Analüüs (tihedus ja poorsus) proovist Kg-53
Metoodika | tihedus ja poorsus |
Isik/asutus | Shogenova, Alla |
Proovi nr | Kg-53 |
Lisainfo | Density and porosity were determined using the water saturation method. For density measurements samples were dried at a temperature 100110 °C and the weight of dry samples (Pd) was determined. Then the samples were saturated with water for 7 days and after that weighed in air (Pw) and water (Pww). From the obtained measurements the following parameters were calculated: dry density = Pd/V = Pd/(Pw Pww), where V represents sample volume; wet density= Pw/(Pw Pww); grain density= Pd/(Pd Pww); effective porosity = (Pw Pd)/(Pw Pww). Research Institute of Earths Crust of St, Petersburg University (Russia) |
Lokaliteet | Kaugatuma 509 puurauk |
Sügavus | 19.7 |
Stratigraafia | Kaugatuma lade |
Litostratigraafia | Kaugatuma kihistu |
Asutus | TalTech geoloogia instituut |
Kirje lisatud | 2013-10-28 |
Kirje muudetud | 2014-01-10 |
Sirvi e-Maapõues