Smirnov, M B; Bordovsky, Oleg K (1985): (Table 1) Elementary composition and concentration of low-polarity dissolved organic matter in waters of the Northwest Indian Ocean and Red Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.756674, Supplement to: Smirnov, MB; Bordovsky, OK (1985): Structural group composition of chloroform extracts of dissolved organic matter in waters of the Northwest Indian Ocean. Oceanology, 25(4), 462-465
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Published: 1985 (exact date unknown) • DOI registered: 2011-02-28
Abstract:
Study of elementary composition of chloroform extracts of dissolved organic matter from water of the Northwestern Indian Ocean has demonstrated that most of specimens have composition close to that of lipids, except that they have practically no nitrogen and phosphorus. Some of extracts have low carbon and hydrogen content. An assumption that low-polarity dissolved organic matter in such waters has lipid composition is not appropriate. It is shown that the proton magnetic resonance method is applicable for determining elementary composition of low-polarity dissolved organic matter.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 9.997778 * Median Longitude: 57.960889 * South-bound Latitude: -16.910000 * West-bound Longitude: 38.088000 * North-bound Latitude: 29.090000 * East-bound Longitude: 67.440000
Minimum DEPTH, water: 0 m * Maximum DEPTH, water: 4900 m
Event(s):
AK22-1905/4 * Latitude: 21.380000 * Longitude: 38.088000 * Elevation: -2071.0 m * Location: Red Sea * Campaign: AKU22 * Basis: Akademik Kurchatov * Method/Device: Multiple investigations (MULT)
AK22-1913 * Latitude: -0.090000 * Longitude: 49.790000 * Elevation: -5080.0 m * Location: Indian Ocean * Campaign: AKU22 * Basis: Akademik Kurchatov * Method/Device: Water sample (WS)
AK22-1929 * Latitude: -7.990000 * Longitude: 60.180000 * Elevation: -180.0 m * Location: Indian Ocean * Campaign: AKU22 * Basis: Akademik Kurchatov * Method/Device: Water sample (WS)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | DEPTH, water | Depth water | m | Geocode | ||
| 6 | Organic matter, dissolved | DOM | mg/l | Smirnov, M B | Wet combustion | |
| 7 | Low-polarity dissolved organic matter | LP DOM | mg/l | Smirnov, M B | Proton magnetic resonance | |
| 8 | Low-polarity organic matter carbon of total organic carbon | LPOMC/TOC | % | Smirnov, M B | Calculated | |
| 9 | Carbon | C | % | Smirnov, M B | Combustion element analyzer | |
| 10 | Hydrogen | H | % | Smirnov, M B | Combustion element analyzer | |
| 11 | Oxygen | O | % | Smirnov, M B | Combustion element analyzer | +S+halogens |
| 12 | Phosphorus | P | % | Smirnov, M B | Combustion element analyzer | |
| 13 | Nitrogen, total | TN | % | Smirnov, M B | Combustion element analyzer | |
| 14 | Ash, volcanic | Volc ash | % | Smirnov, M B | Calculated | |
| 15 | Oxygen/Carbon ratio | O/C | Smirnov, M B | Calculated | atomic |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
337 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Depth water [m] | 6 DOM [mg/l] | 7 LP DOM [mg/l] | 8 LPOMC/TOC [%] | 9 C [%] | 10 H [%] | 11 O [%] | 12 P [%] | 13 TN [%] | 14 Volc ash [%] | 15 O/C |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| AK22-1905/4 | 21.380 | 38.088 | -2071 | 50 | 0.790 | 0.550 | 69.50 | 9.00 | 21.50 | <0.05 | <0.1 | <0.1 | 1.55 | |
| AK22-1905/4 | 21.380 | 38.088 | -2071 | 1000 | 1.230 | 0.835 | 68.03 | 8.80 | 23.17 | <0.05 | <0.1 | <0.1 | 1.55 | |
| AK22-1913 | -0.090 | 49.790 | -5080 | 50 | 0.446 | 0.310 | 12.7 | 69.50 | 9.00 | 21.50 | <0.05 | <0.1 | <0.1 | 1.55 |
