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International Journal on Architectural Science, Volume 8, Number 4, p.98-113, 2011
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98
A DISCUSSION ON THE DESIGN PRINCIPLES OF A PATENTED
PORTABLE DIRECT SUNLIGHT LIGHT-DUTY UNIVERSAL HELIODON
MOUNTED ON A CAMERA TRIPOD
K.P. Cheung
Department of Architecture, The University of Hong Kong, Hong Kong, China
(Received 10 October 2012; Accepted 11 January 2013)
ABSTRACT
Heliodons are physical tools developed to study and test the solar performance of physical building models by
simulating direct sunlight to impinge onto building models, for various desirable combinations of latitude, day,
and time.
In the learning process of architecture students and in professional architecture design processes, small and light
weight working models are always made first for studying various design objectives including solar
performance. The preferred one or two optional designs will then be further developed and formed into physical
models of larger size with more details, and developed into computational models, for in-depth and detailed
study of various design objectives including solar performance.
This paper discusses the design principles of a patented portable direct sunlight light-duty universal heliodon
mounted on a camera tripod which is affordable, easily stored up and assembled for use. The patented heliodon
is useful for testing the direct sunlight effect of small foam board or card board models of buildings, or building
components.
The “universal” capability of a heliodon attributes to its adjustment flexibility to test the model for all simulated
desirable combinations of latitude, day, and time, for any simulated place in the world where the actual building
will be built, from most north places to most south places. The patented heliodon was initially designed for
outdoor operation, using “direct sunlight” available at any place, any time in the world, as the light source, to
avoid light source error of artificial light. Furthermore, this heliodon can be mounted on a camera tripod
commonly used for holding cameras, eliminating the special provision of a heliodon stand which is a key factor
affecting the cost and storage space, and hence the portability and affordability of the heliodon.
1. INTRODUCTION Heliodons are physical tools developed to study
and test the solar performance of building models
by simulating direct sunlight to impinge onto
building models, for various desirable
combinations of latitude, day, and time.
The adjustable variables of heliodons are [1-3]:
- the latitude variable, which defines the sun
paths in relation to the geographical location
[Fig. 3, Fig. 3a],
- the seasonal variation, which relates to the
declination of the sun on a given day [Fig. 3,
Fig. 3a, Table 1],
- hourly change of the sun from East to West
during the day.
The heliodons developed so far could be broadly
categorized into two categories:
- a fixed light source (single lamp or multiple
lamps) [2,7-9], or a moving light source [1,2]
with the building model rotated and/or tilted,
- the building model is placed horizontally and
stationary, and the light source moves [4-6,
10-13].
Since the first heliodon developed in 1931 [1, Fig.
1], traditionally heliodons are tools located in
architectural school laboratories, occupying a
room, and not convenient for practicing architects
to use, because it takes time and effort to transport
the building models to the laboratories.
For convenient and popular use of heliodons, the
size, portability, and affordability of the heliodon
are also important factors. A patented portable
direct sunlight light-duty universal heliodon [14,
Fig. 2] addressing these issues has been developed,
and its design principles are discussed in this paper.
International Journal on Architectural Science
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Fig. 1: Dufton & Beckett Heliodon of 1931 [1, 2, 16, Table 1] Note that d is the solar declination angle [Fig. 3, Table 1], and L is latitude in Northern Hemisphere shown in the above
configuration.
Fig. 2: The patented portable direct sunlight
light-duty universal heliodon [14] - View
showing outdoor operation using direct
sunlight as the light source, mounted on a
camera tripod set at two possible
combinations of latitude, day, and time:
[Fig. 7, Fig. 4, Fig. 5, Fig. 8]
- For Northern Hemisphere : 10 am,
Apparent Solar Time, 45 degree latitude,
5 May or 7 August, noting that the top
point of the globe is the north pole [Fig.
3]
- For Southern Hemisphere : 2 pm,
Apparent Solar Time, 45 degree latitude,
4 Feb or 7 November, noting that the top
point of the globe is the south pole [Fig.
