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A comparative study on optimum insulation thickness of walls and energy savings in equatorial and tropical climate 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 3[.]

Trang 1

5 Modeste Kameni Nematchouaa,⇑, Paola Ricciardia, Sigrid Reiterb, Andrianaharison Yvonc

6 a Department of Civil Engineering and Architecture, University of Pavia, Via Ferrata 1, 27100 Pavia, Italy

7 b LEMA, Faculty of Applied Sciences, University of Liege, Liege, Belgium

8 c Department of Electrical Engineering, National Higher Politechnical School of Antananarivo, Madagascar

10

11 Abstract

12 The increase outdoor temperature acts directly on the indoor climate of buildings In Cameroon, the energy consumption demand in

13 the buildings sector has been rapidly increasing in recent years; so well that energy supply does not always satisfy demand Thermal

insu-14 lation technology can be one of the leading methods for reducing energy consumption in these new buildings However, choosing the

15 thickness of the insulation material often causes high insulation costs In the present study, the optimum insulation thickness, energy

16 saving and payback period were calculated for buildings in Yaounde´ and Garoua cities, located in two climatic regions in Cameroon

17 The economic model including the cost of insulation material and the present value of energy consumption and the cost over a life time of

18 22 years of the building, were used to find the optimum insulation thickness, energy saving, and payback period Materials that extruded

19 polystyrene were chosen and used for two typical wall structures (concrete block (HCB) and compressed stabilized earth block wall

20 (CSEB)) The early cooling transmission loads, according to wall orientations and percentage of radiation blocked were calculated using

21 the explicit finite-difference method under steady periodic conditions As a result, it was found that the west- and east-facing walls are the

22 least favourite in the cooling season, whereas the south and north orientations are the most economical Although wall orientation had a

23 significant effect on the optimum insulation thickness, it had a more significant effect on energy savings In equatorial region (Yaounde´),

24 for south orientation, the optimum insulation thickness was 0.08 m for an energy savings of 51.69 $/m2 Meanwhile, in tropical region

25 (Garoua), for north orientation, the optimum insulation thickness was 0.11 m for an energy savings of 97.82 $/m2

26 Ó 2017 The Gulf Organisation for Research and Development Production and hosting by Elsevier B.V All rights reserved

27

28 Keywords: Energy savings; Optimum insulation; Equatorial and tropical climate; Buildings; Wall orientation

29

30 1 Introduction

31 One of the most efficient ways to reduce the

transmis-32 sion rate of heat and energy consumption to cool and heat

33

buildings is the use of an appropriated thermal insulation

34

in the building envelope An optimum thickness of

insula-35

tion offers minimum total cost, including the cost of

insula-36

tion and energy consumption on the building life (Daouas,

37

2011) In Cameroon, energy consumption in modern and

38

traditional buildings has considerably increased in recent

39

years, and unfortunately, no measure has been taken by

40

the Cameroon government to improve the thermal quality

http://dx.doi.org/10.1016/j.ijsbe.2017.02.001

2212-6090/ Ó 2017 The Gulf Organisation for Research and Development Production and hosting by Elsevier B.V All rights reserved.

⇑ Corresponding author.

E-mail address: kameni.modeste@yahoo.fr (M Kameni Nematchoua).

Peer review under responsibility of The Gulf Organisation for Research

and Development.

H O S T E D BY

Gulf Organisation for Research and Development

International Journal of Sustainable Built Environment

ScienceDirect

www.sciencedirect.com

Trang 2

41 of the building envelope A comfortable environment is

42 necessary for an individual’s health and productivity in a

43 building (Kameni Nematchoua, 2014) A considerable

44 applied insulation thickness on the external walls of the

45 buildings results in significantly lower heat load

transmis-46 sion The cost of the insulation material increases linearly

47 with the thickness of the insulation material (Ozel, 2011)

