Journal cover Journal topic
Biogeosciences An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

IF value: 3.480
IF3.480
IF 5-year value: 4.194
IF 5-year
4.194
CiteScore value: 6.7
CiteScore
6.7
SNIP value: 1.143
SNIP1.143
IPP value: 3.65
IPP3.65
SJR value: 1.761
SJR1.761
Scimago H <br class='widget-line-break'>index value: 118
Scimago H
index
118
h5-index value: 60
h5-index60
BG | Articles | Volume 17, issue 13
Biogeosciences, 17, 3367–3383, 2020
https://doi.org/10.5194/bg-17-3367-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Biogeosciences, 17, 3367–3383, 2020
https://doi.org/10.5194/bg-17-3367-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 03 Jul 2020

Research article | 03 Jul 2020

From fibrous plant residues to mineral-associated organic carbon – the fate of organic matter in Arctic permafrost soils

Isabel Prater et al.

Viewed

Total article views: 1,111 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
875 215 21 1,111 38 6 10
  • HTML: 875
  • PDF: 215
  • XML: 21
  • Total: 1,111
  • Supplement: 38
  • BibTeX: 6
  • EndNote: 10
Views and downloads (calculated since 03 Mar 2020)
Cumulative views and downloads (calculated since 03 Mar 2020)

Viewed (geographical distribution)

Total article views: 844 (including HTML, PDF, and XML) Thereof 839 with geography defined and 5 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

No saved metrics found.

Saved (preprint)

No saved metrics found.

Discussed (final revised paper)

No discussed metrics found.

Discussed (preprint)

No discussed metrics found.
Latest update: 23 Sep 2020
Publications Copernicus
Download
Short summary
Large amounts of soil organic matter stored in permafrost-affected soils from Arctic Russia are present as undecomposed plant residues. This large fibrous organic matter might be highly vulnerable to microbial decay, while small mineral-associated organic matter can most probably attenuate carbon mineralization in a warmer future. Labile soil fractions also store large amounts of nitrogen, which might be lost during permafrost collapse while fostering the decomposition of soil organic matter.
Large amounts of soil organic matter stored in permafrost-affected soils from Arctic Russia are...
Citation
Altmetrics
Final-revised paper
Preprint