3a]
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Table 1: Mean value of the solar declination [Ref. 15, for l99l, noon UT (GMT), adapted from Ref. 16]
DAY JAN FEB MAR APR MAY JUN JUL AUG SEPT OCT NOV DEC
1 -23 01 -17 10 -07 40 +04 27 +15 01 +22 02 +23 08 +18 04 +08 22 -03 06 -14 22 -21 46
2 -22 56 -16 53 -07 17 +04 50 +15 19 +22 10 +23 03 +17 49 +08 00 -03 29 -14 41 -21 55
3 -22 51 -16 35 -06 54 +05 14 +15 37 +22 17 +22 59 +17 34 +07 38 -03 53 -15 00 -22 04
4 -22 45 -16 17 -06 31 +05 36 +15 54 +22 24 +22 54 +17 18 +07 16 -04 16 -15 18 -22 13
5 -22 38 -15 59 -06 08 +05 59 +16 11 +22 31 +22 49 +17 02 +06 54 -04 39 -15 37 -22 20
6 -22 31 -15 41 -05 45 +06 22 +16 28 +22 38 +22 43 +16 46 +06 32 -05 02 -15 55 -22 28
7 -22 24 -15 23 -05 22 +06 45 +16 45 +22 44 +22 37 +16 29 +06 09 -05 25 -16 13 -22 35
8 -22 16 -15 04 -04 59 +07 07 +17 02 +22 50 +22 30 +16 12 +05 47 -05 48 -16 30 -22 42
9 -22 08 -14 45 -04 35 +07 30 +17 18 +22 55 +22 23 +15 55 +05 24 -06 11 -16 48 -22 48
10 -21 59 -14 25 -04 12 +07 52 +17 34 +23 00 +22 16 +15 38 +05 01 -06 34 -17 05 -22 54
11 -21 50 -14 06 -03 48 +08 14 +17 49 +23 04 +22 08 +15 20 +04 39 -06 56 -17 22 -22 59
12 -21 41 -13 46 -03 25 +08 36 +18 05 +23 08 +22 00 +15 02 +04 16 -07 19 -17 38 -23 04
13 -21 31 -13 26 -03 01 +08 58 +18 20 +23 12 +21 52 +14 44 +03 53 -07 41 -17 54 -23 08
14 -21 21 -13 06 -02 37 +09 20 +18 35 +23 15 +21 43 +14 26 +03 30 -08 04 -18 10 -23 12
15 -21 10 -12 45 -02 14 +09 41 +18 49 +23 18 +21 34 +14 07 +03 07 -08 26 -18 26 -23 15
16 -20 59 -12 25 -01 50 +10 03 +19 03 +23 21 +21 24 +13 48 +02 44 -08 48 -18 41 -23 18
17 -20 47 -12 04 -01 26 +10 24 +19 17 +23 23 +21 14 +13 29 +02 21 -09 10 -18 56 -23 21
18 -20 35 -11 43 -01 02 +10 45 +19 30 +23 24 +21 04 +13 10 +01 57 -09 32 -19 10 -23 23
19 -20 23 -11 21 -00 39 +11 06 +19 43 +23 25 +20 53 +12 51 +01 34 -09 54 -19 25 -23 25
20 -20 10 -11 00 -00 15 +11 27 +19 56 +23 26 +20 42 +12 31 +01 11 -10 16 -19 38 -23 26
21 -19 57 -10 38 +00 09 +11 47 +20 08 +23 26.4 +20 31 +12 11 +00 47 -10 37 -19 52 -23 26.3
22 -19 44 -10 17 +00 33 +12 07 +20 21 +23 26 +20 19 +11 51 +00 24 -10 58 -20 05 -23 26.4
23 -19 30 -09 55 +00 56 +12 28 +20 32 +23 26 +20 07 +11 31 +00 01 -11 20 -20 18 -23 26.1
24 -19 16 -09 33 +01 20 +12 47 +20 44 +23 25 +19 55 +11 11 -00 23 -11 41 -20 30 -23 25
25 -19 01 -09 10 +01 44 +13 07 +20 55 +23 24 +19 42 +10 50 -00 46 -11 01 -20 42 -23 24
26 -18 46 -08 48 +02 07 +13 27 +21 05 +23 22 +19 29 +10 29 -01 09 -12 22 -20 54 -23 22
27 -18 31 -08 26 +02 31 +13 46 +21 16 +23 20 +19 16 +10 09 -01 33 -12 42 -21 05 -23 20
28 -18 15 -08 03 +02 54 +14 05 +21 26 +23 18 +19 02 +09 47 -01 56 -13 03 -21 16 -23 18
29 -17 59 +03 18 +14 24 +21 35 +23 15 +18 48 +09 26 -02 19 -13 23 -21 26 -23 15
30 -17 43 +03 41 +14 42 +21 44 +23 11 +18 34 +09 05 -02 43 -13 43 -21 36 -23 11
31 -17 27 +04 04 +21 53 +18 19 +08 43 -14 02 -23 07
