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  • During the experiment were monitored values of soil bulk density and water infiltration rate. Appointed values were measured on experimental field where different soil treatment technologies and different compaction levels (inside and outside of the tracks of agricultural machinery) were applied. Different soil treatments were: loosening, loosening which was preceded by deep loosening (DL), ploughing, ploughing which was preceded by deep loosening (DL). Saturated hydraulic conductivity of the soil (Kfs) was measured at different soil treatments and compaction levels using the single-ring infiltration method (simplified falling-head method – SFH). The results showed statistically significant differences of Kfs between non-compacted and compacted parts of the soil. In the case of loosening technology the range of the results outside of the tracks was from 16.37 to 30.6 mm.h-1 and under the same condition of treatment the values was in the range from 4.88 to 8.58 mm.h-1 inside of tracks. Differences wer
  • During the experiment were monitored values of soil bulk density and water infiltration rate. Appointed values were measured on experimental field where different soil treatment technologies and different compaction levels (inside and outside of the tracks of agricultural machinery) were applied. Different soil treatments were: loosening, loosening which was preceded by deep loosening (DL), ploughing, ploughing which was preceded by deep loosening (DL). Saturated hydraulic conductivity of the soil (Kfs) was measured at different soil treatments and compaction levels using the single-ring infiltration method (simplified falling-head method – SFH). The results showed statistically significant differences of Kfs between non-compacted and compacted parts of the soil. In the case of loosening technology the range of the results outside of the tracks was from 16.37 to 30.6 mm.h-1 and under the same condition of treatment the values was in the range from 4.88 to 8.58 mm.h-1 inside of tracks. Differences wer (en)
Title
  • Impact of land crossing on soil physical properties
  • Impact of land crossing on soil physical properties (en)
skos:prefLabel
  • Impact of land crossing on soil physical properties
  • Impact of land crossing on soil physical properties (en)
skos:notation
  • RIV/60460709:41310/13:60645!RIV15-MSM-41310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • S
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 78995
http://linked.open...ai/riv/idVysledku
  • RIV/60460709:41310/13:60645
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • soil bulk density, water infiltration rate, controlled traffic, soil treatments, soil compaction (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [938DFF46B937]
http://linked.open...v/mistoKonaniAkce
  • Prague
http://linked.open...i/riv/mistoVydani
  • Prague
http://linked.open...i/riv/nazevZdroje
  • 5th International Conference on Trends in Agricultural Engineering 2013, TAE 2013
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Kumhála, František
  • Kroulík, Milan
  • Chyba, Jan
http://linked.open...vavai/riv/typAkce
http://linked.open...ain/vavai/riv/wos
  • 000345059700053
http://linked.open.../riv/zahajeniAkce
number of pages
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  • Česká zemědělská univerzita v Praze
https://schema.org/isbn
  • 978-80-213-2388-9
http://localhost/t...ganizacniJednotka
  • 41310
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