稀土元素在植物中的分异及其概念模型

通过添加外源混合稀土、溶液培养等方式, 研究了稀土元素在大豆植株中的分异特征及其机制. 大豆根和叶中分别出现显著的中稀土(MREE)富集和重稀土(HREE)富集, 茎中出现轻、 重稀土(LREE/HREE)的轻微分异, 同时在以上器官观察到四重效应. 通过X射线吸收光谱(XAS)分析和纳米TiO₂吸附技术分析了根及木质部伤流液中稀土离子的存在形态, 结合其他条件实验结果, 推断稀土元素在根中的分异主要由细胞壁吸附及磷沉淀主导的固定机制造成, 而地上部的分异由内源有机配体作用下的转移机制与固定机制共同造成, 并在此基础上提出了稀土元素在植物中分异的概念模型.     

南方稀土采矿恢复地土壤稀土元素含量及植物吸收特征

通过野外取样调查和室内ICP-MS测定,研究了福建省长汀县稀土矿治理地土壤和主要植物中稀土元素的含量、分布以及转移特征.结果表明:稀土矿治理地的土壤养分含量较低;土壤中稀土元素的含量为507.40～841.37 mg· kg-1,高于对照地土壤的含量.稀土矿治理地土壤中稀土元素主要为交换态,其含量占总量的61％～98％.稀土矿治理地土壤中稀土元素从原来偏单一的交换态转变为多种形态共存,其中有机态含量显著升高.植物根、茎、叶中稀土元素含量分别为40.27～986.01、5.14 ～ 206.58、6.81 ～ 2364.51mg·kg-1.稀土元素在植物各器官中含量水平除芒萁为叶＞根＞茎,其他植物均表现为根＞叶＞茎.根据不同植物吸收和积累稀土元素的差异,可将矿区治理地植物分为富集型和根部囤积型植物.芒萁属于富集型植物,桉树、高羊茅、宽叶雀稗、木荷和油茶属于根部囤积型植物.     

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

ICP－MS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。     

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     

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     

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.     

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.     

氮素形态及配比对夏播菘蓝生长及活性成分含量的影响

以来自山西的菘蓝(Isatis indigotica Fort.)为实验对象,采用盆栽法研究铵态氮(NH4+-N)、硝态氮(NO3--N)和酰胺态氮〔CO(NH2)2〕的不同配比对夏播菘蓝生长,叶和根中的可溶性蛋白质及总氮含量,根中多糖含量,叶中叶绿素相对含量,以及叶中靛玉红和靛蓝、根中(R,S)-告依春的含量和积累量的影响.结果表明:各施氮处理组的单株叶干质量均高于对照(不施用氮素)组,但单株根干质量或高于或低于对照组,其中,T4〔n(铵态氮):n(硝态氮):n(酰胺态氮)=25:75:0〕处理组的单株叶和根干质量均最大,且总体上显著高于对照组及其他施氮处理组(P<005);而施氮处理组的根冠比均显著低于对照组.各施氮处理组叶中的可溶性蛋白质含量与对照均无显著差异,但各施氮处理组根中的可溶性蛋白质含量、叶和根中的总氮含量以及叶中的叶绿素相对含量总体上显著高于对照组,而根中的多糖含量或高于或低于对照组,其中,T6〔n(铵态氮):n(硝态氮):n(酰胺态氮)=0:75:25〕处理组根中的多糖含量和叶中的叶绿素相对含量均最高,T3〔n(铵态氮):n(硝态氮):n(酰胺态氮)=50:50:0〕处理组叶和根中的可溶性蛋白质含量均较高.各施氮处理组叶中靛玉红含量总体上显著高于对照组,多数施氮处理组叶中靛蓝含量则显著低于对照组,但各施氮处理组的单株叶中靛蓝和靛玉红积累量总体上高于对照组;其中,T2〔n(铵态氮):n(硝态氮):n(酰胺态氮)=75:25:0〕处理组叶中靛玉红含量及其单株积累量均最高,T6处理组叶中靛蓝含量最高,而单株叶中靛蓝积累量则以T3处理组最高.各施氮处理组根中(R,S)-告依春含量总体上显著低于对照组,其中,以T1〔n(铵态氮):n(硝态氮):n(酰胺态氮)=100:0:0〕处理组根中(R,S)-告依春含量最高,T4处理组单株根中(R,S)-告依春积累量最高.综合分析结果表明:按不同配比施用不同形态氮素,夏播菘蓝的生长及活性成分含量有明显差异,因此,若以收获叶为目的,结合叶中靛玉红含量,建议施用铵态氮和硝态氮物质的量比为75:25的复合氮肥;若以收获根为目的,结合根中(R,S)-告依春含量,建议施用铵态氮和硝态氮物质的量比为25:75的复合氮肥.     

