 63.3^\circ}$$
  4. Solar azimuth φ (from south, +west), from sinφ = cosδ·sinH/cosβ: $$\sin\phi = \frac{\cos(20.44^\circ)\sin(15^\circ)}{\cos(63.3^\circ)} = 0.540 \Rightarrow \phi = 32.7^\circ\ \text{(west of south, afternoon)}$$
  5. Angle of incidence θ on the tilted east-facing surface (surface azimuth γ = −90° from south), using $$\cos\theta = \cos\beta\cos(\phi-\gamma)\sin\Sigma + \sin\beta\cos\Sigma$$ $$\cos\theta = \cos(63.3^\circ)\cos(122.7^\circ)\sin(45^\circ) + \sin(63.3^\circ)\cos(45^\circ) = 0.460 \Rightarrow \boxed{\theta = 62.6^\circ}$$ The shallower 45° tilt (vs. a steeper collector) points more toward the zenith and less toward the low afternoon sun, but still catches it at a moderate incidence angle rather than a grazing one.
  6. Direct-normal irradiation, ASHRAE clear-sky model, July constants A = 1085 W/m², B = 0.207: $$I_{DN} = \frac{A}{\exp(B/\sin\beta)} = \frac{1085}{\exp(0.207/0.894)} = 861\ \text{W/m}^2$$
  7. Direct component on the tilted surface: $$I_{DT} = I_{DN}\cos\theta = 861\times 0.460 = 396\ \text{W/m}^2$$
  8. Diffuse component (C = 0.136 for July): $$I_{dT} = C\,I_{DN}\frac{1+\cos\Sigma}{2} = 0.136\times 861\times\frac{1+0.707}{2} = 100\ \text{W/m}^2$$
  9. Ground-reflected component (ρᵣ = 0.2): $$I_{rT} = I_{DN}(\sin\beta+C)\,\rho_g\,\frac{1-\cos\Sigma}{2} = 861\times(0.894+0.136)\times 0.2\times\frac{1-0.707}{2} = 26\ \text{W/m}^2$$
  10. Total irradiation on the collector: $$\boxed{I_T = I_{DT}+I_{dT}+I_{rT} = 396+100+26 = 522\ \text{W/m}^2}$$
Problem 3 — final results
QuantityValue
Declination δ20.44°
Solar altitude β63.3°
Solar azimuth φ32.7° W of S
Angle of incidence θ62.6°
Direct-normal Iₑₙ861 W/m²
Direct on collector Iₑ₄396 W/m²
Diffuse on collector Iₜ₄100 W/m²
Ground-reflected Iₛ₄26 W/m²
Total irradiation Iₔ522 W/m²