Nghĩa của từ actinometric bằng Tiếng Việt

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1. For other light sources/actinometric systems, the same approach may be used, but each actinometric system should be calibrated for the light source used.

2. An example of an actinometric procedure is provided in the Annex.

3. In addition, an explanation is given of the latest actinometric results.

4. These new values ought, to be employed in actinometric investigations.

5. Using a four year period of actinometric measurements turbidity parameters according toW.

6. The ICH Q1B guideline specifies actinometric measurement with two ampoules for pharmaceutical products.

7. The actinometric integral-equation of extinction is solved by finite iterations with fast convergence.

8. The author presents a critical study of actinometric measurements of the solar radiation with interference filters, carried out at the Freiburg/Br.

9. If α is not a constant one can obtain a family of turbidity values α and β from the actinometric measurements.

10. The author presents a critical study of actinometric measurements of the solar radiation with interference filters, carried out at the Freiburg/Br. Observatory.

11. Annex Quinine Chemical Actinometry The following provides details of an actinometric procedure for monitoring exposure to a near UV fluorescent lamp (based on FDA/National Institute of Standards and Technology study).

12. ANNEX A. Quinine Chemical Actinometry The following provides details of an actinometric procedure for monitoring exposure to a near UV flourescent lamp (based on FDA/National Institute of Standards and Technology study).

13. The actinometric measurements carried out at Jungfraujoch (3471 m) during the International Polar Year 1932/33 are evaluated for climatological problems and for the determination of the components of the atmospheric turbidity.

14. The daily course of this haze turbidity was examined by actinometric and photometric intensity measurements of direct solar radiation at a station at Locarno (234 m a.s.l.) and at Locarno-Monti Observatory (380 m a.s.l.).

15. Actinometric measurements of the solar intensity in the spectral regions: λ<425, λ<525, λ>630 mμ as well as the total solar intensity for the whole spectrum of the sun have been undertaken at Giza (lat.

16. Measurement series of the upwelling solar radiation above the Baltic Sea and the corresponding actinometric and meteorological observations were carried out during the scientific cruises of the RV “Ayu-Dag” in the summer of 1981 and 1982.

17. To simplify the determination of atmospheric turbidity by actinometric measurements with respect to theSchüepp method, a diagram has been computed from the data ofSchüepp to derive the decadic turbidity coefficientBλ500 from measurements of short wave radiation (JK, λ<625 nm).

18. Samples may be exposed side-by-side with a validated chemical actinometric system to ensure the specified light exposure is obtained, or for the appropriate duration of time when conditions have been monitored using calibrated radiometers/lux meters.

19. Input parameters for the program are astronomical factors, spectral values of extraterrestrial irradiance and of atmospheric absorption coefficients, and the surface albedo. The input parameters for aerosol extinction and the precipitable water of the atmosphere can be taken from actinometric measurements.

20. Actinometric determinations of the daily period of the quantityw of precipitable water in the atmosphere and observations of the vapour pressurewD at the same places give a possibility to study the daily period of exchange of airmasses in mountainous regions, near the coasts and of whole continents in the case of anticyclonic weather.

21. The computations have been accomplished explicitly as far as needed and are sufficient for an examination of the most essential properties of a great number of actinometric instruments. They show the general methods used for computations far enough that the latter may be adapted to special conditions being in question with particular types of instruments.

22. Actinometric measurements of the direct solar intensity in the whole solar spectrum as well as in the wavelength-regions separated by the commonly used filters — OG 1 for yellow and red filter RG 2 or RG 8 for red and infrared — provide the possibility for determining the general turbidity coefficientB, the wavelength exponent α and the precipitable water contentW of the atmosphere.