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      Numerical study for estimation of temperature distribution in solar pond in diverse climatic conditions for all cities of Turkey

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      https://www.riss.kr/link?id=O112856193

      • 저자
      • 발행기관
      • 학술지명
      • 권호사항
      • 발행연도

        2020년

      • 작성언어

        -

      • Print ISSN

        1944-7442

      • Online ISSN

        1944-7450

      • 등재정보

        SCI;SCIE;SCOPUS

      • 자료형태

        학술저널

      • 수록면

        n/a-n/a   [※수록면이 p5 이하이면, Review, Columns, Editor's Note, Abstract 등일 경우가 있습니다.]

      • 구독기관
        • 전북대학교 중앙도서관  
        • 성균관대학교 중앙학술정보관  
        • 부산대학교 중앙도서관  
        • 전남대학교 중앙도서관  
        • 제주대학교 중앙도서관  
        • 중앙대학교 서울캠퍼스 중앙도서관  
        • 인천대학교 학산도서관  
        • 숙명여자대학교 중앙도서관  
        • 서강대학교 로욜라중앙도서관  
        • 계명대학교 동산도서관  
        • 충남대학교 중앙도서관  
        • 한양대학교 백남학술정보관  
        • 이화여자대학교 중앙도서관  
        • 고려대학교 도서관  
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      부가정보

      다국어 초록 (Multilingual Abstract)

      In this study, a numerical investigation for the solar ponds temperature distribution in Turkey was conducted and is compared with the experimental data for a particular district. For this, a prototype salinity‐gradient solar pond with square cross‐section with insulated wall and with seven layers was modeled by considering previously conducted experimental studies, and then, numerical method was conducted by using Finite Element Method with a commercial software COMSOL. Temperature and solar radiation data were taken from General Directorate of Meteorology where they have been measured since 1927. Numerical calculation was performed by taking annual average values of temperature and solar radiation data. The model includes all possibility to calculate temperature distribution of upper convective zone, non‐convective zone, and the heat storage zone where radiative, conductive, and evaporative heat losses were taken into account. Numerical results indicate that during 720 hr of total simulation, maximum temperature was calculated at the end of 600 hr and then temperature remained constant. As the side wall and base were insulated with rock wool, a lot of heat loss was simulated at the top surface of the pond. According to the numerical study in 81 provinces, only one solar pond temperature remained under 300 K in Edirne and solar pond temperatures in five provinces remained under 310 K, and the solar pond temperature for 31 provinces were calculated higher than 320 K.
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      In this study, a numerical investigation for the solar ponds temperature distribution in Turkey was conducted and is compared with the experimental data for a particular district. For this, a prototype salinity‐gradient solar pond with square cross...

      In this study, a numerical investigation for the solar ponds temperature distribution in Turkey was conducted and is compared with the experimental data for a particular district. For this, a prototype salinity‐gradient solar pond with square cross‐section with insulated wall and with seven layers was modeled by considering previously conducted experimental studies, and then, numerical method was conducted by using Finite Element Method with a commercial software COMSOL. Temperature and solar radiation data were taken from General Directorate of Meteorology where they have been measured since 1927. Numerical calculation was performed by taking annual average values of temperature and solar radiation data. The model includes all possibility to calculate temperature distribution of upper convective zone, non‐convective zone, and the heat storage zone where radiative, conductive, and evaporative heat losses were taken into account. Numerical results indicate that during 720 hr of total simulation, maximum temperature was calculated at the end of 600 hr and then temperature remained constant. As the side wall and base were insulated with rock wool, a lot of heat loss was simulated at the top surface of the pond. According to the numerical study in 81 provinces, only one solar pond temperature remained under 300 K in Edirne and solar pond temperatures in five provinces remained under 310 K, and the solar pond temperature for 31 provinces were calculated higher than 320 K.

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