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63 resultados para The electrical double layer

(Table 31) Heavy metal speciations in suspended matter sampled by a separator from the surface water layer in the East Pacific Ocean

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(Table 1) Chemical composition of samples from the red bed layer in DSDP Hole 38-336

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(Table 3-2) Concentrations particulate organic carbon, carbonate carbon, total carbon and d13C-Corg values in suspended mater from the most surface layer of bottom sediments collected by Niemistoe corers in the White Sea in July 2010

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(Appendix B) Biometric measurements for ten characteristics and developmental degree of the spongy surface layer in the Cycladophora sakaii-davisiana lineage of DSDP Hole 19-192

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Light mineral contents in 50-100 µm grain size fraction of the surface sediment layer from the Eastern Arctic seas

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(Appendix C) Biometric measurements for ten characteristics and developmental degree of the spongy surface layer in the Cycladophora cornutoides lineage of DSDP Hole 19-192

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Community respiration and production of oxygen at the sea surface layer (0.1 mm to 5 m) during METEOR cruise M117, Baltic Sea

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Major oxide geochemical compositions of glass shards from disseminated tephra layers in Unit U below the visible ash layer from the Scotia Sea; Tab 4.4

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Stable isotope ratios in abundant components of the benthic boundary layer community during cruise DI222/2

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Stable isotope ratios in abundant components of the benthic boundary layer community during cruise DI229

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(Table 4) Total phytoplankton biomass, biomass of certain algal groups in the upper mixed layer and the water column, and contribution of the algal groups to total biomass of phytoplankton in the southwest Kara Sea on August 9-12, 2007

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(Table 3) Benthic foraminifers in the surface sediment layer of the southern Laptev Sea

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(Table 2) Contents of some chemical components in the surface sediment layer of the Philippine Sea

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(Table 2) Chemical composition of fine grain size fractions of samples from the red bed layer in DSDP Hole 38-336

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(Table 3) Phosphate and silicon concentrations in interstitial water and their fluxes from the surface sedimentary layer into the near-bottom water layer in the Baltic Sea

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