Research Article

Identification of the Hydrogeochemical Processes in Groundwater Using Classic Integrated Geochemical Methods and Geostatistical Techniques, in Amol-Babol Plain, Iran

Table 3

Correlation coefficient matrix of groundwater samples of Amol-Babol Plain.

VariablesTempHCONDTDSDOK+Mg2+Ca2+ ClNa+FTH

Tem0.4320.0450.0000.0270.2600.8360.1960.7450.6720.1590.3950.0180.0220.3340.709
pH0.0640.0710.1340.0470.1930.0010.0000.5080.0020.0000.1780.0310.1860.0000.000
COND0.162−0.1460.0000.0010.0780.0000.0320.2080.0010.0500.0000.0000.0530.0000.287
TDS0.306−0.1220.9850.0000.0740.0000.0930.2260.0020.0370.0000.0000.0260.0000.355
DO−0.1790.161−0.263−0.2870.3080.0310.0380.1810.9150.0160.0160.0050.0000.9010.010
K+0.092−0.1060.1430.145−0.0830.5830.7050.0140.0000.3820.2460.5640.3500.8980.028
Mg2+−0.017−0.2690.3730.351−0.1740.0450.0520.1420.0700.0000.0150.0350.0200.0000.179
Ca2+−0.105−0.3990.1740.1360.168−0.0310.1580.4760.1240.0010.2740.1640.7470.0000.000
−0.0270.0540.1020.099−0.109−0.1980.119−0.0580.0010.8020.1510.0870.5370.5950.574
0.035−0.2540.2670.253−0.0090.3280.1470.125−0.2750.0690.8530.1910.0000.0270.002
0.114−0.2960.1580.169−0.1950.0710.3650.276−0.0200.1470.7630.3200.0000.0000.901
Cl0.0690.1090.7450.719−0.1950.0940.1970.0890.1170.0150.0250.0000.9540.0190.497
Na+0.1910.1750.8560.853−0.2260.0470.171−0.1130.1390.106−0.0810.7370.1180.5980.178
F0.184−0.1080.1570.180−0.3350.0760.188−0.0260.0500.3110.4470.0050.1270.1770.328
TH−0.079−0.4360.3630.324−0.0100.0100.7750.7460.0430.1790.4230.1890.0430.1100.000
−0.030−0.2820.0870.0750.2080.1770.1090.341−0.0460.2440.010−0.055−0.110−0.0800.292

Values in bold are different from 0 with a significance level alpha = 0.05.