Menu
0
Total price
0 €
PRICES include / exclude VAT
Homepage>BS EN ISO 11275:2014 Soil quality. Determination of unsaturated hydraulic conductivity and water-retention characteristic. Wind's evaporation method
Sponsored link
sklademVydáno: 2014-05-31
BS EN ISO 11275:2014 Soil quality. Determination of unsaturated hydraulic conductivity and water-retention characteristic. Wind's evaporation method

BS EN ISO 11275:2014

Soil quality. Determination of unsaturated hydraulic conductivity and water-retention characteristic. Wind's evaporation method

Format
Availability
Price and currency
Anglicky Secure PDF
Immediate download
183.58 €
You can read the standard for 1 hour. More information in the category: E-reading
Reading the standard
for 1 hour
18.36 €
You can read the standard for 24 hours. More information in the category: E-reading
Reading the standard
for 24 hours
55.07 €
Anglicky Hardcopy
In stock
183.58 €
Označení normy:BS EN ISO 11275:2014
Počet stran:18
Vydáno:2014-05-31
ISBN:978 0 580 82151 6
Status:Standard
DESCRIPTION

BS EN ISO 11275:2014


This standard BS EN ISO 11275:2014 Soil quality. Determination of unsaturated hydraulic conductivity and water-retention characteristic. Wind's evaporation method is classified in these ICS categories:
  • 13.080.40 Hydrological properties of soils

This International Standard specifies a laboratory method for the simultaneous determination in soils of the unsaturated hydraulic conductivity and of the soil water-retention characteristic. It is applicable only to measurement of the drying or desorption curve. Application of the method is restricted to soil samples which are, as far as possible, homogeneous. The method is not applicable to soils which shrink in the range of matric head hm = 0 cm to hm = −800 cm.

The range of the determination of the conductivity depends on the soil type. It lies between matric heads of approximately hm = −50 cm and hm = −700 cm.

The range of the determination of the water-retention characteristic lies between matric heads of approximately hm = 0 cm and hm = −800 cm.

NOTE 1 An infiltrometer method can be used to determine hydraulic conductivities near saturation.

NOTE 2 ISO 11274 gives methods to determine the water-retention characteristic for matric heads between 0 cm and −15 000 cm.