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Anthropogenic erosion-induced small-scale soil heterogeneity in South African rangelands

Bibliographic Data

ID5253195
AuthorsJuliane Krenz (0000-0002-5817-843X, University of Basel, corresponding author), P Greenwood (0000-0002-3704-8329, University of Basel), Nikolaus J Kuhn (0000-0003-4869-098X, University of Basel)
Year2021
Volume34
Pages100290
Publication date2021-06-01
Open AccessYes
TypeARTICLE
VenueAnthropocene (JOURNAL)
Journal identifiersISSN: 2213-3054
PublisherElsevier BV (PUBLISHER)
DOI10.1016/j.ancene.2021.100290
OpenAlexW3145515297
LanguageEN
Citations received1
References cited56

Land-use-induced soil erosion in semi-arid drylands induced by land-use changes creates patchworks of soils and vegetation different from those of natural conditions. Knowledge of the highly dynamic spatial heterogeneity in soil properties, not depicted in conventional soil maps, is important for managing land uses sustainably, and for understanding soil-climate interactions. This study carries out analysis of soil redistribution in a degraded rangeland in South Africa, to assess the significance of anthropogenic soil heterogeneity within a small catchment with a silted-up reservoir. Surface soil (N = 51) and soil profile (N = 29) samples were collected from areas of various degrees of degradation and analysed for texture, pH, total nitrogen (TN), total organic carbon (TOC), available phosphorus (P), and potassium (K). Diverse vegetation cover is reflected in a high soil heterogeneity, showing differences in soil texture. Average surface soil nutrient content was significantly higher in vegetated areas (grassland: TOC 1.08 %, TN 0.10 %, P 20.12 mg kg −1 , mixed vegetation: TOC 0.93 %, TN 0.08 %, P 13.54 mg kg −1 , depositional: TOC 1.68 %, TN 0.18 %, P 34.67 mg kg −1 ) than at degraded sites (TOC 0.47 %, TN 0.06 %, P 7.52 mg kg −1 ). K content was low to moderate but did not show any significant difference between landscape units. Potential exists for the formation of distinct young anthropogenic soils on the silted-up reservoir where deposited sediments differed in TOC, TN, P, and profile depth from the shallow natural soils. Consequently, azonal soils on dam-deposits are different from those occurring naturally, and not depicted on conventional soil maps. Their different water and nutrient cycling may affect vegetation and biogeochemical fluxes. Land-use management should consider such soils, as they play an important role in rangeland ecology

Agroforestry · Biology · Erosion · Hydrology (agriculture · Rangeland · Soil carbon · Soil retrogression and degradation · Soil test · Soil texture · Soil water · Total organic carbon · Vegetation (pathology · Aeolian processes and effects · Environmental Science · Rangeland Management and Livestock Ecology · Soil erosion and sediment transport · Ecology · Geology · Soil Science

  • The Potential to Reconstruct 20th Century Soil Organic Carbon Erosion in Rangelands From Small Reservoir Sediments

    Open Access•Lu Li, Juliane Krenz et al.•Land Degradation and Development•2024

  • Soil erosion and the global carbon budget

    Open Access•Rattan Lal•Environment International•2003

  • Biological Feedbacks in Global Desertification

    Open Access•William H Schlesinger, James F Reynolds et al.•Science•1990

Citations per year0.5
Citation span2024 - 2024 (1)
Highly citedNo

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