PRICES include / exclude VAT
Homepage>BS Standards>13 ENVIRONMENT. HEALTH PROTECTION. SAFETY>13.080 Soil quality. Pedology>13.080.10 Chemical characteristics of soils>BS ISO 14869-2:2002 Soil quality. Dissolution for the determination of total element content Dissolution by alkaline fusion
Sponsored link
immediate downloadReleased: 2002-08-06
BS ISO 14869-2:2002 Soil quality. Dissolution for the determination of total element content Dissolution by alkaline fusion

BS ISO 14869-2:2002

Soil quality. Dissolution for the determination of total element content Dissolution by alkaline fusion

Format
Availability
Price and currency
English Secure PDF
Immediate download
151.20 EUR
You can read the standard for 1 hour. More information in the category: E-reading
Reading the standard
for 1 hour
15.12 EUR
You can read the standard for 24 hours. More information in the category: E-reading
Reading the standard
for 24 hours
45.36 EUR
English Hardcopy
In stock
151.20 EUR
Standard number:BS ISO 14869-2:2002
Pages:10
Released:2002-08-06
ISBN:0 580 40190 1
Status:Standard
DESCRIPTION

BS ISO 14869-2:2002


This standard BS ISO 14869-2:2002 Soil quality. Dissolution for the determination of total element content is classified in these ICS categories:
  • 13.080.10 Chemical characteristics of soils

This part of ISO 14869 specifies a method for the dissolution of total contents for the following elements in soils:

Na, K, Mg, Ca, Ti, Mn, Fe, Al, Si.

This list is not exhaustive, and other elements are applicable for determination, provided

  • they are not lost during the fusion process,

  • w > (3 d · V/m)

    where

    w is the mass content of the element, expressed in milligrams per kilogram soil,
    d is the detection limit, in milligrams per litre, for the element and analytical method considered,
    3 is a conventional factor,
    V is the adjusted volume, in litres, of the final solution containing the dissolved sample, and
    m is the mass of the test portion, in kilograms,
  • the determination is not adversely affected by the high salt concentration in the resultant solution.

The flux proposed in this method is suitable for a wide range of materials, among which soil samples are relatively easy to deal with.