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The effect of accelerated soil erosion on hillslope morphology
Abstract
© 2019 John Wiley & Sons, Ltd. Intensive agricultural land use can have detrimental
effects on landscape properties, greatly accelerating soil erosion, with consequent
fertility loss and reduced agricultural potential. To quantify the effects of such
erosional processes on hillslope morphology and gain insight into the underlying dynamics,
we use a twofold approach. First, a statistical analysis of topographical features
is conducted, with a focus on slope and gradient distributions. The accelerated soil
erosion is shown to be fingerprinted in the distribution tails, which provide a clear
statistical signature of this human-induced land modification. Theoretical solutions
are then derived for the hillslope morphology and the associated creep and runoff
erosion fluxes, allowing us to distinguish between the main erosional mechanisms operating
in disturbed and undisturbed areas. We focus our application on the landscape at the
Calhoun Critical Zone Observatory in the US Southern Piedmont, where severe soil erosion
followed intensive cotton cultivation, resulting in highly eroded and gullied hillslopes.
The observed differences in hillslope morphologies in disturbed and undisturbed areas
are shown to be related to the disruption of the natural balance between soil creep
and runoff erosion. The relaxation time required for the disturbed hillslopes to reach
a quasi-equilibrium condition is also investigated. © 2019 John Wiley & Sons, Ltd.
Type
Journal articleSubject
Science & TechnologyPhysical Sciences
Geography, Physical
Geosciences, Multidisciplinary
Physical Geography
Geology
calhoun CZO
hillslope morphology
land degradation
soil erosion
topographic slope
LOESS PLATEAU
LANDSCAPE EVOLUTION
DRAINAGE
DISTRIBUTIONS
CONSERVATION
EQUILIBRIUM
ENVIRONMENT
STABILITY
ROUGHNESS
TRANSPORT
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https://hdl.handle.net/10161/21222Published Version (Please cite this version)
10.1002/esp.4694Publication Info
Bonetti, S; Richter, DD; & Porporato, A (2019). The effect of accelerated soil erosion on hillslope morphology. Earth Surface Processes and Landforms, 44(15). pp. 3007-3019. 10.1002/esp.4694. Retrieved from https://hdl.handle.net/10161/21222.This is constructed from limited available data and may be imprecise. To cite this
article, please review & use the official citation provided by the journal.
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Show full item recordScholars@Duke
Amilcare Porporato
Adjunct Professor in the Department of Civil and Environmental Engineering
Amilcare Porporato earned a Master Degree in Civil Engineering (summa cum laude) in
1992 and his Ph.D. in 1996 from Polytechnic of Turin. He was appointed Assistant Professor
in the Department of Hydraulics of the Polytechnic of Turin, and he moved to Duke
University in 2003, where he is now Full Professor in the Department of Civil and
Environmental Engineering with a secondary appointment with the Nicholas School of
the Environment.
In June 1996, Porporato received the Arturo Parisatti
Daniel D. Richter
Professor in the Division of Earth and Climate Science
Richter’s research and teaching links soils with ecosystems and the wider environment,
most recently Earth scientists’ Critical Zone. He focuses on how humanity is transforming
Earth’s soils from natural to human-natural systems, specifically how land-uses alter
soil processes and properties on time scales of decades, centuries, and millennia.
Richter's book, Understanding Soil Change (Cambridge University Press), co-authored
with his former PhD
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