Note: Declination to north of the Equator is positive, to south is negative; thus for 11 Jan l99l, solar declination
angle was 21 deg 50 min south of the Equator.
2. THE DESIGN PRINCIPLES OF THE
PATENTED PORTABLE DIRECT
SUNLIGHT LIGHT-DUTY UNI-
VERSAL HELIODON
The Dufton & Beckett Heliodon of 1931, [1, Fig. 1]
which is well illustrated and discussed in many
books, and the patented portable direct sunlight
light-duty universal heliodon [Fig. 2], are in fact
both designed on the same basic solar-geographical
principles listed below. The patented heliodon now
reported, however has a more extensive coverage
on application ranges, exhibiting its “universal”
capability:
- The components simulate the sun-earth
system for Northern Hemisphere [Fig. 3].
However, in the patented heliodon now
reported, the sun-earth system for Southern
Hemisphere is also simulated [Fig. 3a].
- It is assumed that sunlight is practically
parallel, and impinges at same angles onto the
buildings,and hence building models, located
at surface of earth, and fictitiously at the
centre of the earth, because the distance of the
earth from the sun (about 150 million km) is
much greater than the diameter of the earth
(about 12,756 km), and the diameter of the
sun (about 1,380,000 km), in the ratio of
about 117590:1:108.
- The day scale surface of The Dufton &
Beckett Heliodon of 1931 [1, Fig. 1], shows
the simulated days for Northern Hemisphere
application, and the lamp holder and the day
scale is detached from the model platform
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base frame. However, in the patented
heliodon now reported [Fig. 1, Fig. 4, Fig. 5,
Fig. 6], the simulated days are marked on the
day scale for both Northern Hemisphere
application, and Southern Hemisphere
application, and the day scale is integrally
attached to the model platform base frame.
For both heliodons, the straight lines marking
the various days, hence the corresponding
solar declination angle [15, 16, Table 1] are
set parallel to the axis of rotation of the model
platform; the same axis being the simulated
earth axis, the axis of rotation for change of
time of a day [Fig. 1, Fig. 2, Fig. 3, Fig. 3a,
Fig. 7, Fig. 8, Fig. 9].
- Apparent solar time is used as the basic time
scale. However, in the patented heliodon now
reported, the outer circular time scale ring is
for Apparent Solar Time indication. Also an
additional inner time scale ring is provided for
local standard time indication, following
established adjustment procedures [10,17,
Table 2, Fig. 15]. In both time scales, the
leading hour number is for use in Northern
Hemisphere application, and the following
hour number is for Southern Hemisphere
applications, thus, “10/14” means 10 am for
Northern Hemisphere application and 14:00,
or 2 pm for Southern Hemisphere application
[2,7,10,15, Fig. 7, Fig. 11, Table 2, Fig. 15].
