FN Archimer Export Format
PT J
TI A dual sensor device to estimate fluid flow velocity at diffuse hydrothermal vents
BT 
AF SARRAZIN, Jozee
   RODIER, Philippe
   TIVEY, M. K.
   SINGH, H.
   SCHULTZ, A.
   SARRADIN, Pierre-Marie
AS 1:1;2:1;3:2;4:2;5:3;6:1;
FF 1:PDG-DOP-DCB-EEP-LEP;2:PDG-DOP-DCB-EEP-LEP;3:;4:;5:;6:PDG-DOP-DCB-EEP;
C1 IFREMER, Ctr Brest, Dept Etud Ecosyst Profonds, Lab Environm Profond, F-29280 Plouzane, France.
   Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.
   Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA.
C2 IFREMER, FRANCE
   WOODS HOLE, USA
   COLL OCEAN & ATMOSPHER SCI, USA
SI BREST
SE PDG-DOP-DCB-EEP-LEP
   PDG-DOP-DCB-EEP
IN WOS Ifremer jusqu'en 2018
   copubli-int-hors-europe
IF 2.593
TC 22
UR https://archimer.ifremer.fr/doc/2009/publication-7299.pdf
LA English
DT Article
CR EXOMAR
   MOMARETO
   MOMARSAT : MONITORING THE MID ATLANTIC RIDGE
BO Unknown
DE ;Diffuse flow;Video imagery;Hot film anemometer;Hydrothermal vent;Fluid flow velocity
AB Numerous attempts have been made over the last thirty years to estimate fluid flow rates at hydrothermal vents, either at the exit of black smoker chimneys or within diffuse flow areas. In this study, we combine two methods to accurately estimate fluid flow velocities at diffuse flow areas. While the first method uses a hot film anemometer that performs high-frequency measurements, the second allows a relatively rapid assessment of fluid flow velocity through video imagery and provides in situ data to calibrate the sensor. Measurements of flow velocities on hydrothermal diffuse flow areas were obtained on the Mid-Atlantic Ridge (MAR). They range from 1.1 to 4.9 mm/s at the substratum level, in low-temperature (4.5-16.4 degrees C) diffuse flow areas from the Tour Eiffel sulfide edifice. A strong correlation was observed between fluid flow velocities and temperature, supporting the possible use of temperature as a proxy to estimate the flow rates in diffuse flow areas where such a simple linear flow/temperature relation is shown to dominate.
PY 2009
PD NOV
SO Deep Sea Research Part I: Oceanographic Research Papers
SN 0967-0637
PU Elsevier
VL 56
IS 11
UT 000271683200012
BP 2065
EP 2074
DI 10.1016/j.dsr.2009.06.008
ID 7299
ER

EF