48 In 2008, it has been shown that more than 50% of the

con-49 sumed total energy in the building has been dedicated to

50 heating and cooling (Kameni Nematchoua, 2015) This

51 percentage is going to rise in the coming years, as the global

52 population continues to increase (Kameni Nematchoua,

53 2015) Thermal insulation is also solicited to reduce the loss

54 of heat in buildings through the envelope

55 Meanwhile, the use of the most efficient energy to cool

56 buildings is the best measure to preserve energy and protect

57 environment (Azmi Aktacir et al., 2010) There are many

58 studies in the literature on the determination of optimum

59 insulation thickness on building walls, and most of them

60 had used the degree day (or degree hour) to calculate the

61 thickness (Ucar and Balo, 2009, 2010; Comakli and

62 Yu¨ksel, 2003; Dombayci et al., 2006; Daouas et al., 2010;

63

Bolattu¨rk, 2008; Yu et al., 2009; Ghrab-Morcos, 0000)

64

For instance, Bolattu¨rk (Bolattu¨rk, 2006) analysed the

65

use of insulation on the external walls of buildings during

66

many seasons, and found that the building inertia

influ-67

ences indoor comfort A good selection of construction

68

materials is very important at the time of conception of

69

building Tsilingiris (Tsilingiris, 2003) developed a

numeri-70

cal algorithm for the cooling load calculation, whileGranja

71

and Labaki (2003)presented a periodic solution of the heat

72

flow through a flat roof using Fourier analysis These

73

results have facilitated the calculation of architects

Fur-74

thermore,Dombayci et al (2006)found the optimum

insu-75

lation thickness of the external wall for different energy

76

sources and different insulation materials The study by

77

Mohsen et al (2001)showed that the insulation of external

78

walls and roofs can increase energy saving by up to 77%

79

Meanwhile, Naouel Daouas et al (2010) found that the

80

most profitable case for insulation is the stone/brick

sand-81

wich wall and expanded polystyrene, with an optimum

82

thickness of 5.7 cm, which achieved energy savings up to

83

58% with a payback period of 3.11 years This work, has

84

allowed to improve the results obtained in Tsilingiris

Nomenclature

As annual energy savings ($m2)

c specific heat (Jkg1K1)

C cost ($)

COP coefficient of performance of air-conditioning

system CDD degree-days (°C days)

g inflation rate (%)

h combined heat transfer coefficient (Wm2K1)

H monthly average of daily global radiation on

horizontal surface (MJ m2day1)

Ho monthly average of daily extraterrestrial

radia-tion on horizontal surface (MJ m2day1)

Hd monthly average of daily diffuse radiation on

horizontal surface (MJ m2day1)

L wall thickness (m)

Lop optimum insulation thickness (m)

I interest rate (%), order of node

Itotal solar radiations on the horizontal surface

(W m2)

Ib direct solar radiations on the horizontal surface

(W m2)

Id diffuse solar radiations on the horizontal surface

(W m2)

I0 hourly extraterrestrial radiation (W m2)

N number of nodes

n lifetime of building (years)

M number of layers of composite wall

pb payback period (years)

qi heat flux density at indoor surface of the wall

(W m2)

Qc annual cooling transmission load (MJ m2)

sd shade level

t time (s)

T temperature (C)

x coordinate direction normal to wall (m)

Greek symbols

a solar absorptivity of outside surface of wall

c surface azimuth angle (°)

d declination angle (°)

k thermal conductivity (W m1K1) / latitude (°)

w hour angle (°)

ws sunset-hour angle for a horizontal surface (°)

q density of material (kg m3)

qr ground reflectivity

Subscripts

el electricity enr energy

I inside ins insulation max maximum value min minimum value

o outside

sa solar-air

t total

2 M Kameni Nematchoua et al / International Journal of Sustainable Built Environment xxx (2017) xxx–xxx

1 March 2017

Trang 3

85 (2003), Granja and Labaki (2003), Dombayci et al (2006).

86 Hanan et al (2011)identified several design-related faults

87 common in Saudi Arabian house design, which contributed

88 to inefficient use of energy.Kemal and Bedri (2003)showed

89 that optimization is based on the lifecycle cost analysis, and

90 obtained an able energy saving by applying optimum

91 insulation thickness.Farshid et al (2014), showed thatthe

92 sustainability scenario could offer, approximately, 100%

93 increase in the optimum thickness of extra insulation

com-94 pared to the Business As Usual scenario (BAU) However,

95 the implication of different life spans of 40, 50 or 60 years,

96 on the optimum measure appeared to be either negligible

97 or very small, depending on the chosen scenario It must

98 be noted that the results obtained in each of these studies

99 differed according to the study places with their climate

100 zone In the Sub-Sahara Africa regions, ambient

tempera-101 tures and solar radiation levels are sufficiently high that,

102 even during winter, buildings do not need energy for

heat-103 ing The roof insulation is as important as that of wall This

104 work is the continuation ofWati and Meukam (2015) The

105 choice of Yaounde and Garoua as the main investigation

106 field cities has not been made randomly Several countries

107 in sub-Saharan Africa and Asia have a climate similar to

108 that of these two cities In this sense, the results can also

109 serve as a standard for construction and design of buildings

110 in these different regions and also improve Existing

ASH-111 RAE database In addition, Yaounde´ and Garoua are

112 two cities with a very high population density in Central

113 Africa These cities are highly threatened by the effects of

114 climate change, which explains the high energy demand

115 for cooling in new residences

116 The aim of the present study was to determine optimum

117 insulation thickness for external walls of buildings in two

118 climate areas of Cameroon Optimization was based on

119 an economic model, in which a lifecycle cost analysis was

120 conducted using one type of insulation material and two

121 typical wall structures The yearly cooling transmission

122 loads according to wall orientations were calculated using

123 explicit finite-difference method under steady periodic

con-124 ditions In addition, the thermal performance of the walls

125 under optimal conditions was also investigated

126 2 Methodology

127 2.1 Analysed cities

128 The Yaounde´ city is built on several hills and enjoys a

129 picturesque setting and a relatively ‘‘fresh” climate It is

130 the capital of the central region and also the Cameroon

131 political capital This city is located between 3°520N and

132 11°310E, then, around of 726 m of altitude Precipitation

133 ranges from 22 mm (January) to 298 mm (October) In

134 February, the average temperature is 24.9°C February is

135 therefore the hottest month of the year August is the

136 coldest month of the year The average temperature is

137 22.2°C during this period Yaounde city is approximately

138 300 km from the Atlantic coast and enjoys a temperate

139

sub-equatorial climate with four seasons, including a long

140

dry season (mid-November to late March), a short rainy

141

season (April to mid-June), a short dry season (mid-June

142

to mid-August) and a long rainy season (mid-August to

143

mid-November) Its population was about 2.5 million in

144

2011, and since the early 1990 s, the population has

145

increased with a growth rate of 7% per year

146

Located between 9°180N and 13°230E, around altitude

147

199 m; Garoua is the capital of the northern region of

148

Cameroon It has approximately 357,000 inhabitants

Gar-149

oua city is the third largest city of Cameroon In this city,

150

scorching heat can be experienced in the late dry season

151

despite the shade provided by the trees that line the main

152

streets, and the average monthly temperature is 26°C in

153

August and 40°C in March (extreme temperatures varied

154

from 17°C to 46 °C) It has Sudanian-type tropical

cli-155

mate It is characterized by a long dry season from October

156

to April and a short rainy season from May to September

157

The total monthly rainfall varies from 0 to 250 mm Its

158

monthly sunshine varies from 194 to 300 h

159

2.2 Mathematical formulation

160

The walls of the modern houses in the sub-Saharan

161

Africa, in general, and in Cameroon, in particular, are

gen-162

erally made with parpen, with a cement coating on each

163

side However, the development of techniques for

stabiliz-164

ing mud brick (mechanical and chemical) has led to a

165

renewed interest in it Thus, to optimize the thickness of

166

the insulation in the walls in modern homes, composite

167

walls are considered (Fig 1)

