Articles | Volume 10, issue 3
https://doi.org/10.5194/esurf-10-581-2022
https://doi.org/10.5194/esurf-10-581-2022
Research article
 | 
10 Jun 2022
Research article |  | 10 Jun 2022

An experimental study of drainage network development by surface and subsurface flow in low-gradient landscapes

Brian G. Sockness and Karen B. Gran

Viewed

Total article views: 1,855 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,408 411 36 1,855 58 29 26
  • HTML: 1,408
  • PDF: 411
  • XML: 36
  • Total: 1,855
  • Supplement: 58
  • BibTeX: 29
  • EndNote: 26
Views and downloads (calculated since 21 Oct 2021)
Cumulative views and downloads (calculated since 21 Oct 2021)

Viewed (geographical distribution)

Total article views: 1,855 (including HTML, PDF, and XML) Thereof 1,765 with geography defined and 90 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 25 Apr 2024
Download
Short summary
To study channel network development following continental glaciation, we ran small physical experiments where networks slowly expanded into flat surfaces. By changing substrate and rainfall, we altered flow pathways between surface and subsurface. Initially, most channels grew by overland flow. As relief increased, erosion through groundwater sapping occurred, especially in runs with high infiltration and low cohesion, highlighting the importance of groundwater in channel network evolution.