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. 2024 Apr 1;14:7685. doi: 10.1038/s41598-024-58235-z

Table 1.

Distribution of the wells monitoring groundwater flow velocities and directions.

Locations Hills of northern Hubei Jianghan Plain Jiuling Mountains Coastal plain on the Leizhou Peninsula
Well number Well ZK106 Well ZK01 Well DR01 Well HT35 Well PH33
Coordinates of the wells

114°1632′E

31°0917′N

114°4214′E

30°4581′N

113°9928′E

29°0830′N

110°4759′E

20°5631′N

110°3793′E

20°6384′N

Lithology of the monitored aquifer Schist Limestone Granite Basalt Basalt
Depth of the well (m) 200 500 870 35 243
Altitude (asl) of the wellhead (m) 130 21 283 14.8 10.8
Altitude of the well base (m) − 70 − 479 − 587 − 20 − 232.2
Groundwater depth (m) 8.6 1.4 2.52 7.1 18.1
Monitoring depth (m) 129 120, 134 120–236 13, 14, 15 21–30
Monitoring elevation (m) 1 − 113 ~ − 99 47 ~ 163 − 0.2 ~ 1.8 − 19.2 ~ − 10.2