168

The outside face of the wall is subjected to variations in

169

temperature ToðtÞ and solar radiation IðtÞ The inside face

170

of wall comes in contact with the indoor air maintained

171

at a fixed temperature for Ti to have better thermal

com-172

fort Each layer, J, of the composite wall is therefore the

173

seat of a unidirectional transfer of heat in the supposed

174

case was defined as in (Kameni Nematchoua, 2015)

175

qjcj@Tj

@t ¼ kj

@2

Tj

178

where j refers to the serial number of the layer (j = 1, ., M

179

for a wall of M layer); x and t are the spatial and temporal

180

coordinates, respectively; Tjis the temperature at the

181

point of coordinates x in layer j and qj, cj and kj are the

182

density, specific heat and thermal conductivity of the

mate-183

rial of layer j, respectively The resolution of Eq (1)

184

requires the determination of the boundary conditions

185

and initial condition Thus, at the initial moment, we

186

assume that all points of the wall have the same

tempera-187

ture (25°C) The outside face conditions and indoor

condi-188

tion are given by Eqs (2) and (3), (see Daouas, 2011),

189

respectively

190

k1 @T

@x

 

x 1 ¼0¼ hoðTo T1Þ þ aI ð2Þ

192

Trang 4

kM

@T

@x

 

195

196 where a is the absorption coefficient and he and hi are the

197 thermal exchange coefficient on the outside and inside

198 faces, respectively Their values (he¼ 22W :m2:K1 and

199 hi¼ 9W :m2:K1) were obtained from a previous study

200 (Ozel, 2011) I is the radiation of short wavelength received

201 by outdoor face wall (vertical), and was obtained using

202 Eq.(4) given inOzel (2011)

203

I¼ IdRbþ1

2qyIhþ1

205

206 where Id; Dh and Ih are the direct radiation, diffuse

207 radiation and global radiation on a horizontal surface,

208 respectively and qy is the albedo of the area assumed to

209 be equal to 0.2 The parameter Rbis given for a vertical

sur-210 face byOzel (2011)

211

Rb¼cos d sin / cos x þ cos d sin c sin x  sin d cos / cos c

cos / cos d cos x þ sin / sin d

ð5Þ

213

214 where d, x, c and / are the solar declination, hourly angle,

215 surface of the azimuth and solar elevation, respectively c is

216 equal to 0 for an inclined surface facing south, 90 for a

217 surface turned towards east, 90 for a surface turned

218 towards west and 180 for a north surface

219 The third term of Eq.(4)designating the diffuse radiance

220 on a vertical surface was obtained from a model developed

221 in El-Sebaii et al (2010) This model uses the simplifying

222 hypothesis of a distribution isotrope of the diffuse radiation

223 that is independent of the ze´nithal and azimuthal angles

224

2.3 Method of solution

225

To solve the above-mentioned problem, a thermal

226

model of an area consisting of a wall was constructed from

227

the component library of Ham-tools developed in the

envi-228

ronment of MATLAB-Simulink simulation (Kolaitis et al.,

229

2013) The Ham-tools has been developed jointly by

230

Chalmers University of Technology (Sweden) and the

231

University of Technology in Denmark (Copenhagen,

Den-232

mark), and is solved numerically using the finite-difference

233

method and a scheme of explicit temporal resolution

234

(Eq (1)).For a stitch of thickness di inside the materials

235

(Fig 2), the thermal balance at node i mesh centre can be

236

written as follows:

237

Tniþ1 Tn

i

Dt ¼ 1

qicidi

Tni1 Tn

i

Ri1þ Ri

þTniþ1 Tn

i

Riþ1þ Ri

ð6Þ

239

240

where i denotes the number of node and n indicates the

241

time step The resistances are defined as (Ozel, 2011):

242

Ri¼ di

2ki

ð7Þ 244

245

where kiis the thermal conductivity of the node material i

246

As the studied wall is composite, a node is placed at every

247

interface between the two materials of different nature The

248

complete modelling of the heat transfer to the node of

con-249

tact is given inNielsen (2002)

250

The thermal balances are given by Eqs (8) and (9),

251

respectively

252

Tnþ11  Tn

1

Dt ¼ 1

qicidout

Tn

2 Tn 1

R2þ R1

þ hoðTo T1Þ þ aI

ð8Þ

254

Fig 1 Typical wall structures (a: hollow concrete block wall, b: CSEB wall) and proposed wall structures (c: insulated hollow concrete block wall, d: insulated CSEB wall).

