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土壤中有机物的原子尺度建模:有机分子和生物聚合物在羟基化α-AlO(0001)表面的吸附。

Atomic-scale modelling of organic matter in soil: adsorption of organic molecules and biopolymers on the hydroxylated α-AlO (0001) surface.

机构信息

Department of Chemistry, University of Sheffield, Sheffield, UK.

出版信息

Philos Trans A Math Phys Eng Sci. 2023 Jul 10;381(2250):20220254. doi: 10.1098/rsta.2022.0254. Epub 2023 May 22.

Abstract

Binding of organic molecules on oxide mineral surfaces is a key process which impacts the fertility and stability of soils. Aluminium oxide and hydroxide minerals are known to strongly bind organic matter. To understand the nature and strength of sorption of organic carbon in soil, we investigated the binding of small organic molecules and larger polysaccharide biomolecules on α-AlO (corundum). We modelled the hydroxylated α-AlO (0001) surface, since these minerals' surfaces are hydroxylated in the natural soil environment. Adsorption was modelled using density functional theory (DFT) with empirical dispersion correction. Small organic molecules (alcohol, amine, amide, ester and carboxylic acid) were found to adsorb on the hydroxylated surface by forming multiple hydrogen bonds with the surface, with carboxylic acid as the most favourable adsorbate. A possible route from hydrogen-bonded to covalently bonded adsorbates was demonstrated, through co-adsorption of the acid adsorbate and a hydroxyl group to a surface aluminium atom. Then we modelled the adsorption of biopolymers, fragments of polysaccharides which naturally occur in soil: cellulose, chitin, chitosan and pectin. These biopolymers were able to adopt a large variety of hydrogen-bonded adsorption configurations. Cellulose, pectin and chitosan could adsorb particularly strongly, and therefore are likely to be stable in soil. This article is part of a discussion meeting issue 'Supercomputing simulations of advanced materials'.

摘要

氧化物矿物表面的有机分子结合是一个关键过程,它影响着土壤的肥力和稳定性。氧化铝和氢氧化物矿物被认为能强烈结合有机物。为了了解土壤中有机碳的吸附性质和强度,我们研究了小分子有机分子和较大的多糖生物分子在α-AlO(刚玉)上的结合。我们模拟了羟基化的α-AlO(0001)表面,因为这些矿物的表面在自然土壤环境中是羟基化的。吸附是通过使用经验色散校正的密度泛函理论(DFT)进行建模的。我们发现小分子(醇、胺、酰胺、酯和羧酸)通过与表面形成多个氢键而吸附在羟基化表面上,其中羧酸是最有利的吸附物。通过吸附酸吸附物和一个羟基到表面铝原子上,我们展示了从氢键吸附物到共价键吸附物的可能途径。然后,我们模拟了生物聚合物的吸附,生物聚合物是土壤中天然存在的多糖片段:纤维素、几丁质、壳聚糖和果胶。这些生物聚合物能够采用多种氢键吸附构型。纤维素、果胶和壳聚糖能够特别强烈地吸附,因此在土壤中可能很稳定。本文是关于“高级材料的超级计算模拟”讨论会议的一部分。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0221/10200349/5be2098d4aeb/rsta20220254f01.jpg

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