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Titlebook: Nuclear Geophysics; Applications in Hydr V.I. Ferronsky Book 2015 Springer International Publishing Switzerland 2015 Groundwater and Hydrog

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樓主: ominous
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發(fā)表于 2025-3-26 22:37:44 | 只看該作者
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發(fā)表于 2025-3-27 04:47:00 | 只看該作者
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發(fā)表于 2025-3-27 06:20:57 | 只看該作者
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發(fā)表于 2025-3-27 12:03:17 | 只看該作者
Penetration Logging Methods and Equipmentented. The solution of a problem is achieved on the basis of combining the soil static penetration test and nuclear logging methods. The first experimental study on the application of the nuclear penetration logging method was started in 1962. The group of methods, which were tested and included in
35#
發(fā)表于 2025-3-27 16:20:07 | 只看該作者
Theoretical Basis of Penetration Logging Testsdulus of compressibility and coefficient of inner ground friction is discussed. Solutions based on the theory of ultimate equilibrium, .mplacement of a spherical probe into an infinite elastic medium, imbedding of spherical sound in elastic media and taking into account creeping in time and a two-di
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發(fā)表于 2025-3-27 18:15:29 | 只看該作者
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發(fā)表于 2025-3-27 22:14:16 | 只看該作者
Application of Penetration Logging Techniques for Geoengineering Exploration penetration logging technique are discussed. The practical application of penetration logging methods in engineering geological and hydrogeological mapping for irrigation and drainage projects in the Alma-Ata (Kazakhstan), Kizil-Orda (Uzbekistan), Saratov (Russia), Kiev (Ukraine), Neman River (Belo
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發(fā)表于 2025-3-28 05:21:16 | 只看該作者
Stable Isotopes in Study of the Global Hydrological Cycleng stable and unstable isotopes of individual elements, in particular by determining the variations in their abundance. Isotope geology deals with both stable and radioactive isotopes. In this chapter the distribution, hydrogeochemistry and geophysics of naturally occurring stable hydrogen and oxyge
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發(fā)表于 2025-3-28 08:16:48 | 只看該作者
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發(fā)表于 2025-3-28 13:39:24 | 只看該作者
Radiogenic Isotopes in Dating of Natural Waters and Sediments .U, .U, .Th, .Th, .Th, .Ra, and .Ra) in natural waters are discussed in this chapter. Methods of dating surface waters, groundwaters, closed reservoirs and bottom sediments are analysed. The values of the radiogenic isotopes in waters are practically independent of chemical factors. It is mainly de
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