In:
Water Resources Research, American Geophysical Union (AGU), Vol. 53, No. 6 ( 2017-06), p. 4709-4724
Abstract:
Relaxation dynamics through internal redistribution of fluids after fast drainage occurs in two stages A quick dissipation within seconds is followed by slow relaxation within several hours due to relaxation of dynamic contact angles Fluid configurations during relaxation are very different from those during quasi‐static drainage and imbibition
Type of Medium:
Online Resource
ISSN:
0043-1397
,
1944-7973
DOI:
10.1002/2016WR019815
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2029553-4
detail.hit.zdb_id:
5564-5
SSG:
13
SSG:
14