- The model platform of The Dufton & Beckett
Heliodon of 1931 [1, Fig. 1], is basically set
for Northern Hemisphere. However, in the
patented heliodon now reported, the model
platform can be set to any desirable latitudes
of both the Northern Hemisphere and the
Southern Hemisphere [Fig. 1, Fig. 2, Fig. 7,
Fig. 8, Fig. 9].
- The model is tilted and moved during
heliodon operation.
- The light source used in The Dufton &
Beckett Heliodon of 1931 [1, Fig. 1], is
commonly an artificial lamp placed
sufficiently far away from the heliodon, yet
giving sufficient illumination onto the
building model being tested. However, in the
patented heliodon now reported, direct
sunlight which is moving, is the preferred
light source. Because of its portability and its
integral provision of the day scale onto the
rotating simulated earth-latitude-time system
assembly, NOW forming an integrated
simulated earth-latitude-time-DAY system
assembly, all mounted on a camera tripod,
will enable quick, efficient, and accurate
operation procedures to be carried out,
yielding accurate results of good light quality.
[Fig. 2, Fig. 7, Fig. 8, Fig. 9, Fig. 9a, Fig. 10]
Of course, an artificial light source can be
used for the patented heliodon now reported
[Fig. 12], but errors will result, because no
artificial light source can truly simulate direct
sunlight. Note that in the photos showing the
operation of the patented heliodon, the
latitude scale component of the patented
documents [14, Fig. 2] has been replaced by
an enhanced latitude component [Fig. 9, Fig.
9a, Fig. 11, Fig. 11a, Fig. 12], based on the
same solar-geographical principle.
Table 2: [adapted from Ref. 10] Adjustment for Local Standard Time (LST) : Illustration on the steps to
adjust the Inner time ring of the patented heliodon to read Local Standard Time RELATIVE TO
Apparent Solar Time (AST), shown by the outer time ring
Apparent solar time of local meridian of Hong Kong University
at 114 deg.8 min. East
12:00 noon (AST) 12:00 noon (AST)
Equation of Time (if slow, add; if fast, subtract) [ 17, Table 3] 8 Nov
16.3 min(sun fast)
20 Feb
13.8 min (sun slow)
Mean Solar Time of Meridian [17] 11:43.7 [a.m.] 12:13.8 [p.m.]
Correction for difference between local meridian (114 deg.8
min. East) of Hong Kong university and the related time zone
meridian at 120 deg. East at rate of 1 deg.=4 min. (If standard
time zone meridian lies to West, subtract the correction, if to
East, add) [17]
23.5 min 23.5 min
Hong Kong Standard Time (watch time, or mobile phone time) 12:7.2 [p.m.] 12:37.3 [p.m.]
For example, to read Hong Kong Standard Time at 8 Nov, the “12:7.2” mark of the Inner LST Time Scale Ring of the
heliodon has to be adjusted to match the “12:00 noon” mark of the Outer AST Time Scale Ring.
To read Local Standard Time (LST) on the Inner Circular Time Scale Ring, RELATIVE TO Apparent Solar Time (AST)
read by the Circular AST Outer Time Scale ring : For the day 20 Feb, the “12:37.3” mark of the Inner LST Time Scale Ring
[i.e. Hong Kong Standard Time] of the heliodon has to be adjusted to match the “12:00 noon” mark of the Outer AST Time
Scale Ring [Fig. 15].
