Stabilization of soil organic matter by earthworms is connected with physical protection rather than with chemical changes of organic matter

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F17%3A43895741" target="_blank" >RIV/60076658:12310/17:43895741 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/60077344:_____/17:00474994 RIV/00216208:11310/17:10359864

Výsledek na webu

<a href="https://ac.els-cdn.com/S0016706116308163/1-s2.0-S0016706116308163-main.pdf?_tid=c3fd1326-f918-11e7-a3f5-00000aab0f6c&acdnat=1515927222_2eb57f3c216cf8928c58756821fc03e7" target="_blank" >https://ac.els-cdn.com/S0016706116308163/1-s2.0-S0016706116308163-main.pdf?_tid=c3fd1326-f918-11e7-a3f5-00000aab0f6c&acdnat=1515927222_2eb57f3c216cf8928c58756821fc03e7</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.geoderma.2016.11.017" target="_blank" >10.1016/j.geoderma.2016.11.017</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Stabilization of soil organic matter by earthworms is connected with physical protection rather than with chemical changes of organic matter

Popis výsledku v původním jazyce

Earthworms are important drivers for the formation of soil structure and play a key role in soil organic matter (SOM) dynamics. Our previous long-term (126 weeks) laboratory experiment showed that carbon (C) loss declined through time in soil when litter was mixed and consumed by earthworms (Lumbricus rubellus). Eventually, the C loss was lower than in treatments where litter was mechanically mixed into soil with exclusion of earthworms. However, it is not clear if the solely physical manipulation of soil or biological activity of earthworms lead to different SOM quality, which would result in a distinction in C loss and consequently C sequestration. Thus, we differentiated between physical (mechanical mixing) and earthworm effects on SOM composition. Two types of soil were used in the experiment: clay and sand, and these were incubated with alder (Alnus glutinosa) and willow (Salix caprea) litter, respectively. The combination of soils and litter types corresponds to the natural combinations at the sampling sites. To explain underlying mechanisms of a lower C loss in the earthworm vs. mechanically mixed treatment, we separated SOM fractions in order to gain pools defined in the Rothamsted model. Chemical differences between initial litter and the active and slow pool of SOM obtained by fractionation were studied. No significant differences between the earthworm and mechanically mixed treatment were found in C, nitrogen (N), and phenol contents, composition of major chemical groups of litter studied by solid-state C-13 NMR spectroscopy, and composition of aromatic components of SOM studied by analytical pyrolysis (Py GC/MS). This lack of differences in chemical composition suggests that greater SOM sequestration in the earthworm treatment is likely to be connected with physical protection of SOM inside cast aggregates rather than with chemical changes in SOM mediated by earthworms.

Název v anglickém jazyce

Stabilization of soil organic matter by earthworms is connected with physical protection rather than with chemical changes of organic matter

Popis výsledku anglicky

Earthworms are important drivers for the formation of soil structure and play a key role in soil organic matter (SOM) dynamics. Our previous long-term (126 weeks) laboratory experiment showed that carbon (C) loss declined through time in soil when litter was mixed and consumed by earthworms (Lumbricus rubellus). Eventually, the C loss was lower than in treatments where litter was mechanically mixed into soil with exclusion of earthworms. However, it is not clear if the solely physical manipulation of soil or biological activity of earthworms lead to different SOM quality, which would result in a distinction in C loss and consequently C sequestration. Thus, we differentiated between physical (mechanical mixing) and earthworm effects on SOM composition. Two types of soil were used in the experiment: clay and sand, and these were incubated with alder (Alnus glutinosa) and willow (Salix caprea) litter, respectively. The combination of soils and litter types corresponds to the natural combinations at the sampling sites. To explain underlying mechanisms of a lower C loss in the earthworm vs. mechanically mixed treatment, we separated SOM fractions in order to gain pools defined in the Rothamsted model. Chemical differences between initial litter and the active and slow pool of SOM obtained by fractionation were studied. No significant differences between the earthworm and mechanically mixed treatment were found in C, nitrogen (N), and phenol contents, composition of major chemical groups of litter studied by solid-state C-13 NMR spectroscopy, and composition of aromatic components of SOM studied by analytical pyrolysis (Py GC/MS). This lack of differences in chemical composition suggests that greater SOM sequestration in the earthworm treatment is likely to be connected with physical protection of SOM inside cast aggregates rather than with chemical changes in SOM mediated by earthworms.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

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OECD FORD obor

40104 - Soil science

Projekt

<a href="/cs/project/GAP504%2F12%2F1288" target="_blank" >GAP504/12/1288: Úloha funkčních vlastností listů rostlin při akumaulaci půdní organické hmoty během primární sukcese</a><br>

Návaznosti

S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2017

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Geoderma

ISSN

0016-7061

e-ISSN

—

Svazek periodika

289

Číslo periodika v rámci svazku

MAR 1 2017

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

7

Strana od-do

29-35

Kód UT WoS článku

000392771300004

EID výsledku v databázi Scopus

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