Detail publikace

Large-scale permafrost degradation as a primary factor in Larix sibirica forest dieback in the Khentii massif, northern Mongolia

JUŘIČKA, D. NOVOTNÁ, J. HOUŠKA, J. PAŘÍLKOVÁ, J. HLADKÝ, J. PECINA, V. CIHLÁŘOVÁ, H. BURNOG, M. ELBL, J. ROSICKÁ, Z. BRTNICKÝ, M. KYNICKÝ, J.

Originální název

Large-scale permafrost degradation as a primary factor in Larix sibirica forest dieback in the Khentii massif, northern Mongolia

Typ

článek v časopise ve Web of Science, Jimp

Jazyk

angličtina

Originální abstrakt

The objective of this study is to investigate the potential causes of widespread Larix sibirica Ledeb. Mortality observed in the Khentii massif of northern Mongolia. The ratio of deadwood to living trees in affected stands in the Goricho region, the southernmost study site situated close to the Gobi Desert, was as high as 3.6:1. Moisture fluctuations monitored over 2 years using electrical impedance spectrometry revealed that the Goricho study site had higher soil moisture levels than the two less affected sites Barun Bayan and Dzun Bayan. High soil moisture was recorded in an area characterized by highly skeletal soils, ones with more than 35% by volume of rock fragments, and comparatively shallow soil horizons, from valley to mountains. The layer of permafrost influencing hydrogeological processes is much deeper in the Goricho region compared to the undisturbed study sites. Redundancy analysis confirmed a significant number of dead L. sibirica on sites with developed soils. Live forest stands, however damaged, grow in this region on well-drained scree slopes or on rocky bastions. The mass mortality observed for L. sibirica may be directly linked to accelerated permafrost thaw in the area bordered by the Tuul and the Terelj Rivers. Our assumption is that L. sibirica root system necrosis occurred as a result of long-term waterlogging of developer soils with high spatial heterogeneity, normally able to absorb high quantities of groundwater. The areas unaffected were scree fields and rocky bastions characterized by adequate drainage. All of our findings support the primary stages of large-scale permafrost thaw, i.e., correlating increases in soil moisture with increasing permafrost active layer thickness.

Klíčová slova

Larix sibirica; Mortality; Permafrost thawing; Waterlogging; Mongolia

Autoři

JUŘIČKA, D.; NOVOTNÁ, J.; HOUŠKA, J.; PAŘÍLKOVÁ, J.; HLADKÝ, J.; PECINA, V.; CIHLÁŘOVÁ, H.; BURNOG, M.; ELBL, J.; ROSICKÁ, Z.; BRTNICKÝ, M.; KYNICKÝ, J.

Vydáno

1. 2. 2020

Nakladatel

Springer Berlin Heidelberg

Místo

Berlin

ISSN

1993-0607

Periodikum

Journal of Forestry Research

Ročník

31

Číslo

1

Stát

Čínská lidová republika

Strany od

197

Strany do

208

Strany počet

12

URL

https://doi.org/10.1007/s11676-018-0866-4

BibTex

@article{BUT153395,
  author="David {Juřička} and Jitka {Novotná} and Jakub {Houška} and Jana {Pařílková} and Jan {Hladký} and Václav {Pecina} and Hana {Cihlářová} and Marcela {Burnog} and Jakub {Elbl} and Zdena {Rosická} and Martin {Brtnický} and Jindřich {Kynický}",
  title="Large-scale permafrost degradation as a primary factor in Larix sibirica forest dieback in the Khentii massif, northern Mongolia",
  journal="Journal of Forestry Research",
  year="2020",
  volume="31",
  number="1",
  pages="197--208",
  doi="10.1007/s11676-018-0866-4",
  issn="1993-0607",
  url="https://doi.org/10.1007/s11676-018-0866-4"
}