Campus Units

Ecology, Evolution and Organismal Biology

Document Type

Article

Publication Version

Accepted Manuscript

Publication Date

11-15-2017

Journal or Book Title

Geoderma

Volume

306

First Page

67

Last Page

72

DOI

10.1016/j.geoderma.2017.07.013

Abstract

Iron (Fe) redox cycling and sorption/complexation reactions influence numerous soil biogeochemical processes, and the precise, rapid, and low-cost determination of reactive Fe pools is critical for understanding these dynamics. Colorimetric methods are often used to measure Fe, yet assay conditions vary widely among studies, and the robustness of these methods and their potential interferences remain poorly characterized. Here, we developed optimized ferrozine methods (modified from water and sediment protocols) to determine Fe concentrations in three common soil extractions: reduced (Fe(II)) and oxidized Fe (Fe(III)) in 0.5M HCl (FeHCl), and Fe extracted by citrate-ascorbate (Feca) and citrate-dithionite (Fecd). These methods were adapted for 96-well microplates by employing increased buffer concentrations and longer incubation times relative to published cuvette methods. Iron quantitation was sensitive to the final pH of the reaction mixture and duration of incubation period, factors that have varied widely in previous studies. We obtained consistent results with an assay pH near 7, half hour incubations for FeHCl, and one hour incubations for Feca and Fecd. These ferrozine methods compared favorably with inductively coupled plasma optical emission spectrometry (ICP-OES) across a broad range of soils, including Oxisols, Mollisols, and Inceptisols with as much as 18% organic C. Iron determination in HCl extractions from 158 tropical forest soil samples with widely varying C content was not influenced by dissolved organic carbon (DOC) or phenolics at lower Fe concentrations (< 2.5 mg g-1 soil), and showed only minor effects (< 6% overestimation) at higher Fe concentrations. This was likely due to co-variation between Fe and DOC, which measured as high as 691 mg C l-1 in a cloud forest soil extract. These microplate-based ferrozine methods can be applied to quantify several reactive soil Fe phases with high precision and throughput, minimal interference, and low cost relative to ICP-OES.

Comments

This is a manuscript of an article published as Huang, Wenjuan, and Steven J. Hall. "Optimized high-throughput methods for quantifying iron biogeochemical dynamics in soil." Geoderma 306 (2017): 67-72. doi: 10.1016/j.geoderma.2017.07.013. Posted with permission.

Creative Commons License

Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License
This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License.

Copyright Owner

Elsevier B.V.

Language

en

File Format

application/pdf

Available for download on Friday, November 15, 2019

Published Version

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