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rdf:type
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Description
| - A colluvial soil with a 380 cm deep humus enriched horizon was studied in a loess region of South Moravia, Czech Republic, which is characterized by a strong soil material re-deposition. Distribution of soil properties within the colluvial soil profile was used for distinguishing the different sedimentation phases and understanding colluvial soil formation. The colluvial profile is stratified into different horizons distinguishable by in the profile. Low organic carbon content (0.6-0.8%) and increased carbonate content (up to 8%) in the upper 260 cm idicates a rapid change of the soil cover and significant admixture of loess parent material in the sediment. An abrupt increase of organic carbon content (2%) and no carbonates between 300 and 380 cm, is evidence of a buried Chernozem at this depth. Antropogenically induced substances, such as pesticide residues or increased nutrient content, connected to agricultural practices, enables the detection of sedimantation periods.
- A colluvial soil with a 380 cm deep humus enriched horizon was studied in a loess region of South Moravia, Czech Republic, which is characterized by a strong soil material re-deposition. Distribution of soil properties within the colluvial soil profile was used for distinguishing the different sedimentation phases and understanding colluvial soil formation. The colluvial profile is stratified into different horizons distinguishable by in the profile. Low organic carbon content (0.6-0.8%) and increased carbonate content (up to 8%) in the upper 260 cm idicates a rapid change of the soil cover and significant admixture of loess parent material in the sediment. An abrupt increase of organic carbon content (2%) and no carbonates between 300 and 380 cm, is evidence of a buried Chernozem at this depth. Antropogenically induced substances, such as pesticide residues or increased nutrient content, connected to agricultural practices, enables the detection of sedimantation periods. (en)
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Title
| - Identification of Neolithic to Modern erosion-sedimentation phases using geochemical approach in a loess covered sub-catchemnt of South Moravia, Czech Republic
- Identification of Neolithic to Modern erosion-sedimentation phases using geochemical approach in a loess covered sub-catchemnt of South Moravia, Czech Republic (en)
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skos:prefLabel
| - Identification of Neolithic to Modern erosion-sedimentation phases using geochemical approach in a loess covered sub-catchemnt of South Moravia, Czech Republic
- Identification of Neolithic to Modern erosion-sedimentation phases using geochemical approach in a loess covered sub-catchemnt of South Moravia, Czech Republic (en)
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skos:notation
| - RIV/60460709:41210/13:60214!RIV14-MZE-41210___
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http://linked.open...avai/predkladatel
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
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http://linked.open...iv/cisloPeriodika
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/60460709:41210/13:60214
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - Colluvium, Soil erosion, Risk elements, Organochlorine pesticides, Chernozem (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...odStatuVydavatele
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http://linked.open...ontrolniKodProRIV
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http://linked.open...i/riv/nazevZdroje
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...vavai/riv/projekt
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http://linked.open...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Chuman, Tomáš
- Mihaljevič, Martin
- Penížek, Vít
- Šefrna, Luděk
- Drábek, Ondřej
- Zádorová, Tereza
- Volf, Šimon
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http://linked.open...ain/vavai/riv/wos
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issn
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number of pages
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http://localhost/t...ganizacniJednotka
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