Soil survey near Tiksi, Sibera

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Observation site
Soil survey was carried out in tundra near Tiksi from 1997 to 2000. Figs 1 and Fig. 2 shows location of Tiksi and observation sites in surveyed area, respectively. Series of soil moisture content and temperature at 5-cm detpth were measured on the transect lines (4 red lines in Fig. 2) with 25-m intervals.
About 40 sites were selected along the transect lines and dug with size of 50 cm x 50 cm on the frozen ground (observation pits). There were tweny four pits (#0 - #23 in Fig. 2) with 250-m intervals and six pits (#23 - #29 in Fig. 2) with 50-m intervals on the transect lines. The active layer soil in the surveyed area were classified into five types based on soil water regime and vegetation (Watanabe et al., 2000). Some pits (#33 - #34 in Fig. 2) were also selected at a place where typical soil types was found (where ground surface was covered with typical vegetation).

Photograh at the pit
At each pit, surface condition, thickness and horizons of the activelayer were directly observed. Photographs of the observation pits are listed in PhotoList. The photograph for #22 is missing. Most observations were performed in rain or cloudy day. The ground water level in the wetland was close to ground surface level. Therefore, some pits (#3-4, #6-8, #16-18 and #25.5) were difficlult to be taken photograp. There were fully water-logged (+ 5 cm or more) or inundating.
In PhotoList, photoguraps about following information were also listed.

  • Core: Wells with diametter of about 6 cm were bored around the transient lines.
  • Surface conditions: The vegetation cover of tundra soil was classified into four types: sedge dominance, moss dominance, mixed, and bare (frost boil or gravels). Each type was also divided by the moisture conditions.
  • Microscopic image: The horizon widespread in this area (Peat (He) and Silt (B)) were microscopically obserbed.

    Horizons and some physical conditions at the pit
    The elevation, horizons and temperature profile were shown in Fig. 3 Detail informations of soil horizons and temperatures are also availavle from Watanabe et al., 2000. Using the wall of the pit, profiles of temperature, water content, bulk density, hydraulic conductivity, and thermal conductivity were measured (Watanabe et al., 2000).


    Watanabe et al., 2000: Properties and horizons of active layer soils in tundra at Tiksi, Siberia, J. Japan Soc. Hydrol. & Water Resour. Vol. 13, No. 1, pp. 9-16.
    25 December, 2001
    Anual changes in soil temperatures at different depth of the pits (#21-29, shown in Fig. 2)
  • 1997.8-1998.7, MS-Excel data (3.1 MB)
  • 1998.7-1999.8, MS-Excel data (2.8 MB)
    15 October, 2002