“…Cheng et al (2018) had to invoke an additional "macropore conductivity" on top of the "matrix K sat " determined by Hassler et al (2011). Indeed, point-measured K sat -values are often reported to be lower than the "block permeabilities" of whole hillslopes (Brooks et al, 2004;Chappell et al, 1998;Pirastru et al, 2017;Wen & Gomez-Hernandez, 1996) or the "effective" parameter values derived with catchment models (e.g., Beven, 1989;Blöschl & Sivapalan, 1995;Chappell et al, 1998;Mertens et al, 2005;Koppe et al, 2022). Apart from the presence of "soil pipes" (Chappell, 2010;Elsenbeer & Vertessy, 2000;Kinner & Stallard, 2004) not captured by point measurements, a further explanation of this discrepancy may include "runoff-runon" processes (Bonell & Williams, 1986), where local IOF generated on patches of low-permeability soil, re-infiltrates in more permeable patches on the way to the stream (cf.…”