4 M Kameni Nematchoua et al / International Journal of Sustainable Built Environment xxx (2017) xxx–xxx

1 March 2017

Trang 5

Tnþ1N  Tn

N

Dt ¼ 1

qicidin

Tn

N 1 Tn N

RN 1þ RN

þ hiðTi TNÞ

ð9Þ

257

258 The numeric solution gives the temporal evolution of

259 the temperature to every internal node of the wall and on

260 internal and external face of the wall The density of heat

261 flux transmitted to the zone is given by El-Sebaii et al

262 (2010)

263

qcðtÞ ¼ hiðTi TNðtÞÞ if Ti> TN

0 if Ti6 TN



ð10Þ

265

266 The maximum step size of the time adopted in our

267 model is an hour, and the hourly exterior conditions are

268 considered

269 2.4 Hourly exterior conditions

270 The monthly averages of the minimum and daily

max-271 ima of temperature of every month on a relatively long

per-272 iod (1984–2005) were first calculated from the archives of

273 the Department of Meteorology (Directorate of National

274 Meteorology) These values were used to estimate the

mid-275 dle hourly values of temperature of every month from the

276 model of cosine (Safeeq and Fares, 2011), as shown in

277 Eq.(11)

278

Tt¼Tmax Tmin

2 cos

pðt  aÞ 12

þTmaxþ Tmin

280

281 where Ttis the temperature at time tðhÞ starting from

mid-282 night (in the range of 1–24); Tmaxand Tminare the minimum

283 and maximum daily temperature, respectively and a is the

284 hour of the day at which temperature is maximum In the

285 present study, the parameter a was considered as 14, as

286 reported bySafeeq and Fares (2011), De Wit (1978)

287 The daily averages of the diffuse and global radiances on

288 a horizontal surface of every month were obtained by

289 dividing the number of day of the month considered, and

290 the monthly averages of one relatively long period

291 (1985–2005) was obtained from Sola (2014) The hourly

292 averages of the diffuse and global radiances were obtained

293 from the model of decomposition of Lui and Jordan and

294 Collares-Pereira (Basunia et al., 2012), considering the

295 15th day of the month as the representative day Figs 3

296 and 4show the monthly diurnal averages of temperatures

297

and solar radiation levels in Garoua and Yaounde´,

298

respectively

299

The outdoor temperature varied from 17.6°C to 40.9 °C

300

with a standard deviation (SD) of 0.97 A peak was

301

obtained in March at around 2 pm This peak persisted till

302

April and then fell by 3.9°C in May From May, a light

303

reduction in the air temperature was observed until the

304

month of November when the temperature appeared to

305

increase The global radiation was about 1000 W/m2from

306

January to March, and the direct normal radiation

307

increased up to 825 W/m2 in January, while the diffuse

308

radiation was around 300 W/m2, except for the period

309

from November to January (Fig 3) In the equatorial zone

310

(Yaounde), the climatic conditions were more favourable;

311

the outdoor air temperature varied from 21.5°C to 31.7 °

312

C (SD = 0.74), and the horizontal global radiation was

313

rarely 800 W/m2 (Fig 4) Generally, the global radiation

314

was more important in tropical region than equatorial

315

region But, almost equal in January and February in the

316

two regions These different studied elements testified the

317

unequal variation in the energies used for the cooling of

318

the buildings in these regions The climatic conditions of

319

these cities were often very unfavourable to compare with

320

those of the city of Jeddahen (Hanan et al., 2011)