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Table 3: Mean value of the equation of time, in minutes at Apparent Solar noon [adapted from The
Nautical Almanac 1991, HMSO, UK. Ref. 16]
DAY JAN FEB MAR APR MAY JUN JUL AUG SEPT OCT NOV DEC
1 3.4 13.6 12.5 4.0 2.9 2.3 3.7 6.3 0.1 10.2 16.4 11.2
2 3.9 13.7 12.3 3.7 3.0 2.2 3.9 6.3 0.2 10.5 16.4 10.7
3 4.3 13.8 12.0 3.4 3.1 2.0 4.1 6.2 0.5 10.8 16.4 10.4
4 4.8 13.9 11.8 3.1 3.2 1.8 4.3 6.1 0.8 11.1 16.4 10.0
5 5.2 14.0 11.6 2.8 3.3 1.7 4.5 6.0 1.2 11.5 16.4 9.6
6 5.7 14.1 11.4 2.5 3.4 1.5 4.6 5.9 1.5 11.7 16.4 9.1
7 6.1 14.1 11.2 2.3 3.5 1.3 4.8 5.8 1.8 12.0 16.3 8.7
8 6.6 14.2 10.9 2.0 3.5 1.1 5.0 5.7 2.2 12.3 16.3 8.3
9 7.0 14.2 10.7 1.7 3.6 0.9 5.1 5.6 2.5 12.6 16.2 7.8
10 7.4 14.2 10.4 1.4 3.6 0.7 5.3 5.4 2.9 12.9 16.1 7.4
11 7.8 14.3 10.2 1.2 3.7 0.5 5.4 5.3 3.2 13.1 16.0 6.9
12 8.2 14.3 9.9 0.9 3.7 0.3 5.5 5.1 3.5 13.4 15.9 6.5
13 8.6 14.2 9.6 0.6 3.7 0.1 5.7 4.9 3.9 13.6 15.8 6.0
14 8.9 14.2 9.3 0.4 3.7 0.1 5.8 4.8 4.3 13.9 15.6 5.5
15 9.3 14.2 9.1 0.1 3.7 0.3 5.9 4.6 4.6 14.1 15.5 5.1
16 9.7 14.1 8.8 0.1 3.7 0.6 6.0 4.4 5.0 4.3 5.3 4.6
17 6.0 14.1 8.5 0.3 3.7 0.8 6.1 4.2 5.3 14.5 15.1 4.1
18 10.3 14.0 8.2 0.6 3.6 1.0 6.2 3.9 5.7 14.7 14.9 3.6
19 10.6 13.9 7.9 0.8 3.6 1.2 6.3 3.7 6.1 14.9 14.7 3.1
20 10.9 13.8 7.6 1.0 3.5 1.4 6.3 3.5 6.4 15.1 14.5 2.6
21 11.2 13.7 7.3 1.2 3.5 1.6 6.4 3.2 6.8 15.3 14.2 2.1
22 11.5 13.6 7.0 1.4 3.4 1.9 6.4 3.0 7.1 15.4 14.0 1.6
23 11.8 13.4 6.7 1.6 3.3 2.1 6.5 2.7 7.5 15.6 13.7 1.1
24 12.0 13.3 6.4 1.8 3.3 2.3 6.5 2.5 7.8 15.7 13.4 0.6
25 12.3 13.2 6.1 2.0 3.2 2.5 6.5 2.2 8.2 15.9 13.1 0.1
26 12.5 13.0 5.8 2.2 3.1 2.7 6.5 1.9 8.5 16.0 12.8 0.4
27 12.7 12.8 5.5 2.3 3.0 2.9 6.5 1.6 8.9 16.1 12.5 0.9
28 12.9 12.6 5.2 2.5 2.8 3.1 6.5 1.4 9.2 16.2 12.2 1.4
29 13.1 - 4.9 2.6 2.7 3.3 6.5 1.1 9.5 16.2 11.8 1.9
30 13.3 - 4.6 2.8 2.6 3.5 6.4 0.8 9.9 16.3 11.5 2.3
31 13.4 - 4.3 - 2.5 - 6.4 0.4 - 16.4 - 2.8
Note: Apparent Solar Time + Equation of Time = Mean Solar Time (fictional). The bold faced numbers
indicate days in which the sun is slow, [25 Dec -15 April, 14 Jun-1 Sept] and normal fonts indicate days in
which the sun is fast [2 Sept-24 Dec, 16 Apr-13 Jun].
