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.     

稀土元素在小麦体内分配行为的研究

采用水培,土培试验及中子活化分析技术,在作物生长效应曲线研究的基础上,系统地研究了稀土远征顷作物体内的含量、吸收、分布和转移等行为。所获结果表明,名稀土元素在作物体现人的分配行为受生物的内外因素与稀土来源、自身特征和元素间关系的影响,是作物稀土元素分配行为已有研究成果的重要补充与深化,并为土壤施用稀土元素提供促进一步的科学依据。     

茶园土壤类型对铁观音茶叶稀土元素分布和组成的影响

为探明铁观音茶的质量安全状况,追溯隐患来源,对福建安溪县不同土壤茶园的铁观音茶叶进行稀土元素的分布、组成、迁移和富集能力进行研究。结果表明,安溪县红壤、黄红壤、黄壤茶园稀土组成均以镧、铈、钕、钇为主,但具体组成特征各异。3种类型土壤茶园铁观音茶叶片、叶柄稀土元素组成均以钇、镧、铈、钕4种元素为主,且含量均以第3叶第2叶第1叶叶柄。同种土壤类型茶园铁观音茶树不同部位叶片的稀土元素组成特征类似,但叶与叶柄对稀土元素的吸收能力不同。土壤类型对茶叶稀土元素的累积有显著影响,黄红壤茶园的茶叶稀土元素含量要显著低于红壤、黄壤茶园的(P0.05)。土壤与茶叶中稀土元素组成的相关系数为0.886～0.985,P 0.001,表明二者稀土元素组成密切相关。因此,铁观音茶叶中稀土元素累积、分布与茶园土壤类型有显著相关性。     

鱼体(去鳃)和鱼鳃对不同形态铜的积累特征

在实验室条件下研究实验鱼Ｐａｒａｃｈｅｉｒｏｄｏｎ对人工河水中不同形态的积累特征,对比了鱼体（去鳃）和鱼鳃对铜吸收量的差异,并探讨了鱼对铜的吸收机理。研究结果表明,实验鱼鳃部和体内铜积累量均随水相游离铜浓度增高,暴露时间增长而增加,但鳃部积累浓度较鱼体其余部分高一个数量级,其从水相富集铜的速率显著高于鱼体。     

稀土元素对小麦幼苗氮素吸收及其同化的影响

稀土元素浸种能够促进小麦(Triticum aestivum L.)幼苗对NO_3~-的吸收,提高硝酸还原酶活力。这些效应与稀土浓度有关,低浓度有促进作用,高浓度则有抑制作用。稀土元素处理还能促进小麦幼苗体内NO_3~-的同化还原,使硝态氮含量降低,氨基氮含量增加,促进了氮素代谢过程。     

有机物料对土壤镉形态及其生物有效性的影响

采用盆栽试验,研究了淹水种稻条件下添加猪粪和泥炭对红壤和潮土中内源和外源Cd形态及其生物有效性的影响。结果表明,土壤中内源Cd在各形态之间的分布比较均匀;添加外源Cd时Cd主要分布于交换态,从分蘖期到成熟期,内源Cd交换态普遍升高,添加外源Cd时交换态普遍降低。有机物料对内源Cd交换态的影响不显著,但当添加外源Cd时则对交换态有显著影响,在不添加外源Cd的条件下,有机物料普遍促进水稻根系对Cd的吸收。在添加外源Cd的条件下,有机物料普遍抑制水稻根系对Cd的吸收,猪粪的抑制效果强于泥炭,水稻根系对Cd与Fe的累积呈显著抑制作用。     

氮素形态对小白菜生长和碳氮积累的影响

水培条件下,研究不同氮素形态(硝态氮、铵态氮、甘氨酸、谷氨酰胺、丙氨酸、牛血清蛋白,以及甘氨酸与硝态氮、牛血清蛋白与硝态氮的混合氮源)对小白菜生长和碳氮积累的影响.结果表明:不同氮素形态对小白菜质量、碳氮积累量、可溶性蛋白质含量、可溶性糖含量和游离氨基酸含量的影响不同;硝态氮处理下小白菜地上部分和根的干质量与鲜质量均最大;甘氨酸对小白菜根系的生长及碳氮积累具有明显的促进作用;在3种氨基酸中,谷氨酰胺更有利于小白菜地上部分的生长和氮积累.聚类分析表明,9种氮素形态处理按营养效应大小分为:硝态氮、谷氨酰胺＞甘氨酸与硝态氮混合氮源、牛血清蛋白与硝态氮混合氮源、甘氨酸、铵态氮＞丙氨酸、牛血清蛋白、对照.有机氮源可以作为小白菜生长的氮源,不同的氮素形态对植物产生的生理效应不同.     

稀土元素对生物机体剂量效应的研究

综述了稀土元素对生物机体的剂量效应,包括稀土对生物体生长发育、内分泌系统、体内分布及其引发的疾病、细胞毒性及抗诱变、抗癌等影响,以期为稀土在生物学领域的进一步应用提供参考.     

不同轮作制度对淮北白浆土团聚体及其有机碳的积累与分布的影响

淮北白浆土是苏鲁交界地区主要低产土壤 ,同时也是我国黄淮地区商品粮生产基地的重要土壤资源。该土壤除了剖面发生分异强烈、土壤理化性质不良外 ,有机碳匮乏是其主要肥力限制因子 [1]。土壤有机碳不但是维持和培育土壤质量的关键组成成分 ,而全球土壤有机碳每年分解释放大气 CO2 而且达到 0 .1～ 5.4C Pg·年 -1,土壤碳 0 .1 %的变化将导致大气圈 CO2 浓度 1 mg· L - 1的变化。因而其存储和释放的变化与大气 CO2 动态有密切的关系 [9,10 ] 。农业土壤对大气 CO2 的截存贡献是研究陆地系统对大气 CO2 的汇效应 (sink effect)的焦点 …     

黄粉虫幼虫对硒的生物积累

在饲料中添加含硒化合物喂养黄粉虫Tenebrio molitor L.幼虫,测定幼虫硒含量、粪便硒含量和体重的变化,计算黄粉虫幼虫特定生长率及幼虫对硒生物积累系数,分析黄粉虫有效积累硒的条件。结果表明,饲料硒含量在15~20mg/kg时,幼虫硒含量明显提高,对硒的生物积累系数高于其它试验组水平,饲料硒含量过高,幼虫硒含量降低,正常生长受到抑制。黄粉虫幼虫特定生长率、取食量、排粪量、干物质含量随着饲料硒含量的增加而降低,死亡率、粪便硒含量随着饲料硒含量的增加而增大。饲料硒含量为15～20mg/kg时黄粉虫幼虫对硒的生物积累效果最好。     

稀土元素对红霉素发酵的影响

通过对红霉素发酵培养基中添加稀土元素的研究,确定了几种能对发酵效价有提高作用的稀土元素及其浓度,当其中镧La^3＋、钕Nd^3＋和铈Ce^4＋离子浓度分别为50mg／L、50mg/L和100mg／L时对提高红霉素效价水平最显著,提高了32％、25％和25％,并且对改善红霉素组分也有明显作用,红霉素A组分相对百分含量分别提高18．9％、32．7％和34．4％,红霉素B组分分别减少24．1％、58．6％和62．1％。     

Contents and the biogeochemical characteristics of rare earth elements in wheat seeds

Contents of fifteen rare earth elements (REEs) in the seeds ofsixty breeds of wheat collected from seed bank were measured byinductively coupled plasma mass spectrometry (ICP-MS). The distributionpatterns of contents of REEs in wheat seeds (n = 58) wereobserved and compared with their average level in soils (n =364). Differences among regions and between spring and winter wheat weretested. Comparison with literature data was also made. The results showthat the content of REEs in wheat seed ranges between10^–11 g · g^–1 and10^–8 g · g^–1, 3–4 orderof magnitudes lower than that in soils. The distribution patterns arethat light REEs enriched and the Eu-anomaly is weak, similar to the soilcase. No obvious differences were found among different regions andbreeds. The data obtained in this study represent the contents of thefifteen REEs in wheat seeds.     

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。     

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.     

稀土元素对谷氨酸发酵的影响

通过对谷氨酸发酵培养基中添加稀土元素的研究,确定了几种能对发酵产酸有提高作用的稀土元素及其浓度,其中La^3 、Ce^4 、Nd^3 离子浓度分别为100mg/L、10mg/L、1mg／L时能提高产酸水平,而Sm^3 、Y^3 离子对发酵基本上没有影响。     

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.     

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.