Inositol hexakisphosphate (IP 6 ) is often the dominant form of soil organic phosphorus (P), but is rarely investigated because of the analytical difficulties encountered in its extraction, separation, and detection in environmental samples. In particular, recent advances in the study of soil organic P with 31 P nuclear magnetic resonance (NMR) have been of limited use for the study of IP6, because the technique does not discriminate between IP 6 and other forms of P. This was addressed by developing a novel analytical procedure using the retentive properties of gel-filtration gels for IP 6, which allows the combined selective extraction and pre-concentration of IP 6 from soil extracts with determination by 31 P NMR. While the technique is still in the developmental stage, the results demonstrate that the gel does not interfere with 3113 NMR analysis and retains IP6 to concentrations well above those required to give clear spectral signals. The technique has considerable potential for application to the study of IP 6 in soil extracts and water samples and, with development, could help to answer fundamental questions regarding the dynamics of organic P in the environment.T HE MOST ABUNDANT CLASS of organic phosphorus (P) compounds in the environment is the inositol phosphates, a family of six congeners of hexahydroxy cyclohexane (inositol) that exist as inositol in various states of phosphorylation (bound to between 1 and 6 phosphate ions) (Fig. 1). Nine stereoisomers of inositol phosphates exist; the myo stereoisomer is by far the most common in nature, although neo-, scyllo-, and chiro-inositol phosphates have been reported in terrestrial and aquatic environments (Cosgrove, 1980). The dominant form of inositol phosphate in the environment is myo-inositol hexakisphosphate (IP 6 ), which constitutes the major organic P compound in soils and aquatic sediments (Harrison, 1987; Suzumura and Kamatani, 1995). Despite its abundance, it remains poorly understood and little reliable information exists on the sources, pools, and dynamics of IP6 in the environment (Turner et al., 2002). The role of IP6 in supplying P to plants and algae is largely unknown and even its origins remain unclear in many cases (L'Annunziata, 1975). Research into IP6 has been limited by the lack of suitable analytical techniques for its determination in environmental samples, the main problems being poor recoveries of IP6 from soils by conventional extractants and from anion exchange columns during sample cleanup and separation (Anderson, 1964;Martin, 1970;Irving