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铁膜在水稻(Oryza sativa L.)根中砷和镉积累中的作用的新见解。

A new insight into the role of iron plaque in arsenic and cadmium accumulation in rice (Oryza sativa L.) roots.

机构信息

Chongqing Vocational Institute of Engineering, Chongqing 402260, China.

Institute of Soil and Fertilizer, Guizhou Academy of Agricultural Sciences, Guiyang 550006, China.

出版信息

Ecotoxicol Environ Saf. 2023 Apr 1;254:114714. doi: 10.1016/j.ecoenv.2023.114714. Epub 2023 Mar 6.

Abstract

Iron plaque, naturally iron-manganese (hydr)oxides adhered to the surface of rice roots, controls the sequestration and accumulation of arsenic (As) and cadmium (Cd) in the paddy soil-rice system. However, the effects of the paddy rice growth on the iron plaque formation and As and Cd accumulation of rice roots are often neglected. This study explores the distribution characteristics of iron plaques on rice roots and their effects on As and Cd sequestration and uptake via cutting the rice roots into 5 cm segments. Results indicated that the percentages of rice root biomass of 0-5 cm, 5-10 cm, 10-15 cm, 15-20 cm, and 20-25 cm are 57.5 %, 25.2 %, 9.3 %, 4.9 %, and 3.1 %, respectively. Iron (Fe) and manganese (Mn) concentrations in iron plaques on rice roots of various segments are 41.19-81.11 g kg and 0.94-3.20 g kg, respectively. Increased tendency of Fe and Mn concentrations from the proximal rice roots to the distal rice roots show that iron plaque is more likely to deposit on the distal rice roots than proximal rice roots. The DCB-extractable As and Cd concentrations of rice roots with various segments are 694.63-1517.23 mg kg and 9.00-37.58 mg kg, displaying a similar trend to the distribution characteristics of Fe and Mn. Furthermore, the average transfer factor (TF) of As (0.68 ± 0.26) from iron plaque to rice roots was significantly lower than that of Cd (1.57 ± 0.19) (P < 0.05). There was a significant positive correlation between the Cd sequestration in iron plaque and the Cd accumulation in rice roots (R = 0.97, P < 0.01). Still, a similar correlation wasn't observed between As sequestration in iron plaque and As accumulation in rice roots (R = -0.04, and P > 0.05). These results indicated that the formed iron plaque might act as a barrier to As uptake by rice roots and a facilitator to Cd uptake. This study provides insight into the role of iron plaque in the sequestration and uptake of As and Cd in paddy soil-rice systems.

摘要

铁斑块,即天然铁锰(水合)氧化物附着在水稻根表面,控制着砷(As)和镉(Cd)在稻田土壤-水稻系统中的固持和积累。然而,水稻生长对铁斑块形成以及水稻根中砷和镉积累的影响往往被忽视。本研究通过将水稻根切成 5cm 段,探讨了铁斑块在水稻根上的分布特征及其对砷和镉固持和吸收的影响。结果表明,0-5cm、5-10cm、10-15cm、15-20cm 和 20-25cm 长度的水稻根生物量百分比分别为 57.5%、25.2%、9.3%、4.9%和 3.1%。不同段水稻根铁斑块中的铁(Fe)和锰(Mn)浓度分别为 41.19-81.11gkg 和 0.94-3.20gkg。从水稻根近端到远端,Fe 和 Mn 浓度呈增加趋势,表明铁斑块更容易在水稻根远端沉积。不同段水稻根中 DCB 可提取的 As 和 Cd 浓度分别为 694.63-1517.23mgkg 和 9.00-37.58mgkg,呈现出与 Fe 和 Mn 分布特征相似的趋势。此外,As 从铁斑块向水稻根的平均转移因子(TF)(0.68±0.26)显著低于 Cd(1.57±0.19)(P<0.05)。铁斑块中 Cd 的固持量与水稻根中 Cd 的积累量呈显著正相关(R=0.97,P<0.01)。然而,铁斑块中 As 的固持量与水稻根中 As 的积累量之间没有观察到类似的相关性(R=-0.04,P>0.05)。这些结果表明,形成的铁斑块可能成为水稻根吸收 As 的障碍,而成为 Cd 吸收的促进剂。本研究为铁斑块在稻田土壤-水稻系统中砷和镉的固持和吸收中的作用提供了新的见解。

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