Forms and Lability of Phosphorus in Humic Acid Fractions of Hord Silt Loam Soil

Phosphorus has long been known to be present in soil humic fractions, but little is known about specific P forms in humic fractions or their lability. We extracted the mobile humic acid (MHA) and recalcitrant calcium humate (CaHA) fractions from a Nebraska Hord silt loam soil (a fine‐silty, mixed, superactive, mesic Cumulic Haplustoll) under continuous corn ( Zea mays L.) receiving either inorganic fertilizer or animal manure. Solution 31 P nuclear magnetic resonance spectroscopy demonstrated that P in both MHA and CaHA was predominantly present in organic forms, mostly as orthophosphate monoesters. Spiking experiments indicated no phytate present in these humic fractions, but scyllo ‐inositol P was identified in all samples. Potato phosphatase hydrolyzed some humic‐bound P. Fungal phytase released more humic‐bound P, which may come from scyllo ‐inositol P. No additional P was released by including nuclease. Ultraviolet (UV) irradiation increased soluble inorganic P in MHA fractions, but total hydrolyzable P in MHA fractions did not increase, suggesting that the portion of P that was UV labile was also enzymatically hydrolyzable. In contrast, UV irradiation increased soluble inorganic P and total hydrolyzable P in CaHA fractions, which suggests that UV‐labile P in CaHA fractions did not overlap with enzymatically hydrolyzable P. Fertilization management did not significantly alter the lability of humic P in these humic fractions. This research has the potential to improve P management by increasing our knowledge of P lability for more efficient crop uptake.