@article{fdi:40370,
  title = {{H}ydrodynamics of {E}bri{\'e} lagoon as revealed by a chemical and isotopic study},
  author = {{G}uiral, {D}aniel and {F}ehri, {A}.},
  editor = {},
  language = {{ENG}},
  abstract = {{T}o determine the origin and the circulation of waters in the different areas of the {E}bri{\'e} lagoon ({I}vory {C}oast), ionic concentrations ({K}+, {C}l-) and isotopic ... measurements were performed. {S}ixty stations were sampled. {C}hemical and isotopic analyses were made thrice during a hydrological cycle : in may 1986, at the end of the great dry season; in {O}ctober 1986, during the maximum of rainfall, in december 1987, after the {C}omoe river peak flow. {F}rom a hydrodynamical point of view, the results reported in this work indicate that the lagoon comprises four distinctive areas. {T}he first is filled with freshwater all the year round and is characterized by an weak isotopic enrichment (these waters are of continental origin and annually renewed); the second corresponds to oligohaline waters ... (waters essentially of continental origin and poorly renewed); the third area is constituted of a mixure of waters of continental and oceanic origins. {T}he latter group can be separated into two subgroups : a group completely renewed by oceanic water during the dry season and another group totally renewed by freshwater during the rainy and flood seasons. ({D}'apr{\`e}s r{\'e}sum{\'e} d'auteur)},
  keywords = {{LAGUNE} ; {ZONE} {COTIERE} ; {CIRCULATION} {DE} {L}'{EAU} ; {ANALYSE} {CHIMIQUE} ; {ANALYSE} {ISOTOPIQUE} ; {CYCLE} {HYDROLOGIQUE} ; {CARACTERISTIQUE} {CHIMIQUE} ; {COTE} {D}'{IVOIRE} ; {EBRIE} {LAGUNE}},
  booktitle = {},
  journal = {{H}ydrobiologia},
  volume = {245},
  numero = {},
  pages = {65--74},
  ISSN = {0018-8158},
  year = {1992},
  DOI = {10.1007/{BF}00764766},
  URL = {https://www.documentation.ird.fr/hor/fdi:40370},
}