Plant and Soil

, Volume 53, Issue 1, pp 55–65

The availability of P from phosphate-goethite bridging complexes. Desorption and uptake by ryegrass

Authors

  • R. L. Parfitt
    • Soil Bureau, D.S.I.R.
Article

DOI: 10.1007/BF02181879

Cite this article as:
Parfitt, R.L. Plant Soil (1979) 53: 55. doi:10.1007/BF02181879

Summary

Pot trials using phosphated-goethite (bridging complex) as the source of P for ryegrass were established. No P was readily available to ryegrass until the surface was >40% covered with phosphate ions. Availability increased as the P level in solution increased up to 2 μM. Maximum availability was attained when the initial concentration of P in solution was 2 μM which occurred at about 75% coverage on geothite. Mycorrhiza increased the availability of phosphate at a level of about 0.5–2 μM P (60–70% coverage of the goethite surface).

Laboratory experiments showed that citrate ions were particularly effective in displacing P from goethite and the Olsen reagent was a good predictor of P availability to ryegrass.

Key Words

Aluminium hydrous oxides Goethite Iron hydrous oxides Mycorrhiza Phosphate Root exudates Ryegrass

Copyright information

© Martinus Nijhoff Publishers 1979