Numerical Investigation of Relationship between Bursting Proneness and Mechanical Parameters of Coal

Table 2

Coal specimens and values of bursting proneness indices accompanied by geological conditions of the sites from which the specimens were taken.

Specimens	Bursting proneness					Coal mine	Location	Geological conditions	Reference
	Rc	WET	KE	Dt	Results
No. 1	27.26	9.36	12.02	12.11	High	Zhaogu	Henan, China	Large amounts of faults and subsidiary fold structures	Su et al. [42]
No. 2	25.13	8.12	7.49	23.75	High	Tangshan	Hebei, China	Existence of primary folds and large amounts of island longwall mining face	Pan et al. [44]
No. 3	24.58	7.52	7.79	31.56	High	Tangshan	Hebei, China	Existence of primary folds and large amounts of island longwall mining face	Pan et al. [44]
No. 4	22.70	7.70	9.82	45.78	High	Mentougou	Beijing, China	Existence of thrust faults and overturned rock strata. Fold structures such as syncline and anticline existed alternately	Okubo et al. [47]
No. 5	21.24	7.84	5.98	29.51	High	Tangshan	Hebei, China	Existence of primary folds and large amounts of island longwall mining face	Pan et al. [44]
No. 6	21.08	7.25	13.44	22.70	High	Mentougou	Beijing, China	Existence of thrust faults and overturned rock strata. Fold structures such as syncline and anticline existed alternately	Okubo et al. [47]
No. 7	20.68	7.51	6.91	56.27	High	Sanjiaohe	Shanxi, China	A series of developed folds and subsidiary faults existence	Li et al. [46]
No. 8	20.39	6.12	13.26	51.68	High	Pingdingshan	Henan, China	A series of faults and folds existence	Su et al. [48]
No. 9	20.33	7.02	4.93	29.87	High	Mentougou	Beijing, China	Existence of thrust faults and overturned rock strata. Fold structures such as syncline and anticline existed alternately	Okubo et al. [47]
No. 10	20.24	6.97	5.80	28.78	High	Pingdingshan	Henan, China	Large amounts of faults and subsidiary fold structures	Su et al. [48]
No. 11	19.53	7.53	5.19	49.79	High	Zhaogu	Henan, China	Large amounts of faults and subsidiary fold structures	Su et al. [42]
No. 12	18.65	6.91	4.26	45.41	High	Zhangcun	Shanxi, China	Coal seams existed in a monocline fold structure	Su et al. [49]
No. 13	16.71	6.34	3.35	38.88	High	Qianqiu	Henan, China	Large synclines, reverse fault structures, and extreme thick roof strata	Pan et al. [44]
No. 14	16.65	6.29	5.12	42.32	High	Chengjiao	Henan, China	Wide and gentle slope fold structures accompanied by a number of faults	Su et al. [23]
No. 15	16.09	5.85	3.59	25.32	High	Qianqiu	Henan, China	Large synclines, reverse fault structures, and extreme thick roof strata	Pan et al. [44]
No. 16	15.82	5.45	2.87	50.88	High	Qianqiu	Henan, China	Large synclines, reverse fault structures, and extreme thick roof strata	Pan et al. [44]
No. 17	14.88	5.83	4.62	58.19	High	Zhangcun	Shanxi, China	Coal seams existed in a monocline fold structure	Su et al. [49]
No. 18	12.40	4.60	2.40	167.23	Low	Pingdingshan	Henan, China	A series of faults and folds existence	Su et al. [48]
No. 19	11.46	4.78	3.59	26.45	Low	Chengjiao	Henan, China	Wide and gentle slope fold structures accompanied by a number of faults	Su et al. [23]
No. 20	11.03	4.03	3.98	187.85	Low	Jixi	Heilongjiang, China	Large amounts of fault structures	Zhang et al. [45]
No. 21	10.41	2.73	2.01	267.32	Low	Pingdingshan	Henan, China	A series of faults and folds existence	Su et al. [48]
No. 22	9.08	3.51	2.26	368.00	Low	Chengjiao	Henan, China	Wide and gentle slope fold structures accompanied by a number of faults	Su et al. [23]
No. 23	8.67	2.97	2.62	110.45	Low	Pingdingshan	Henan, China	A series of faults and folds existence	Su et al. [48]
No. 24	6.87	2.48	0.64	548.20	None	Pingdingshan	Henan, China	A series of faults and folds existence	Su et al. [48]
No. 25	6.64	1.99	1.88	517.06	None	Chengjiao	Henan, China	Wide and gentle slope fold structures accompanied by a number of faults	Su et al. [23]
No. 26	6.07	0.89	1.29	514.40	None	Chengjiao	Henan, China	Wide and gentle slope fold structures accompanied by a number of faults	Su et al. [23]
No. 27	4.98	1.02	1.23	426.13	None	Chengjiao	Henan, China	Wide and gentle slope fold structures accompanied by a number of faults	Su et al. [23]