Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Max Ganteaume"'
Publikováno v:
Thermochimica Acta. 221:255-262
Resume L'eau incluse est l'un des constituants des coraux fossiles. Nous avons mesure par thermogravimetrie, la part d'eau adsorbee et surtout le pourcentage d'eau incluse qui semble constant pour les coraux qui ne contiennent que de l'aragonite (1,7
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::496be4cc0f3f71cb459c0461a02af016
https://doi.org/10.1016/0040-6031(93)85070-p
https://doi.org/10.1016/0040-6031(93)85070-p
Publikováno v:
Thermochimica Acta. 178:81-98
A new solution calorimeter (the Calsol) is described. This conduction calorimeter (heat fluxmeter) is differential and rotating. The sensitive part of the temperature regulator is placed between the thermostat and the outer case, and a microcomputer
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9982c06d4871ae0de1488e931da9931
https://doi.org/10.1016/0040-6031(91)80300-8
https://doi.org/10.1016/0040-6031(91)80300-8
Autor:
Michel Bernat, Max Ganteaume, Christian Zahra, Dominique Lapraz, Jean-Emmanuel Bokilo, Philibert Iacconi, Alain Baumer
Publikováno v:
Thermochimica Acta. 170:121-137
The aragonite fossil corals exhibit an intense natural thermoluminescence between 300°C and 450°C. The transformation of this biogenic aragonite into calcite begins at 260°C and is completed around 450°C. It is accompanied by a rapid loss of wate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::af259758bcb4d63d202af1c15428ce1e
https://doi.org/10.1016/0040-6031(90)80530-c
https://doi.org/10.1016/0040-6031(90)80530-c
Publikováno v:
European Journal of Mineralogy. 2:297-304
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c69e7c033e056f5a503087a649dba5f1
https://doi.org/10.1127/ejm/2/3/0297
https://doi.org/10.1127/ejm/2/3/0297
Autor:
Martine Decressac, Max Ganteaume
Publikováno v:
Thermochimica Acta. 80:51-74
The changes in Gibbs energy, enthalpy, and entropy for the protonation of phenylalanine anion (L) and for the formation of complexes ML+ and ML2 (M = Cu2+ or Co2+) are reported for I = 1 M (Na)Cl at 25°C. The results are compared with those of other
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::39c9f05b1beedd950ee7324756e7dc17
https://doi.org/10.1016/0040-6031(84)87183-x
https://doi.org/10.1016/0040-6031(84)87183-x
Autor:
Max Ganteaume, Martine Decressac
Publikováno v:
Thermochimica Acta. 80:35-49
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91677e22b1e8345f7aee879d2d4121dc
https://doi.org/10.1016/0040-6031(84)87182-8
https://doi.org/10.1016/0040-6031(84)87182-8
Publikováno v:
Chemical Geology. 54:311-318
Sedimentary phosphate apatite is a phosphocalcium carbo-apatite. For this kind of structure, two possibilities exist for PO 3− 4 CO 2− 3 replacement: one corresponds to PO 3− 4 ( CO 2− 3 , F − ) with substitution ratio x , the other one to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4aed0b84106cc8f0b5059e0b6f836cba
https://doi.org/10.1016/0009-2541(86)90145-2
https://doi.org/10.1016/0009-2541(86)90145-2
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
The molar absorption coefficients for the OH stretching vibrations of 16 hydrothermally prepared hydroxyfluorapatites Ca5(PO4)3(OH)xF1-x have been determined. The coefficients vary with composition, reaching a maximum at x = 0.8. At low OH concentrat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::91abfa65aead4d0a70d6a103e739d81c
https://www.persee.fr/doc/bulmi_0180-9210_1985_num_108_2_7864
https://www.persee.fr/doc/bulmi_0180-9210_1985_num_108_2_7864