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     

长期施锌条件下土壤-植物系统植物营养元素的分布特征

对黄土高原旱地连续17a施用锌肥条件下植物营养元素在土壤-植物系统中的分布特征进行研究,结果表明：长期施用锌肥0～40cm土层土壤的碳、氮元素含量高于对照处理,而40～100cm土层土壤的碳、氮含量低于对照处理;0～100cm土层土壤全磷含量高于对照,而有效磷含量低于对照。施锌冬小麦茎、叶和籽粒中氮含量高于不施锌处理,而壳中氮含量低于对照处理,施锌后氮素在冬小麦茎、叶、籽粒和整个植株中的累积量高于对照,籽粒和茎中磷的含量低于对照,植株中磷的积累量也低于对照。     

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.     

Eu3+对山黧豆中的氨基酸及蛋白质代谢作用的研究

对山黧豆(Lathyrus sativus L.)幼苗整株,喷施一定浓度的Eu3+溶液吸收后,对其相关的生理指标进行测试,结果表明与水喷比较,根中丝氨酸、甘氨酸、丙氨酸、蛋氨酸、亮氨酸、脯氨酸、胱氨酸与对照持平,缬氨酸、酪氨酸、苯丙氨酸、组氨酸略有升高外,其余均低于对照;茎中除精氨酸、脯氨酸、色氨酸略高于对照外,其余均低于对照;叶中除蛋氨酸、色氨酸略高于对照外,其余均低于对照.游离氨基酸总量增加时,茎＞根＞叶,减少时,根＜茎＜叶.蛋白质含量经Eu3+ 处理茎中减少,根和叶中增加;水解酶比活性根＞茎＞叶;Na+、K+-ATPase活力却表现根＞茎＞叶的趋势.表明Eu3+ 对山黧豆生理活性代谢起到一定的调节作用.     

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。     

不同有机肥对土壤镉锌生物有效性的影响

在南方典型稻田设置连续4年施用猪粪、鸡粪、稻草的定位试验,监测施用不同有机肥条件下土壤及水稻植株镉(Cd)、锌(Zn)含量的变化,研究有机肥对土壤Cd、Zn活性及其交互作用的影响.结果表明: 施用有机肥(猪粪、鸡粪、稻草)对土壤全Cd、有效态Cd含量及Cd活性皆无显著影响,但有增加土壤Cd全量的趋势,且显著增加土壤全Zn、有效态Zn含量及Zn活性.施用猪粪、鸡粪、稻草皆可降低稻米Cd含量,降Cd效果为猪粪>鸡粪>稻草,猪粪处理水稻稻米、茎、叶Cd含量分别比对照下降37.5%、44.0%、36.4%;鸡粪处理水稻米、茎、叶Cd含量分别比对照下降22.5%、33.8%、22.7%;而稻草处理水稻米Cd含量比对照下降7.5%,但茎、叶Cd含量比对照分别增加8.2%、22.7%;施用猪粪、鸡粪降低稻米Cd含量主要是降低了水稻植株对土壤Cd的富集,而施用稻草则主要是降低了水稻茎Cd向稻米的转运.施用有机肥还增加了水稻茎Zn含量,施用猪粪、鸡粪、稻草的水稻茎Zn含量比单施化肥分别增加53.4%、41.2%、13.9%,但对水稻稻米、叶Zn含量无显著影响.Zn、Cd在土壤、植株茎中皆表现出显著的拮抗作用,土壤及水稻茎Zn含量的增加显著抑制了水稻米、茎、叶对Cd的吸收积累,且随土壤有效态Zn/Cd含量比值的增加,Zn、Cd竞争土壤吸附不是抑制水稻吸收积累Cd的主控因子,而Zn、Cd竞争吸收才是影响水稻吸收积累Cd的主控因子.     

