欢迎登录材料期刊网

材料期刊网

高级检索

利用十水硫酸钠作为相变储热体系的主体成分,加入一定量的氯化钠,可以适当降低体系的相变温度,达到更适合人类使用的27℃左右的室温范围。同时针对十水硫酸钠的相分离、过冷问题,加入一定量的增稠剂和成核剂,使相变储热体系更加稳定。用DSC法测定了该储热体系的相变温度和相变焓,最终确定了相变焓较高、相变温度在室温范围内的以十水硫酸钠为主体成分的相变储热体系的最佳配方。

The phase transition temperature of the Na2 SO4·10H2 O phase change material was successfully re-duced to 27℃ by using a certain amount of NaCl. For the problem of phase separation and supercooling,adding a certain amount of thickening agent and nucleating agent made the phase change system more stable. The phase transition temperature and the enthalpy of the system was measured by DSC,then the best recipes with high enthalpy and room temperature was determined.

参考文献

[1] Mohammed M F;Amar M K;Siddique A K R et al.A review on phase change energy storage:materi-als and applications[J].Energy Conversion & Management,2004,45:1597-1615.
[2] 凌双梅,高学农,尹辉斌.低温相变蓄热材料研究进展[J].广东化工,2007(03):48-51,55.
[3] 刘欣;徐涛;高学农 等.十水硫酸钠的过冷和相分离探究[J].化工进展,2011,30:755-758.
[4] 曾翠华,张仁元.无机水合盐相变储热材料的过冷性研究[J].能源研究与信息,2005(01):44-49.
[5] 黄金,柯秀芳.无机水合盐相变材料Na2SO4·10H2O的研究进展[J].材料导报,2008(03):63-67.
[6] 黄保军,蔡金阳,闫玲玉,郑直.相变温度可调的水合盐相变材料的仿生合成及热学性能研究[J].化工新型材料,2013(02):132-134.
[7] Stephen B Marks .The effect of crystal size on the thermal Energy storage capacity of thickened Glauber's salt[J].SOLAR ENERGY,1983,30(1):45.
[8] 孙鑫泉.十水硫酸钠体系潜热蓄热材料的研究[J].杭州大学学报(自然科学版),1990(02):195.
[9] Dipak R Biswas .Thermal energy storage using so-dium sulfate decahydrate and water[J].Solar En-ergy,1987,19(1):99.
[10] 沈艳华 .有机/无机复合储能相变材料的制备及性能研究[D].江苏:南京工业大学,2005.
[11] Marliacy P.;Bouroukba M.;Schuffenecker L.;Solimando R. .Thermodynamics of crystallization of sodium sulfate decahydrate in H2O-NaCl-Na2SO4: application to Na2SO4 center dot 10H(2)O-based latent heat storage materials[J].Thermochimica Acta: An International Journal Concerned with the Broader Aspects of Thermochemistry and Its Applications to Chemical Problems,2000(1/2):85-94.
[12] 黄金;柯秀芳.{?}相变材料NaSO4@10H2 O的脱水过程及相分离分析[J].材料导报网刊,2008(1):24-26.
上一张 下一张
上一张 下一张
计量
  • 下载量()
  • 访问量()
文章评分
  • 您的评分:
  • 1
    0%
  • 2
    0%
  • 3
    0%
  • 4
    0%
  • 5
    0%