MnAs and MnFeP1-xAsx-based magnetic refrigerants: a review

被引:8
作者
Habiba, Ume E.
Khattak, Khurram Shehzad
Ali, Shahid
Khan, Zawar Hussain
机构
[1] Shandong Univ Sci & Technol, Coll Earth Sci & Engn, Qingdao 266590, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266071, Peoples R China
[3] Peking Univ, Schooi Earth & Space Sci, Beijing 100871, Peoples R China
[4] PetroChina, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China
[5] PetroChina Changqing Oilfield Co, Expiorat & Dev Res Inst, Xian 710021, Shaanxi, Peoples R China
来源
MATERIALS RESEARCH EXPRESS | 2020年 / 157卷 / 04期
基金
中国国家自然科学基金;
关键词
magnetic refrigerants; magnetic refrigeration; magnetocaloric effect; Curie temperature; magnetic entropy change; Adiabatic temperature change; PHASE-TRANSITIONS; MAGNETOCALORIC PROPERTIES; ENTROPY CHANGE; COMPOUND; PRESSURE;
D O I
10.1017/S0016756819000682
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This paper presents a comparative analysis of MnAs and MnFeP1-xAsx family and its alloys from magnetic refrigeration perspective. A thorough literature review was undertaken and to the best of authors knowledge, all samples (similar to 100 samples) with their Curie temperature (T-c) in the range 260-340 K have been reported. For contrastive analysis, samples have been grouped based on their structural and experimental conditions such as magnetic field and sample composition etc. For comparative analysis, all variables of magnetocaloric effect (MCE), e.g., T-c, magnetic entropy change (divide Delta SMdivide delta C-13(ethane)). Through comparing the geochemical characteristics of gases in the southern and northern parts of the gas field, the reasons for the carbon isotopic reversal in the southern Jingbian gas field were determined to be high thermal maturity and mixing action. When thermal maturity reaches a critical value, the carbon isotope value of ethane becomes relatively more depleted with thermal maturity. Although the carbon isotope value of methane increases with thermal maturity, the extent is relatively smaller. Finally, the rare phenomenon of delta C-13(methane) > delta C-13(ethane) occurs. High thermal maturity leads to the secondary thermal cracking of gases. Mixing of the cracked gases and primary gases also leads to carbon isotopic reversal. Both of the above mechanisms share a common premise, which is high thermal maturity.
引用
收藏
页码:527 / 538
页数:12
相关论文
共 72 条
[1]  
[Anonymous], 2007, OFF J EUR UNION
[2]  
[Anonymous], 2016, CIRE ANTILLES GUYANE
[3]   EXPERIMENTAL SIMULATION IN A CONFINED SYSTEM AND KINETIC MODELING OF KEROGEN AND OIL CRACKING [J].
BEHAR, F ;
KRESSMANN, S ;
RUDKIEWICZ, JL ;
VANDENBROUCKE, M .
ORGANIC GEOCHEMISTRY, 1992, 19 (1-3) :173-189
[4]   LIGHT-HYDROCARBONS IN RECENT TEXAS CONTINENTAL-SHELF AND SLOPE SEDIMENTS [J].
BERNARD, BB ;
BROOKS, JM ;
SACKETT, WM .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1978, 83 (NC8) :4053-4061
[5]   Carbon isotope fractionation of Thermoanaerobacter kivui in different growth media and at different total inorganic carbon concentration [J].
Blaser, Martin B. ;
Dreisbach, Lisa K. ;
Conrad, Ralf .
ORGANIC GEOCHEMISTRY, 2015, 81 :45-52
[6]   Carbon and hydrogen isotopic reversals in deep basin gas: Evidence for limits to the stability of hydrocarbons [J].
Burruss, R. C. ;
Laughrey, C. D. .
ORGANIC GEOCHEMISTRY, 2010, 41 (12) :1285-1296
[7]   C5-C13 light hydrocarbons of crude oils from northern Halahatang oilfield (Tarim Basin, NW China) characterized by comprehensive two-dimensional gas chromatography [J].
Chang, Xiangchun ;
Shi, Bingbing ;
Han, Zuozhen ;
Li, Tiantian .
JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING, 2017, 157 :223-231
[8]   ORIGIN OF GASEOUS HYDROCARBONS IN SUBSURFACE ENVIRONMENTS - THEORETICAL CONSIDERATIONS OF CARBON ISOTOPE DISTRIBUTION [J].
CHUNG, HM ;
GORMLY, JR ;
SQUIRES, RM .
CHEMICAL GEOLOGY, 1988, 71 (1-3) :97-103
[9]   New guidelines for δ13C measurements [J].
Coplen, TB ;
Brand, WA ;
Gehre, M ;
Gröning, M ;
Meijer, HAJ ;
Toman, B ;
Verkouteren, RM .
ANALYTICAL CHEMISTRY, 2006, 78 (07) :2439-2441
[10]   COMPARISON OF STABLE ISOTOPE REFERENCE SAMPLES [J].
COPLEN, TB ;
KENDALL, C ;
HOPPLE, J .
NATURE, 1983, 302 (5905) :236-238