O'Regan, Matthew; Moran, K; Baxter, C D P; Cartwright, J; Vogt, Christoph; Kölling, Martin (2012): (Table 1) Consolidation tests from different Holes of IODP Expedition 302 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.788555, In: O'Regan, M et al. (2012): Consolidation tests, elastic properties and grain size measurements at the consolidations samples from different Holes of IODP Expedition 302 [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.788585
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
O'Regan, Matthew; Moran, K; Baxter, C D P; Cartwright, J; Vogt, Christoph; Kölling, Martin (2010): Towards ground truthing exploration in the central Arctic Ocean: a Cenozoic compaction history from the Lomonosov Ridge. Basin Research, 22, 215-235, https://doi.org/10.1111/j.1365-2117.2009.00403.x
Project(s):
Coverage:
Median Latitude: 87.927255 * Median Longitude: 139.450005 * South-bound Latitude: 87.921180 * West-bound Longitude: 139.365010 * North-bound Latitude: 87.933330 * East-bound Longitude: 139.535000
Date/Time Start: 2004-08-19T00:00:00 * Date/Time End: 2004-08-26T00:00:00
Minimum Elevation: -1209.0 m * Maximum Elevation: -1206.2 m
Event(s):
302-M0002A (ACEX-M2A) * Latitude: 87.921180 * Longitude: 139.365010 * Date/Time: 2004-08-19T00:00:00 * Elevation: -1209.0 m * IGSN: IBCR0302RHTS001 * Penetration: 270.1 m * Recovery: 214.68 m * Location: Arctic Ocean * Campaign: Exp302 (Arctic Coring Expedition, ACEX) * Basis: CCGS Captain Molly Kool (Vidar Viking)
302-M0003A (ACEX-M3A) * Latitude: 87.933330 * Longitude: 139.535000 * Date/Time: 2004-08-26T00:00:00 * Elevation: -1206.2 m * IGSN: IBCR0302RHUS001 * Penetration: 15 m * Recovery: 14.85 m * Location: Arctic Ocean * Campaign: Exp302 (Arctic Coring Expedition, ACEX) * Basis: CCGS Captain Molly Kool (Vidar Viking)
Comment:
Two estimates of the pre-consolidation pressure are derived for each test (1) is calculated from the e- log(sigmaE) and (2) from e- log(sigmaE).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | O'Regan, Matthew | DSDP/ODP/IODP sample designation | ||
| 3 | Sample, optional label/labor no | Lab no | O'Regan, Matthew | |||
| 4 | Lithologic unit/sequence | Unit | O'Regan, Matthew | |||
| 5 | Void Ratio description | Void Ratio | O'Regan, Matthew | |||
| 6 | Depth, composite revised | Depth comp r | rmcd | O'Regan, Matthew | ||
| 7 | Axial effective stress | SigmaA ef | kPa | O'Regan, Matthew | signma E | |
| 8 | Preconsolidation pressure | Pc | kPa | O'Regan, Matthew | P'c (1); empty fields = average | |
| 9 | Preconsolidation pressure | Pc | kPa | O'Regan, Matthew | P'c (2) | |
| 10 | Overconsolidation ratio | Pc/Po | O'Regan, Matthew | |||
| 11 | Strain | Epsilon | % | O'Regan, Matthew | Strain to P' c | |
| 12 | Void Ratio description | Void Ratio | O'Regan, Matthew | initial void ratio | ||
| 13 | Compression index | Cc | O'Regan, Matthew | |||
| 14 | Recompression/expansion index | Ce | O'Regan, Matthew |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
123 data points
Data
| 1 Event | 2 Sample label | 3 Lab no | 4 Unit | 5 Void Ratio | 6 Depth comp r [rmcd] | 7 SigmaA ef [kPa] (signma E) | 8 Pc [kPa] (P'c (1); empty fields = average) | 9 Pc [kPa] (P'c (2)) | 10 Pc/Po | 11 Epsilon [%] (Strain to P' c) | 12 Void Ratio (initial void ratio) | 13 Cc | 14 Ce |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 302-M0003A | 302-M0003A-3H-3 | 3A-3H3, A | 1.2 | 1.274 | 18.62 | 130.0 | 115 | 95 | 6.5 | 1.99 | 0.433 | 0.107 | |
| 302-M0003A | 302-M0003A-3H-3 | 3A-3H3, B | 1.2 | 1.196 | 18.67 | 130.0 | 150 | 105 | 5.5 | 1.883 | 0.405 | 0.107 | |
| 302-M0003A | 302-M0003A-3H-3 | 116 | 0.89 | ||||||||||
| 302-M0002A | 302-M0002A-10X-1 | 2A-10X1, A | 1.3 | 1.054 | 42.97 | 300.0 | 280 | 200 | 8.0 | 1.764 | 0.375 | 0.095 | |
| 302-M0002A | 302-M0002A-10X-1 | 2A-10X1, B | 1.3 | 1.023 | 43.02 | 300.0 | 160 | 180 | 6.0 | 1.639 | 0.341 | 0.086 | |
| 302-M0002A | 302-M0002A-10X-1 | 205 | 0.68 | ||||||||||
| 302-M0002A | 302-M0002A-20X-1 | 2A-20X1, A | 1.3 | 1.069 | 87.61 | 617.0 | 360 | 320 | 8.0 | 1.785 | 0.355 | 0.086 | |
| 302-M0002A | 302-M0002A-20X-1 | 2A-20X1, B | 1.3 | 1.076 | 87.66 | 617.0 | 305 | 305 | 9.0 | 1.764 | 0.353 | 0.104 | |
| 302-M0002A | 302-M0002A-20X-1 | 323 | 0.52 | ||||||||||
| 302-M0002A | 302-M0002A-38X-5 | 2A-38X5, A | 1.4 | 1.108 | 171.11 | 1288.0 | 800 | 1050 | 10.5 | 2.452 | 0.509 | 0.123 | |
| 302-M0002A | 302-M0002A-38X-5 | 2A-38X5, B | 1.4 | 1.168 | 171.16 | 1288.0 | 700 | 750 | 8.5 | 2.376 | 0.491 | 0.133 | |
| 302-M0002A | 302-M0002A-38X-5 | 825 | 0.64 | ||||||||||
| 302-M0002A | 302-M0002A-53X-2 | 2A-53X2, A | 2 | 3.487 | 229.74 | 1687.0 | 1050 | 1025 | 10.5 | 7.433 | 1.415 | 0.100 | |
| 302-M0002A | 302-M0002A-53X-2 | 825 | 0.61 |