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Fig. 3: The sun-earth system primarily set for Northern Hemisphere - Solar Geometric Parameters
Illustrated on the Globe shown for noon time of Apparent Solar Time System [7, 14]. For studying places
on Southern Hemisphere, it is advisable to rotate the diagram and replace the model platform to the
desirable latitude of Southern Hemisphere, so that the South Pole is at the top of the page.
Notes:
1. N-S is the axis of the earth for Northern Hemisphere. S-N is the axis of the earth for Southern Hemisphere.
2. In the diagram L is drawn equal to L’ for minimizing lines on the diagram, i.e. L=L’=45 degree.
3. For Northern Hemisphere: At latitude L, the horizontal plane is making an angle φ= L with the N-S axis if
the earth. At Equator, L=L’0, the horizontal plane is normal to the equatorial plane, and parallel to the N-S
axis. At North pole, L=90 degree, the horizontal plane is parallel to the equatorial plane, and normal to the
N-S axis.
4. For southern Hemisphere: At latitude L’, the horizontal plane is making an angle φ= L’ with the S-N axis of
the earth. At Equator, L’=L=0, the horizontal plane is normal to the equatorial plane, and parallel to the S-N
axis. At South pole, L’=90 degree, the horizontal plane is parallel to the equatorial plane, and normal to the
S-N axis.
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Fig. 3a: The sun-earth system- primarily set for Southern Hemisphere - Solar Geometric Parameters
Illustrated on the Globe shown for noon time of Apparent Solar Time System [7, 14]. For studying places
on Northern Hemisphere, it is advisable to rotate the diagram and replace the model platform to the
desirable latitude of Northern Hemisphere, so that the North Pole is at the top of the page.
Notes:
1. S-N is the axis of the earth for Southern Hemisphere. N-S is the axis of the earth for Northern Hemisphere.
2. In the diagram L’ is drawn equal to L for minimizing lines on the diagram, i.e. L’=L=45 degree.
3. For Southern Hemisphere: At latitude L’, the horizontal plane is making an angle φ= L’with the S-N axis of
the earth . At Equator, L’=L=0, the horizontal plane is normal to the equatorial plane, and parallel to the S-N
axis. At South pole, L’=90 degree, the horizontal plane is parallel to the equatorial plane, and normal to the
S-N axis.
4. For Northern Hemisphere: At latitude L, the horizontal plane is making an angle φ= L with the N-S axis of
the earth . At Equator, L= L’=0, the horizontal plane is normal to the equatorial plane, and parallel to the N-
S axis. At North pole, L=90 degree, the horizontal plane is parallel to the equatorial plane, and normal to the
N-S axis.
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Fig. 4: The Front view of the patented heliodon assembly set at 12:00 Apparent Solar Time and 90
degree latitude, showing The combined N. Hemisphere-S. Hemisphere Day Selector of the patented
heliodon. For Northern Hemisphere application, the north pole is at the top of the globe [Fig. 3]. For
Southern Hemisphere application, the south pole is at the top of the globe [Fig. 3a]. See Fig. 8 for Right
Side View.
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Fig. 5: The combined Northern Hemisphere-Southern Hemisphere Day Selector of the patented heliodon,
showing the principles of determining the marking positions of the day[s] onto the Day Selector scale [Fig.
4, Fig. 8, Fig. 6] in relation to the dimensions of the gnomon, and solar declination angle [Table 1]
corresponding to each day.
Fig. 6: The Design of Day Selector Scale using the sundial principle for setting the desirable day, showing
the trigonometric relationship of the actual height of the tip of the gnomon and solar declination angles
[Table 1, Fig. 4, Fig. 5, Fig. 8].
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Fig. 7: The top view of the patented light duty universal heliodon [14, Fig. 2], set at 12:00 of Apparent
solar time, 90 degree latitude.
Notes:
1. The model platform can be adjusted to the desirable latitude angle, and locked. The north, south direction for
Northern Hemisphere and Southern Hemisphere are in opposite direction.
