At the beginning of the 20th century the task of reviewing all available literature across different scientific fields was initiated by professor Raýman, the general secretary of the Czech Academy of Emperor Franz Joseph for Science, Literature and Arts (CASLA). The first review for 1901 (in Czech language) appeared in the CASLA Bulletin during 1902. However, later, until the 1914 review, which was partially published in 1916, the reviews only consisted of physics reports. Usually, about five authors wrote the physical review covering different fields. Beginning in 1903, the review was also published as a separate book. The first 10 years of physical reviews referenced about 15 thousands papers from all available global literature., Jan Valenta., and Obsahuje bibliografii
Motto: "Pevnolátkové osvětlování je dnes tam, kde byl Internet v 80. letech. Stejně jako jsme tehdy nemohli předpovědět, jaký bude Internet, dnes, o 30 let později, nedokážeme předvídat, co všechno se stane se světelnou technikou a osvětlováním v příštích dekádách. Víme jen, že to bude úžasné a krásné." Roland Haitz, During its long evolution, techniques for artificial lighting used four main principles: combustion, incandescence, gas discharge and luminescence. The injection electroluminescence (taking place in light-emitting diodes, LED) is probably the most efficient way of converting electricity into light. In this paper we describe the main advantages and disadvantages of LED based light sources, as well as some topics of current research such as laser based light sources. Finally, the possible health effects of artificial lighting are briefly discussed., Jan Valenta, Ivan Pelant., and Obsahuje seznam literatury
After G. N. Lewis (1875-1946) proposed the term “photon” in 1926, many physicists adopted it as a more apt name for Einstein’s light quantum. However, Lewis’ photon was a concept of a very different kind, something few physicists knew or cared about. In fact, it turns out that the term “photon” was not novel, as the same term was proposed or used earlier, apparently independently, by at least four other scientists. Three of the four early proposals were related to physiology or visual perception, and only one to quantum physics. Priority belongs to the American physicist and psychologist L. T. Troland (1889-1932), who coined the word in 1916, and five years later it was independently introduced by the Irish physicist J. Joly (1857-1933). Then in 1925 a French physiologist, René Wurmser (1890-1993), wrote about the photon, and in July 1926 his compatriot, the physicist F. Wolfers (ca. 1890-1971), did the same in the context of optical physics. None of the four pre-Lewis versions of “photon” were well known and they were soon forgotten., Kdy se objevil termín "foton" a v jakém kontextu? O tom pojednává tento článek významného dánského historika fyziky H. S. Kragha. Obecně se soudí, že za "foton" vděčíme slavnému americkému chemikovi G. N. Lewisovi, který tento termín stvořil roku 1926. Je to pravda, ale Kragh ukazuje jednak, že to bylo v jiném kontextu, než jak chápeme foton dnes, jednak, že několik jiných badatelů navrhlo a použilo termín foton již před Lewisem - na ně se však zapomnělo. Nakonec tedy můžeme konstatovat, že "foton" se zrodil několikrát v období deseti let zhruba před sto lety. (jv), Helge S. Kragh., and Obsahuje bibliografické odkazy
The western part of the Bohemian Massif (Vogtland/West-Bohemia region at the Czech-German border) is characterized by relatively frequent intraplate earthquake swarms and by other manifestations of current geodynamic activity, such as mofettes, mineral and thermal springs. In this study we analyze variations of groundwater level in four hydrological wells in the region during the years 2005-2010. Monitoring during the previous time interval of 2000-2004 is also mentioned and used for comparison. Two of the wells are located in the epicentral region of Nový Kostel, and the other wells are more distant. The time interval includes the 2008 earthquake swarm when all the wells displayed a noticeable drop in the water level. This effect was observed up to epicentral distances of nearly 30 km, which exceeds the distances of hydrological changes observed during previous earthquake swarms. Moreover, it seems that a small rise in the water level preceded the intervals of increased seismic activity, which could represent a certain precursory phenomenon. On the other hand, the hydrological changes in the Nový Kostel area were relatively small, indicating that this epicentral area is not hydrologically linked with the seismically active fault at depth. Consequently, more suitable localities for hydrological monitoring should be sought in a broader vicinity of Nový Kostel., Renata Gaždová, Oldřich Novotný, Jiří Málek, Jan Valenta, Milan Brož and Petr Kolínský., and Obsahuje bibliografii
The history of semiconductor injection lasers is briefly outlined and the need for lasers integrated on Si chips is explained. Several approaches to overcome inadequate properties of silicon are followed; including (i) silicon nanocrystals and other lowdimensional structures (ii) Si Raman laser, (iii) rare-earth doped Si, and (iv) non-silicon-material lasers integrated to Si chips. Finally, the recent germanium laser is described., Jan Valenta., and Obsahuje bibliografii
