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

Murray, James W (2004): Pore Water Chemistry of TT183_4_ISS [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.143173

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

RIS CitationBibTeX CitationShow MapGoogle Earth

Related to:
Murray, James W; Kuivila, K M (1990): Organic matter diagenesis in the northeast Pacific: transition from aerobic red clay to suboxic hemipelagic sediments. Deep-Sea Research Part A. Oceanographic Research Papers, 37(1), 59-80, https://doi.org/10.1016/0198-0149(90)90029-U
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3970141: Silicon Cycling in the World Ocean
Coverage:
Latitude: 35.011667 * Longitude: -127.953333
Date/Time Start: 1984-09-03T00:00:00 * Date/Time End: 1984-09-03T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 0.540 m
Event(s):
TT183_4_ISS * Latitude: 35.011667 * Longitude: -127.953333 * Date/Time: 1984-09-03T00:00:00 * Elevation: -4772.0 m * Campaign: TT183 * Basis: Thomas G. Thompson (1964) * Method/Device: In situ sampler (ISS)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
OxygenO2µmol/lMurray, James W
Oxygen, flux, sediment oxygen demandSODmmol/m2/dayMurray, James WCalculated
Nitrate[NO3]-µmol/lMurray, James W
Nitrate[NO3]-µmol/lMurray, James W
SilicateSi(OH)4µmol/lMurray, James W
SilicateSi(OH)4µmol/lMurray, James W
Size:
62 data points

Data

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


Depth sed [m]

O2 [µmol/l]

SOD [mmol/m2/day]

[NO3]- [µmol/l]

[NO3]- [µmol/l]

Si(OH)4 [µmol/l]

Si(OH)4 [µmol/l]
0.000155.00.27
0.000154.037.037.0164.0164.0
0.020118.044.042.0195.0185.0
0.05046.0200.0
0.11092.044.045.0205.0200.0
0.14082.045.0205.0
0.17044.045.0200.0200.0
0.200103.050.0217.0
0.23047.0226.0
0.26047.0217.0226.0
0.29082.049.047.0215.0226.0
0.34051.047.049.0226.0226.0
0.39062.047.050.0231.0
0.44062.046.050.0226.0215.0
0.49048.049.0217.0231.0
0.54062.047.050.0215.0231.0