Experimental Verifications of Abnormal Chlorinity appearing in Natural Deep-Sea Gas Hydrate
The chloride anion is known to be the most abundant salt ion in sea water. At the regions such as ODP Sites 1249 and 1250 the highly enriched chloride concentration is observed in a zone extended from near the sediment surface (~1 mbsf) to depths about 25 mbsf. Here, we designed the in-situ elect...
| Main Authors: | , , , , , |
|---|---|
| Language: | English |
| Published: |
2008
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/2429/1154 |