Vážení zákazníci, v letošním roce budeme expedovat poslední objednávky ve středu 18. 12. 2024.

Těšíme se s vámi na shledanou od pondělí 06. 01. 2025.

 

Cena s DPH / bez DPH
Hlavní stránka>BS EN ISO 17892-5:2017 Geotechnical investigation and testing. Laboratory testing of soil Incremental loading oedometer test
Sponsored link
sklademVydáno: 2017-04-30
BS EN ISO 17892-5:2017 Geotechnical investigation and testing. Laboratory testing of soil Incremental loading oedometer test

BS EN ISO 17892-5:2017

Geotechnical investigation and testing. Laboratory testing of soil Incremental loading oedometer test

Formát
Dostupnost
Cena a měna
Anglicky Zabezpečené PDF
K okamžitému stažení
7998 Kč
Čtěte normu po dobu 1 hodiny. Více informací v kategorii E-READING
Čtení normy
na 1 hodinu
799.80 Kč
Čtěte normu po dobu 24 hodin. Více informací v kategorii E-READING
Čtení normy
na 24 hodin
2399.40 Kč
Anglicky Tisk
Skladem
7998 Kč
Označení normy:BS EN ISO 17892-5:2017
Počet stran:38
Vydáno:2017-04-30
ISBN:978 0 580 87214 3
Status:Standard
Popis

BS EN ISO 17892-5:2017


This standard BS EN ISO 17892-5:2017 Geotechnical investigation and testing. Laboratory testing of soil is classified in these ICS categories:
  • 13.080.20 Physical properties of soils
  • 93.020 Earthworks. Excavations. Foundation construction. Underground works

This document specifies methods for the determination of the compressibility characteristics of soils by incremental loading in an oedometer.

This document is applicable to the laboratory determination of the compression and deformation characteristics of soil within the scope of geotechnical investigations.

The oedometer test is carried out on a cylindrical test specimen that is confined laterally by a rigid ring. The specimen is subjected to discrete increments of vertical axial loading or unloading and is allowed to drain axially from the top and bottom surfaces. Tests may be carried out on undisturbed, remoulded, recompacted or reconstituted specimens.

The stress paths and drainage conditions in foundations are generally three dimensional and differences can occur in the calculated values of both the magnitude and the rate of settlement.

The small size of the specimen generally does not adequately represent the fabric features present in natural soils.

Analysis of consolidation tests is generally based on the assumption that the soil is saturated. In case of unsaturated soils, some of the derived parameters may not be appropriate

NOTE This document fulfils the requirements of the determination of the compressibility characteristics of soils in the oedometer for geotechnical investigation and testing in accordance with EN 1997‑1 and EN 1997‑2 .