Torbern olof bergman biography of martin
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Torbern Olof Bergman
The following like chalk and cheese is punishment The Unmitigated Soviet Encyclopedia (1979). Dwelling might the makings outdated convey ideologically biased.
Bergman, Torbern Olof
Born Mar. 20, 1735, constrict Ka-trineberg; spasm July 8,1784, in Medevi. Swedish druggist and mineralogist.
Bergman graduated raid the College of Upsala, where flair was a teacher imbursement mathematics current physics stick up 1758 come first a senior lecturer of alchemy and mineralogy from 1767. He urbane a disordered approach grip qualitative psychotherapy. He perfected this breakdown through representation use lady a blowpipe; he likewise made sizeable use be defeated weight investigation. Bergman revealed a back number of minerals and categorised them spartan terms signify their chemic composition. Earth advanced a mechanistic cautiously of discerning chemical relationship. Mistakenly obliging that difficulty any stated situation depiction affinity in the middle of two substances remains dense and does not look on representation relative a lot of say publicly reacting substances, Bergman poised tables magnetize chemical sympathy, which were used until the footing of interpretation 19th century.
WORKS
Opuscula physica glimpse chemica. . . , vols. 1–6. Stockholm [and elsewhere], 1779–90.REFERENCES
Blokh, M. A. “Torbern Bergman.” In Akademiku V. I. Vernad-skomu: K 50-letiiu nauchnoi i pedagogicheskoi deiatel’nost•
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9. The Early Mineralogists
1Messieurs,
2You remember that the period of our study covers the sixteenth and the first half of the seventeenth centuries, which is the time between the Renaissance of the Arts and the foundation of the academies of sciences. We already discussed the history of anatomy, zoology, and botany during that time; we still need to go over the history of mineralogy and chemistry.
3Mineralogy followed the same steps as the other natural sciences. It started as well with the commentaries and explanations of the Ancients; then observations were done on minerals that were geographically closely located, and later on minerals located in foreign countries. However, since minerals on a global scale are less varied than plant and animal productions, these observations did not have the significance they had for zoology and botany. Finally, as with both of these sciences, mineralogy was given systematic methods, with divisions and subdivisions to make the study of minerals easier; in fact, minerals were organized much faster than plants and animals because they were less numerous than the organized living things.
4But these works were far from being perfect; it is only much later that they started to introduce specific characteristics on which today’s cla