FN Archimer Export Format
PT J
TI Le néphéloïde benthique au large du Rhône. Transferts particulaires à l'interface continent-océan
OT The bottom nepheloid layer off the rhone river mouth - particulate transfer at the land-ocean interaction
BT 
AF NAUDIN, JJ
   CAUWET, G
   LEVEAU, M
   LOCHET, F
   PAUC, H
   ROMANO, JC
   SEMPERE, R
AS 1:;2:;3:;4:;5:;6:;7:;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 FAC SCI LUMINY,CTR OCEANOL MARSEILLE,CNRS,URA 41,F-13288 MARSEILLE 9,FRANCE
C2 FAC SCI LUMINY,CTR OCEANOL MARSEILLE,CNRS,URA 41,F-13288 MARSEILLE 9,FRANCE
IF 0.662
TC 13
UR https://archimer.ifremer.fr/doc/00101/21230/18847.pdf
LA French
DT Article
DE ;BOTTOM NEPHELOID LAYER;PARTICULATE MATTER;CURRENT MEASUREMENTS;HYDROLOGY
AB Particulate matter from the bottom nepheloid layer, off the Rhone river mouth was sampled with a newly-designed frame code-named SYMPHY. Several spreading phases of the Rhodanian suspensions on the continental shelf were evidenced by currentmeter records, particulate matter analyses, CTD and nephelometric measurements. These data permitted the study of the mechanisms which control the aging of the suspensions during their transfer to a sea with very small amplitude tides. The bottom nepheloid layer can be defined as a vertical concentration gradient resulting from an equilibrium between the horizontal (Rhodanian inputs) and the vertical (surface nepheloid layer) components of the particulate flux. The variability of this equilibrium, controlled by hydrodynamic fluctuations, involves different residence times and permits modifications of the nature of suspensions by biogeochemical processes.
PY 1992
SO Oceanologica Acta
SN 0399-1784
PU Gauthier-Villars
VL 15
IS 6
UT A1992KQ50000005
BP 621
EP 638
ID 21230
ER

EF