Site Information

Site number:
732
Authors:
IBC,GGC,MRB,DIC
Date recorded:
1994/01/03
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 centre of the southern end or the undisturbed part of an experimental area
Altitude:
75 m
Aspect:
SE
Slope:
5 °
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:
30 cm
Frozen type:
Hard frozen and ice cemented with segregated ice
Frozen comment:
30

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
732a 0 – 5 cm
732b 5 – 10 cm
732c 10 – 17 cm
732d 17 – 24 cm
732e 24 – 30 cm
732f 30 – 48 cm top of frozen ground
732g 48 – 78 cm
732h 78 – 84 cm
732i 84 – 112 cm

Sample Data

Physical Data
Sample nameDepth descriptionTop (cm)Base (cm)Bulk DensityDry Bulk DensityGravimetric MoistureVol. Moisture (BD=2)
732a 0-5 0 5 1.75
732b 5-10 5 10 3.94
732c 10-17 10 17 6.59
732d 17-24 17 24 7.55
732e 24-30 24 30 9.38
732f 30-48 30 48 1.58 30.54
732g 48-78 48 78 1.68 24.93
732h 78-84 78 84 2.8 25.99
732i 84-112 84 112 1.9 19.44
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
732a 10.0
732b 57.0
732c 51.0
732d 50.0
732e 38.0
732f 31.0
732g 26.0
732h 31.0
732i 37.0
Clay Mineralogy
Sample nameMicaIHMHIV - IHMICHLVTHIVCHLSMCHL SMFE - CHLHTQTZFLDHBCALNotes
732a :
732b :
732c :
732d :
732e :
732f :
732g :
732h :
732i :

Photos

Photo record:
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