(Table 1) Mineral phosphorus contents in bottom sediments and interstitial waters of the Southeast Atlantic
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| Formato: | Dataset Open Access |
| Lenguaje: | en |
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PANGAEA
1972
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| _version_ | 1867170911934742528 |
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| author | Baturin, Gleb N |
| author_facet | Baturin, Gleb N |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Concentrations of mineral phosphorus in interstitial waters from sediments of the Southeast Atlantic generally increases from the ocean bed to the continental slope and shelf. In diatomaceous oozes of the Southwest Africa shelf, phosphorus concentration in fresh interstitial waters reaches 2.5 mg/l in absence of phosphorite concretions and 0.1-0.7 mg/l in their presence. After prolonged storage of samples concentration of dissolved mineral phosphorus sometimes increases up to 7-8 mg/l. The key factor regulating phosphorus content of solid and liquid phases of unaltered sediments are content and composition of organic matter. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_757085 |
| institution | PANGAEA |
| language | en |
| publishDate | 1972 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Mineral phosphorus contents in bottom sediments and interstitial waters of the Southeast Atlantic Baturin, Gleb N AK3-101GC; AK3-108; AK3-130GC; AK3-137GC; AK3-140GC; AK3-143; AK3-152; AK3-153GC; AK3-157GC; AK3-160; AK3-53-2; AK3-59GC; AK3-87GC; AK3-95GC; AK3-98GC; Akademik Kurchatov; AKU3; Archive of Ocean Data; ARCOD; Atlantic Ocean; Calcium carbonate; Calculated from weight loss after drying at 105°C; Carbon, organic, total; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eh, Pt-electrode; Elevation of event; Event label; GC; Grab; GRAB; Gravity corer; Latitude of event; Longitude of event; Oxidation reduction (RedOx) potential; pH; pH meter; Phosphate; Phosphorus; Sediment type; Water content, wet mass; Wet chemistry Concentrations of mineral phosphorus in interstitial waters from sediments of the Southeast Atlantic generally increases from the ocean bed to the continental slope and shelf. In diatomaceous oozes of the Southwest Africa shelf, phosphorus concentration in fresh interstitial waters reaches 2.5 mg/l in absence of phosphorite concretions and 0.1-0.7 mg/l in their presence. After prolonged storage of samples concentration of dissolved mineral phosphorus sometimes increases up to 7-8 mg/l. The key factor regulating phosphorus content of solid and liquid phases of unaltered sediments are content and composition of organic matter. |
| title | (Table 1) Mineral phosphorus contents in bottom sediments and interstitial waters of the Southeast Atlantic |
| topic | AK3-101GC; AK3-108; AK3-130GC; AK3-137GC; AK3-140GC; AK3-143; AK3-152; AK3-153GC; AK3-157GC; AK3-160; AK3-53-2; AK3-59GC; AK3-87GC; AK3-95GC; AK3-98GC; Akademik Kurchatov; AKU3; Archive of Ocean Data; ARCOD; Atlantic Ocean; Calcium carbonate; Calculated from weight loss after drying at 105°C; Carbon, organic, total; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Eh, Pt-electrode; Elevation of event; Event label; GC; Grab; GRAB; Gravity corer; Latitude of event; Longitude of event; Oxidation reduction (RedOx) potential; pH; pH meter; Phosphate; Phosphorus; Sediment type; Water content, wet mass; Wet chemistry |
| url | https://doi.org/10.1594/PANGAEA.757085 |