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通过对土壤提取物进行粒径分辨和元素特征分析来理解土壤硒的积累和生物可利用性。

Understanding soil selenium accumulation and bioavailability through size resolved and elemental characterization of soil extracts.

机构信息

Eawag, Swiss Federal Institute of Aquatic Science and Technology, Department of Water Resources and Drinking Water (W+T), Überlandstrasse 133, 8600, Dübendorf, Switzerland.

ETH Zurich, Swiss Federal Institute of Technology, Department of Environment Systems Sciences (D-USYS), Institute of Biogeochemistry and Pollutant Dynamics (IBP), Group of Inorganic Environmental Geochemistry, Universitätstrasse 16, 8092, Zurich, Switzerland.

出版信息

Nat Commun. 2022 Nov 15;13(1):6974. doi: 10.1038/s41467-022-34731-6.

Abstract

Dietary deficiency of selenium is a global health threat related to low selenium concentrations in crops. Despite the chemical similarity of selenium to the two more abundantly studied elements sulfur and arsenic, the understanding of its accumulation in soils and availability for plants is limited. The lack of understanding of soil selenium cycling is largely due to the unavailability of methods to characterize selenium species in soils, especially the organic ones. Here we develop a size-resolved multi-elemental method using liquid chromatography and elemental mass spectrometry, which enables an advanced characterization of selenium, sulfur, and arsenic species in soil extracts. We apply the analytical approach to soils sampled along the Kohala rainfall gradient on Big Island (Hawaii), which cover a large range of organic carbon and (oxy)hydroxides contents. Similarly to sulfur but contrarily to arsenic, a large fraction of selenium is found associated with organic matter in these soils. However, while sulfur and arsenic are predominantly found as oxyanions in water extracts, selenium mainly exists as small hydrophilic organic compounds. Combining Kohala soil speciation data with concentrations in parent rock and plants further suggests that selenium association with organic matter limits its mobility in soils and availability for plants.

摘要

饮食中硒的缺乏是一个全球性的健康威胁,这与农作物中硒浓度低有关。尽管硒在化学上与两种研究得更为充分的元素硫和砷相似,但人们对其在土壤中的积累及其对植物的有效性的了解是有限的。对土壤硒循环的理解不足在很大程度上是由于缺乏用于表征土壤中硒形态的方法,特别是有机硒形态的方法。在这里,我们开发了一种使用液相色谱和元素质谱的按粒径区分的多元素方法,该方法能够对土壤提取物中的硒、硫和砷形态进行高级表征。我们将该分析方法应用于在夏威夷大岛的 Kohala 降雨梯度上采集的土壤样本,这些土壤样本涵盖了很大范围的有机碳和(氧)氢氧化物含量。与硫类似,但与砷相反,这些土壤中很大一部分硒与有机物有关。然而,虽然硫和砷主要以含氧阴离子的形式存在于水提取物中,但硒主要以小的亲水性有机化合物的形式存在。将 Kohala 土壤形态数据与母岩和植物中的浓度相结合,进一步表明,硒与有机物的结合限制了其在土壤中的迁移性和对植物的有效性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6b74/9666626/acd36a31461b/41467_2022_34731_Fig1_HTML.jpg

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