Department of Ecosystem Science and Management , University of Wyoming , Laramie , Wyoming 82071 , United States.
Department of Life & Environmental Sciences and Sierra Nevada Research Institute , University of California , Merced , California 95343 , United States.
Environ Sci Technol. 2020 Feb 18;54(4):2257-2267. doi: 10.1021/acs.est.9b05278. Epub 2020 Jan 28.
Sequential chemical extraction has been widely used to study soil phosphorus (P) dynamics and inform nutrient management, but its efficacy for assigning P into biologically meaningful pools remains unknown. Here, we evaluated the accuracy of the modified Hedley extraction scheme using P K-edge X-ray absorption near-edge structure (XANES) spectroscopy for nine carbonate-free soil samples with diverse chemical and mineralogical properties resulting from different degrees of soil development. For most samples, the extraction markedly overestimated the pool size of calcium-bound P (Ca-P, extracted by 1 M HCl) due to (1) P redistribution during the alkaline extractions (0.5 M NaHCO and then 0.1 M NaOH), creating new Ca-P via formation of Ca phosphates between NaOH-desorbed phosphate and exchangeable Ca and/or (2) dissolution of poorly crystalline Fe and Al oxides by 1 M HCl, releasing P occluded by these oxides into solution. The first mechanism may occur in soils rich in well-crystallized minerals and exchangeable Ca regardless of the presence or absence of CaCO, whereas the second mechanism likely operates in soils rich in poorly crystalline Fe and Al minerals. The overestimation of Ca-P simultaneously caused underestimation of the pools extracted by the alkaline solutions. Our findings identify key edaphic parameters that remarkably influenced the extractions, which will strengthen our understanding of soil P dynamics using this widely accepted procedure.
连续化学提取已广泛用于研究土壤磷(P)动态并为养分管理提供信息,但它将 P 分配到具有生物学意义的库中的效果尚不清楚。在这里,我们使用 P K 边 X 射线吸收近边结构(XANES)光谱评估了改良 Hedley 提取方案的准确性,该方案用于研究 9 个无碳酸盐土壤样本,这些样本具有不同的化学和矿物特性,源于不同程度的土壤发育。对于大多数样本,由于(1)碱性提取过程中的 P 再分配(用 0.5 M NaHCO3 提取,然后用 0.1 M NaOH),通过在 NaOH 解吸的磷酸盐和可交换的 Ca 之间形成 Ca 磷酸盐,从而创建新的 Ca-P,以及(2)1 M HCl 溶解了结晶度较差的 Fe 和 Al 氧化物,将这些氧化物中包含的 P 释放到溶液中,提取 1 M HCl 时显著高估了钙结合磷(Ca-P)的库大小。第一种机制可能发生在富含结晶良好的矿物和可交换 Ca 的土壤中,无论是否存在 CaCO3,而第二种机制可能发生在富含结晶度较差的 Fe 和 Al 矿物的土壤中。对 Ca-P 的高估同时导致对碱性溶液提取的库的低估。我们的发现确定了显著影响提取的关键土壤参数,这将增强我们对使用这种广泛接受的程序的土壤 P 动态的理解。