Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Clotilde Bertin"'
Autor:
AUDE BEAUGER, CARLOS E. WETZEL, ELISABETH ALLAIN, CLOTILDE BERTIN, OLIVIER VOLDOIRE, VINCENT BRETON, LORY-ANNE BAKER, SOFIA KOLOVI, DAVID BIRON, LUC ECTOR
Publikováno v:
Phytotaxa
Phytotaxa, 2022, 538 (1), pp.55-73. ⟨10.11646/phytotaxa.538.1.5⟩
Phytotaxa, 2022, 538 (1), pp.55-73. ⟨10.11646/phytotaxa.538.1.5⟩
International audience; During a survey done on the mineral springs in the French Massif Central region, a new Chamaepinnularia species (Bacillariophyceae) was found and is hereby described: Chamaepinnularia salina Beauger, C.E.Wetzel, Allain & Ector
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::df2497ca8df62b49f8b2870c10b21dac
https://zenodo.org/record/6332002
https://zenodo.org/record/6332002
Publikováno v:
Applied Geochemistry
Applied Geochemistry, Elsevier, 2014, 40, pp.104-118. ⟨10.1016/j.apgeochem.2013.11.006⟩
Applied Geochemistry, Elsevier, 2014, 40, pp.104-118. ⟨10.1016/j.apgeochem.2013.11.006⟩
International audience; The bio-diversity (vegetation and fauna) of peatlands, like all wetland ecosystems, is very fragile as it requires specific wet conditions. Over the past 20 years, increasing efforts have been made to restore degraded wetlands
Publikováno v:
Chemical Geology
Chemical Geology, Elsevier, 2010, 276 (1-2), pp.119-127. ⟨10.1016/j.chemgeo.2010.06.008⟩
Chemical Geology, Elsevier, 2010, 276 (1-2), pp.119-127. ⟨10.1016/j.chemgeo.2010.06.008⟩
Water circulation in the peat bog of a maar depression in the Massif Central (France) was traced with lithium isotopes on water samples collected in the area from springs, surface- and groundwaters, as well as on solid samples taken from peat bogs. L
Autor:
Alain C.M. Bourg, Clotilde Bertin
Publikováno v:
Water, Air, and Soil Pollution. 86:101-116
A chemical survey of the water of the Lot River (Southwestern France) was conducted for 26 h. Water temperature, pH, dissolved oxygen and zinc exhibited a diurnal cycle. These variations are caused by biological activity in the river (photosynthesis
Autor:
Clotilde Bertin, Alain C.M. Bourg
Publikováno v:
Water Research. 29:1729-1736
The geochemical and granulometric characteristics of sediments from three sites in the Lot River basin contaminated by heavy metals (cadmium, lead and zinc) were studied over a period of three years. Total heavy metal concentrations show little varia
Autor:
Clotilde Bertin, Alain C.M. Bourg
Publikováno v:
Environmental Science & Technology. 28:794-798
Natural dissolved 222 Rn concentration increases with distance as Lot River water infiltrates into an alluvial aquifer. At distances greater than 150 m from the river, 222 Rn has a constant value of ca. 55 Bq L -1 . This is in agreement with the theo
Autor:
Clotilde Bertin, Alain C.M. Bourg
Publikováno v:
Environmental Science & Technology. 28:868-876
The hydrogeochemistry of river water and groundwater in a hydraulic configuration where river water infiltrates into an alluvial aquifer was monitored monthly over a 14-month period. Trends could be seen for temperature, pH, and dissolved O 2 and Mn.
Publikováno v:
Geophysical Research Abstracts
EGU General Assembly 2011
EGU General Assembly 2011, Apr 2011, Vienne, Austria. pp.EGU2011-3797
HAL
EGU General Assembly 2011
EGU General Assembly 2011, Apr 2011, Vienne, Austria. pp.EGU2011-3797
HAL
International audience; Water circulation in the peat bog of a maar depression in the Massif Central (France) was traced with lithium isotopes on water samples collected in the area from springs, surface-and groundwaters, as well as on solid samples
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::b4aef84380fc6c152085f3acd0f02cb8
https://hal-brgm.archives-ouvertes.fr/hal-00582489/file/EGU2011-3797.pdf
https://hal-brgm.archives-ouvertes.fr/hal-00582489/file/EGU2011-3797.pdf
Autor:
Alain C.M. Bourg, Clotilde Bertin
Publikováno v:
Environmental Science & Technology. 27:661-666
Summary and Conclusions The chemical changes in the infiltration flow path from the Lot River to an adjacent aquifer were followed using chloride as an indicator of physical mixing of the river water with groundwater. The chemical reactivity close to