"Changes in some physical properties of soils in the chronosequence of self-overgrown dumps of the Sokolov quarry-dump complex, Czechia"@en . "8"^^ . . "3" . "\u0160ustr, Vladim\u00EDr" . "RU - Rusk\u00E1 federace" . . . "10.1134/S1064229312030076" . "RIV/60077344:_____/12:00377750!RIV13-AV0-60077344" . "Kur\u00E1\u017E, M." . . "45" . . . "Kur\u00E1\u017E, V." . "Romanov, O. V." . "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." . "Frouz, Jan" . . . . "000301977300006" . "126704" . "7"^^ . . "Changes in some physical properties of soils in the chronosequence of self-overgrown dumps of the Sokolov quarry-dump complex, Czechia" . "[6AF33F068FC7]" . "Mako, A." . "RIV/60077344:_____/12:00377750" . "I, P(2B08023)" . "Cejpek, J." . . . "Abakumov, E. V." . "physical properties of soils; chronosequence of self-overgrown dumps; Sokolov quarry-dump complex"@en . "Changes in some physical properties of soils in the chronosequence of self-overgrown dumps of the Sokolov quarry-dump complex, Czechia"@en . "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 . "2"^^ . . . "Eurasian Soil Science" . . "1064-2293" . "Changes in some physical properties of soils in the chronosequence of self-overgrown dumps of the Sokolov quarry-dump complex, Czechia" . . . .