2. The OUTER Circular Apparent Solar Time ring is fixed, while the INNER Circular time ring can be turned,
following established steps [2, 7, 10, Table 2] to read local standard time
3. The globe is added to help users to understand the sun-earth system simulated. For Northern Hemisphere
application, the north pole is at the top of the globe [Fig. 3]. For Southern Hemisphere application, the south
pole is at the top of the globe [Fig. 3].
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Fig. 8: Right Side view of the patented heliodon assembly [14, Fig. 1], set at 12:00 of Apparent solar time,
90 degree latitude, showing The combined N. Hemisphere-S. Hemisphere Day Selector. For Northern
Hemisphere application, the north pole is at the top of the globe [Fig. 3]. For Southern Hemisphere
application, the south pole is at the top of the globe [Fig. 3a]. See Fig. 4 for the Front View.
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Fig. 9: Testing of a cardboard model using the
patented universal light duty heliodon mounted
on a camera tripod [14], placed outdoor, with a
weak state of direct sunlight of 1 Jan 2013, 3.15
pm, Hong Kong Local Time, as the light source,
set at two possible combinations of latitude, day,
and time: [Fig. 4, Fig. 5, Fig. 7, Fig. 8]
- For Northern Hemisphere : 10 am, Apparent
Solar Time, 45 degree latitude, 5 May or 7
August, noting that the top point of the globe
is the north pole [Fig. 3]
- For Southern Hemisphere : 2 pm, Apparent
Solar Time, 45 degree latitude, 4 Feb or 7
November, noting that the top point of the
globe is the south pole [Fig. 3a]
Note: In the above photo, the latitude scale of the
patented documents [14, Fig. 2] has been replaced
by an enhanced latitude scale [Fig. 9a, Fig. 11, Fig.
11a, 12], based on the same solar-geographical
principle.
Fig. 9a: The patented heliodon set for the
conditions mentioned in Fig. 9, showing
enlarged view of the components, with the
latitude scale of the patented documents [14,
Fig. 2] now replaced by an enhanced latitude
scale [Fig. 9, Fig. 11, Fig. 11a, Fig. 12], based on
the same solar-geographical principle.
Fig. 10: Enlarged view of the direct sunlight
effect on a cardboard model, tested by the
patented universal light duty heliodon mounted
on a camera tripod [14], placed outdoor, with a
weak state of direct sunlight of 1 Jan 2013, 3.15
pm, Hong Kong Local Time, as the light source,
set for the conditions mentioned in Fig. 9.
Fig. 11: Enlarged view of the Enhanced Latitude
Scale [Fig. 11a] of the demonstrated prototype
of the patented heliodon, which replaces the
same component shown in the patented
documents, [14, Fig. 2], both designed on the
same solar-geographical principle. The attitude
is set at 45 degree. Apparent Solar Time (AST)
is set at 10 a m for Northern Hemisphere, same
as 2 p m [i.e. 14 hour] for Southern Hemisphere,
in the outer time scale ring, which thus reads
“10/14” [Fig. 7]. Inner time scale ring, used for
setting Local Standard Time-LST [Table 2],
meets the outer AST time scale ring at the same
markings, as LST is not used in the test.
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Fig. 11a: The Enhanced Latitude Scale [Fig. 11] of the demonstrated prototype of the patented heliodon,
which replaces the same component shown in the patented documents, [14, Fig. 2, Fig. 8] both designed
on the same solar-geographical principle.
Fig. 12: Illustration of setting up the patented portable direct sunlight light-duty universal heliodon [14],
incorporating Enhanced Latitude Scale [Fig. 11, Fig. 11a], indoor using a tungsten lamp as the light
source at 3 m from the heliodon, inheriting light source error on light quality and deviation from being
parallel.
