Evolution of sandy soils within deflation hollows in shifting areas of sand - a case study from the Błędów Desert (Poland)
Areas of shifting sand are important places for testing the effects of abiotic and biotic factors on soil morphology and evolution, where aeolian processes cause dynamic changes in the natural environment. The main aim of the study was to determine the evolution of soils within deflation hollows in...
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Published in | Soil and water research Vol. 12; no. 3; pp. 161 - 169 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Prague
Czech Academy of Agricultural Sciences (CAAS)
01.01.2017
Czech Academy of Agricultural Sciences |
Subjects | |
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Abstract | Areas of shifting sand are important places for testing the effects of abiotic and biotic factors on soil morphology and evolution, where aeolian processes cause dynamic changes in the natural environment. The main aim of the study was to determine the evolution of soils within deflation hollows in shifting sands. In the context of this purpose, representative study areas were selected: (1) a reference surface in a plantation forest with soils undisturbed by aeolian processes – one pedon, (2) an active deflation hollow – two pedons, (3) a deflation hollow stabilized by reforestation (forest planting ca. 30 and ca. 100 years ago – two pedons). Soil morphology and micromorphology as well as several physical and chemical properties were analyzed. In a deflation hollow, the studied soils are found at various stages of development, mostly characterized by a relatively rapid accumulation of soil organic matter. A well-developed buried illuvial B horizon as an ‘ortstein’ material can limit aeolian erosion to a certain depth, while above these horizons aeolian erosion and accumulation remain active. History of changes in the environment is to a substantial degree reflected in morphology and micromorphology of the studied soils. |
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AbstractList | Areas of shifting sand are important places for testing the effects of abiotic and biotic factors on soil morphology and evolution, where aeolian processes cause dynamic changes in the natural environment. The main aim of the study was to determine the evolution of soils within deflation hollows in shifting sands. In the context of this purpose, representative study areas were selected: (1) a reference surface in a plantation forest with soils undisturbed by aeolian processes – one pedon, (2) an active deflation hollow – two pedons, (3) a deflation hollow stabilized by reforestation (forest planting ca. 30 and ca. 100 years ago – two pedons). Soil morphology and micromorphology as well as several physical and chemical properties were analyzed. In a deflation hollow, the studied soils are found at various stages of development, mostly characterized by a relatively rapid accumulation of soil organic matter. A well-developed buried illuvial B horizon as an ‘ortstein’ material can limit aeolian erosion to a certain depth, while above these horizons aeolian erosion and accumulation remain active. History of changes in the environment is to a substantial degree reflected in morphology and micromorphology of the studied soils. |
Author | DREWNIK, Marek GUS, Magdalena |
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CitedBy_id | crossref_primary_10_1016_j_rsase_2024_101253 crossref_primary_10_1007_s00248_023_02333_4 crossref_primary_10_1016_j_geoderma_2021_115535 crossref_primary_10_3390_ijms241713605 crossref_primary_10_1177_09596836231185838 |
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SubjectTerms | Accumulation aeolian processes Biotic factors Chemical properties Deflation Developmental stages drift sand Eolian processes Evolution Morphology Organic matter Organic soils ortstein podzolization Reforestation Sand Sandy soils soil development Soil dynamics Soil erosion Soil morphology Soil organic matter |
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Title | Evolution of sandy soils within deflation hollows in shifting areas of sand - a case study from the Błędów Desert (Poland) |
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