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  • Abstract: In the Czech Republic chernozems are among the most fertile soils and are intensively farmed. It turns out that when using intensification measures, enlarging fields, using substandard farming practices and cultivating wide-row crops, water erosion becomes a major problem. The result is degradation of physical properties, compaction and depletion of the most fertile part of the soil - topsoil. For wider pedological characteristics a plot with chernozem on loess affected by water erosion has been selected. Three probes were dug and described at three places of the slope and physical characteristics of topsoil and subsoil were conducted along with grain size analysis with the determination of carbonates in the topsoil, subsoil and in the loess cover to the depth of one meter. Physical analysis showed that the eroded slope suffers a serious problem of soil compaction. Porosity in the topsoil and subsoil is around the critical value of 45% or below. Minimum air capacity indicates critical condition of most horizons. On average, the topsoil and subsoil classifies as loamy soil type. The grain size is dusty loam. Loess exhibits relatively high homogenity which does not dramatically change with depth, not even on the plots with the risk of land erosion. The highest carbonate content in the topsoil and subsoil is on the hillside, where occures mixing of the loess to the topsoil horizon. In the loess, the contents of CaCO3 are highly variable. Mean values range from 13.2 to 17.9% of the carbonates with a standard deviation of 2.99.
  • Abstract: In the Czech Republic chernozems are among the most fertile soils and are intensively farmed. It turns out that when using intensification measures, enlarging fields, using substandard farming practices and cultivating wide-row crops, water erosion becomes a major problem. The result is degradation of physical properties, compaction and depletion of the most fertile part of the soil - topsoil. For wider pedological characteristics a plot with chernozem on loess affected by water erosion has been selected. Three probes were dug and described at three places of the slope and physical characteristics of topsoil and subsoil were conducted along with grain size analysis with the determination of carbonates in the topsoil, subsoil and in the loess cover to the depth of one meter. Physical analysis showed that the eroded slope suffers a serious problem of soil compaction. Porosity in the topsoil and subsoil is around the critical value of 45% or below. Minimum air capacity indicates critical condition of most horizons. On average, the topsoil and subsoil classifies as loamy soil type. The grain size is dusty loam. Loess exhibits relatively high homogenity which does not dramatically change with depth, not even on the plots with the risk of land erosion. The highest carbonate content in the topsoil and subsoil is on the hillside, where occures mixing of the loess to the topsoil horizon. In the loess, the contents of CaCO3 are highly variable. Mean values range from 13.2 to 17.9% of the carbonates with a standard deviation of 2.99. (en)
Title
  • The detailed characterization of land threatened by water erosion with soil type chernozem on loess at Dambořice
  • The detailed characterization of land threatened by water erosion with soil type chernozem on loess at Dambořice (en)
skos:prefLabel
  • The detailed characterization of land threatened by water erosion with soil type chernozem on loess at Dambořice
  • The detailed characterization of land threatened by water erosion with soil type chernozem on loess at Dambořice (en)
skos:notation
  • RIV/62156489:43210/14:00230044!RIV15-MSM-43210___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • S
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 10565
http://linked.open...ai/riv/idVysledku
  • RIV/62156489:43210/14:00230044
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • water erosion; loess; chernozem (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [0B7DA8382773]
http://linked.open...v/mistoKonaniAkce
  • Brno, Czech Republic
http://linked.open...i/riv/mistoVydani
  • Brno, Czech Republic
http://linked.open...i/riv/nazevZdroje
  • MendelNet 2014 - Proceedings of International PhD Students Conference
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Jandák, Jiří
  • Hammerová, Anna
  • Šimečková, Jana
  • Mičulková, Beáta
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
number of pages
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  • Mendel University in Brno
https://schema.org/isbn
  • 978-80-7509-174-1
http://localhost/t...ganizacniJednotka
  • 43210
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