Proc. IODP, 341, Data report: permeability, grain size, biogenic silica, and clay minerals of Expedition 341 sediments from Sites U1417 and U1418

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Chapter contents Abstract Introduction Methods Permeability tests Grain size analyses Silica analyses Clay mineral analyses Results Acknowledgments References Figures F1. Site locations. F2. Permeability test system. F3. X-ray diffraction analysis. F4. Shipboard porosity and permeability results, Site U1417. F5. Shipboard porosity and permeability results, Site U1418. Tables T1. Mineral mixtures for calibration of normalization factors. T2. Results from laboratory permeability tests and grain size analyses. T3. Results from amorphous silica analyses. T4. X-ray diffraction results for bulk mineral standard mixtures. T5. Normalization factors for X-ray diffraction of bulk mineral standard mixtures. T6. Bulk sediment X-ray diffraction results. T7. Clay-size fraction X-ray diffraction results. PDF file			Previous \| Next doi:10.2204/iodp.proc.341.202.2017 References ASTM International, 1990. Standard test method for measurement of hydraulic conductivity of saturated porous materials using a flexible wall permeameter (Standard D5084-70). In Annual Book of ASTM Standards: Philadelphia (American Society for Testing and Materials), 63-70. Biscaye, P.E., 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):803-831. http://dx.doi.org/10.1130/0016-7606(1965)76[803:MASORD]2.0.CO;2 Coakley, J.P., and Syvitski, J.P.M., 1991. SediGraph technique. In Syvitski, J.P.M. (Ed.), Principles, Methods, and Application of Particle Size Analysis: Cambridge, UK (Cambridge University Press), 129-142. http://dx.doi.org/10.1017/CBO9780511626142.013 Daigle, H., and Screaton, E.J., 2015. Evolution of sediment permeability during burial and subduction. Geofluids, 15(1-2):84-105. http://dx.doi.org/10.1111/gfl.12090 DeMaster, D.J., 1981. 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Recent advances in subseafloor hydrogeology: focus on basement-sediment interactions, subduction zones, and continental slopes. Hydrogeology Journal, 18(7):1547-1570. http://dx.doi.org/10.1007/s10040-010-0636-7 Sharqawy, M.H., Lienhard, J.H., V, and Zubair, S.M., 2010. Thermophysical properties of seawater: a review of existing correlations and data. Desalination and Water Treatment, 16(1-3):354-380. http://dx.doi.org/10.5004/dwt.2010.1079 Spinelli, G.A., and Hutton, A., 2013. Data report: amorphous silica content of sediment from Sites C0011 and C0012 in the Shikoku Basin on the NanTroSEIZE transect. In Saito, S., Underwood, M.B., Kubo, Y., and the Expedition 322 Scientists, Proceedings of the Integrated Ocean Drilling Program, 322: Tokyo (Integrated Ocean Drilling Program Management International, Inc.). http://dx.doi.org/10.2204/iodp.proc.322.204.2013 Spinelli, G.A., and Underwood, M.B., 2004. 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