Ha, Sangbeom; Lee, Jae Il; Bak, Young-Suk; Yoo, Kyu-Cheul; Khim, Boo-Keun (2024): Clay mineral composition of gravity core DG12-GC01 obtained on the Drygalski Basin in the Ross Sea [dataset]. PANGAEA, https://doi.pangaea.de/10.1594/PANGAEA.966443 (DOI registration in progress), In: Ha, S et al. (2024): Sediment properties, geochemical proxies, clay mineral composition and diatom assemblage of gravity cores obtained on the Drygalski Basin in the Ross Sea since Last Glacial Maximum [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.966442
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
The samples for clay mineral compositions were collected from GC01 and GC04 at 10 or 20 cm intervals. The organic matter was removed using 10% H2O2, and the fine fraction (<63 μm) was separated using a sieve. The fraction under 2 μm was extracted using Stokes' law, smeared on the slide, and air-dried following Stokke and Carson (1973). An air-dried slide was treated with ethylene-glycol for 24 h. X-ray diffraction (XRD) was performed using a Siemens/Brucker D5005 at Gyeongsang National University with Cu-Kα radiation (40 kV, 35mA). The clay mineral composition was identified based on the basal reflections recorded in the XRD patterns, following the methods of Brown and Brindley (1980) and Moore and Reynolds (1989). The four major clay minerals (illite, smectite, chlorite, and kaolinite) were estimated by semi-quantitative calculation using the method of Biscaye (1965). The analytical precision for the clay mineral composition was approximately ±5%.
Keyword(s):
Related to:
Ha, Sangbeom; Lee, Jae Il; Bak, Young-Suk; Yoo, Kyu-Cheul; Khim, Boo-Keun (2023): Paleoenvironmental reconstruction of glaciomarine sediments in the Drygalski Basin of the western Ross Sea since the Last Glacial Maximum. Sedimentary Geology, 456, 106495, https://doi.org/10.1016/j.sedgeo.2023.106495
References:
Biscaye, Pierre Eginton (1965): Mineralogy and sedimentation of recent deep sea clay in the Atlantic Ocean and adjacent seas and oceans. Geological Society of America, Bulletin, 76(7), 803-832, https://doi.org/10.1130/0016-7606(1965)76%5B803:MASORD%5D2.0.CO;2
Brown, G; Brindley, G W (1980): X-ray Diffraction Procedures for Clay Mineral Identification. In: Brindley, GW, Brown, G (eds.), Crystal Structures of Clay Minerals and their X-Ray Identification, Mineralogical Society of Great Britain and Ireland, Colchester and London, 305-360, https://doi.org/10.1180/mono-5.5
Moore, Duane M; Reynolds, Robert C Jr (1989): X-Ray Diffraction and the Identification and Analysis of Clay Minerals.
Stokke, Per R; Carson, Bobb (1973): Variation in Clay Mineral X-Ray Diffraction Results with the Quantity of Sample Mounted. Journal of Sedimentary Research, Vol. 43, 957-964, https://doi.org/10.1306/74D728C4-2B21-11D7-8648000102C1865D
Coverage:
Latitude: -74.727400 * Longitude: 166.103600
Date/Time Start: 2012-01-10T00:00:00 * Date/Time End: 2012-01-10T00:00:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 2.40 m
Event(s):
DG12-GC01 (DG12-01) * Latitude: -74.727400 * Longitude: 166.103600 * Date/Time: 2012-01-10T00:00:00 * Elevation: -1028.0 m * Location: Drygalski Basin * Campaign: DG12 (Drygalski Basin 2012) * Method/Device: Gravity corer (GC)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Ha, Sangbeom | Geocode | |
| 2 | Smectite | Sme | % | Ha, Sangbeom | X-ray diffraction (Siemens/Bruker D5005) | |
| 3 | Illite | Ill | % | Ha, Sangbeom | X-ray diffraction (Siemens/Bruker D5005) | |
| 4 | Kaolinite | Kln | % | Ha, Sangbeom | X-ray diffraction (Siemens/Bruker D5005) | |
| 5 | Chlorite | Chl | % | Ha, Sangbeom | X-ray diffraction (Siemens/Bruker D5005) |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
64 data points