Lookup NU author(s): Professor David Manning
Full text for this publication is not currently held within this repository. Alternative links are provided below where available.
The availability of phosphorus in soils is controlled by the ability of plants to dissolve phosphate-bearing minerals, including apatite and feldspars. To satisfy the requirement of plants for phosphate, mineral dissolution competes with precipitation such as, for example, reactions involving lead or other heavy metals. Plants exude organic acid anions that very effectively enhance mineral dissolution but that may also liberate harmful solutes, such as aluminium. To make readily soluble chemical fertilisers, apatite in igneous and sedimentary rocks is mined and processed; in organic farming, phosphate-rich rocks are crushed and applied directly to the soil, relying on compounds produced by plant roots (exudates) to extract the phosphorus that plants need.
Author(s): Manning DAC
Publication type: Article
Publication status: Published
Print publication date: 01/04/2008
ISSN (print): 1811-5209
ISSN (electronic): 1811-5217
Publisher: Mineralogical Association of Canada
Altmetrics provided by Altmetric