• Aucun résultat trouvé

Dikes on permafrost: predicting thaw and settlement

N/A
N/A
Protected

Academic year: 2021

Partager "Dikes on permafrost: predicting thaw and settlement"

Copied!
10
0
0

Texte intégral

Loading

Figure

Figure  I (a)  is  a  schematic  representation  of  a  dike  and  forebay.  The  dike  may  be  pervious  or  impervious  to  water  flow
FIG.  2.  Schematic  ground thermal  regime.
FIG. 3.  Unfrozen  moisture  content  (after Williams  1968).
FIG.  4.  Comparison of  calculated and observed  thaw  rates, Kelsey.
+2

Références

Documents relatifs

Tourneret, “Nonlinear- ity detection in hyperspectral images using a polynomial post- nonlinear mixing model.,” IEEE Transactions on Image Pro-. cessing

A p p l y i n g sound-absorbing materials such as acoustical tile, cork or carpet to the surface of a wall, floor, or door does not subsean~iallg decrease sound

by the presence of fibrous cap discontinuity with a communication between the lumen and the inner core of a plaque or with a cavity formation within the plaque. B, Plaque erosion

/ La version de cette publication peut être l’une des suivantes : la version prépublication de l’auteur, la version acceptée du manuscrit ou la version de l’éditeur. Access

We are interested in the following metrics: (1) the overhead of our solution on the performance of dom0 services; (2) the overhead of our solution on the performance of user VMs;

To do so, the service and the network infrastructure are configured through techniques like software-defined networking (SDN) and network function virtualization (NFV) to enable

ثحبلاب فيرعتلا.. - إ :ثحبلا ةيلاكش يف اىريثأتل ةيبرتلا فيدايم فم اماى اناديم اىدعاوقو ايمظنب ةيضايرلاو ةيندبلا ةيبرتلا ربتعت إ .حلاصلا فطاوملا