Arctic vegetation cover seen as a porous media : Numerical assessment of hydraulic and thermal properties of Sphagnum moss, lichen and peat from Western Siberia.
Authors: Cazaurang Simon , Marcoux Manuel , Pokrovsky Oleg S. , Loiko Sergey V. , Lim Artem G. , Audry Stéphane , Shirokova Liudmila S. , Orgogozo Laurent 
Published: March 2022

&lt;p&gt;&lt;span&gt;&lt;em&gt;Sphagnum &lt;/em&gt;&lt;/span&gt;&lt;span&gt;moss, lichen and peat are widely present in arctic regions, covering millions of km&amp;#178; in permafrost-dominated regions. This multi-component low vegetation strata plays a key role in surfaces fluxes in these areas, as they are the most widespread interface between the atmosphere and the geosphere. Therefore, characterizing their transfer properties such as hydraulic and thermal conductivities is crucial for climate change impacts forecasting in arctic regions. In this work, 12 samples were collected in a discontinuous permafrost arctic area (Khanymey Research Station, Russian Federation) and dried to ensure their conservation. Collected samples have been digitally reconstructed by X-ray scanning. After having assessed morphological and hydraulic properties using numerical analysis of the obtained 3D digital tomographies (Cazaurang et al, submitted), we aim here at developing and using both experimental and numerical &lt;/span&gt;&lt;span&gt;methodologies to characterize thermal properties of these samples of &lt;/span&gt;&lt;span&gt;&lt;em&gt;Sphagnum&lt;/em&gt;&lt;/span&gt;&lt;span&gt;, lichen and peat. &lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span&gt;This new study consist in comparisons of numerically and experimentally estimated thermal properties for contributing to the existing knowledge on &lt;/span&gt;&lt;span&gt;&lt;em&gt;Sphagnum&lt;/em&gt;&lt;/span&gt;&lt;span&gt;, lichen and peat transfer properties. Experiments consist of a steady-state thermal conductivity estimation using a hot plate source on real arctic vegetation cover samples. For this purpose, samples are placed in a confined thermal atmosphere and a constant heat flux is applied at sample base. Thermal conductivity is then retrieved with the resolution of Fourier&amp;#8217;s heat conduction law. Similarly, numerical computations are conducted on the same digital reconstructions than those used for hydraulic properties determination. Simulations consist of a numerical reproduction of previously described experiments, allowing to strengthen the analysis of the experimental data. Additionally, the definition of representative elementary volumes of the studied samples is also undertaken using the numerical results.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span&gt;Compiling these &lt;/span&gt;&lt;span&gt;assessments&lt;/span&gt;&lt;span&gt; of transfer properties will represent &lt;/span&gt;&lt;span&gt;essential&lt;/span&gt;&lt;span&gt; information to simulate the dynamics of the permafrost underneath the arctic bryophytic layers &lt;/span&gt;&lt;span&gt;with a&lt;/span&gt;&lt;span&gt; devoted catchment-scale permafrost models. For instance in the framework of the HiPerBorea project (hiperborea.omp.eu), this approach will be used to forecast the impacts of climate warming on boreal permafrost-dominated catchments. &lt;/span&gt;&lt;/p&gt;