Effect of collector slope and orientation on solar energy utilization [Günes enerjisi toplayicilarinda egim ve yönlendirmenin yararlanabilirlige etkisi]

Küçük Resim Yok

Tarih

2012

Dergi Başlığı

Dergi ISSN

Cilt Başlığı

Yayıncı

Erişim Hakkı

info:eu-repo/semantics/closedAccess

Özet

The study is based upon the measured values of daily global and diffuse solar radiation on a horizontal surface which are taken in Izmir, Turkey. The optimum tilt angle of solar collector is determined between 0° and 61° and changed by the time period through the year. In winter (December, January, and February) the tilt should be 55,7°, in spring (March, April, and May) 18,3°, in summer (June, July, and August) 4,3°, and in autumn (September, October, and November) 43°. Annually, optimum tilt is found to be 30,3° as a fixed tilt throughout the year. Also, these measured values are compared with other equations put forward for calculating the optimum tilt angles. Small deviations are observed between 2,87o and 5,90o. The equations that give a result higher then 3o as a deviation are not suitable to calculate the optimum tilt angle. If solar collector is installed on the monthly optimum tilt angle, optimum azimuth angle (?) has to be 0o for all months of the year. However, azimuth angle of the solar collector has to be (?=± 60°) if the slope is chose (ß?60°) in April. In addition, azimuth angle of the solar collector has to be (?= ±75°) if the slope is chose (ß?40°) in May and August, azimuth angle of the solar collector has to be (?= ±90°) if the slope is chose (ß?30°) in June and July, azimuth angle of the solar collector has to be (?= ±45°) if the slope is chose (ß?70°) in September.

Açıklama

Anahtar Kelimeler

Clearness index, Optimum tilt angle, Solar collector, Solar radiation, Surface azimuth angle

Kaynak

Journal of the Faculty of Engineering and Architecture of Gazi University

WoS Q Değeri

Scopus Q Değeri

Q2

Cilt

27

Sayı

4

Künye