Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Daigle, Hugh (2015): (Table 1) Porosity measurements, median pore diameter of pore sizes and volume fractions of bulk sediment from different Holes of IODP site 333 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.855293, Supplement to: Daigle, H (2014): Microporosity development in shallow marine sediments from the Nankai Trough. Marine Geology, 357, 293-303, https://doi.org/10.1016/j.margeo.2014.09.041

Always quote citation above when using data! You can download the citation in several formats below.

Published: 2015-11-26DOI registered: 2015-12-28

RIS CitationBibTeX Citation ShareShow MapGoogle Earth

Abstract:
Microporosity by performing low pressure nitrogen adsorption measurements on 13 shallow marine mudstone samples from the Nankai Trough offshore Japan. The samples were from two reference Sites on the incoming Philippine Sea Plate, and one Site above the accretionary prism. I determined pore size distributions using the Barrett–Joyner–Hallenda (BJH) model, and merged these with existing mercury injection capillary pressure (MICP) measurements to construct a full distribution covering micro- to macropores. I found that overall pore sizes decrease with consolidation, and that microporosity content (pores < 2 nm in diameter) is influenced mainly by mineralogy, with some influence of diagenetic processes. A small amount of microporosity (~ 0.25% of bulk sediment volume) is present in these sediments at the time of burial, presumably contained mainly in clays. Additional microporosity may develop as a result of alteration of volcanic ash at the reference Sites, and may be related to diagenetic processes that create zones of anomalous high porosity. Comparisons with porewater chemistry (K+, Ca2 +, Sr, Si) show inconsistent relationships with microporosity development and cannot confirm or deny the role of ash alteration in this process. The strongest correlation observed at the three Sites was between microporosity volume and clay mineral fraction. This suggests that microporosity content is determined mainly by detrital clay abundance and development of clay as an ash alteration product, with some contribution from amorphous silica cement precipitated in the zones of anomalous high porosity.
Coverage:
Median Latitude: 32.870658 * Median Longitude: 136.849572 * South-bound Latitude: 32.748245 * West-bound Longitude: 136.681480 * North-bound Latitude: 33.156992 * East-bound Longitude: 136.917363
Minimum DEPTH, sediment/rock: 21.87 m * Maximum DEPTH, sediment/rock: 301.77 m
Event(s):
333-C0011D * Latitude: 32.829060 * Longitude: 136.882083 * Elevation: -4050.5 m * Recovery: 351.49 m * Campaign: Exp333 (NanTroSEIZE Stage 2: Subduction Inputs 2 and Heat Flow) * Basis: Chikyu * Method/Device: Drilling/drill rig (DRILL)
333-C0012C * Latitude: 32.748245 * Longitude: 136.917362 * Elevation: -3510.5 m * Recovery: 128.62 m * Campaign: Exp333 (NanTroSEIZE Stage 2: Subduction Inputs 2 and Heat Flow) * Basis: Chikyu * Method/Device: Drilling/drill rig (DRILL)
333-C0012D * Latitude: 32.748335 * Longitude: 136.917363 * Elevation: -3510.5 m * Recovery: 66.38 m * Campaign: Exp333 (NanTroSEIZE Stage 2: Subduction Inputs 2 and Heat Flow) * Basis: Chikyu * Method/Device: Drilling/drill rig (DRILL)
Comment:
Sediment depth is given in mbsf. Pore size at splice = point at which MICP and N2 pore size distributions were merged.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventDaigle, Hugh
2Sample code/labelSample labelDaigle, HughDSDP/ODP/IODP sample designation
3DEPTH, sediment/rockDepth sedmDaigle, HughGeocode
4Porosity, fractionalPoros fracDaigle, HughMercury Injection Capillary Pressure analysis (MICP)
5Porosity, fractionalPoros fracDaigle, HughMercury injection and Nitrogen adsorption (MICP+N2)
6Porosity, fractionalPoros fracDaigle, HughCalculated, see reference(s)of moisture and density (MAD) measurements
7SizeSizeµmDaigle, HughCalculated, see reference(s)pore size at splice
8VolumeVol%Daigle, HughCalculated, see reference(s)of micropores
9VolumeVol%Daigle, HughCalculated, see reference(s)of mesopores
10VolumeVol%Daigle, HughCalculated, see reference(s)of macropores
11PorosityPoros% volDaigle, HughCalculated, see reference(s)of bulk volume microporosity
12DiameterصmDaigle, HughCalculated, see reference(s)median pore diameter from merged MICP + N2 pore size distribution
Size:
130 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML