Soil organic matter mobilization by re-compaction of old forest skid trails

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • Meisam Nazari
  • Malte Horvat
  • Rainer Georg Joergensen
  • Stephan Peth

Externe Organisationen

  • Universität Kassel
Forschungs-netzwerk anzeigen

Details

OriginalspracheEnglisch
Aufsatznummer103173
FachzeitschriftEuropean journal of soil biology
Jahrgang98
PublikationsstatusVeröffentlicht - Juni 2020
Extern publiziertJa

Abstract

Wood harvesting is restricted to a system of permanent skid trails in order to minimize the soil disturbance and damage. Therefore, it is not the compaction of previously undisturbed forest soil, but the re-compaction of already existing skid trails that is of practical relevance when investigating machinery-induced wood harvest effects on soil properties. This study investigated the effects of machinery-induced re-compaction on soil physical, chemical, and microbiological properties of an old skid trail in a spruce forest by wheeling 8 times with a maximum total load of 32.2 Mg, using a genuine old skid trail as a control. Re-compaction significantly increased the bulk density and reduced the porosity, whereas the soil organic carbon (SOC) and total nitrogen (N) contents were not significantly affected. However, re-compaction reduced the SOC/total N ratio by 10%, suggesting considerable SOC mineralization after re-compaction. K 2SO 4 extractable C contents were increased by 94% at 0–3 cm and 67% at 7–10 cm depth after re-compaction. This led to 20% and 90% increased microbial biomass C/soil organic C (MBC/SOC) ratios at 0–3 cm and at 7–10 cm depth, respectively. In contrast, the ergosterol/MBC ratio was significantly decreased by 10% at 0–3 cm and by about 30% at 7–10 cm depth by re-compaction, apparently due to the promotion of bacteria and mobilization of soil organic matter.

ASJC Scopus Sachgebiete

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Soil organic matter mobilization by re-compaction of old forest skid trails. / Nazari, Meisam; Horvat, Malte; Joergensen, Rainer Georg et al.
in: European journal of soil biology, Jahrgang 98, 103173, 06.2020.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Nazari M, Horvat M, Joergensen RG, Peth S. Soil organic matter mobilization by re-compaction of old forest skid trails. European journal of soil biology. 2020 Jun;98:103173. doi: 10.1016/j.ejsobi.2020.103173
Nazari, Meisam ; Horvat, Malte ; Joergensen, Rainer Georg et al. / Soil organic matter mobilization by re-compaction of old forest skid trails. in: European journal of soil biology. 2020 ; Jahrgang 98.
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abstract = "Wood harvesting is restricted to a system of permanent skid trails in order to minimize the soil disturbance and damage. Therefore, it is not the compaction of previously undisturbed forest soil, but the re-compaction of already existing skid trails that is of practical relevance when investigating machinery-induced wood harvest effects on soil properties. This study investigated the effects of machinery-induced re-compaction on soil physical, chemical, and microbiological properties of an old skid trail in a spruce forest by wheeling 8 times with a maximum total load of 32.2 Mg, using a genuine old skid trail as a control. Re-compaction significantly increased the bulk density and reduced the porosity, whereas the soil organic carbon (SOC) and total nitrogen (N) contents were not significantly affected. However, re-compaction reduced the SOC/total N ratio by 10%, suggesting considerable SOC mineralization after re-compaction. K 2SO 4 extractable C contents were increased by 94% at 0–3 cm and 67% at 7–10 cm depth after re-compaction. This led to 20% and 90% increased microbial biomass C/soil organic C (MBC/SOC) ratios at 0–3 cm and at 7–10 cm depth, respectively. In contrast, the ergosterol/MBC ratio was significantly decreased by 10% at 0–3 cm and by about 30% at 7–10 cm depth by re-compaction, apparently due to the promotion of bacteria and mobilization of soil organic matter. ",
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author = "Meisam Nazari and Malte Horvat and Joergensen, {Rainer Georg} and Stephan Peth",
note = "Funding Information: The authors thank the German Federal Ministry of Food and Agriculture (BMEL) for funding the “Bodmech” project with the funding code 22028715 . We are grateful to Gabriele Dormann, Markus Hammer-Weis, Margit Rode and Pouria Sadeghianfar for providing skillful technical assistance. ",
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AU - Nazari, Meisam

AU - Horvat, Malte

AU - Joergensen, Rainer Georg

AU - Peth, Stephan

N1 - Funding Information: The authors thank the German Federal Ministry of Food and Agriculture (BMEL) for funding the “Bodmech” project with the funding code 22028715 . We are grateful to Gabriele Dormann, Markus Hammer-Weis, Margit Rode and Pouria Sadeghianfar for providing skillful technical assistance.

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Y1 - 2020/6

N2 - Wood harvesting is restricted to a system of permanent skid trails in order to minimize the soil disturbance and damage. Therefore, it is not the compaction of previously undisturbed forest soil, but the re-compaction of already existing skid trails that is of practical relevance when investigating machinery-induced wood harvest effects on soil properties. This study investigated the effects of machinery-induced re-compaction on soil physical, chemical, and microbiological properties of an old skid trail in a spruce forest by wheeling 8 times with a maximum total load of 32.2 Mg, using a genuine old skid trail as a control. Re-compaction significantly increased the bulk density and reduced the porosity, whereas the soil organic carbon (SOC) and total nitrogen (N) contents were not significantly affected. However, re-compaction reduced the SOC/total N ratio by 10%, suggesting considerable SOC mineralization after re-compaction. K 2SO 4 extractable C contents were increased by 94% at 0–3 cm and 67% at 7–10 cm depth after re-compaction. This led to 20% and 90% increased microbial biomass C/soil organic C (MBC/SOC) ratios at 0–3 cm and at 7–10 cm depth, respectively. In contrast, the ergosterol/MBC ratio was significantly decreased by 10% at 0–3 cm and by about 30% at 7–10 cm depth by re-compaction, apparently due to the promotion of bacteria and mobilization of soil organic matter.

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