Clayey soils have very low permeability due to their fine-grained structure. The constant head test is generally suitable for coarse-grained soils like sand and gravel, which allow faster water flow. On the other hand, the falling head test is better suited for fine-grained soils like clay because it can more accurately measure the slow rate of flow through such soils.
In the falling head test, the rate at which the water level falls in a standpipe is monitored, allowing precise calculation of permeability even in low-permeability soils.
Hence, the falling head test is most appropriate for laboratory measurement of permeability in clayey soils.