Mots-clés
Actuel ; Bassin-versant ; Cours d'eau éphémère ; Dynamique du paysage ; Ecoulement fluvial ; Ecoulement hypodermique ; Ecoulement superficiel ; Erosion des sols ; Erosion hydrique ; Etats-Unis ; North Carolina ; Piedmont ; Ravinement ; Réseau de drainage ; Siècle 18 ; Utilisation du solDrainage network ; Eighteenth Century ; Ephemeral stream ; Gully erosion ; Land use ; Landscape dynamics ; North Carolina ; Overland flow ; Piedmont ; Present time ; Soil erosion ; Stream flow ; Subsurface flow ; United States of America ; Water erosion ; WatershedAbarrancamiento ; Actual ; Aprovechamiento del suelo ; Carolina del Norte ; Cuenca hidrográfica ; Dinámica del paisaje ; Erosión de los suelos ; Erosión hídrica ; Escorrentíafluvial ; Escorrentíahipodérmica ; Escorrentíasuperficial ; Estados Unidos ; Piemonte ; Red de drenaje ; Siglo 18Channel network extent in the context of historical land use, flow generation processes, and landscape evolution in the North Carolina Piedmont
Auteur(s) et Affiliation(s)
JEFFERSON, A.J.
Dept. of Geography and Earth Sciences, Univ. of North Carolina, Charlotte, Etats-Unis
Dept. of Geology, State Univ., Kent, Etats-Unis
MCGEE, R.W.
Dept. of Geography and Earth Sciences, Univ. of North Carolina, Charlotte, Etats-Unis
Hart and Hickman, Charlotte, Etats-Unis
Description :
In 6 study areas in the North Carolina Piedmont, 100 channel heads were mapped in fully-forested watersheds, revealing a channel initiation relationship between contributing area and local slope. Flow in these channels is generated by subsurface and overland flow. The measured relative slope exponent is lower than expected based on literature values of ~2 for forested watersheds with subsurface and overland flow, suggesting that the channel network extent may reflect a former hydrological regime. However, geomorphic evidence of recovery in channel heads within fully forested watersheds is greater than those with present day pasture. Channel network extent appears to be sensitive to land use change, with recovery beginning within decades of afforestation. Channel initiation mapping and area-slope relationships are shown to be useful tools for interpreting geomorphic effects of land use change.
Type de document :
Article de périodique
Source :
Earth surface processes and landforms, issn : 0197-9337, 2013, vol. 38, n°. 6, p. 601-613, nombre de pages : 13, Références bibliographiques : 2 p.
Date :
2013
Editeur :
Pays édition : Royaume-Uni, Chichester, Wiley
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)