The Estimation of Reservoir Temperature for Thermal Springs Using the Integrated Multicomponent Geothermometry Method at Changbai Mountain, Northeastern Songliao Basin, China

Table 1

Hydrogeochemical data of selected thermal water samples from the Changbai Mountain volcanic region (mg/L).

Sample no.	Water sample types	T (°C)	pH	K^+	Na^+	Ca^2+	Mg^2+	Cl^-	SO4^2-	HCO3^-	Si	TDS	Hydrochemical type
G01	Julong springs	84	7.34	19.42	347.40	37.20	3.22	114.43	—	903.02	76.08	1471.79	HCO3-Na
G02		82	7.12	20.02	363.15	37.20	4.30	104.89	—	897.21	77.33	1596.75	HCO3-Na
G03	Jinjiang springs	36	6.65	13.48	168.70	31.89	19.33	30.67	16.98	603.95	49.06	1000.13	HCO3-Na
G04		45	7.05	21.94	284.30	30.12	11.81	53.50	21.23	827.53	56.43	1034.88	HCO3-Na
G05		55	6.76	19.56	235.10	30.12	16.11	47.79	—	752.03	64.22	1246.94	HCO3-Na
G06		58	6.65	25.62	285.95	33.66	13.94	59.12	21.23	871.08	83.38	1506.38	HCO3-Na
G07	Shibadaogou springs	35.5	7.04	10.82	324.40	31.89	6.44	123.97	84.92	702.67	24.468	1344.8	HCO3-Na
G08		35	7.03	10.61	308.10	35.43	13.96	123.97	84.92	720.09	23.52	1354.38	HCO3-Na
G09		35	7.34	10.81	328.70	30.12	19.33	133.50	106.15	711.38	24.67	1400.10	HCO3-Na
G10	Xianrenqiao springs	44	7.80	9.94	326.10	31.89	13.96	133.50	297.22	371.66	32.30	1261.56	HCO3·SO4-Na
G11	Cold ground water	9	6.96	1.22	3.10	8.86	4.30	2.85	8.49	46.46	11.64	100.50	HCO3-Ca·Mg