X-ray absorption spectroscopy and theoretical investigations of the effect of extended ligands in potassium organic matter interaction

被引:1
|
作者
Richardson, Jocelyn A. [1 ]
Kim, Hoshin [2 ]
Kas, Joshua J. [3 ]
You, Xiao [1 ]
Andersen, Amity [4 ]
Ginovska, Bojana [2 ]
Bhattacharjee, Arunima [4 ]
Sarangi, Ritimukta [1 ]
机构
[1] SLAC Natl Accelerator Lab, Stanford Synchrotron Radiat Lightsource, 2575 Sand Hill Rd, Menlo Pk, CA 94025 USA
[2] Pacific Northwest Natl Lab, Phys Sci Div, Phys & Computat Sci Directorate, 902 Battelle Blvd, Richland, WA 99354 USA
[3] Univ Washington Seattle, Dept Phys, Box 351560, Seattle, WA 98195 USA
[4] Pacific Northwest Natl Lab, Environm Mol Sci Div, Earth & Biol Sci Directorate, 3335 Innovat Blvd, Richland, WA 99354 USA
来源
JOURNAL OF CHEMICAL PHYSICS | 2024年 / 160卷 / 04期
基金
美国国家卫生研究院;
关键词
ECTOMYCORRHIZAL FUNGI; MOLECULAR-DYNAMICS; MG2+ DEFICIENCY; OXALIC-ACID; BASIS-SETS; ATOMS; PHLOGOPITE; PARAMETERS; CATALYSTS; MINERALS;
D O I
10.1063/5.0183603
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Potassium (K) is an essential nutrient for plant growth, and despite its abundance in soil, most of the K is structurally bound in minerals, limiting its bioavailability and making this soil K reservoir largely inaccessible to plants. Microbial biochemical weathering has been shown to be a promising pathway to sustainably increase plant available K. However, the mechanisms underpinning microbial K uptake, transformation, storage, and sharing are poorly resolved. To better understand the controls on microbial K transformations, we performed K K-edge x-ray absorption near-edge structure (XANES) spectroscopy on K-organic salts, including acetate, citrate, nitrate, oxalate, and tartrate, which are frequently observed as low molecular weight organic acids secreted by soil microbes, as well as humic acid, which acts as a proxy for higher molecular weight organic acids. The organic salts display feature-rich K XANES spectra, each demonstrating numerous unique features spanning similar to 13 eV range across the absorption edge. In contrast, the spectra for humic acid have one broad, wide feature across the same energy range. We used a combination of time-dependent density functional theory and the Bethe-Salpeter equation based approach within the OCEAN code to simulate the experimental spectra for K-nitrate (KNO3) and K-citrate [K-3(C6H5O7)<middle dot>H2O] to identify the electronic transitions that give rise to some of the outlying and unique spectral features in the organic salts. KNO3 has both the lowest and highest lying energy features, and K-3(C6H5O7)<middle dot>H2O is produced by several soil microbes and is effective at mineral weathering. Our results analyze the K-organic salt bonding in detail to elucidate why the spectral shapes differ and indicate that the K K-edge XANES spectra are associated with the entire ligand despite similar first-shell bonding environments around the K center. The improved understanding of K bonding environments with organic ligands and their use for interpretation of the K-XANES spectra provides an important toolkit to understand how K is transformed by microbial processes and made bioavailable for plant uptake.
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页数:12
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