Site Information

Site number:
733
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 and eastern side of 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:
24 cm
Frozen type:
Hard frozen and ice cemented with segregated ice
Frozen comment:
24

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
733a 0 – 8 cm
733b 8 – 16 cm
733c 16 – 24 cm
733d 24 – 39 cm
733e 39 – 52 cm top of frozen ground
733f 52 – 69 cm
733g 69 – 82 cm
733h 82 – 97 cm
733i 97 – 110 cm

Sample Data

Physical Data
Sample nameDepth descriptionTop (cm)Base (cm)Bulk DensityDry Bulk DensityGravimetric MoistureVol. Moisture (BD=2)
733a 0-8 0 8 1.72
733b 8-16 8 16 3.87
733c 16-24 16 24 5.02
733d 24-39 24 39 2.01 8.4
733e 39-52 39 52 1.93 21.03
733f 52-69 52 69 1.56 25.44
733g 69-82 69 82 2.37 23.71
733h 82-97 82 97 1.72 19.88
733i 97-110 97 110 2.12 14.69
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
733a 33.0
733b 58.0
733c 54.0
733d 31.0
733e 62.0
733f 60.0
733g 61.0
733h 59.0
733i 37.0
Clay Mineralogy
Sample nameMicaIHMHIV - IHMICHLVTHIVCHLSMCHL SMFE - CHLHTQTZFLDHBCALNotes
733a :
733b :
733c :
733d :
733e :
733f :
733g :
733h :
733i :

Photos

Photo record:
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