| AK22-1913 | -0.090 | 49.790 | -5080 | 250 | 0.635 | 0.440 | 30.7 | 69.50 | 9.00 | 21.50 | <0.05 | <0.1 | <0.1 | 1.55 |
| AK22-1913 | -0.090 | 49.790 | -5080 | 1500 | 1.030 | 0.420 | 38.2 | 40.76 | 4.81 | 54.43 | <0.05 | <0.1 | <0.1 | 1.42 |
| AK22-1913 | -0.090 | 49.790 | -5080 | 4900 | 0.284 | 0.200 | 21.8 | 70.00 | 9.50 | 20.50 | <0.05 | <0.1 | <0.1 | 1.63 |
| AK22-1929 | -7.990 | 60.180 | -180 | 0 | 0.600 | 0.380 | 15.0 | 63.00 | 8.00 | 29.00 | <0.05 | <0.1 | <0.1 | 1.53 |
| AK22-1929 | -7.990 | 60.180 | -180 | 25 | 0.520 | 0.365 | 18.2 | 70.25 | 9.18 | 20.27 | <0.05 | <0.1 | <0.1 | 1.57 |
| AK22-1929 | -7.990 | 60.180 | -180 | 120 | 0.484 | 0.160 | 10.7 | 33.15 | 3.65 | 63.20 | <0.05 | <0.1 | <0.1 | 1.32 |
| AK22-1935 | -16.910 | 64.510 | -3930 | 5 | 0.340 | 0.250 | 73.00 | 9.70 | 17.30 | <0.05 | <0.1 | <0.1 | 1.60 | |
| AK22-1935 | -16.910 | 64.510 | -3930 | 500 | 0.240 | 0.185 | 12.3 | 76.00 | 10.50 | 13.50 | <0.05 | <0.1 | <0.1 | 1.70 |
| AK22-1935 | -16.910 | 64.510 | -3930 | 900 | 0.274 | 0.210 | 19.1 | 76.00 | 10.50 | 13.50 | <0.05 | <0.1 | <0.1 | 1.70 |
| AK22-1935 | -16.910 | 64.510 | -3930 | 3610 | 0.150 | 0.120 | 7.4 | 79.42 | 11.35 | 9.23 | <0.05 | <0.1 | <0.1 | 1.72 |
| AK22-1949 | 0.020 | 64.930 | -3633 | 5 | 0.092 | 0.066 | 2.6 | 72.00 | 10.00 | 18.00 | <0.05 | <0.1 | <0.1 | 1.67 |
| AK22-1949 | 0.020 | 64.930 | -3633 | 50 | 0.238 | 0.170 | 13.0 | 73.00 | 9.70 | 17.30 | <0.05 | <0.1 | <0.1 | 1.60 |
| AK22-1949 | 0.020 | 64.930 | -3633 | 1200 | 0.350 | 0.275 | 27.6 | 78.85 | 10.97 | 10.18 | <0.05 | <0.1 | <0.1 | 1.67 |
| AK22-1949 | 0.020 | 64.930 | -3633 | 3600 | 0.338 | 0.270 | 22.5 | 79.26 | 11.42 | 9.32 | <0.05 | <0.1 | <0.1 | 1.73 |
| AK22-1958 | 18.980 | 67.290 | -3920 | 5 | 0.360 | 0.270 | 18.0 | 74.70 | 10.22 | 15.08 | <0.05 | <0.1 | <0.1 | 1.64 |
| AK22-1958 | 18.980 | 67.290 | -3920 | 75 | 0.190 | 0.130 | 7.5 | 67.36 | 9.20 | 23.44 | <0.05 | <0.1 | <0.1 | 1.64 |
| AK22-1958 | 18.980 | 67.290 | -3920 | 250 | 0.116 | 0.090 | 6.9 | 77.47 | 11.17 | 11.36 | <0.05 | <0.1 | <0.1 | 1.73 |
| AK22-1958 | 18.980 | 67.290 | -3920 | 500 | 0.061 | 0.048 | 3.6 | 78.50 | 11.50 | 10.00 | <0.05 | <0.1 | <0.1 | 1.73 |
| AK22-1958 | 18.980 | 67.290 | -3920 | 1100 | 0.098 | 0.078 | 4.6 | 79.97 | 11.96 | 8.07 | <0.05 | <0.1 | <0.1 | 1.78 |
| AK22-1958 | 18.980 | 67.290 | -3920 | 3600 | 0.328 | 0.270 | 16.8 | 81.25 | 11.83 | 6.98 | <0.05 | <0.1 | <0.1 | 1.75 |
| AK22-1960 | 23.000 | 67.440 | -460 | 8 | 0.154 | 0.105 | 8.1 | 70.00 | 9.50 | 20.50 | <0.05 | <0.1 | <0.1 | 1.65 |
| AK22-1960 | 23.000 | 67.440 | -460 | 80 | 0.364 | 0.130 | 7.2 | 35.80 | 4.20 | 60.00 | <0.05 | <0.1 | <0.1 | 1.41 |
| AK22-1960 | 23.000 | 67.440 | -460 | 200 | 0.148 | 0.105 | 8.8 | 68.72 | 9.26 | 21.82 | <0.05 | <0.1 | <0.1 | 1.62 |
| AK22-1960 | 23.000 | 67.440 | -460 | 500 | 0.230 | 0.180 | 14.8 | 76.81 | 11.00 | 12.19 | <0.05 | <0.1 | <0.1 | 1.72 |
| AK22-1965 | 29.090 | 49.170 | -44 | 7 | 0.708 | 0.240 | 10.6 | 34.00 | 4.00 | 62.00 | <0.05 | <0.1 | <0.1 | 1.40 |
| AK22-1965 | 29.090 | 49.170 | -44 | 20 | 0.784 | 0.240 | 8.2 | 30.47 | 3.47 | 66.06 | <0.05 | <0.1 | <0.1 | 1.37 |
| AK22-1965 | 29.090 | 49.170 | -44 | 40 | 0.200 | 0.140 | 2.5 | 71.48 | 9.94 | 18.58 | <0.05 | <0.1 | <0.1 | 1.69 |
| AK22-1971 | 22.500 | 60.250 | -1980 | 7 | 0.250 | 0.170 | 7.7 | 69.00 | 9.50 | 20.50 | <0.05 | <0.1 | <0.1 | 1.65 |
| AK22-1971 | 22.500 | 60.250 | -1980 | 25 | 0.280 | 0.190 | 8.0 | 69.00 | 9.50 | 20.50 | <0.05 | <0.1 | <0.1 | 1.65 |
| AK22-1971 | 22.500 | 60.250 | -1980 | 500 | 0.465 | 0.255 | 12.2 | 54.86 | 7.35 | 37.79 | <0.05 | <0.1 | <0.1 | 1.61 |
| AK22-1971 | 22.500 | 60.250 | -1980 | 1380 | 0.800 | 0.290 | 16.2 | 36.57 | 4.52 | 58.91 | <0.05 | <0.1 | <0.1 | 1.48 |