Antarcticite: A Phase Change Material for Thermal Energy Storage-Experiments and Simulation

Antarcticite, CaCl2 center dot 6H(2)O, is an ideal phase change material (PCM) due to its high-energy storage density and good thermal conductivity. In this chapter, supercooling and subsequent solidification behavior of antarcticite are studied based on the cooling curve method and DSC measurement....

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Main Authors: Gu, Xiaobin, Niu, Jingjing, Qin, Shan
Other Authors: Qin, S (reprint author), Peking Univ, Sch Earth & Space Sci, MOE, Key Lab Orogen Belts & Crustal Evolut, 5 Yiheyuan Rd, Beijing, Peoples R China., Peking Univ, Sch Earth & Space Sci, MOE, Key Lab Orogen Belts & Crustal Evolut, 5 Yiheyuan Rd, Beijing, Peoples R China.
Format: Conference Object
Language:English
Published: 11th International Congress for Applied Mineralogy (ICAM) 2015
Subjects:
Online Access:https://hdl.handle.net/20.500.11897/450168
https://doi.org/10.1007/978-3-319-13948-7_14
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spelling ftpekinguniv:oai:localhost:20.500.11897/450168 2023-05-15T13:56:48+02:00 Antarcticite: A Phase Change Material for Thermal Energy Storage-Experiments and Simulation Gu, Xiaobin Niu, Jingjing Qin, Shan Qin, S (reprint author), Peking Univ, Sch Earth & Space Sci, MOE, Key Lab Orogen Belts & Crustal Evolut, 5 Yiheyuan Rd, Beijing, Peoples R China. Peking Univ, Sch Earth & Space Sci, MOE, Key Lab Orogen Belts & Crustal Evolut, 5 Yiheyuan Rd, Beijing, Peoples R China. 2015 https://hdl.handle.net/20.500.11897/450168 https://doi.org/10.1007/978-3-319-13948-7_14 en eng 11th International Congress for Applied Mineralogy (ICAM) 11th International Congress for Applied Mineralogy (ICAM).2015,125-135. 1485120 http://hdl.handle.net/20.500.11897/450168 doi:10.1007/978-3-319-13948-7_14 WOS:000380768800015 SCI Antarcticite Phase change material Supercooling Simulation CALCIUM-CHLORIDE HEXAHYDRATE NUCLEATION Conference 2015 ftpekinguniv https://doi.org/20.500.11897/450168 https://doi.org/10.1007/978-3-319-13948-7_14 2021-08-01T10:58:04Z Antarcticite, CaCl2 center dot 6H(2)O, is an ideal phase change material (PCM) due to its high-energy storage density and good thermal conductivity. In this chapter, supercooling and subsequent solidification behavior of antarcticite are studied based on the cooling curve method and DSC measurement. The results show that the minor SrCl2 center dot 6H(2)O as the nucleator and carboxymethyl cellulose as the thickening agent could significantly reduce supercooling and partly restrain the phase separation. Moreover, we incorporated antarcticite as PCM into building envelopes in four different cases, and the simulation of the heat transfer processes showed that the temperature fluctuation could be reduced to about 2 degrees C in the best case. CPCI-S(ISTP) sqin@pku.edu.cn 125-135 Conference Object Antarc* Peking University Institutional Repository (PKU IR) 125 135
institution Open Polar
collection Peking University Institutional Repository (PKU IR)
op_collection_id ftpekinguniv
language English
topic Antarcticite
Phase change material
Supercooling
Simulation
CALCIUM-CHLORIDE HEXAHYDRATE
NUCLEATION
spellingShingle Antarcticite
Phase change material
Supercooling
Simulation
CALCIUM-CHLORIDE HEXAHYDRATE
NUCLEATION
Gu, Xiaobin
Niu, Jingjing
Qin, Shan
Antarcticite: A Phase Change Material for Thermal Energy Storage-Experiments and Simulation
topic_facet Antarcticite
Phase change material
Supercooling
Simulation
CALCIUM-CHLORIDE HEXAHYDRATE
NUCLEATION
description Antarcticite, CaCl2 center dot 6H(2)O, is an ideal phase change material (PCM) due to its high-energy storage density and good thermal conductivity. In this chapter, supercooling and subsequent solidification behavior of antarcticite are studied based on the cooling curve method and DSC measurement. The results show that the minor SrCl2 center dot 6H(2)O as the nucleator and carboxymethyl cellulose as the thickening agent could significantly reduce supercooling and partly restrain the phase separation. Moreover, we incorporated antarcticite as PCM into building envelopes in four different cases, and the simulation of the heat transfer processes showed that the temperature fluctuation could be reduced to about 2 degrees C in the best case. CPCI-S(ISTP) sqin@pku.edu.cn 125-135
author2 Qin, S (reprint author), Peking Univ, Sch Earth & Space Sci, MOE, Key Lab Orogen Belts & Crustal Evolut, 5 Yiheyuan Rd, Beijing, Peoples R China.
Peking Univ, Sch Earth & Space Sci, MOE, Key Lab Orogen Belts & Crustal Evolut, 5 Yiheyuan Rd, Beijing, Peoples R China.
format Conference Object
author Gu, Xiaobin
Niu, Jingjing
Qin, Shan
author_facet Gu, Xiaobin
Niu, Jingjing
Qin, Shan
author_sort Gu, Xiaobin
title Antarcticite: A Phase Change Material for Thermal Energy Storage-Experiments and Simulation
title_short Antarcticite: A Phase Change Material for Thermal Energy Storage-Experiments and Simulation
title_full Antarcticite: A Phase Change Material for Thermal Energy Storage-Experiments and Simulation
title_fullStr Antarcticite: A Phase Change Material for Thermal Energy Storage-Experiments and Simulation
title_full_unstemmed Antarcticite: A Phase Change Material for Thermal Energy Storage-Experiments and Simulation
title_sort antarcticite: a phase change material for thermal energy storage-experiments and simulation
publisher 11th International Congress for Applied Mineralogy (ICAM)
publishDate 2015
url https://hdl.handle.net/20.500.11897/450168
https://doi.org/10.1007/978-3-319-13948-7_14
genre Antarc*
genre_facet Antarc*
op_source SCI
op_relation 11th International Congress for Applied Mineralogy (ICAM).2015,125-135.
1485120
http://hdl.handle.net/20.500.11897/450168
doi:10.1007/978-3-319-13948-7_14
WOS:000380768800015
op_doi https://doi.org/20.500.11897/450168
https://doi.org/10.1007/978-3-319-13948-7_14
container_start_page 125
op_container_end_page 135
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