Photography started to be applied in sciences shortly after the announcement of the daguerreotype in 1839 and become one of the most important supporting disciplines for science. This review concentrates on the history of scientific research on photographing processes which was conducted at Charles University. The most important was development of sensitometry which started by work of Vojtěch Šafařík (1829-1902) who thoroughly studied the dry proces. Photographic work in the Institute of Physics (IP) of the Czech part of "Carlo-Ferdinand University" was initiated due to studies of X-rays (from 1895) and later the Institute of Photochemistry and Scientific Photography was founded within IP by Professor Viktorin Vojtěch (1879-1948). In 1950-s this institute disappear and splitted into chemical part (colloidal chemistry and photochemistry) at Faculty of Natural Sciences and physical part (photophysics, studies of latent image and silver halogenides) at Faculty of Mathematics and Physics under leadership of Professor Ladislav Zachoval (1906-1982). His follower Professor Karel Vacek then turned interest from scientific photography into modern subjects of chemical physics and biophysics., Jan Valenta., and Obsahuje bibliografii
Local seismicity of the Hronov-Poříčí Fault Zone is studied using two-year continuous seismic data from four seismic stations in the area. Newly developed software for automatic seismic events detection is introduced - it is based on the method used at the Icelandic seismic network. Twelve major local earthquakes are detected, localized and their magnitudes are estimated. Simultaneously, groundwater levels are continuously monitored in three wells in the area. Multiple-filtering method, originally used for processing of broadband and dispersed seismic signals, is modified and used for the frequency-time analysis of the water level data. Dominant tidal influence on the groundwater level variations is shown. Theoretical tidal potential for all three well locations is computed. Groundwater data and tidal potential are bandpass filtered to focus on the semidiurnal periods. Mutual amplitude ratio and phase shift between both quantities are computed. Each of the three wells exhibits different pattern of the groundwater level variations with respect to tides. A distinct change in the phase shift is observed at the VS-3 well in the second half of 2009. In the same time span, increased seismic activity is also observed. However, other two wells do not exhibit any evidence of such phase shift. Detailed groundwater level data analysis does not prove any significant rises or drops of the groundwater levels in 28 day intervals around the detected local events. In contras t, unexplained groundwater level drop in the V-34 well is obser ved 18 hours before the teleseismic Tohoku earthquake, Japan, March 11, 2011, Mw = 9.0., Petr Kolínský, Jan Valenta and Renata Gaždová., and Obsahuje bibliografické odkazy
The Hronov-Poříčí Trough represents the easternmost part of the Trutnov-Náchod Depression. The NW-SE striking structure was formed due to the post-Cretaceous flexural folding and is filled with the Upper Cretaceous sediments. Both the NE and SW margins of the trough are bounded by flexures with the Upper Cretaceous strata dipping 40-60° towards the axis of the trough. The NE flexure is situated close to the parallel Hronov-Poříčí Fault Zone. Up to now, it is not fully known, in what extent the normal faulting was involved in the evolution of the structure. From the geomorphological point of view, the normal fault constraints of the trough seem to be acceptable, as the surface topography of its present margins exhibit many signs typical for fault scarps. However, the existence of a fault system bounding all round the Hronov-Poříčí Trough has not b een proved by any geological research. Hence the geophysical research was carried out on both sides of the NW part of the trough to support one of these hypothesis. Five geoelectrical profiles were measured in the area and the fault system was proved on the NE side of the trough. On the SW boundary the fault system was not found. Thus it seems, that the NE boundary is controlled by fault tectonics, whereas the SW boundary is rather formed by a simple flexure., Jan Valenta, Vladimír Stejskal and Petra Štěpančíková., and Obsahuje bibliografické odkazy
This paper combines morphostructural analysis and geophysical methods in order to link the faults monitored inside Strašín Cave with faults and lineaments in the vicinity of the cave. The studied site is situated in SW Bohemia, at the foothills of the Bohemian Forest Mts. Main goal is to combine the morphostructural, morphometrical and geophysical methods in order to identify the fault system, monitored inside the cave. This will allow relevant interpretation of the observed movements in the frame of the local tectonic environment. The results show that the monitored faults are observable in the geophysical profiles and, using our knowledge of the structural setting, we have been able to link them with mapped tectonic structures in the vicinity of the cave. Thus, it has been demonstrated that even where outcrops are absent, the faults can be traced and that the monitored faults are significant enough to yield relevant data on tectonic movements. In addition, the combined resistivity and gravimetry profiles reveal a possible new, presently unknown, cave located 20 m below the surface about 200 m northnortheast of Strašín Cave., Filip Hartvich and Jan Valenta., and Obsahuje bibliografii