321

3 Thermal performance of the uninsulated wall

322

Hence forth, the composite walls presented in

323

Fig 1a and b will be designated as wall 1 and wall 2, whose

324

outside faces were exposed to the climatic conditions of the

325

cities of Yaounde and Garoua, respectively The solar

radi-326

ation calculations were made for the 15th day of the hottest

327

month of each of the two climates as indicated by Jeddahen

328

(Hanan et al., 2011); i.e., March for Garoua and January

329

for Yaounde The month of January was chosen for

330

Yaounde´, because of the importance of the amplitude of

331

the diurnal temperature variations The thermophysical

332

properties of the materials used are given in Table 1

333

3.1 Effect of wall orientation

334

Fig 5, shows the remarkable effect of wall orientation

335

on the heat flux density on the internal face of every wall

336

model The peak density of the flux on the internal surface

Fig 2 Numeric model.

Trang 6

Fig 3 Monthly diurnal averages of temperatures and solar radiation levels in Garoua.

Fig 4 Monthly diurnal averages of temperatures and solar radiation levels in Yaounde´.

6 M Kameni Nematchoua et al / International Journal of Sustainable Built Environment xxx (2017) xxx–xxx

1 March 2017

Trang 7

337 of walls (1) and (2) was higher when they were oriented

338 towards east in the tropical climate (Garoua) during the

339 representative day of the month of March

340 (Fig 5a and b) This is due to the fact that this facing is

341 the one that receives more radiance of short wavelength

342 when the outside temperature reaches its maximal value

343 (around 14 h) These heat fluxes of the density peaks on

344 the interior wall faces were observed at around 20 h in

345 the case of wall 1 and at about 24 h in the case of wall 2

346 The thermal inertia difference between the two types of

347 walls could be the origin of this shift Indeed, in March,

ini-348 tially, the heat flux density was 30 W/m2, it has decreased

349 up to 5 W/m2 around of 10 h, then begin to increase till

350 20 h, where it reaches 40 W/m2 In January, at the same

351 time, the heat flux density was near to 25 W/m2 (South

352 facing)

353 During the representative day of the month of January,

354 in Yaounde´, the peak density of heat flux on the internal

355

face of each type of wall was observed when the wall was

356

oriented southwards (Fig 5c and d) This is due to the fact

357

that south face receives more solar energy than east, west

358

and north faces at that moment or when the outdoor

tem-359

perature exhibits maximum variation As stated previously,

360

the difference between the hours when peaks appear and

361

their values are due to the thermal inertia difference

362

between the two types of walls In the equatorial region

363

(yaounde), the heat flow density flux was less important

364

than tropical region (Garoua) In March (Yaounde´), at

365

first time, the heat flux density was 25 W/m2, then, it has

366

decreased up to 15 W/m2, around of 13 h, till 23 h, then

367

it increased and reaches 25 W/m2 In January it increased

368

linearily However, the heat flow density flux on the

inte-369

rior layer of the wall when it was oriented towards north

370

was weaker than that noted when it was oriented towards

371

other directions (south, east and/or west) This could be

372

due to the fact that the north wall received very little solar

373

energy during the representative days of the months

con-374

sidered in the two climates (Fig 5) The wall orientation

375

influences the heat flux density on its internal face

How-376

ever,Fig 5shows that for the compressed stabilized earth

377

brick (CSEB) (wall 2), fluctuations within the surface

con-378

ditions were significantly reduced, when compared with

379

those shown by the concrete block wall (wall 1) This is

380

due to the good capacity of the earth bricks to store heat,

Fig 5 Effect of wall orientation on the hourly variation of the inside surface heat flux density in Garoua [(a) and (b)] and Yaounde´ [(c) and (d)] for the two wall structures.

Table 1

Material properties ( Meukam et al., 2004; Sisman et al., 2007 ).

