(Table 1) Chemical composition of interstitial waters from the area of gas hydrate generation, Sea of Okhotsk

DOI

Distributions of halogens (Cl, Br and I) in interstitial waters from sediments containing methane hydrate and in water of the hydrate itself are presented. High concentrations of halogens do not occur in interstitial waters from sediments that contain gas hydrates. The main reason for their low concentrations is the poverty of organic matter in sediments.

Supplement to: Pavlova, Galina A; Pashkina, Valeriya I (1989): Distribution of halogens in interstitial waters of the Sea of Okhotsk as related to hydrate generation. Oceanology, 29(3), 329-333

Identifier
DOI https://doi.org/10.1594/PANGAEA.757758
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.757758
Provenance
Creator Pavlova, Galina A; Pashkina, Valeriya I
Publisher PANGAEA
Publication Year 1989
Rights Creative Commons Attribution-NoDerivs 3.0 Unported; https://creativecommons.org/licenses/by-nd/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 220 data points
Discipline Earth System Research
Spatial Coverage (155.178W, 50.513S, 155.301E, 50.572N); Sea of Okhotsk