(Table 2) Shear strength, active layer depth and soil characteristics of retrogressive thaw slumps on Herschel Island and King Point ...

Survey squares are shown in Figure 4 of the article. An average of 30 measurements were performed in each square to determine active-layer depth and shear strength. The measurements were performed within three days at the beginning of August 2006. The shear strength values were originally given in N...

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Bibliographic Details
Main Authors: Lantuit, Hugues, Pollard, Wayne H, Couture, Nicole, Fritz, Michael, Schirrmeister, Lutz, Meyer, Hanno, Hubberten, Hans-Wolfgang
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
Event label
Latitude of event
Longitude of event
Site
Sample amount
Shear strength, primary
Active layer depth
Standard deviation
Median, grain size
Soil moisture
Carbon, organic, total
Multiple investigations
Beckman Coulter Laser diffraction particle size analyzer LS 200
Carbon and nitrogen and sulfur CNS isotope element analyzer, Elementar, Vario EL III
CA-Land_2006_YukonCoast
AWI Arctic Land Expedition
Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn
Arctic
Herschel Island
Coulter
King Point
permafrost
Online Access:https://dx.doi.org/10.1594/pangaea.810041
https://doi.pangaea.de/10.1594/PANGAEA.810041
Description
Summary:Survey squares are shown in Figure 4 of the article. An average of 30 measurements were performed in each square to determine active-layer depth and shear strength. The measurements were performed within three days at the beginning of August 2006. The shear strength values were originally given in N/m**2 and were converted to kPa by dividing by 1000. ...

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