- pore saturation coefficient
- коэффициент насыщенности пор
Большой англо-русский и русско-английский словарь. 2001.
Большой англо-русский и русско-английский словарь. 2001.
коэффициент насыщенности пор — — [http://slovarionline.ru/anglo russkiy slovar neftegazovoy promyishlennosti/] Тематики нефтегазовая промышленность EN pore saturation coefficient … Справочник технического переводчика
rock — rock1 rockless, adj. rocklike, adj. /rok/, n. 1. a large mass of stone forming a hill, cliff, promontory, or the like. 2. Geol. a. mineral matter of variable composition, consolidated or unconsolidated, assembled in masses or considerable… … Universalium
Rock — /rok/, n. a male given name. * * * I In geology, a naturally occurring and coherent aggregate of minerals. The three major classes of rock igneous, sedimentary, and metamorphic are based on the processes that formed them. These three classes are… … Universalium
hydrosphere — /huy dreuh sfear /, n. the water on or surrounding the surface of the globe, including the water of the oceans and the water in the atmosphere. [1885 90; HYDRO 1 + SPHERE] * * * Discontinuous layer of water at or near the Earth s surface. It… … Universalium
Nuclear magnetic resonance in porous media — Nuclear magnetic resonance (NMR) in porous media covers the application of using NMR as a tool to study the structure of porous media and various processes occurring in them.[1] This technique allows the determination of characteristics such as… … Wikipedia
HYDROGÉOLOGIE — L’hydrogéologie est la science des eaux souterraines. Elle a pour objet l’étude du rôle des matériaux constituant le sol et le sous sol et des structures géologiques dans l’origine, la distribution et le mode de gisement, les modalités de… … Encyclopédie Universelle
Porosity — or void fraction is a measure of the void (i.e., empty ) spaces in a material, and is a fraction of the volume of voids over the total volume, between 0–1, or as a percentage between 0–100%. The term is used in multiple fields including… … Wikipedia
Loi de Darcy — La loi expérimentale de Darcy ou loi de Darcy a été établie par Henry Darcy. Elle est notamment utile pour calculer les écoulements souterrains de l eau ou d un liquide, verticalement à travers le sol vers la nappe par exemple, ou au travers d un … Wikipédia en Français