About: Changes in some physical properties of soils in the chronosequence of self-overgrown dumps of the Sokolov quarry-dump complex, Czechia     Goto   Sponge   NotDistinct   Permalink

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  • The water-physical properties (bulk density, air conductivity, texture, water content, and temperature dynamics) were studied in a chronosequence of soils developing on self-overgrowing quarry-dump complexes in the area of Sokolov, Czechia. The area overgrown for 12 years was covered by a thin grass cover; osiers were observed after 20 years of overgrowth; a broadleaved forest was found on a plot after 45 years of overgrowth. The particle-size distribution in the soil was determined using peptization by pyrophosphate and the FAO method. When the soil was prepared by the FAO method, a predominance of physical clay (62-72%) in the dump material was revealed; at the use of pyrophosphate peptization, the content of this fraction was lower (18-19%). The observed differences can be due to the incomplete degradation of the microaggregates composed of clay particles during the peptization by pyrophosphate.
  • The water-physical properties (bulk density, air conductivity, texture, water content, and temperature dynamics) were studied in a chronosequence of soils developing on self-overgrowing quarry-dump complexes in the area of Sokolov, Czechia. The area overgrown for 12 years was covered by a thin grass cover; osiers were observed after 20 years of overgrowth; a broadleaved forest was found on a plot after 45 years of overgrowth. The particle-size distribution in the soil was determined using peptization by pyrophosphate and the FAO method. When the soil was prepared by the FAO method, a predominance of physical clay (62-72%) in the dump material was revealed; at the use of pyrophosphate peptization, the content of this fraction was lower (18-19%). The observed differences can be due to the incomplete degradation of the microaggregates composed of clay particles during the peptization by pyrophosphate. (en)
Title
  • Changes in some physical properties of soils in the chronosequence of self-overgrown dumps of the Sokolov quarry-dump complex, Czechia
  • Changes in some physical properties of soils in the chronosequence of self-overgrown dumps of the Sokolov quarry-dump complex, Czechia (en)
skos:prefLabel
  • Changes in some physical properties of soils in the chronosequence of self-overgrown dumps of the Sokolov quarry-dump complex, Czechia
  • Changes in some physical properties of soils in the chronosequence of self-overgrown dumps of the Sokolov quarry-dump complex, Czechia (en)
skos:notation
  • RIV/60077344:_____/12:00377750!RIV13-AV0-60077344
http://linked.open...avai/riv/aktivita
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  • I, P(2B08023)
http://linked.open...iv/cisloPeriodika
  • 3
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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  • 126704
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  • RIV/60077344:_____/12:00377750
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  • physical properties of soils; chronosequence of self-overgrown dumps; Sokolov quarry-dump complex (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • RU - Ruská federace
http://linked.open...ontrolniKodProRIV
  • [6AF33F068FC7]
http://linked.open...i/riv/nazevZdroje
  • Eurasian Soil Science
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
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  • 45
http://linked.open...iv/tvurceVysledku
  • Frouz, Jan
  • Abakumov, E. V.
  • Cejpek, J.
  • Kuráž, M.
  • Kuráž, V.
  • Mako, A.
  • Romanov, O. V.
  • Šustr, Vladimír
http://linked.open...ain/vavai/riv/wos
  • 000301977300006
issn
  • 1064-2293
number of pages
http://bibframe.org/vocab/doi
  • 10.1134/S1064229312030076
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