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在非饱和土壤的根际中富集水铁矿可提高养分保留能力,同时限制砷和铀的植物吸收。

Ferrihydrite enrichment in the rhizosphere of unsaturated soil improves nutrient retention while limiting arsenic and uranium plant uptake.

机构信息

Nebraska Water Center, part of the Robert B. Daugherty Water for Food Global Institute, Water Sciences Laboratory, University of Nebraska, Lincoln, NE 68583-0844, United States.

Nebraska Water Center, part of the Robert B. Daugherty Water for Food Global Institute, Water Sciences Laboratory, School of Natural Resources, University of Nebraska, Lincoln, NE 68583-0844, United States.

出版信息

Sci Total Environ. 2022 Feb 1;806(Pt 4):150967. doi: 10.1016/j.scitotenv.2021.150967. Epub 2021 Oct 14.

Abstract

Improvement of nutrient use efficiency and limiting trace elements such as arsenic and uranium bioavailability is critical for sustainable agriculture and food safety. Arsenic and uranium possess different properties and mobility in soils, which complicates the effort to reduce their uptake by plants. Here, we postulate that unsaturated soil amended with ferrihydrite nanominerals leads to improved nutrient retention and helps reduce uptake of these geogenic contaminants. Unsaturated soil is primarily oxic and can provide a stable environment for ferrihydrite nanominerals. To demonstrate the utility of ferrihydrite soil amendment, maize was grown in an unsaturated agricultural soil that is known to contain geogenic arsenic and uranium. The soil was maintained at a gravimetric moisture content of 15.1 ± 2.5%, typical of periodically irrigated soils of the US Corn Belt. Synthetic 2-line ferrihydrite was used in low doses as a soil amendment at three levels (0.00% w/w (control), 0.05% w/w and 0.10% w/w). Further, the irrigation water was fortified (~50 μg L each) with elevated arsenic and uranium levels. Plant dry biomass at maturity was ~13.5% higher than that grown in soil not receiving ferrihydrite, indicating positive impact of ferrihydrite on plant growth. Arsenic and uranium concentrations in maize crops (root, shoot and grain combined) were ~ 20% lower in amended soils than that in control soils. Our findings suggest that the addition of low doses of iron nanomineral soil amendment can positively influence rhizosphere geochemical processes, enhancing nutrient plant availability and reduce trace contaminants plant uptake in sprinkler irrigated agroecosystem, which is 55% of total irrigated area in the United States.

摘要

提高养分利用效率和限制砷和铀等微量元素的生物可利用性对于可持续农业和食品安全至关重要。砷和铀在土壤中的性质和迁移性不同,这增加了减少其被植物吸收的难度。在这里,我们假设用铁水羟化物纳米矿物改良不饱和土壤会导致养分保留得到改善,并有助于减少这些地质污染物的吸收。不饱和土壤主要是氧化的,可以为铁水羟化物纳米矿物提供稳定的环境。为了证明铁水羟化物土壤改良剂的实用性,我们在一种已知含有地质砷和铀的不饱和农业土壤中种植了玉米。土壤的重量含水量保持在 15.1±2.5%,这是美国玉米带定期灌溉土壤的典型含水量。我们以低剂量将合成的 2 线铁水羟化物用作土壤改良剂,添加水平为三个等级(0.00%w/w(对照)、0.05%w/w 和 0.10%w/w)。此外,灌溉水中还添加了砷和铀的含量(各约 50μg/L)。在成熟时,植物的干生物量比不接受铁水羟化物的土壤中生长的植物高出约 13.5%,这表明铁水羟化物对植物生长有积极影响。在改良土壤中,玉米作物(根、茎和谷物合计)中的砷和铀浓度比对照土壤中的浓度低约 20%。我们的研究结果表明,添加低剂量的铁纳米矿物土壤改良剂可以积极影响根际地球化学过程,增强养分的植物可用性,并减少在喷灌农业生态系统中植物对痕量污染物的吸收,美国总灌溉面积的 55%为喷灌。

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