Preferential Water Infiltration Path in a Slow-Moving Clayey Earthslide Evidenced by Cross-Correlation of Hydrometeorological Time Series (Charlaix Landslide, French Western Alps)

Table 3

Hydraulic properties measured on the study site and comparison with the Avignonet landslide [36, 56]. IR: infiltration rate; SIR: saturated infiltration rate after Beerkan tests.

Unit	IR (× 10^−5 m/s)		SIR (× 10^−5 m/s)
	Charlaix	Avignonet	Charlaix	Avignonet
Moraines	1.48	2.7	1	1
Laminated clays			0.57	0.3
Along fractures	7.7	5		4