|
|
|
|||||||||||||||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
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 1100 k.y. and establish a natural benchmark of only 150 ± 100 t km2 yr1. Second, we find that land use practices have increased modern sediment yields as derived from reservoir sedimentation rates, which average over periods of 10100 yr to as much as 15 x 103 t km2 yr1. 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
This article has been cited by other articles:
![]() |
I. J. Larsen, L. H. MacDonald, E. Brown, D. Rough, M. J. Welsh, J. H. Pietraszek, Z. Libohova, J. de Dios Benavides-Solorio, and K. Schaffrath Causes of Post-Fire Runoff and Erosion: Water Repellency, Cover, or Soil Sealing? Soil Sci. Soc. Am. J., June 29, 2009; 73(4): 1393 - 1407. [Abstract] [Full Text] [PDF] |
||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |