Sur l'unité d'origine du bleu de l'eauSpring, Walthère ![]() in Bulletin de la Classe des Sciences. Académie Royale de Belgique (1899), (2), 72-80 Spring, W. Bull. Acad. roy. Belg. (1899), 72; SciFinder (Chemical Abstracts Service: Columbus, OH); https://scifinder.cas.org (accessed July 8, 2010). Tyndall's experiments have been repeated and it was ... [more ▼] Spring, W. Bull. Acad. roy. Belg. (1899), 72; SciFinder (Chemical Abstracts Service: Columbus, OH); https://scifinder.cas.org (accessed July 8, 2010). Tyndall's experiments have been repeated and it was found that suspended particles do not give a blue color to the water. Further experiments showed that fluorescence was not a factor, and the final conclusion reached is that the blue color of water is due simply and solely to the fact that water is blue in color. Reprinted with the permission of the American Chemical Society. Copyright © 2010. American Chemical Society (ACS). All Rights Reserved. [less ▲] Detailed reference viewed: 6 (1 ULg) Sur l'utilisation de la variabilité de sujet pour corriger l'habileté: méthode et premiers résultatsMagis, David ; Scientific conference (2006, November) Detailed reference viewed: 3 (0 ULg) Sur la capacité de saturation des combinaisons colloïdesSpring, Walthère ![]() in Archives des Sciences Physiques et Naturelles (1911), XXX Spring, W. Archives des Sciences Physiques et Naturelles (1911), 30, 561-71; SciFinder (Chemical Abstracts Service: Columbus, OH); https://scifinder.cas.org (accessed July 8, 2010). cf. C. A., 4, 138, 969 ... [more ▼] Spring, W. Archives des Sciences Physiques et Naturelles (1911), 30, 561-71; SciFinder (Chemical Abstracts Service: Columbus, OH); https://scifinder.cas.org (accessed July 8, 2010). cf. C. A., 4, 138, 969, 1911. This is a report of some suggestive expts. on the mutual adsorption relations of saponin, lampblack and filter paper. When varying amts. of saponin are added to a standard suspension of lampblack in water the solns. of high and of low conc. settle faster than do the intermediate ones. There is an optimum stability at a conc. of saponin between 2.0 and 3.5%. In an elec. field saponin moves toward the anode, lampblack toward the cathode. When saponin is added to a lampblack suspension and an elec. current is passed the lampblack moves toward the anode-a reversal of the direction which it exhibits when alone. When a suspension of lampblack is poured through a filter the paper retains a part of the lampblack and this retained portion cannot be removed by washing with water, even when the filter is reversed. But if a soln. of saponin be poured through the blacked filter a portion of the retained lampblack is given up and passes through with the soln. A crayon made by molding a mixture of wet clay with lampblack or finely ground graphite marks paper easily and leaves a mark which is erased with difficulty. If, however, a soln. of saponin be used to moisten the clay-lampblack mixture the crayon is harder, marks paper with difficulty and the mark is easily erased. Similar results are obtained when the paper, instead of the crayon, is impregnated with saponin. When filter paper pulp is mixed with a lampblack suspension and collected on a cloth filter, the pulp retains some of the lampblack and the amt. so retained is sensibly independent of the conc. of lampblack in the original suspension. The author makes certain applications to the action of soapy substances in the cleansing of fabrics and concludes that there exists a limiting "saturation capacity in the combinations between colloids" which is analogous to the saturation of one atom by chem. combination with another. [This conclusion is quite out of accord with the existing knowledge of the form of the absorption isotherm and is not supported by the evidence presented. Reprinted with the permission of the American Chemical Society. Copyright © 2010. American Chemical Society (ACS). All Rights Reserved. [less ▲] Detailed reference viewed: 15 (1 ULg) Sur la cause de l'absence de coloration de certaines eaux limpides naturellesSpring, Walthère ![]() in Recueil des Travaux Chimiques des Pays-Bas et de la Belgique. 2e série (1898), XVII Spring, W. Recueil des Travaux Chimiques des Pays-Bas (1898), 17, 359-75; SciFinder (Chemical Abstracts Service: Columbus, OH); https://scifinder.cas.org (accessed July 8, 2010). Compare Abstr., 1884, 259 ... [more ▼] Spring, W. Recueil des Travaux Chimiques des Pays-Bas (1898), 17, 359-75; SciFinder (Chemical Abstracts Service: Columbus, OH); https://scifinder.cas.org (accessed July 8, 2010). Compare Abstr., 1884, 259, and Bull. Acad. roy. Belg., 1886, [iii], 12, 814, and 1897, [iii], 34, 578. Although it is well recognised that pure water is blue when viewed through a thickness greater than 1 metre, the only natural waters which appear blue are those of mountain streams which have their origin in the ice and snow of great altitudes. Berzelius has stated (Jabresbericht, 1830, 9, 207) that the extraordinarily clear water of Lake Wettern, in Sweden, is perfectly colourless when viewed through a thickness of more than 32 feet, and has hence raised objection to the view that pure water is blue. The author has previously shown (loc. cit.) that if water contains one ten-millionth part of its weight of colloidal ferric hydroxide, it no longer appears blue, but green in colour; with quantities greater than this, the colour is yellow or brown. By macerating fragments of a red rock, such as a Devonian schist, during several weeks with frequently renewed hot caustic potash, and subsequently washing with water by repeated decantation, a point is ultimately reached when the red coloring-matter ceases to subside from the washing water, even after standing several months; the particles of suspended ferric oxide (haematite) are no longer visible under a magnifying power of 150 diameters, and probably correspond with the dust of the Devonian epoch. On adding a few drops of this turbid solution to a large volume of pure water, the latter is rendered perfectly clear and colourless when viewed through a thickness of 6 metres. When the proportion of ferric oxide, however, is increased, the water quenches more and more of the transmitted light, until it finally becomes opaque, although appearing red by reflected light. These observations explain the fact that terrestrial waters rarely appear blue. That the waters of Alpine streams are generally blue is probably due to their being entirely free from suspended anhydrous ferric oxide; the cosmic dust with which they are often contaminated consists principally of meteoric iron, which possesses different optical properties from haematite, and is incapable of destroying the natural blue colour of the water. Reprinted with the permission of the American Chemical Society. Copyright © 2010. American Chemical Society (ACS). All Rights Reserved. [less ▲] Detailed reference viewed: 5 (1 ULg) Sur la cause de l'absence de coloration de certaines eaux limpides naturellesSpring, Walthère ![]() in Bulletin de l'Académie Royale des Sciences, des Lettres et des Beaux-arts de Belgique. Sciences. 3e série (1898), XXXVI(9-10), 266-276 Spring, W. Bulletin de la Classe des Sciences, Academie Royale de Belgique (1898), 38(3), 266-76 ; SciFinder (Chemical Abstracts Service: Columbus, OH); https://scifinder.cas.org (accessed July 8, 2010 ... [more ▼] Spring, W. Bulletin de la Classe des Sciences, Academie Royale de Belgique (1898), 38(3), 266-76 ; SciFinder (Chemical Abstracts Service: Columbus, OH); https://scifinder.cas.org (accessed July 8, 2010). Tying to its earlier reports over the role of the iron compounds and the humin substances with the feature of the coloring of water and over the elimination of this substances under influence of sunlight, etc. (Bulletin Acad. roy. Bolgique [3] 34. 578; C. 98. I. 410 and Rec. trav. chim. Pays-Bas 17. 202; C. 98. II. 224) author the cause of the colorlessness many discusses clear waters, about what already Berzelius (Annual Report f. Chemistry 9. 207) expressed its astonishment. Terrestrial water only very rarely will appear blue, since in all ground are traces of hematite, and this the blue color water for our eye compensates. On the other hand the glaciers and the snow of high peaks do not contain hematite, water from high regions throw their blue and therefore can maintain their color. Furthermore the influence of the iron compounds on the coloring water is very differenct, depending on whether they are in the form of their hydrates or anhydrous oxides in the water; into latter trap they step with the Humin or the organic substances water not into reaction, the water more generally continues to appear colorless. Reprinted with the permission of the American Chemical Society. Copyright © 2010. American Chemical Society (ACS). All Rights Reserved. [less ▲] Detailed reference viewed: 4 (1 ULg) Sur la cause de l'apnéeFredericq, Léon ![]() in Archives de Biologie (1900), XVII Detailed reference viewed: 2 (0 ULg) Sur la cause de l'apnéeFredericq, Léon ![]() in Bulletin de l'Académie Royale des Sciences, des Lettres et des Beaux-Arts de Belgique. Sciences (1900) Detailed reference viewed: 6 (0 ULg) Sur la cause de la direction du clivage des phyllades et des schistesSpring, Walthère ![]() in Bulletin de la Classe des Sciences. Académie Royale de Belgique (1902), (2), 150-154 Detailed reference viewed: 4 (0 ULg) Sur la cause de la fétidité de certains calcairesSpring, Walthère ![]() in Annales de la Société Géologique de Belgique (1889), XVI Detailed reference viewed: 6 (0 ULg) Sur la chaleur des alliages de plomb et d'étainSpring, Walthère ![]() in Bulletin de l'Académie Royale des Sciences, des Lettres et des Beaux-arts de Belgique. Sciences. 3e série (1886), XI(5), 355-404 Detailed reference viewed: 6 (1 ULg) Sur la chaleur des alliages de plomb et d'étainSpring, Walthère ![]() in Bulletin de la Société Chimique de Paris. Nouvelle série (1886), XLVI Detailed reference viewed: 5 (1 ULg) Sur la chaleur spécifique du peroxyde d'hydrogèneSpring, Walthère ![]() in Bulletin de l'Académie Royale des Sciences, des Lettres et des Beaux-arts de Belgique. Sciences. 3e série (1895), XXIX(4), 479-489 Detailed reference viewed: 35 (1 ULg) Sur la circulation céphalique croisée ou échange de sang carotidien entre deux animauxFredericq, Léon ![]() in Bulletin de l'Académie Royale des Sciences, des Lettres et des Beaux-Arts de Belgique. Sciences (1887), XIII Detailed reference viewed: 9 (0 ULg) Sur la circulation céphalique croisée ou échange de sang carotidien entre deux animauxFredericq, Léon ![]() in Archives de Biologie (1887), X Detailed reference viewed: 5 (0 ULg) Sur la concentration moléculaire des solutions d’albumine et de selsFredericq, Léon ![]() in Bulletin de l'Académie Royale des Sciences, des Lettres et des Beaux-Arts de Belgique. Sciences (1902) Detailed reference viewed: 3 (0 ULg) Sur la concentration moléculaire des solutions d’albumine et de selsFredericq, Léon ![]() in Archives de Biologie (1902), XX Detailed reference viewed: 2 (0 ULg) Sur la concentration moléculaire des tissus solides des animaux d’eau douceFredericq, Léon ![]() in Annales de la Société de Médecine de Gand (1876) Detailed reference viewed: 3 (0 ULg) Sur la concentration moléculaire du sang et des tissus chez les animaux aquatiquesFredericq, Léon ![]() in Bulletin de l'Académie Royale des Sciences, des Lettres et des Beaux-Arts de Belgique. Sciences (1901) Detailed reference viewed: 4 (0 ULg) Sur la concentration moléculaire du sang et des tissus chez les animaux aquatiquesFredericq, Léon ![]() in Archives de Biologie (1904), XX Detailed reference viewed: 4 (0 ULg) Sur la concurrence entre "relatifs" et "démonstratifs de liaison" chez les historiens latins : l'exemple de TaciteLongrée, Dominique ![]() in Bolkestein, Machtelt; Pinkster, Harm; Kroon, Caroline (Eds.) et al Theory and description in Latin linguistics, Selected papers from the Eleventh International Colloquium on Latin Linguistics, Amsterdam, June 24-29, 2001 (2002) Detailed reference viewed: 12 (0 ULg) |
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