Functional Group Specific Phytic Acid Adsorption at the Ferrihydrite-Water Interface
1Department of Natural Resources and Environmental Sciences , University of Illinois at Urbana-Champaign , Urbana , 61801 , United States.
Environmental Science & Technology
|June 12, 2019
Summary
Phytic acid adsorption on ferrihydrite is pH-dependent, with inner-sphere complexation dominating. Specific phosphate groups show preferential binding, influencing phosphorus dynamics in soils.
Area of Science:
- Soil Chemistry
- Environmental Science
- Mineralogy
Background:
- Phytic acid is the primary organic phosphorus form in soils.
- It strongly adsorbs to iron (Fe) and aluminum (Al) minerals.
- Understanding adsorption is key to soil phosphorus cycling.
Purpose of the Study:
- Investigate phytic acid adsorption mechanisms at the ferrihydrite-water interface.
- Determine the influence of pH on adsorption.
- Identify specific binding sites and functional groups involved.
Main Methods:
- Batch adsorption experiments.
- Zeta potential measurements.
- In situ P K-edge X-ray absorption near edge structure (XANES) spectroscopy.
- Solution 31P nuclear magnetic resonance (NMR) spectroscopy.
Main Results:
- Ferrihydrite's isoelectric point decreased with increasing phytic acid concentration.
- Adsorption decreased from pH 5 to 9 and increased with ionic strength.
- Spectroscopic data confirmed inner-sphere complexation.
- Solution 31P NMR identified preferential binding of P1,3 and P2 phosphate groups at pH 5 and 8.5.
Conclusions:
- Phytic acid adsorption on ferrihydrite is a surface complexation process.
- Adsorption is strongly influenced by pH and ionic strength.
- Specific phosphate groups (P1, P2, P3) are most active in binding to ferrihydrite.
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