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Statements

Subject Item
n2:RIV%2F60076658%3A12220%2F10%3A00012526%21RIV11-MSM-12220___
rdf:type
n9:Vysledek skos:Concept
dcterms:description
Soil organic matter (SOM) can be divided into three main pools: labile, stable and inert. Research over recent years has focused on the labile fraction (LF), as it is considered a quickly reactive indicator of soil productivity and health, and important as a supply of energy for soil micro-organisms. A wide spectrum of analytical methods has been used to determine and/or evaluate LF, based on physical, chemical and biochemical principles. The advantages and disadvantages of each technique are explored in this work, but none of the methods can determine LF sufficiently, either because a part of the LF is not involved or because further characterisation is missing. Although analytical methods are widely used to evaluate changes in soil management or organic carbon turnover, the practical question of the quantity and quality of SOM cannot be answered completely. It is also suggested that future research should focus on the interactions among SOM fractions and their better chemical and functional charact Soil organic matter (SOM) can be divided into three main pools: labile, stable and inert. Research over recent years has focused on the labile fraction (LF), as it is considered a quickly reactive indicator of soil productivity and health, and important as a supply of energy for soil micro-organisms. A wide spectrum of analytical methods has been used to determine and/or evaluate LF, based on physical, chemical and biochemical principles. The advantages and disadvantages of each technique are explored in this work, but none of the methods can determine LF sufficiently, either because a part of the LF is not involved or because further characterisation is missing. Although analytical methods are widely used to evaluate changes in soil management or organic carbon turnover, the practical question of the quantity and quality of SOM cannot be answered completely. It is also suggested that future research should focus on the interactions among SOM fractions and their better chemical and functional charact Soil organic matter (SOM) can be divided into three main pools: labile, stable and inert. Research over recent years has focused on the labile fraction (LF), as it is considered a quickly reactive indicator of soil productivity and health, and important as a supply of energy for soil micro-organisms. A wide spectrum of analytical methods has been used to determine and/or evaluate LF, based on physical, chemical and biochemical principles. The advantages and disadvantages of each technique are explored in this work, but none of the methods can determine LF sufficiently, either because a part of the LF is not involved or because further characterisation is missing. Although analytical methods are widely used to evaluate changes in soil management or organic carbon turnover, the practical question of the quantity and quality of SOM cannot be answered completely. It is also suggested that future research should focus on the interactions among SOM fractions and their better chemical and functional charact
dcterms:title
Methods for determination of labile soil organic matter: An overview Methods for determination of labile soil organic matter: An overview Methods for determination of labile soil organic matter: An overview
skos:prefLabel
Methods for determination of labile soil organic matter: An overview Methods for determination of labile soil organic matter: An overview Methods for determination of labile soil organic matter: An overview
skos:notation
RIV/60076658:12220/10:00012526!RIV11-MSM-12220___
n3:aktivita
n6:Z
n3:aktivity
Z(MSM6007665806)
n3:cisloPeriodika
2
n3:dodaniDat
n12:2011
n3:domaciTvurceVysledku
n15:4724976
n3:druhVysledku
n11:J
n3:duvernostUdaju
n5:S
n3:entitaPredkladatele
n17:predkladatel
n3:idSjednocenehoVysledku
270705
n3:idVysledku
RIV/60076658:12220/10:00012526
n3:jazykVysledku
n18:cze
n3:klicovaSlova
soil organic matter; organic carbon; labile fraction; decomposition; analytical method
n3:klicoveSlovo
n4:organic%20carbon n4:labile%20fraction n4:decomposition n4:soil%20organic%20matter n4:analytical%20method
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[359E259C5D82]
n3:nazevZdroje
Journal of Agrobiology
n3:obor
n16:DF
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
1
n3:rokUplatneniVysledku
n12:2010
n3:svazekPeriodika
27
n3:tvurceVysledku
Strosser, Eduard
n3:zamer
n14:MSM6007665806
s:issn
1803-4403
s:numberOfPages
12
n13:organizacniJednotka
12220