Chemical Composition Variations of Altered and Unaffected Coals from the Huaibei Coalfield, China: Implications for Maturity

被引:5
|
作者
Feng, Songbao [1 ,2 ]
Wei, Qiang [1 ,2 ]
Li, Xianqing [3 ,4 ]
机构
[1] Suzhou Univ, Sch Resources & Civil Engn, Suzhou 234000, Peoples R China
[2] Natl Engn Res Ctr Coal Mine Water Hazard Controll, Suzhou 234000, Peoples R China
[3] China Univ Min & Technol Beijing, State Key Lab Coal Resources & Safe Min, Beijing 100083, Peoples R China
[4] China Univ Min & Technol Beijing, Coll Geosci & Surveying Engn, Beijing 100083, Peoples R China
基金
中国国家自然科学基金;
关键词
chemical composition; structure of organic matter; altered coal; Wolonghu coal mine; Huaibei Coalfield; HUAINAN COALFIELD; BITUMINOUS COAL; MINE; INTRUSIONS; GEOCHEMISTRY; CONTACT; ANHUI; SEAM;
D O I
10.3390/en14113028
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
The composition characteristics of altered coals in the Huaibei Coalfield, China, was investigated through a comparative analysis between altered and unaffected coals from the Wolonghu, Taoyuan and Renlou coal mines. Results indicated that the altered coals in Wolonghu coal mine are mostly anthracite coals, with a maximum vitrinite reflectance of 1.6-3.9% (average of 2.9%). Coals from Wolonghu coal mine were mainly consisted of vitrinite (66.2-97.0%), followed by inertinite (2.0-4.0%) and exinite (0.4-6.9%). Differences in volatile matter content were observed between the altered coals in Wolonghu coal mine and unaffected coals from neighboring coal mines, implying that the chemical composition and maturity of coals were changed after magmatic alteration. In addition, differences in hydrogen element were noted among the coals from Wolonghu, Renlou and Taoyuan coal mines, and the phenomenon of "deficient in hydrogen element" was observed in Wolonghu coals. The aliphatic hydrocarbon structure parameters suggested that the aliphatic chain lengths of Wolonghu coals are shorter than those of coal samples from the Renlou and Taoyuan coal mines. In addition, maturity is positively correlated with hydrogen enrichment degree, but negatively related with aliphatic hydrocarbon structure. Coals from Renlou and Taoyuan coal mines showed great weight loss with various heating rates at temperatures of 0-1000 degrees C, whereas those from Wolonghu coal mine had less weight loss.
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页数:17
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