Numerical simulation of atmospheric transmittance between heliostats and heat receiver in Tower-Type solar thermal power station

被引:2
作者
Shen, Yanbo [1 ,4 ]
Jia, Beixi [1 ,4 ]
Wang, Chuanhui [2 ]
Yang, Wei [3 ]
Chen, Hao [2 ]
机构
[1] China Meteorol Adm, Publ Meteorol Serv Ctr, Beijing 100081, Peoples R China
[2] Anhui Publ Meteorol Serv Ctr, Hefei 230031, Peoples R China
[3] Anhui Climate Ctr, Hefei 230031, Peoples R China
[4] CMA Key Open Lab Transforming Climate Resources Ec, Chongqing 401147, Peoples R China
基金
中国国家自然科学基金;
关键词
Atmospheric transmittance; Tower-type solar thermal power station; Near-surface boundary layer; Model simulation; CLOUD COVER; RADIATION; ATTENUATION; AEROSOLS; PLANT;
D O I
10.1016/j.solener.2023.112107
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Based on the Simple Model for Atmospheric Transmission of Sunshine and meteorological observations, a simulation method for atmospheric transmittance between tower solar thermal power heliostats and heat receivers is developed. This method is verified by the vertical radiation observations in Tianjin, China. The results indicate remarkable differences between the simulated global horizontal irradiation (GHI) and the observations under different weather types, and the magnitude of the difference is mainly influenced by near-surface visibility and cloud cover. However, the ratios of the simulated GHI at the altitude of 40 m to that of 200 m are basically consistent with the observations, with deviations of less than 0.02 for more than 97 % of the moments, indicating this method is applicable to simulating the ratio of GHI at different heights. Results show a 20-m increase in altitude leads to an increase of 0.009 % in atmospheric transmittance within 200 m above the ground. Due to the influence of meteorology, the atmospheric transmittance shows obvious diurnal and seasonal variations. Assuming the vertical altitude of a heat receiver is 200 m and its horizontal distance from a heat receiver is 50 m, the average atmospheric transmittance between them is 94.72 %, and the transmittance drops to 76.49 % at the horizontal distance of 1000 m. This method estimates atmospheric transmittance between heliostats and heat receiver, and provides reference for the design of tower type solar thermal power station and the evaluation of the operation status.
引用
收藏
页数:7
相关论文
共 33 条
[1]   Effect of Aerosols, Tropospheric NO2 and Clouds on Surface Solar Radiation over the Eastern Mediterranean (Greece) [J].
Alexandri, Georgia ;
Georgoulias, Aristeidis K. ;
Balis, Dimitris .
REMOTE SENSING, 2021, 13 (13)
[2]   One year of solar extinction measurements at Plataforma Solar de Almeria. Application to solar tower plants [J].
Ballestrin, J. ;
Carra, E. ;
Monterreal, R. ;
Enrique, R. ;
Polo, J. ;
Fernandez-Reche, J. ;
Barbero, J. ;
Marzo, A. ;
Alonso-Montesinos, J. ;
Lopez, G. ;
Batlles, F. J. .
RENEWABLE ENERGY, 2019, 136 :1002-1011
[3]   Solar extinction measurement system based on digital cameras. Application to solar tower plants [J].
Ballestrin, J. ;
Monterreal, R. ;
Carra, M. E. ;
Fernandez-Reche, J. ;
Polo, J. ;
Enrique, R. ;
Rodriguez, J. ;
Casanova, M. ;
Barbero, F. J. ;
Alonso-Montesinos, J. ;
Lopez, G. ;
Bosch, J. L. ;
Batlles, F. J. ;
Marzo, A. .
RENEWABLE ENERGY, 2018, 125 :648-654
[4]   Solar radiation attenuation in solar tower plants [J].
Ballestrin, Jesus ;
Marzo, Aitor .
SOLAR ENERGY, 2012, 86 (01) :388-392
[5]   Atmospheric horizontal extinction determined with a single digital camera-based system in the scope of solar power tower plants [J].
Barbero, F. J. ;
Alonso-Montesinos, J. ;
Ballestrin, J. ;
Carra, M. E. ;
Fernandez-Reche, J. .
MEASUREMENT, 2020, 149
[6]   The impact of cloud cover on the net radiation budget of the Greenland ice sheet [J].
Cawkwell, FGL ;
Bamber, JL .
ANNALS OF GLACIOLOGY, VOL 34, 2002, 2002, 34 :141-149
[7]   Vertical distribution characteristics of PM in the surface layer of Guangzhou [J].
Deng, Xuejiao ;
Li, Fei ;
Li, Yuanhong ;
Li, Jianyong ;
Huang, Hongzhi ;
Liu, Xiantong .
PARTICUOLOGY, 2015, 20 :3-9
[8]  
Dincer Furkan., 2010, Smart Grid and Renewable Energy, V1, P47, DOI [DOI 10.4236/sgre.2010.11007, 10.4236/sgre.2010.11007, DOI 10.4236/SGRE.2010.11007]
[9]   RELATIONSHIPS BETWEEN VERTICAL ATTENUATION AND SURFACE METEOROLOGICAL RANGE [J].
ELTERMAN, L .
APPLIED OPTICS, 1970, 9 (08) :1804-&
[10]   Brown carbon: a significant atmospheric absorber of solar radiation? [J].
Feng, Y. ;
Ramanathan, V. ;
Kotamarthi, V. R. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2013, 13 (17) :8607-8621