Step 1: Statement (I) claims that isotropic and homogeneous aquifers seldom occur in nature. In real aquifers, hydraulic conductivity commonly varies with position (heterogeneity) and with direction at a point (anisotropy), because of layered deposition, varying grain size, fractures and geological history. The isotropic, homogeneous aquifer is a simplifying idealisation used mainly to make the governing groundwater flow equations solvable, not something actually found in the field. So Statement (I) is correct.
Step 2: Statement (II) describes how a pumping test is actually carried out: while the main well is pumped at a steady rate, water level drawdown is measured over time in observation wells, some placed close to the pumped well and others farther away, so that the drawdown pattern with distance and time can be used to estimate aquifer transmissivity and storativity. This matches standard pumping test procedure, so Statement (II) is correct too.
Step 3: Both statements agree with accepted groundwater hydrology practice, so the correct choice is that both Statement (I) and Statement (II) are correct, option 1.