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Statements

Subject Item
n2:RIV%2F60460709%3A41210%2F11%3A52559%21RIV12-MSM-41210___
rdf:type
skos:Concept n13:Vysledek
dcterms:description
The labile fraction of soil organic carbon (SOC) in terms of its quantity is a sensitive but dynamic indicator of the reactive agent in soils. If it is to be considered as a feature of soil quality, the value of its quantity should be completed by data on its quality. It can be expressed by the value of the rate constant of microbial oxidation k(bio) of this fraction or by data on chemical stability during hydrolysis or oxidation. If the quality of SOC labile fraction is not determined, at least the ratio of C(MIC):C(org) should be given. The adjustment of soil acidity increases the microbial activity of soils, therefore the quantity of SOC labile fraction and k(bio) decrease proportionately to the increasing stability of soil organic matter. During a 5-year period after the liming the soils acidify again and this process passes the faster the lesser their ion exchange capacity and buffering are. The quantity of the labile fraction of SOC raises again, its stability decreases and k(bio) raises again. The labile fraction of soil organic carbon (SOC) in terms of its quantity is a sensitive but dynamic indicator of the reactive agent in soils. If it is to be considered as a feature of soil quality, the value of its quantity should be completed by data on its quality. It can be expressed by the value of the rate constant of microbial oxidation k(bio) of this fraction or by data on chemical stability during hydrolysis or oxidation. If the quality of SOC labile fraction is not determined, at least the ratio of C(MIC):C(org) should be given. The adjustment of soil acidity increases the microbial activity of soils, therefore the quantity of SOC labile fraction and k(bio) decrease proportionately to the increasing stability of soil organic matter. During a 5-year period after the liming the soils acidify again and this process passes the faster the lesser their ion exchange capacity and buffering are. The quantity of the labile fraction of SOC raises again, its stability decreases and k(bio) raises again.
dcterms:title
Relationships between quality and quantity of soil labile fraction of the soil carbon in Cambisols after liming during a 5-year period Relationships between quality and quantity of soil labile fraction of the soil carbon in Cambisols after liming during a 5-year period
skos:prefLabel
Relationships between quality and quantity of soil labile fraction of the soil carbon in Cambisols after liming during a 5-year period Relationships between quality and quantity of soil labile fraction of the soil carbon in Cambisols after liming during a 5-year period
skos:notation
RIV/60460709:41210/11:52559!RIV12-MSM-41210___
n13:predkladatel
n19:orjk%3A41210
n3:aktivita
n7:Z
n3:aktivity
Z(MSM6007665806), Z(MSM6046070901)
n3:cisloPeriodika
5
n3:dodaniDat
n5:2012
n3:domaciTvurceVysledku
n17:3646149
n3:druhVysledku
n14:J
n3:duvernostUdaju
n6:S
n3:entitaPredkladatele
n12:predkladatel
n3:idSjednocenehoVysledku
226429
n3:idVysledku
RIV/60460709:41210/11:52559
n3:jazykVysledku
n15:eng
n3:klicovaSlova
soil organic carbon (SOC), labile fraction SOC, quality and quantity, effect of soil reaction adjustment, time changes
n3:klicoveSlovo
n9:labile%20fraction%20SOC n9:quality%20and%20quantity n9:effect%20of%20soil%20reaction%20adjustment n9:time%20changes n9:soil%20organic%20carbon%20%28SOC%29
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[1DFC00A0302D]
n3:nazevZdroje
Plant, Soil and Environment
n3:obor
n18:GD
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
6
n3:rokUplatneniVysledku
n5:2011
n3:svazekPeriodika
57
n3:tvurceVysledku
Borová-Batt, J. Peterka, Jiří Pezlarová, J. Kolář, Ladislav Vaněk, Václav Kužel, Stanislav
n3:wos
000291215400001
n3:zamer
n4:MSM6046070901 n4:MSM6007665806
s:issn
1214-1178
s:numberOfPages
8
n16:organizacniJednotka
41210