土壤-植物系统中稀土元素与氮磷养分的交互作用

土壤－植物系统中稀土元素与N,P养分交互作用属农田稀土安全性评价研究的前沿,土壤中稀土元素与N,P交互作用直接关系到稀土对农田土壤生产力的影响以及稀土对农作物的增产机理和生态环境安全性的评价,就土壤－植物系统中有关稀土元素与N,P交互作用的研究作简要综述,提出今后应加强作物根际,农田土壤表层以及植物体内稀土与N,P养分之间交互作用的研究。     

稀土元素对农田生态系统的影响研究进展

稀土矿的开采和冶炼、稀土农用等导致农田土壤稀土元素含量不断积累,对农田生态系统结构和功能稳定产生严重的影响。综述了近20年来国内外农田生态系统稀土元素的主要来源、分配和输出,土壤和植物中稀土元素的测定方法,稀土元素对农田生态系统中植物、微生物、动物以及人类健康影响的研究进展。探讨了农田生态系统稀土元素的毒性评价和稀土污染土壤的修复措施。最后提出开展稀土元素对农田生态系统影响研究还需要加强的一些问题。     

长期喷施稀土对土壤-植物(小麦)系统中稀土元素分布、累积及运移的影响

在我国施用稀土时间最长的黑龙江省花园农场,研究比较了施用稀土12 a和不施稀土的对照处理上小麦和土壤中的稀土元素的分布、累积及运移.结果表明,长期叶面喷施稀土并未造成耕层土壤和下部土层的稀土元素的累积.成熟期小麦植株各部位的稀土元素含量顺序为根>叶>茎、壳;稀土元素主要累积在根部,其次是叶,茎和壳累积较少.喷施处理小麦根部的稀土元素累积量高于对照,叶部也有此趋势,而茎、壳等部位差异不大.根、茎、叶、壳稀土元素分布模式与土壤中相似,与施用的常乐稀土差别较大;长期喷施稀土未曾造成籽粒中稀土元素的明显累积.     

长期施用稀土对小麦植株中稀土元素含量及分布的影响

在我国施用稀土时间最长的黑龙江花园农场,研究了连续１２ａ叶面喷施稀土对小麦植株及土壤中稀土元素总含量和分布模式的影响。结果表明：连续１２ａ叶施稀土没有造成土壤中元素含量及分布模式的变化;对小麦拔节始期（喷施稀土７ｄ）后叶部的影响较大,Ｌａ,Ｃｅ最明显增高,叶部稀土元素分布模式与“常乐”稀土中的相一致,与土壤中稀土元素分布模式不同,而在小麦拔节始期的根部、小麦成熟期的根、茎、叶、壳等部位稀土元素分布     

稀土离子与Ca~(2 )在生物体内的相互作用机制及应用

稀土元素在生物领域内的研究,可以分为两个方面：稀土的生物效应和稀土在其它研究中的应用．稀土元素的生物效应,主要集中在动物和医学领域．由于稀土元素的离子半径及化学性质和钙离子很相似,因此在研究稀土的生物效应时,对稀土离子与钙离子的关系颇为重视．稀土作为一种特殊的研究工具,在许多生物学研究领域中,克服了一些因其它方法的局限而不能得到的结果或简化了其中的过程．     

镧暴露对鲤鱼脑和肌肉中酶和脂质过氧化水平的影响

稀土元素是镧系元素和钇、钪两种元素的统称。自20世纪70年代人们揭示了稀土元素的作用效果后,稀土元素已被广泛应用于农、畜牧及水产养殖业。农业上适当使用微量稀土,能促进植物生长发育,作物增产。饲料里添加稀土,能促进畜、禽和水产养殖动物的生长,提高饲料利用率等。但随着稀土元素的广泛应用,必定导致大量的可溶性稀土进入水生生态环境,因此研究稀土对水体的影响,特别是对水生动植物有机体的长期潜在影响,将显得极为重要。过氧化物酶（POD）、超氧化物歧化酶（SOD）广泛存在于鱼体中,是鱼体抗氧化作用的重要酶类,过氧化脂质（LPO）含量反映着机体脂质过氧化物形成速率的强度,SOD、POD活性以及LPO含量都可以用来评价污染物对水生生物的影响。     

长期喷施稀土对土壤—植物（小麦）系统中稀土元素分布,累积及运移…

在我国施用稀土时间最长的黑龙江省花园农场,研究比较了施用稀土１２ａ和不施稀土的对照处理上小麦和土壤中的稀土元素的分布、累积及运移。结果表明,长 期叶面稀土未造成耕土壤和下部土层的稀土元素的累积,成熟期小麦植株各部的稀土元素含量顺序为根＞叶＞茎、壳;稀土元素主要累积在根部,其次是叶,茎和壳累积较少。喷施处理小麦根部的稀土元素累量高于对照,叶部也有此趋势,而茎,壳等部位差异不大。根、茎、叶、壳稀土元素     

稀土离子与Ca2+在生物体内的相互作用机制及应用

稀土元素在生物领域内的研究,可以分为两个方面：稀土的生物效应和稀土在其它研究中的应用。稀土元素的生物效应,集中在动物和医学领域。     

稀土抗菌效应及应用的研究进展

稀土元素具有多种生物效应, 除了对农作物的增产作用外, 在医药方面还具有抗菌的作用, 近年来, 不少学者针对稀土元素的抗菌效应展开了相关的研究。本文介绍了稀土在抗菌领域的研究及应用, 包括稀土化合物对微生物生长的Hormesis效应、稀土化合物与抗生素的协同作用、稀土配合物的合成、以及稀土在抗菌材料上的应用等几个方面的内容, 并对稀土化合物及其配合物的抗菌机理进行了探讨, 最后, 展望了稀土化合物及配合物在抗菌领域的应用前景及研究重要性。     

有机配体对稀土元素在小麦体内积累和分异的影响

采用营养液培养和添加外源混合稀土等方法,研究了有机配体柠檬酸、EDTA和DTPA对稀土元素在小麦的根和叶中积累与分异的影响。结果表明,低浓度有机配体对小麦根和叶中的稀土元素,尤其是轻稀土元素的积累有轻微的促进作用,随浓度的升高则表现出显著的降低作用。有机配体对重稀土的作用比轻稀土强,使根和叶中稀土元素的分布曲线向重稀土相对亏缺的方向发展。3种配体对轻、重稀土分异的作用强度为:EDTA>DTPA>柠檬酸。通过VM INTEQ计算表明,在EDTA和DTPA作用下小麦叶中稀土元素的积累与轻、重稀土的分异主要由溶液中呈自由离子态稀土元素的含量和组成控制;柠檬酸作用下小麦叶中稀土元素的变化与自由离子态稀土的含量和组成关系较弱,推测REE-柠檬酸络合物可被小麦直接吸收并运转到小麦的叶中。     

Microcalorimetric study of the effect of Ce(III) on metabolic activity of mitochondria isolated from indice rice 9311

Rare earth elements (REEs) have beneficial influence on plant growth and are widely used in agriculture practice, but little is known about behavior of the REEs on mitochondria in plant cells. Thermogenic metabolic curves were determined by the ampoule method at 303 K using a TAM air isothermal microcalorimeter in mitochondria isolated from indice rice 9311 (Oryza sativa L.), and the effect of Ce(III) on mitochondrial metabolism was investigated. By analyzing the obtained heat flux curves, the crucial parameters such as activity recovery rate constant (k) and maximum heat power (P(m)) were investigated. Application of Ce3+ in concentrations ranging from 0 to 120 microg/ml significantly increased k and P(m) values, with the maximum reaching 261 and 180% of the control, respectively. Concentrations from 140 to 150 microg/ml had the opposite effect. These results were consistent with previous reports on the effects of REEs on plant growth. It was concluded that the Ce(III)-induced change of mitochondrial metabolic activity is a possible mechanism by which Ce(III) influenced indice rice 9311 growth.     

Bioaccessibility and health risk assessment of rare earth elements in Porphyra seaweed species

In this study, the content and bioaccessibility of rare earth elements (REEs) in Porphyra spp. Samples before and after thermal treatments were investigated. Additionally, the risks of REEs exposure to human health were assessed. REEs content significantly reduced after thermal processing (P < 0.01), and the removal rate of REEs was approximately 30%. Thermal treatment increased REEs bioaccessibility from 44% to 64.34%. The concentration and bioaccessibility of Ce, La, Y, Nd were high in raw and thermally treated Porphyra samples, and there was no correlation between REEs content and bioaccessibility. Based on the following parameters: highest content of REEs in the studied seaweed samples (13.45 mg/kg), the highest daily seafood consumption (44.9 g/day), and the highest bioaccessibility (64.34%), the ratio of the calculated daily intake (DI) to daily allowable intake by diet (DAI_diet) of REEs did not exceed the reference value in rare earth mining areas or under extreme conditions. The DI via seafood consumption would be exceeded when the content of REEs in the seafood sample is greater than 15.77 mg/kg. In this study, the concentration of REEs did not exceed 15.77 mg/kg in any sample. Thus, the human health risks of REEs associated with seafood are low.     

稀土元素在赣南非稀土矿区和不同稀土矿区土壤-铁芒萁(Dicranopteris linearis)系统中的分布、累积和迁移

ICP-M法测定了江西赣南地区非稀土矿区和4处不同稀土矿区内,土壤-铁芒萁系统中15个稀土元素的含量,并对稀土元素在土壤剖面层及铁芒萁植物体内的分布、迁移特征进行了研究.结果表明,稀土元素总量在土壤剖面层的底土层含量最高,但表土层铈相对富集.稀土元素在铁芒萁植物体内的分布规律是叶、根＞茎＞叶柄.铁芒萁根中稀土元素的丰度与其母土表土层,尤其是母土表土层可溶态稀土元素的分布模式基本相似.稀土元素在铁芒萁体内的迁移过程中,发生了明显的分馏作用,茎、叶柄、叶中的重稀土相对贫乏.     

Bioaccumulation of rare earth elements in cultured hela cells

HeLa S-3 cells were grown in minimal essential medium supplemented with 10% calf serum and 1 mM L-glutamine without adding any rare earth elements (REEs). Exponentially growing cells were collected, and dried materials were used to analyze their REE content by inductively coupled plasma-mass spectrometry. The results showed that the cells accumulated REEs in individually different manners; namely the accumulation ratio was higher in the lighter REEs than in the heavier REEs. To deduce the implication of the accumulation of REEs in HeLa cells, the accumulation ratios for REEs were compared with those of other biologically important elements. It was seen that the accumulation ratios obtained for REEs (from 31.8 [Ce] to 14.7 [Lu]) were intermediate among those of many bioelements: Fe (124), Mg (54.5), K (38.8), Cr (12.7), Na (11.8), Mn (11.3), Zn (10.7), Ca (8.8), and V (6.7).     

Rare earth elements and relation between their potential bioavailability and soil properties, Nidda catchment (Central Germany)

Rare earth elements (REEs) are widely used in industry and the entry of REEs into the pedosphere is assumed. Data about REEs in soils are scarce since only a few studies discuss their ecologically relevant behavior. Hence, we investigated total contents (aqua regia digestion) and potentially bioavailable contents (EDTA extraction) of REEs in soils from the Nidda catchment in Hesse (Central Germany). The study site covers a 1,600 km² sized area and 232 soil samples from 63 soil profiles were examined. The total REE content varied considerably, ranging from 544 mg kg^?1 to 41 mg kg^?1 (mean 201.1 mg kg^?1) with a high proportion of light REEs. Highest REE contents were found in the soilscape VB, followed by LVB, WNE, T, WSW and BF with the smallest concentrations. With respect to the parent material the contents decreased in the following order: basalt > clay slate > loess > sandstone. On average 15.9% of the total REEs belong to the potentially bioavailable fraction. They range greatly by a factor of 100, between 1.3 and 171.3 mg kg^?1 (average 33.5 mg kg^?1). Remarkably, Yttrium has a maximum available proportion of 75%. In contrast, Ce showed the highest total contents with the smallest potentially bioavailable proportion of all elements. Regression analyses established relation between soil properties and the potential bioavailability of REEs. Around 53% (range from 29.9 to 76.8%) of the REE’s potential bioavailability variations could be explained by the chosen variables (pH, clay and C_org contents and the total element concentrations). Occurrence patterns and concentrations of REEs lie within the range of the results found in the available literature. Bioavailability is linked to soil properties and varies greatly according to the individual element. In comparison with the chosen soil properties the pH value shows the least impact on bioavailability.     

Accumulation and fractionation of rare earth elements (REEs) in the naturally grown Phytolacca americana L. in southern China

The widespread use of rare earth elements (REEs) has resulted in problems for soil and human health. Phytolacca americana L. is a herbaceous plant widely distributed in Dingnan county of Jiangxi province, China, which is a REE mining region (ion absorption rare earth mine) and the soil has high levels of REEs. An investigation of REE content of P. americana growing naturally in Dingnan county was conducted. REE concentrations in the roots, stems, and leaves of P. americana and in their rhizospheric soils were determined. Results showed that plant REEs concentrations varied among the sampling sites and can reach 1040 mg/kg in the leaves. Plant REEs concentrations decreased in the order of leaf > root > stem and all tissues were characterized by a light REE enrichment and a heavy REE depletion. However, P. americana exhibited preferential accumulation of light REEs during the absorption process (from soil to root) and preferential accumulation of heavy REEs during the translocation process (from stem to leaf). The ability of P. americana to accumulate high REEs in the shoot makes it a potential candidate for understanding the absorption mechanisms of REEs and for the phytoremediation of REEs contaminated soil.     

Fractionations of rare earth elements in plants and their conceptive model

Fractionations of rare earth elements (REEs) and their mechanisms in soybean were studied through application of exogenous mixed REEs under hydroponic conditions. Significant enrichment of middle REEs (MREEs) and heavy REEs (HREEs) was observed in plant roots and leaves respectively, with slight fractionation between light REEs (LREEs) and HREEs in stems. Moreover, the tetrad effect was observed in these organs. Investigations into REE speciation in roots and in the xylem sap using X-ray absorption spectroscopy (XAS) and nanometer-sized TiO2 adsorption techniques, associated with other controlled experiments, demonstrated that REE fractionations should be dominated by fixation mechanism in roots caused by cell wall absorption and phosphate precipitation, and by the combined effects of fixation mechanism and transport mechanism in aboveground parts caused by solution complexation by intrinsic organic ligands. A conceptive model was established for REE fractionations in plants based on the above studies.     

Fractionations of rare earth elements in plants and their conceptive model

Fractionations of rare earth elements (REEs) and their mechanisms in soybean were studied through application of exogenous mixed REEs under hydroponic conditions. Significant enrichment of middle REEs (MREEs) and heavy REEs (HREEs) was observed in plant roots and leaves respectively, with slight fractionation between light REEs (LREEs) and HREEs in stems. Moreover, the tetrad effect was observed in these organs. Investigations into REE speciation in roots and in the xylem sap using X-ray absorption spectroscopy (XAS) and nanometer-sized TiO₂ adsorption techniques, associated with other controlled experiments, demonstrated that REE fractionations should be dominated by fixation mechanism in roots caused by cell wall absorption and phosphate precipitation, and by the combined effects of fixation mechanism and transport mechanism in aboveground parts caused by solution complexation by intrinsic organic ligands. A conceptive model was established for REE fractionations in plants based on the above studies.