Alekseeva, Tatyana N; Sval'nov, Vyacheslav N (2000): (Table 3) Grain size composition of sediments from the drilling core TK-9240 measured by methods of Petelin and Atterberg [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.761780, In supplement to: Alekseeva, TN; Sval'nov, VN (2000): On the techniques for grain-size analysis of fine-grained sediments. Translated from Okeanologiya, 2000, 40(2), 304-312, Oceanology, 40(2), 281-288
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Latitude: 77.090000 * Longitude: 104.440000
Minimum DEPTH, sediment/rock: 6 m * Maximum DEPTH, sediment/rock: 48 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Size fraction > 0.063 mm, sand | >63 µm | % | Alekseeva, Tatyana N | Grain size analysis after Petelin (1967, Nauka, Moscow) | by Petelin method |
3 | Size fraction 0.063-0.002 mm, silt, mud | 63-2 µm | % | Alekseeva, Tatyana N | Grain size analysis after Petelin (1967, Nauka, Moscow) | by Petelin method |
4 | Size fraction < 0.002 mm, clay | <2 µm | % | Alekseeva, Tatyana N | Grain size analysis after Petelin (1967, Nauka, Moscow) | by Petelin method |
5 | Size fraction > 0.063 mm, sand | >63 µm | % | Alekseeva, Tatyana N | Grain size analysis after Atterberg | by Atterberg method |
6 | Size fraction 0.063-0.002 mm, silt, mud | 63-2 µm | % | Alekseeva, Tatyana N | Grain size analysis after Atterberg | by Atterberg method |
7 | Size fraction < 0.002 mm, clay | <2 µm | % | Alekseeva, Tatyana N | Grain size analysis after Atterberg | by Atterberg method |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
120 data points
Data
1 Depth sed [m] | 2 >63 µm [%] (by Petelin method, Grain size...) | 3 63-2 µm [%] (by Petelin method, Grain size...) | 4 <2 µm [%] (by Petelin method, Grain size...) | 5 >63 µm [%] (by Atterberg method, Grain si...) | 6 63-2 µm [%] (by Atterberg method, Grain si...) | 7 <2 µm [%] (by Atterberg method, Grain si...) |
---|---|---|---|---|---|---|
6 | 1.06 | 39.80 | 59.14 | 0.87 | 43.36 | 55.77 |
8 | 2.10 | 37.76 | 60.14 | 2.87 | 40.67 | 56.46 |
10 | 0.80 | 26.55 | 72.65 | 0.38 | 27.95 | 71.67 |
12 | 0.34 | 26.52 | 73.14 | 0.21 | 26.96 | 72.83 |
14 | 0.27 | 26.37 | 73.36 | 0.10 | 31.19 | 68.71 |
16 | 0.16 | 26.93 | 72.91 | 0.11 | 29.83 | 70.06 |
18 | 0.47 | 27.57 | 71.96 | 0.65 | 34.25 | 65.10 |
20 | 0.38 | 27.26 | 72.36 | 0.28 | 32.66 | 67.06 |
22 | 0.22 | 29.50 | 70.28 | 0.17 | 34.89 | 64.94 |
24 | 0.41 | 27.24 | 72.35 | 0.31 | 32.77 | 66.92 |
26 | 1.66 | 26.38 | 71.96 | 1.20 | 28.46 | 70.34 |
30 | 46.12 | 28.48 | 25.40 | 49.73 | 29.63 | 20.64 |
32 | 56.49 | 24.18 | 19.33 | 54.42 | 30.99 | 14.59 |
34 | 38.88 | 30.87 | 30.25 | 42.31 | 31.82 | 25.87 |
38 | 10.32 | 42.21 | 47.47 | 8.30 | 47.02 | 44.68 |
40 | 0.24 | 36.51 | 63.25 | 0.28 | 41.04 | 58.68 |
42 | 26.64 | 37.67 | 35.69 | 23.63 | 40.37 | 36.00 |
44 | 33.36 | 34.69 | 31.95 | 33.22 | 35.95 | 30.83 |
46 | 32.78 | 35.19 | 32.03 | 31.82 | 36.88 | 31.30 |
48 | 41.99 | 28.87 | 29.14 | 43.67 | 30.03 | 26.30 |