土壤中铁的异质性及其与水叶(Talinum Triangulaire L.)吸收铁的关系

Ogunlade-Anibasa, G.O., Aniki, S.O., Ameh, P.T., .. Igwemmar, N.C
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摘要

本研究调查了土壤中铁(Fe)的异质性与水叶(Talinum triangulaire)对铁的吸收之间的关系。在温室盆栽实验中,水叶在三种处理下生长,即对照(添加 0mg/kg 铁)、均质(添加 1000mg/kg 铁)和异质(模拟现实异质),在苗圃中初始生长四周后再生长六周。)收获时,植物样本经切割、清洗、干燥、碾磨成粉末,用硝酸(HNO3)酸解后,使用原子吸收光谱仪(AAS)Thermos Fisher Scientific Model 3000 ICE 分析铁的浓度。对照组、同质处理和异质处理的根部铁平均浓度分别为 1263 ±154mg/kg、1504 ±178mg/kg和 1393mg/kg ±140mg/kg。对照、同质处理和异质处理的嫩枝铁平均浓度分别为 904 ±174u mg/kg、1401±117 mg/kg 和 1045 ±95 mg/kg。不同处理之间的芽和根铁浓度差异无统计学意义(P >0.005)。然而,同质处理比对照高 0.19 倍,比异质处理高 0.07 倍。 根中的铁含量是对照的 0.35 倍,是异质处理的 0.25 倍。对照组、同质处理和异质处理的浓度系数分别为 0.1118、0.1498 和 0.1258。不同处理之间浓度系数的相似性表明,无论土壤浓度如何变化,水叶都是铁的积累者,对铁具有亲和力。这些发现表明,水叶具有从不同土壤条件中高效获取铁元素的机制。总之,这项研究提供了初步证据,证明水叶对土壤中铁的分布变化有很强的适应能力,这对改进水叶的栽培具有重要意义。不过,建议进一步研究水叶中管理铁动员和吸收的特定基因和过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Iron Heterogeneity in Soil and its Relation to its Uptake by Water Leaf (Talinum Triangulaire L.)
This study investigated the relationship between iron (Fe) heterogeneity in soil and Fe uptake by water leaf (Talinum triangulaire). A greenhouse pot experiment was conducted with water leaf grown under three treatments; control (0mg/kg Fe added), homogeneous (1000mg/kg Fe added), and heterogeneous (simulated realistic heterogeneity) for six weeks after initial establishment in the nursery for four weeks). At harvest, plant samples were cut, washed, dried, milled into powder and analyzed for iron concentrations using the Atomic Absorption Spectrometer (AAS) Thermos Fisher Scientific Model 3000 ICE after acid digest by Nitric acid (HNO3). The mean root Fe concentrations of the control, homogeneous and heterogeneous treatments were 1263 ±154mg/kg, 1504 ±178mg/kg and 1393mg/kg ±140mg/kg respectively. The mean shoot Fe concentrations of the control, homogeneous and heterogeneous treatments were 904 ±174u mg/kg, 1401±117 mg/kg and 1045 ±95 mg/kg respectively. There was no statistically significant difference (p >0.005) in shoot and root Fe concentration between treatments. However, the homogeneous treatment was 0.19 times higher than the control and 0.07 times higher than the heterogeneous treatment.  Iron level in the roots was 0.35 times high as the control and 0.25 times higher than the heterogeneous treatment. The Concentration factors for the control, homogeneous, and heterogeneous treatments were 0.1118, 0.1498 and 0.1258 respectively. The similarity in concentration factor between treatments showed that it is an accumulator of Fe and has the affinity for Fe irrespective of the varied soil concentrations. These findings indicate that water leaf possesses mechanisms enabling efficient Fe acquisition from variable soil conditions. Overall, the study provides initial evidence that water leaf is resilient to variability in soil Fe distribution, holding implications for its improved cultivation. However, further research on the specific genes and processes governing iron mobilization and uptake in water leaf is recommended.
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