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Fig. 13: Testing of a cardboard model of a building façade using the patented universal light duty
heliodon mounted on a camera tripod [14], placed outdoor, with a strong state of direct sunlight of 5 Jan
2013, 2.45 pm, Hong Kong Local Time, as the light source, set at two possible combinations of latitude,
day, and time:
- For Northern Hemisphere : façade facing South, 10 am, Apparent Solar Time, 45 degree latitude, 22
Dec, Winter Solstice in Northern Hemisphere, noting that the top point of the globe is the north pole
[Fig. 3]
- For Southern Hemisphere : façade facing North, 2 pm, Apparent Solar Time, 45 degree latitude, 21
Jun, “Winter Solstice in Southern Hemisphere”, noting that the top point of the globe is the south pole
[Fig. 3a]
Fig. 14: Enlarged views (Front view at Left, Back Side view at Right) of direct sunlight effect on
cardboard model of a building façade using the patented universal light duty heliodon mounted on a
camera tripod [14], placed outdoor, with a strong state of direct sunlight of 5 Jan 2013, 2.45 pm, Hong
Kong Local Time, as the light source, set for the conditions mentioned in Fig. 13.
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Fig. 15: Illustration on setting the Inner time
ring of the patented heliodon to read Local
Standard Time (LST) on the Inner Circular
Time Scale Ring, RELATIVE TO Apparent
Solar Time (AST) read by the Circular AST
Outer Time Scale ring : For the day 20 Feb, the
“12:37.3” mark of the Inner LST Time Scale
Ring [i.e. Hong Kong Standard Time] of the
heliodon has to be adjusted to match the “12:00
noon” mark of the Outer AST Time Scale Ring
[Table 2]. In the time rings, one small division
represents a difference of 5 minutes of time.
3. CONCLUSION
The Dufton & Beckett Heliodon of 1931, [1, Fig. 1]
used a separate day scale for holding the lamp
which simulates the sun and its varying positions
over the year, i.e. solar declination [Table 1],
allowing light source error, while the adjustable
earth-latitude-time system assembly is detached.
However the reported patented heliodon
incorporates an integral Day Selector Scale onto
the earth-latitude-time system assembly, NOW
forming an innovative integrated simulated
earth-latitude-time-DAY system assembly, all
mounted on a camera tripod. This assembly
makes the patented heliodon portable, conveniently
to be taken to anyway using various light sources,
primarily with sunlight as the light source for
obtaining accuracy of shadow boundaries and good
lighting quality over the tested model surfaces.
Since direct sunlight is practically parallel, using
artificial light source will induce the inheriting light
source error on light quality and deviation from
being parallel.
Since the components are demountable and can be
stored inside a box about the size of an A4 paper
[297 mm x 210 mm, OR 11.69 inch x 8. 27 inch ]
of 100 mm thick [ 4 inch thick] , and the common
camera tripod is used as the support, the reported
patented heliodon has demonstrated the
convenience of its storage and transportation, and
its affordability for students and architects.
It is expected that this reported patented heliodon
will help educate effectively the architecture and
building students, and will be a convenient,
portable and affordable tool to be used by the
building and architecture profession, and the
general public on solar architecture design, thus
arousing the general public in wider acceptance and
demand on more integration of solar design into
buildings, contributing to building a sustainable
world.
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Sin, “A light duty universal direct sunlight
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118-128 (2001).
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http://www.bse.polyu.edu.hk/researchCentre/Fire_
Engineering/summary_of_output/journal/IJAS/V2/
p.118-128.pdf
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http://www.bse.polyu.edu.hk/researchCentre/Fire_
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p.46-58.pdf
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(2002).
http://www.bse.polyu.edu.hk/researchCentre/Fire_
Engineering/summary_of_output/journal/IJAS/V3/
p.51-60.pdf
14. Kwok Pun Cheung, US Patent No. US6523270 B1.
A Universal Heliodon-Sundial, patent issued by US
Patent Office on 25 February 2003.
http://hub.hku.hk/handle/10722/142203,
also searchable at
http://portal.uspto.gov/external/portal/!ut/p/
15. K.P. Cheung, “An alternative solar chart and its use
in a case study”, Architectural Science Review,
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