UA DE EN ES FR IT NL PL BY PT
the European climate
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sections
  • Two-dimensional anomalies of heat conductivity
  • the Analysis of a superficial thermal stream
  • Explosive tectonics and a thermal field evropy
  • the Thermal stream and an arrangement of ruptures
  • the Thermal stream, capacity of a bark
  • Value of researches of a thermal stream
  • Geothermal data on bolgarii
  • the Thermal stream in velikobritanii
  • geotermija vengrii
  • the Field of a thermal stream in territory gdr
  • Measurements of a thermal stream frg
  • the Preliminary card of a thermal stream gretsii
  • the Thermal stream in danii
  • Konduktivnyj a thermal stream in islandii
  • Temperature a gradient in ispanii
  • the Thermal stream in italii
  • the Thermal stream in velikobritanii. Heat conductivity

    you are: the Thermal stream in velikobritanii

    When there was a core, almost all values of factor of heat conductivity on which it was informed, have been received with use of a method of the divided core on the samples sated with water in the conditions of vacuum. Bullard and Niblett and Benfild have given the detailed description of the methods of measurement. Bullard and Niblett as the basic standard used the crystal quartz verified with quartz glass. Accuracy of measurements Benfilda on the average made +4,7% though errors in some of its measurements reached 8,9%. He considers, that nonplanar surfaces of samples of the rocks, creating distinctions in a thickness of a layer of greasing which it used for improvement of thermal contact between breed and brass disks were the reason of it. Bullard and Niblett for contact improvement used autotractor oil or silikonovuju greasing and achieved in the samples of high degree of smoothness; therefore accuracy of their measurements, obviously, was above, than at Benfilda. At checks with reference quartz the error appeared less than 1%, but in measurements of unknown values they did not consider a question on errors of measurements.

    Bott, etc., Tammemagi and Uajldon, and also Richardson and Oksburg used the methods of the divided core similar described Berchem, with application polikarbonatnyh auxiliary standards which were periodically calibrated on quartz. In Richardson's measurements and Oksburga the relative error of reproducibility at measurement on one unknown sample has made 4%. Tammemagi and Uajldon have estimated accuracy of the measurements in ±2%. In a chink the Uinterborn-valve it has been executed about 600 measurements of factor of heat conductivity with use of a needle probe. Application of this method on samples not completely litifitsirovannyh deposits immediately after their extraction from a chink allows to spend measurements before drying of breeds. As such deposits possess high porosity, often happens difficultly to reproduce the natural maintenance in them waters by means of laboratory procedures of saturation. Therefore the way of a needle probe possesses advantage in comparison with the divided core and other methods of the established mode in which thorough training of samples is required. One more advantage is speed of measurement as thus it is easy to investigate much is exemplary and by that it is possible to reduce to a minimum of a problem of reception of representative sample.

    When there was no core, heat conductivity measurements were spent Oksburgom, etc. and Uajldonom, etc. on shlame, taken of a chisel solution. These researchers used a method ' pill-boxing ', described in work Sassa and dr. Errors in this method arise because of uncertainty of porosity and contaminations shlama a material of several stratigraficheskih the horizons opened with a chink.


    sections
  • Two-dimensional anomalies of heat conductivity
  • the Analysis of a superficial thermal stream
  • Explosive tectonics and a thermal field evropy
  • the Thermal stream and an arrangement of ruptures
  • the Thermal stream, capacity of a bark
  • Value of researches of a thermal stream
  • Geothermal data on bolgarii
  • the Thermal stream in velikobritanii
  • geotermija vengrii
  • the Field of a thermal stream in territory gdr
  • Measurements of a thermal stream frg
  • the Preliminary card of a thermal stream gretsii
  • the Thermal stream in danii
  • Konduktivnyj a thermal stream in islandii
  • Temperature a gradient in ispanii
  • the Thermal stream in italii
  • las secciones
  • las anomalías Bidimensionales de la termoconductividad
  • el Análisis del flujo superficial térmico
  • la tectónica Explosiva y el campo térmico evropy
  • el flujo Térmico y la disposición de las rupturas
  • el flujo Térmico, la potencia kory
  • el Significado de las investigaciones del flujo térmico
  • los datos Geotérmicos por bolgarii
  • el flujo Térmico en velikobritanii
  • la Geotermia vengrii
  • Paul del flujo térmico en el territorio gdr
  • las Medidas del flujo térmico frg
  • la tarjeta Preliminar del flujo térmico gretsii
  • el flujo Térmico en danii
  • Konduktivnyj el flujo térmico en islandii
  • De temperatura el gradiente en ispanii
  • el flujo Térmico en italii
  • les paragraphes
  • dvumernye les anomalies de la conductibilité de la chaleur
  • l'Analyse du flux de chaleur superficiel
  • la tectonique Explosive et le champ thermique evropy
  • le Flux de chaleur et la disposition des ruptures
  • le Flux de chaleur, la capacité de l'écorce
  • la Signification des études du flux de chaleur
  • les données Géothermiques selon bolgarii
  • le Flux de chaleur à velikobritanii
  • la Géothermie vengrii
  • Paul du flux de chaleur sur le territoire gdr
  • les Mesures du flux de chaleur frg
  • la carte Préalable du flux de chaleur gretsii
  • le Flux de chaleur à danii
  • Konduktivnyj le flux de chaleur à islandii
  • De température le gradient à ispanii
  • le Flux de chaleur à italii