Analytical Solutions for Steady-State Multiwell Aquifer Tests in Rectangular Aquifers by Using Double Fourier Transform: A Case Study in the Ordos Plateau, China

Table 3

Key results of single-well aquifer tests.

Wells	Aquifer thickness (m)	Drawdown in pumping wells (m)	Flow rate (m^3/h)	OBS I	OBS II	OBS III	Hydraulic conductivity (m/d)
				Drawdown in observations wells (m)/distance to the pumping well (m)
							OBS I&II	OBS II&III	OBS I&III
HT12	118.06	7.35	161.92	1.02/5.19	0.53/24.82	0.31/64.42	16.84	22.79	18.69
HT17	96.74	4.78	175.33	1.17/4.35	0.83/10.16	0.30/43.29	17.45	19.04	18.42
HT26	91.05	16.63	162.52	1.58/5.15	0.93/24.89	0.60/64.67	16.76	19.90	17.82
HT28	98.66	8.52	173.10	1.07/4.92	0.60/33.79	0.25/66.89	27.71	13.13	21.47
				Note: drawdown/distance			Average: 19.17