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

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 conc...

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Bibliographic Details
Main Authors: Pavlova, Galina A, Pashkina, Valeriya I
Format: Dataset
Language:English
Published: PANGAEA 1989
Subjects:
Alkalinity
total
Ammonium
Archive of Ocean Data
ARCOD
Bromide/Chlorine ratio
Bromine
Calculated
Chloride
Comment
Depth
bottom/max
sediment/rock
top/min
Eh
Pt-electrode
Elevation of event
Event label
Iodine
Iodine/Bromine ratio
Latitude of event
Longitude of event
MULT
Multiple investigations
Oxidation reduction (RedOx) potential
Phosphorus in orthophosphate
Pisc-1403
Pisc-1418-1
Pisc-1423
Sea of Okhotsk
Titration
Okhotsk
Methane hydrate
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.757758
https://doi.org/10.1594/PANGAEA.757758
Description
Summary: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.

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