Analysis (density and porosity analysis) from sample 101989
General info
| Method | density and porosity analysis |
| Person/Institution | Shogenov |
| Sample number |
101989
|
| Remarks | 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) |
| Reference | Shogenova et al., 2005a |
| Dataset | Geochemistry and petrophysics of the Mehikoorma core |
| Locality |
Mehikoorma 421 borehole
|
| Depth | 149.2 |
| Stratigraphy |
Narva Stage
|
| Lithostratigraphy |
Kernave Formation
|
| Institution | Department of Geology, TalTech |
| Date added | 2013-10-28 |
| Date changed | 2014-01-10 |
Results
| Parameter | Value | Text | Error |
|---|---|---|---|
| Dry density [kg/m3] | 2455 | ||
| Wet density [kg/m3] | 2603 | ||
| Grain density [kg/m3] | 2883 | ||
| Porosity [%] | 14.83 |
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