螯合剂对重金属超量积累植物Thlaspi caerulescens的锌、铜、锰和铁吸收的影响

由螯合剂EDTA和DTPA对重金属超量积累植物Thlaspicaerulescens吸收Zn、Cu、Mn、Fe和P的影响表明：营养液含Zn10μnol／L几条件下,植株地上部全Zn含量和根系吸Zn速率分别达到1681mgkg-1干重和448mgkg-1根干重d－1;43．2μmol／L的EDTA或DTPA处理显著抑制植株的生长,也减少植株单位根重吸收的Zn量,降低地上部和根系全Zn、全Cu、全Mn含量和可溶态含量,增加地上部的全Fe和全P含量;所有处理中地上部全Zn和可溶态Zn含量均明显高于根系,说明T．caerulescens吸收的Zn大部分运向地上部。与Fe（Ⅲ）EDTA处理相比,Fe（Ⅲ）EDDHA处理植株的单位很重吸收Zn总量和地上部全Zn含量均较高。     

缺氮和复氮对菘蓝幼苗生长及氮代谢的影响

对基质育苗后水培的菘蓝进行缺氮与复氮处理,分析其生长情况及氮代谢产物含量的变化,探讨缺氮和复氮对菘蓝幼苗生长及氮代谢的影响,以提高菘蓝产量和品质以及栽培过程中的氮素利用效率。结果显示:(1)正常供氮条件下,菘蓝幼苗的叶绿素含量、谷氨酰胺合成酶(GS)活性、硝态氮含量、靛玉红含量为最高,而其株高、主根直径、根的鲜重与干重、叶的鲜重与干重、根系活力均最小。(2)缺氮处理增加了菘蓝幼苗的主根直径和根干重,提高其根系活力和硝酸还原酶(NR)活性,促进游离氨基酸在叶中的积累;但降低了GS的活性,也降低了叶中硝态氮、可溶性蛋白、靛玉红及根中游离氨基酸的含量;缺氮对叶中靛蓝的含量无明显影响。(3)复氮处理增加了菘蓝幼苗的株高、主根长、根鲜重、叶鲜重、叶干重,提高了其根系活力,降低了NR和GS的活性;与对照相比,复氮降低了叶中硝态氮含量,提高了叶中可溶性蛋白、靛蓝及根中游离氨基酸的含量,但对叶中游离氨基酸和靛玉红含量影响较小。研究表明,缺氮后再复氮有利于菘蓝幼苗叶的生长,同时有利于增加其叶内靛蓝含量,从而提高其产量和品质。     

镧在草-菇-土系统中的循环与生物富集效应

利用稀土镧肥种植牧草南非马唐,采用含镧牧草栽培杏鲍菇和以菇渣作为有机肥种植牧草进行连续性试验,研究镧在草-菇-土系统中的分配与生物富集情况。结果表明：施镧处理的南非马唐和杏鲍菇各器官的镧元素含量均高于不施镧处理,其中镧在牧草南非马唐中的分布为根>叶>茎,镧在杏鲍菇中的分布为菌盖>菌柄;外源镧进入土壤以后,南非马唐不同器官的镧元素生物富集系数均随着镧施入量的增加而增大,其中以根的镧生物富集系数最大,介于0.443—0.580之间。除高剂量（M4）处理外,叶和茎的镧生物富集系数不同处理间无显著差异,但根出现明显变化;含镧牧草栽培杏鲍菇和菇渣种植南非马唐后,不同器官的镧含量无显著增加,说明镧残留在草-菇-土系统中迁移转化效率降低。     

Bioaccumulation of cerium and neodymium by <Emphasis Type="Italic">Bacillus cereus</Emphasis> isolated from rare earth environments of Chavara and Manavalakurichi,India

Rare earth elements (REEs) are among the common minerals in the Rare earth environment that are very precious and also enhance soil properties. The aim of this present study is to evaluate the accumulation of REEs by bacterial isolates of rare earth environment. Morphological and biochemical characterization were done for 37 bacterial isolates and also molecular studies were carried out using 16S rRNA sequencing method. The assessment of REEs composition in soil samples of Chavara and Manavalakurichi analyzed using Inductively Coupled Plasma-Mass Spectrometry (ICP-MS) showed the abundance of Cerium and Neodymium among lanthanides. The bioaccumulation study of rare earth elements by Bacillus cereus were accomplished employing FT-IR spectrum and ICP-OES analysis. The significant accumulation of rare earth elements especially Cerium and Neodymium was noticed in Bacillus cereus isolated from rare earth environment.     

Accumulation and fractionation of rare earth elements (REEs) in wheat: controlled by phosphate precipitation, cell wall absorption and solution complexation

Previous studies on rare earth element (REE) bioaccumulation have focused on their accumulation rate and fractionation, but the processes involved remain unclear. In this study, the accumulation and fractionation of REEs in wheat (Triticum aestivum L.) were investigated using solution culture with exogenous mixed REEs. A decrease in REE contents was observed from the roots to the tops of wheat. Significant fractionations of REEs were found in wheat organs as compared to the exogenous mixed REEs. Middle REE (MREE, the elements from Sm to Gd) enrichment and an M-type tetrad effect (an effect that can cause a split of REE patterns into four consecutive convex segments) were observed in the roots, which were probably caused by phosphate precipitation of REEs in/on the roots and absorption of REEs to root cell walls. Light REE (LREE, the elements from La to Eu) and heavy REE (HREE, the elements from Gd to Lu) enrichments were observed in the stems and leaves, respectively, accompanied by conspicuous W-type tetrad effects (an opposite effect to the M-type tetrad effect) in the REE patterns. HREE enrichment decreased from the older to the younger leaves and increased upwards within a single leaf. It is suggested that the solution complexation that occurred in the xylem vessels plays an important role in REE fractionations in the above-ground parts of wheat.     

Role of ligands in accumulation and fractionation of rare earth elements in plants

Few studies have been carried out on the effects of ligands on rare earth element (REE) bioaccumulation processes. In this study, the effects of phosphate (Pi, an inorganic ligand) and citrate (an organic ligand) on accumulation and fractionation of REEs in wheat were investigated using aqueous culture with extraneous mixed REEs (MRE). The results show that initial Pi solution culture at various levels followed by exposure to a fixed-MRE solution did not significantly change the total concentrations of REEs (SigmaREE) in roots, whereas the SigmaREE in leaves dramatically decreased with increasing levels of Pi applied. Simultaneous culture of wheat with mixture of MRE and citrate solutions caused obvious decreases of the SigmaREE in both roots and leaves. Compared with MRE, significant fractionations of REEs were found in wheat organs when no ligand was applied. Notable middle REE (MREE) enrichment and M-type tetrad effect were observed in the roots, and heavy REE (HREE) enrichment and W-type tetrad effect existed in the leaves. Pi treatments did not significantly affect the fractionations of REEs in the roots, but enrichment of HREEs in the leaves slightly increased at the highest level of Pi applied. Fractionations of REEs in both roots and leaves decreased with increasing levels of citrate applied; at higher levels of citrate (> or =150 microM), no above fractionation features were observed in wheat, but light REE (LREE) enrichment existed in the roots and leaves. The results indicate that ligands might play important roles in accumulation and fractionation of REEs during bioaccumulation processes.     

