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Une recherche sur le taux de chlorinité de l’eau interstitielle dans le lit de La Slack
| Content Provider | Semantic Scholar |
|---|---|
| Author | Nooter, Kees Liebregts, F. |
| Copyright Year | 1971 |
| Abstract | The supposition that the Slack, a river in northwestern France discharging directly into the sea, has a significantly higher chlorinity in its bottom sediments than in the overflowing river water, is confirmed. A device to take samples of sediment from the river bottom has been constructed and is described in this publication. To obtain the interstitial water, the sample is simply centrifuged. A peculiar phenomenon, which could not be explained, is that after a regular decrease of the interstitial chlorinities, a considerable increase (to > 1.5 ‰) takes place at a distance of some 2½ kilometres from the mouth. The interstitial chlorinity in the estuarine part of the river proved to be almost constant, regardless of the tidal cycle. |
| Starting Page | 23 |
| Ending Page | 30 |
| Page Count | 8 |
| File Format | PDF HTM / HTML |
| DOI | 10.1163/26660644-04101004 |
| Volume Number | 41 |
| Alternate Webpage(s) | http://www.repository.naturalis.nl/document/547518 |
| Alternate Webpage(s) | https://doi.org/10.1163/26660644-04101004 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |
