Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Geology Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Geology; April 2007; v. 35; no. 4; p. 303-306; DOI: 10.1130/G23109A.1
© 2007 Geological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via ISI Web of Science (3)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Vanacker, V.
Right arrow Articles by Kubik, P.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Restoring dense vegetation can slow mountain erosion to near natural benchmark levels

Veerle Vanacker*,1, Friedhelm von Blanckenburg1, Gerard Govers2, Armando Molina2, Jean Poesen2, Jozef Deckers3 and Peter Kubik4

1 Institute for Mineralogy, University of Hannover, Callinstrasse 3, 30167 Hannover, Germany
2 Physical and Regional Geography, Katholieke Universiteit Leuven, Celestijnenlaan 200E, 3001 Heverlee, Belgium
3 Division of Soil and Water Management, Katholieke Universiteit Leuven, Celestijnenlaan 200E, 3001 Heverlee, Belgium
4 Paul Scherrer Institute, Institute of Particle Physics, ETH Hoenggerberg, CH-8093 Zurich, Switzerland

Tropical mountain areas may undergo rapid land degradation as demographic growth and intensified agriculture cause more people to migrate to fragile ecosystems. To assess the extent of the resulting damage, an erosion rate benchmark against which changes in erosion can be evaluated is required. Benchmarks reflecting natural erosion rates are usually not provided by conventional sediment fluxes, which are often biased due to modern land use change, and also miss large, episodic events within the measuring period. To overcome this, we combined three independent assessment tools in the southern Ecuadorian Andes, an area that is severely affected by soil erosion. First, denudation rates from cosmogenic nuclides in river sediment average over time periods of 1–100 k.y. and establish a natural benchmark of only 150 ± 100 t km–2 yr–1. Second, we find that land use practices have increased modern sediment yields as derived from reservoir sedimentation rates, which average over periods of 10–100 yr to as much as 15 x 103 t km–2 yr–1. Third, our land cover analysis has shown us that vegetation cover exerts first-order control over present-day erosion rates at the catchment scale. Areas with high vegetation density erode at rates that are characteristically similar to those of the natural benchmark, regardless of whether the type of vegetation is native or anthropogenic. Therefore, our data suggest that even in steep mountain environments sediment fluxes can slow to near their natural benchmark levels with suitable revegetation programs. A set of techniques is now in place to evaluate the effectiveness of erosion mitigation strategies.

Key Words: erosion • vegetation cover • human impact • land use change • cosmogenic nuclides • Andes







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Geological Society of America