Distribution and bioaccumulation of trace elements and lanthanides in apples from Northwestern Italy

BackgroundTransfer of metals from soil to plant is a possible route of contamination for the food chain. This investigation focused on the occurrence of 40 elements in the “Red Apple of Cuneo”, an Italian excellence and a Protected Geographical Indication (P.G.I.). Four cultivars were considered: Red Delicious (Jeromine) and Gala (Bukeye, Brookfield, Schniga).MethodsTrace elements and rare earth elements (REEs) detection was performed by an Inductively Coupled Plasma-Mass Spectrometer (ICP-MS) previous homogenization of samples and microwave acid digestion. One-way analysis of variance (ANOVA) with Bonferroni correction was employed to for statistical analysis.ResultsConcentrations of metals in the four apples cultivars were quite comparable, Al and Rb were the most represented nonessential elements while Fe, Cu and Zn between the essential; REEs were found at negligible concentrations. Bioaccumulation factors demonstrated an extremely low capacity of bioaccumulation from soil to fruit.ConclusionsThe analysis performed on the “Red Apple of Cuneo” has shown that this product is safe for human consumption since metals were recovered at concentrations of no concern and lower than those registered in apples from other countries.Since each production area is characterized by a typical elemental pattern the multielemental profile based on the analysis of 40 elements could be useful to relate products to their region of origin. Differences between the four apple cultivars were instead not significant to discriminate between them.     

Effects of rare earth elements and REE-binding proteins on physiological responses in plants

Rare earth elements (REEs), which include 17 elements in the periodic table, share chemical properties related to a similar external electronic configuration. REEs enriched fertilizers have been used in China since the 1980s. REEs could enter the cell and cell organelles, influence plant growth, and mainly be bound with the biological macromolecules. REE-binding proteins have been found in some plants. In addition, the chlorophyll activities and photosynthetic rate can be regulated by REEs. REEs could promote the protective function of cell membrane and enhance the plant resistance capability to stress produced by environmental factors, and affect the plant physiological mechanism by regulating the Ca2? level in the plant cells. The focus of present review is to describe how REEs and REE-binding proteins participate in the physiological responses in plants.     

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).     

Accumulation of rare earth elements in human bone within the lifespan

For the first time, the contents of rare earth elements (REEs) in a rib bone of a healthy human were determined. The mean value of the contents of Ce, Dy, Er, Gd, La, Nd, Pr, Sm, Tb, and Yb (10 elements out of 17 total REEs), as well as the upper limit of means for Ho, Lu, Tm, and Y (4 elements) were measured in the rib bone tissue of 38 females and 42 males (15 to 55 years old) using inductively coupled plasma mass spectrometry (ICP-MS). We found age-related accumulation of REEs in the bone tissue of healthy individuals who lived in a non-industrial region. It was calculated that during a lifespan the content of REEs in a skeleton of non-industrial region residents may increase by one to two orders of magnitude. Using our results as indicative normal values and published data we estimated relative Gd accumulation in the bone tissue of patients according to magnetic resonance imaging with contrast agent and La accumulation in the bone tissue of patients receiving hemodialysis after treatment with lanthanum carbonate as a phosphate binder. It was shown that after such procedures contents of Gd and La in the bone tissue of patients are two to three orders of magnitude higher than normal levels. In our opinion, REEs incorporation may affect bone quality and health similar to other potentially toxic trace metals. The impact of elevated REEs content on bone physiology, biochemistry and morphology requires further investigation.     

Urinary Monitoring of Exposure to Yttrium, Scandium, and Europium in Male Wistar Rats

On the assumption that rare earth elements (REEs) are nontoxic, they are being utilized as replacements of toxic heavy metals in novel technological applications. However, REEs are not entirely innocuous, and their impact on health is still uncertain. In the past decade, our laboratory has studied the urinary excretion of REEs in male Wistar rats given chlorides of europium, scandium, and yttrium solutions by one-shot intraperitoneal injection or oral dose. The present paper describes three experiments for the suitability and appropriateness of a method to use urine for biological monitoring of exposure to these REEs. The concentrations of REEs were determined in cumulative urine samples taken at 0?C24?h by inductively coupled plasma atomic emission spectroscopy, showing that the urinary excretion of REEs is <2?%. Rare earth elements form colloidal conjugates in the bloodstream, which make high REEs accumulation in the reticuloendothelial system and glomeruli and low urinary excretion. The high sensitivity of inductively coupled plasma?Cargon emission spectrometry analytical methods, with detection limits of <2???g/L, makes urine a comprehensive assessment tool that reflects REE exposure. The analytical method and animal experimental model described in this study will be of great importance and encourage further discussion for future studies.