In:
Vadose Zone Journal, Wiley, Vol. 19, No. 1 ( 2020-01)
Kurzfassung:
Rock outcrops change infiltrability and water flow behavior in a karst soil. The soil hydraulic conductivity ( K ) is spatially variable in a karst area The K is also particularly high at the soil–rock interface. Runoff from outcrops is guided by the rock surface, root channels, and soil fauna burrows.
Materialart:
Online-Ressource
ISSN:
1539-1663
,
1539-1663
Sprache:
Englisch
Verlag:
Wiley
Publikationsdatum:
2020
ZDB Id:
2088189-7