The Monomolecular-Layer Selective Adsorption of Amino Acids on Microbial Proto-Dolomite Induced by the Cyanobacterium Leptolyngbya Boryana

IF 2.9 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY
Yanyang Zhao, Yishui Han, Xiao Gao, Xiangyu Wei, Chao Han, Zhaopeng Wang, Karim Benzerara, Maurice E. Tucker and Zuozhen Han*, 
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Abstract

Microbially mediated mineralization is widely recognized as a key pathway for proto-dolomite formation, with extracellular polymeric substances (EPS), especially amino acids, considered important mediators. Yet, the surface interactions between amino acids and proto-dolomite remain insufficiently characterized. In this study, we examined the adsorption behavior of four representative amino acids─aspartic acid (Asp), arginine (Arg), glycine (Gly), and proline (Pro)─on organic-free proto-dolomite (Cpdol) synthesized by the cyanobacterium Leptolyngbya boryana. Experiments were conducted across a range of pH and salinity conditions, and amino acid concentrations were measured using high-performance liquid chromatography. The adsorption data were well described by Langmuir isotherms, indicating a monomolecular-layer selective adsorption model. Adsorption capacity varied among amino acids (Asp > Gly > Pro > Arg) and showed a positive correlation with pH and a negative correlation with salinity. Based on density functional theory (DFT) calculations, the adsorption energies of the four amino acids were evaluated on seven crystal surfaces of proto-dolomite. The results indicate that surface complexation between carboxyl groups and surface metal ions is the primary mechanism driving adsorption. Under higher pH conditions, the deprotonated amino group can further enhance adsorption by lowering the adsorption energy. These findings suggest that, beyond acidic amino acids, surface complexation of various environmentally responsive amino acids may play an important role in regulating the early-stage formation of proto-dolomite in microbial environments.

Abstract Image

蓝细菌诱导原白云岩上氨基酸的单分子层选择性吸附
微生物介导的矿化被广泛认为是原白云岩形成的关键途径,细胞外聚合物质(EPS),特别是氨基酸,被认为是重要的介质。然而,氨基酸与原白云岩之间的表面相互作用仍然没有充分的表征。在这项研究中,我们研究了四种具有代表性的氨基酸──天冬氨酸(Asp)、精氨酸(Arg)、甘氨酸(Gly)和脯氨酸(Pro)──在蓝细菌合成的无有机原白云石(Cpdol)上的吸附行为。实验在一系列pH和盐度条件下进行,并使用高效液相色谱法测量氨基酸浓度。Langmuir等温线很好地描述了吸附数据,表明其为单分子层选择性吸附模型。不同氨基酸的吸附量不同(Asp >;通用电气的在专业的在Arg),与pH呈正相关,与盐度负相关。基于密度泛函理论(DFT)计算,计算了4种氨基酸在原白云岩7个晶面上的吸附能。结果表明,羧基与表面金属离子之间的表面络合是驱动吸附的主要机制。在较高的pH条件下,去质子化的氨基可以通过降低吸附能进一步增强吸附。这些发现表明,除了酸性氨基酸外,各种环境响应氨基酸的表面络合可能在微生物环境中调节原始白云岩的早期形成中起重要作用。
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来源期刊
ACS Earth and Space Chemistry
ACS Earth and Space Chemistry Earth and Planetary Sciences-Geochemistry and Petrology
CiteScore
5.30
自引率
11.80%
发文量
249
期刊介绍: The scope of ACS Earth and Space Chemistry includes the application of analytical, experimental and theoretical chemistry to investigate research questions relevant to the Earth and Space. The journal encompasses the highly interdisciplinary nature of research in this area, while emphasizing chemistry and chemical research tools as the unifying theme. The journal publishes broadly in the domains of high- and low-temperature geochemistry, atmospheric chemistry, marine chemistry, planetary chemistry, astrochemistry, and analytical geochemistry. ACS Earth and Space Chemistry publishes Articles, Letters, Reviews, and Features to provide flexible formats to readily communicate all aspects of research in these fields.
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