‘Local gradient’ and between-site variability of erosion rate on badlands in the Karoo, South Africa

David Favis-Mortlock, John Boardman, Ian D L Foster, Philip Greenwood

Research output: Contribution to JournalArticle

Abstract

Site-average values of local gradient, defined as the steepest slope angle measured at a point, are a powerful predictor of long-term rates of soil loss as measured by erosion pins on the non-channel floor portions of ten badland study sites in the Karoo area of South Africa. Local gradient may be easily measured using a smartphone clinometer. The successful use of local gradient here is in strong contrast to the previous failure of other site-specific attributes, including other measures of gradient and relief, to explain between-site variation in erosion rate on these study sites. Each measurement of local gradient may be thought of as a sample of the site’s microtopography. Microrelief is a strong determinant of the emergent patterns of inter-channel overland flow, and hence of the patterns of inter-channel erosion by flow. Local gradient changes most rapidly during the initial stages of channel incision. When channels are established, local gradient changes more slowly leading to almost-parallel retreat of channel sidewalls. A sensitivity analysis suggests that measurements of local gradient are not all equal with regard to prediction of long-term erosion rate. A greater share of predictive power is contributed by measurements made on very steep or vertical channel side wall areas, and a lesser share is contributed by measurements made on interfluves.
Original languageEnglish
Pages (from-to)871-883
Number of pages13
JournalEarth Surface Processes and Landforms
Volume43
Early online date22 Dec 2017
DOIs
Publication statusPublished - 30 Mar 2018

Fingerprint

badlands
erosion rate
erosion
microrelief
microtopography
slope angle
channel flow
overland flow
sensitivity analysis
relief
Africa
prediction
soil

Keywords

  • Karoo
  • badlands
  • clinometer app
  • local gradient
  • microtopography
  • soil erosion

Cite this

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abstract = "Site-average values of local gradient, defined as the steepest slope angle measured at a point, are a powerful predictor of long-term rates of soil loss as measured by erosion pins on the non-channel floor portions of ten badland study sites in the Karoo area of South Africa. Local gradient may be easily measured using a smartphone clinometer. The successful use of local gradient here is in strong contrast to the previous failure of other site-specific attributes, including other measures of gradient and relief, to explain between-site variation in erosion rate on these study sites. Each measurement of local gradient may be thought of as a sample of the site’s microtopography. Microrelief is a strong determinant of the emergent patterns of inter-channel overland flow, and hence of the patterns of inter-channel erosion by flow. Local gradient changes most rapidly during the initial stages of channel incision. When channels are established, local gradient changes more slowly leading to almost-parallel retreat of channel sidewalls. A sensitivity analysis suggests that measurements of local gradient are not all equal with regard to prediction of long-term erosion rate. A greater share of predictive power is contributed by measurements made on very steep or vertical channel side wall areas, and a lesser share is contributed by measurements made on interfluves.",
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‘Local gradient’ and between-site variability of erosion rate on badlands in the Karoo, South Africa. / Favis-Mortlock, David; Boardman, John; Foster, Ian D L; Greenwood, Philip.

In: Earth Surface Processes and Landforms, Vol. 43, 30.03.2018, p. 871-883.

Research output: Contribution to JournalArticle

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