Materials q(kg=m 3 ) c(J =kg=K) kðW =m=KÞ

Hollow concrete block 1250 880 0.67

Trang 8

381 when compared with that of the concrete block These

382 results showed that CSEB, similar to stone wall (Daouas

383 et al., 2010), improves the indoor climate

384 3.2 Effect of shading

385 Fig 6, shows the shade effect on the heat flux density on

386 the internal layer of wall 1 and wall 2 This effect was noted

387 for the orientations of the wall where the heat flux density

388 on the internal layer presented the most elevated peaks

389 either on the ‘‘East face” in Garoua or ‘‘South face” in

390 Yaounde In the case of wall 1, there was a strong

reduc-391 tion in the peaks, whereas wall 2 showed a practically

uni-392 form reduction during 24 h It seen that the heat flux

393 density decreases with increasing shade level Under the

394 same climatic conditions and same orientation, the heat

395 flux density on the inside of wall 1 and wall 2 was different

396 (Figs 5 and 6) Meanwhile, the daily thermal gains through

397 these two types of walls, obtained by integrating those

mea-398 sured for 24 h as the function given in Eq (9), were very

399 close Thus, at the time of determination of the optimum

400 insulation thickness, only wall 1 was used and these results

401 were valid for wall 2

402

4 Optimum insulation thickness

403

The insulated wall reduces yearly transmission load,

404

which is the main input parameter of any optimum

insula-405

tion thickness model

406

4.1 Yearly cooling load calculation

407

The cooling period in the climatic zones under field

408

spread throughout the year or nearly the yearly quantity

409

of energy Qc received by indoor wall was determined by

410

integrating the values obtained for 1 year as the function

411

qcðtÞ given by Eq (9) Fig 7 shows the variation in the

412

yearly cooling load with insulation thickness in Yaounde´

413

and Garoua In the two climates, the thermal gains through

414

the east and west faces were practically equal and higher

415

than those of the south or north faces The thermal gains

416

through the south face were higher than those through

417

the north face because the zones of survey were in the

418

northern hemisphere, where the northward-oriented walls

419

received less solar energy than the southward-oriented

420

ones Nevertheless, irrespective of the orientation of the

421

wall, the yearly thermal gains decreased with the thickness

Fig 6 Effect of solar shading on the inside surface heat flux in Garoua [(a) and (b)] and Yaounde´ [(c) and (d)].

8 M Kameni Nematchoua et al / International Journal of Sustainable Built Environment xxx (2017) xxx–xxx

1 March 2017

Trang 9

422 of the insulator These results are similar to those found in

423 the literature (Daouas, 2011; Kameni Nematchoua, 2014;

424 Ozel, 2011; Azmi Aktacir et al., 2010) On the whole, the

425 yearly thermal gains were found to be more important

426 for the climate of Garoua than for the climate of Yaounde´,

427 because the heat degree is more important in Garoua than

428 in Yaounde´ (Kemajou, 2011)

429 Fig 8a and b shows the influence of the obstruction of

430 radiations of short wavelengths on the yearly thermal gains

431 through east or west face in the two considered climatic

432 zones This effect was particularly remarkable when the

433 thickness of the insulator was weak In general, the yearly

434 thermal gains decreased with the percentage of radiation

435 blocked The last result is similar to those obtained in the

436 literature (Ozel, 2013)

437 4.2 Economic analysis

438 The installation of the insulator contributes to the

439 reduction in the air-conditioning load and thus reduction

440

in the electricity invoice This reduction is especially

441

important when the thickness of the insulator is large

442

However, to install an insulator, an initial investment is

443

required, which increases with the thickness of the

insula-444

tor The total expense bound to the wall considered during

445

the lifecycle of a building is a function of the thickness of

446

the thermal insulator installed, price of kilowatt-hour of

447

the electric energy, interest rates and inflation of the

cur-448

rency considered It is important to determine the insulator

449

thickness that minimizes this total amount (Ct), which is

450

equal to the sum of the present cost of the energy

con-451

sumed during the time of existence of the building and

452

the insulation cost (Daouas et al., 2010)

453

Ct¼ CenrPWF þ Ci¼ CenrPWF þ CinsLins ð12Þ 455

456

where Cenr ($=m2year) is the yearly cost of the electric

457

energy consumed bound to the thermal gains through

458

one square metre of wall; PWF is the ‘‘present worth

459

facto”; Cið$=m3Þ is the cost of one cubic metre of insulator

460

and LiðmÞ is the insulation thickness Cenrdepends on the

Fig 7 Cooling transmission load vs insulation thickness for the climate of Garoua (a) and Yaounde´ (b).

