Site Information

Site number:
731
Authors:
IBC,GGC,MRB,DIC
Date recorded:
1994/01/02
Reason Sampled:
Soil moisture, permafrost monitoring and soil climate measurement
Description:
A gently sloping area forming a small bench on a moderately steep slope between Crater Hill and the east coast of Ross Island approximately 150m northwest from the Scott Base buildings; drill hole and access tube site located in the southern end or the undisturbed part of an experimental area
Altitude:
75 m
Aspect:
SE
Slope:
7 °
Location Data
Observer IBC GGC
GPS No
Latitude Longitude DMS 77° 51' S 166° 46' E 77° 51' S 166° 48' E
Latitude Longitude DD -77.850 166.767 -77.850 166.800
Latitude longitude precision DD 0.008 0.008 0.008 0.008
Locality Pram Point, Scott Base
Survey not recorded

Climate

Soil climate zone:
Coastal mountain
Site temperature profile
Depth (cm)Soil temp (°C)Notes
0 17 surface
Estimated mean annual temperature:
-18 °C
Frozen ground depth:
0 cm
Frozen type:
Hard frozen and ice cemented with segregated ice
Frozen comment:
At ground surface

Geology

Geological setting:
The deposit comprises volcanics of the McMurdo Volcanics Formation mainly as scoriaceous flows; the surface materials are a thin cover of mainly fractured bedrock with addition of glacially derived granular and pebble clasts from outside the immediate area; the volcanic bedrock has been considerably fractured by freeze thaw; the surface age is probably very late Pleistocene (Ross Sea Glaciation) having been modified by McMurdo Sound filling glacial ice
Patterned ground:
Weakly developed and without distinctive trough expression or well developed net pattern
Surface weathering or surface features:
Surface clasts show some slight wind polsh but no surface oxidation; pavement between larger clasts is predominantly granular- pebble sized; some thin surface salt accumulations are formed near patches of snow melt

Soil

Soil parent material:
Fragmented bouldery volcanic bedrock with some additions of glaciogenic finer materials, in part with some modification by slope drift processes; surface of the soil to approximately 30cm depth was removed by bulldozer
Previous disturbance:
No evidence of past mechanical disturbance at the immediate trial site area but moderate foot traffic disturbance is very likely; present disturbance includes the presence of numerous particles of introduced organic and inorganic materials
Soil weathering stage:
6 1 (Campbell & Claridge 1975)
Soil moisture status:
Xerous to subxerous; soil is moist below the surface; some moisture derived from small transient snow banks
Biological activity:
A few small patches of yellow lichen and some moss in the general vicinity
Profile Description
HorizonDepthDescription
731a -2 – 0 cm
731b 0 – 8 cm
731c 8 – 16 cm
731d 16 – 25 cm
731e 25 – 37 cm top of frozen ground
731f 37 – 50 cm
731g 50 – 66 cm
731h 66 – 84 cm
731i 84 – 105 cm

Sample Data

Physical Data
Sample nameDepth descriptionTop (cm)Base (cm)Bulk DensityDry Bulk DensityGravimetric MoistureVol. Moisture (BD=2)
731a 2-0 -2 0 0.36
731b 0-8 0 8 2.56
731c 8-16 8 16 3.85
731d 16-25 16 25 4.9
731e 25-37 25 37 1.15 32.51
731f 37-50 37 50 1.72 37.87
731g 50-66 50 66 1.97 25.44
731h 66-84 66 84 2.12 33.5
731i 84-105 84 105 1.69 15.28
Particle size distribution
Sample name< 2 mm2 - 0.5 mm0.5 - 0.25 mm0.25 - 0.1 mm0.1 - 0.05 mm0.05 - 0.02 mm0.02 - 0.002 mm< 0.002 mmFe2O3CaCO3Notes
731a 10.0
731b 57.0
731c 51.0
731d 50.0
731e 38.0
731f 31.0
731g 26.0
731h 31.0
731i 37.0
Clay Mineralogy
Sample nameMicaIHMHIV - IHMICHLVTHIVCHLSMCHL SMFE - CHLHTQTZFLDHBCALNotes
731a :
731b :
731c :
731d :
731e :
731f :
731g :
731h :
731i :

Photos

Photo record:
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