In:
Soil Science Society of America Journal, Wiley, Vol. 72, No. 3 ( 2008-05), p. 786-790
Abstract:
It is unclear whether persulfate digestions completely liberate P associated with mineral colloids in soil solutions and aqueous soil extracts. We tested a modified persulfate digestion using aqueous soil extracts and suspensions of goethite, gibbsite, illite, and montmorillonite that were exposed to 24 μmol P L −1 as orthophosphate (ortho‐P) or myo‐inositol hexaphosphate (IHP). Digestion was performed by autoclaving (121°C, 60 min) 5 mL of extract or suspension after the addition of 1 mL of solution, which contained 150 mmol L −1 K 2 O 8 S 2 and 180 mmol L −1 H 2 SO 4 Subsequently, 0.7 mL of 188 mmol L −1 ascorbic acid was added and the sample was heated in a water bath at 95°C for 60 min. For the samples where P was sorbed onto goethite and gibbsite, recoveries of total P were 97.2 ± 3.7% (ortho‐P) and 102 ± 3.7% (IHP). For the samples where P was sorbed onto clay minerals, average total P recoveries were 99.2 ± 5.1% (ortho‐P) and 106 ± 3.0% (IHP). No differences between total P concentrations measured in persulfate‐digested soil extracts or with an additional digestion with HF and HNO 3 were detected.
Type of Medium:
Online Resource
ISSN:
0361-5995
,
1435-0661
DOI:
10.2136/sssaj2007.0178N
Language:
English
Publisher:
Wiley
Publication Date:
2008
detail.hit.zdb_id:
241415-6
detail.hit.zdb_id:
2239747-4
detail.hit.zdb_id:
196788-5
detail.hit.zdb_id:
1481691-X
SSG:
13
SSG:
21