Trang 10

461 yearly thermal gains through the unit wall surfaceðQcÞ, the

462 price of energy kilowatt-hour (Cel) and the coefficient

463 of performance of the air-conditioning unit, as given in

464 Eq.(13)

465

Cenr¼QcCel

467

468 PWF is a function of the interest rates and inflation, and

469 is expressed as (Daouas et al., 2010)

470

PWF ¼Xn

u¼1

1þ i

1þ d

 u

¼1þ i

d i 1

1þ i

1þ d

 n

sii–d ð14Þ

472

473

PWF ¼ n

1þ i if i¼ g ð15Þ

475

476 where n is the yearly lifecycle of the building, i is the

477 currency inflation rate and d is the interest rate The

478 pay-back period b is calculated by solving the following

479 equation for b:

480

Ci

482

483 where Ci=AS is the simple pay-back period that does not

484 take interest rate into account and AS is the amount of

485 the annual savings obtained by insulation

486 The energy savings ($/m2) obtained during the lifetime

487 of the insulation material can be calculated as (Kameni

488 Nematchoua, 2015):

489

ES¼ Cto Ctins ð17Þ 491

492

where Ctoand Ctinsare the total cost of cooling without and

493

with insulation, respectively The energy saving can be

494

expressed as% by the following equation (Kameni

495

Nematchoua, 2015):

496

ES

Cto100¼ 1 Ctins

Cto

498 499

The results obtained from the above-mentioned method

500

can be compared with those of the degree-day method In

501

fact, the degree-day method has been used by several

502

authors to estimate the optimal insulation thickness In this

503

method, the yearly transmission load per unit of wall area

504

is estimated (in J=m2) by the following equation (Kameni

505

Nematchoua, 2015):

506

Qc ¼ 86400:U:CDD ð19Þ 508

509

where CDD is the annual cooling degree-day (in°C days)

510

whose values for the climate of Garoua and Yaounde´ are

511

1315 and 361, respectively These values are calculated from

512

the meteorological data (from Directorate of National

513

Meteorology) for a long period (20 years) The annual

cool-514

ing degree-day can be obtained by the summation of the

515

positive difference between the mean daily temperature

516

and the fixed indoor base temperature (25°C) over the

517

whole year The mean daily temperature can be calculated

518

by adding the maximum and minimum temperatures for

519

the day, and then dividing it by 2ASHRAE (2009)

520

The overall heat transfer coefficient of the wall can be

521

expressed by Eq.(20)

522

Roþ Rinsþ Rwþ Ri

ð20Þ 524

525

where Ro and Ri are the heat resistance due to convective

526

transfer on the outside and inside surface of the wall,

527

respectively and Rins and Rw are the heat resistance of the

528

insulation layer and rest of the wall, respectively

529

The total cost (cost of energy and insulation) is given as

530

(Kameni Nematchoua, 2015):

531

Ct¼0:024CDD

COP

1

RtþL ins

k ins

!

CelPWF þ CinsLins ð21Þ

533 534

where Linsand kinsare the thickness and thermal

conductiv-535

ity of the insulating material, respectively

Fig 8 Effect of solar radiation blocked on yearly cooling load in Garoua

(a) and Yaounde´ (b).

Table 2 The parameters used in the calculations ( Sisman et al., 2007; Institut de l’e´nergie et de l’environnement de la Francophonie, 0000 ).

Electricity for cooling

Expanded polystyrene Cost ($/m 3 ) 164.32

10 M Kameni Nematchoua et al / International Journal of Sustainable Built Environment xxx (2017) xxx–xxx

1 March 2017

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