不同有机肥对土壤镉锌生物有效性的影响

在南方典型稻田设置连续4年施用猪粪、鸡粪、稻草的定位试验,监测施用不同有机肥条件下土壤及水稻植株镉(Cd)、锌(Zn)含量的变化,研究有机肥对土壤Cd、Zn活性及其交互作用的影响.结果表明:施用有机肥(猪粪、鸡粪、稻草)对土壤全Cd、有效态Cd含量及Cd活性皆无显著影响,但有增加土壤Cd全量的趋势,且显著增加土壤全Zn、有效态Zn含量及Zn活性.施用猪粪、鸡粪、稻草皆可降低稻米Cd含量,降Cd效果为猪粪>鸡粪>稻草,猪粪处理水稻稻米、茎、叶Cd含量分别比对照下降37.5%、44.0%、36.4%;鸡粪处理水稻米、茎、叶Cd含量分别比对照下降22.5%、33.8%、22.7%;而稻草处理水稻米Cd含量比对照下降7.5%,但茎、叶Cd含量比对照分别增加8.2%、22.7%;施用猪粪、鸡粪降低稻米Cd含量主要是降低了水稻植株对土壤Cd的富集,而施用稻草则主要是降低了水稻茎Cd向稻米的转运.施用有机肥还增加了水稻茎Zn含量,施用猪粪、鸡粪、稻草的水稻茎Zn含量比单施化肥分别增加53.4%、41.2%、13.9%,但对水稻稻米、叶Zn含量无显著影响.Zn、Cd在土壤、植株茎中皆表现出显著的拮抗作用,土壤及水稻茎Zn含量的增加显著抑制了水稻米、茎、叶对Cd的吸收积累,且随土壤有效态Zn/Cd含量比值的增加,Zn、Cd竞争土壤吸附不是抑制水稻吸收积累Cd的主控因子,而Zn、Cd竞争吸收才是影响水稻吸收积累Cd的主控因子.     

感耦等离子体发射光谱法研究土壤-铁芒萁系统中稀土元素的分布、累积和迁移特征

用感耦等离子体发射光谱法(ICP-AES)测定了江西赣南地区非稀土矿区和处不同稀土矿区内,土壤-铁芒萁系统中La、Ce、Pr、Nd、Sm、Gy、Db、Yb和Y的含量,并对其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,土壤剖面层的底土层含量最高,但表土层铈相对富集.稀土元素总量(∑REE)在铁芒萁植物体内的分布规律是叶＞根＞茎＞叶柄,单一稀土元素的分布规律各异,La、Ce、Pr、Nd的分布规律表现为:叶＞根＞茎＞叶柄;Sm和Gd在不同采样点表现为叶＞根＞茎＞叶柄或根＞叶＞茎＞叶柄;Dy、Yb和Y均有3种不同的分布模式:叶＞根＞茎＞叶柄、根＞叶＞茎＞叶柄及根＞茎＞叶＞叶柄.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.     

叶面喷施烯效唑对盐胁迫下大豆幼苗生理及解剖结构的影响

以大豆栽培品种‘中黄13’为试验材料,在筛选合适的盐胁迫及烯效唑(S3307)浓度基础上,采用大豆幼苗期盐胁迫以及叶面喷施S3307的方法,分析比较相关生理指标及营养器官(根、茎和叶)解剖结构的差异,从组织结构形态和生理两方面探讨叶面喷施S3307对大豆苗期盐胁迫的缓解效应及其作用机制。结果显示:(1)与正常生长的对照相比,盐胁迫下大豆根和叶中硫代巴比妥酸反应物的含量均显著增加,叶绿素含量显著降低;而且叶片较薄,海绵组织和栅栏组织细胞排列混乱;根部中柱所占比例较对照明显变小,但皮层所占比例变大,外表皮细胞向内凹陷,次生导管平均孔径较小且含有侵填体;茎部解剖结构的变化与根部相类似。(2)叶面喷施80mg/L S3307后,盐胁迫大豆植株根和叶中硫代巴比妥酸反应物和叶绿素含量均恢复到接近对照的水平,且根、茎和叶解剖结构变化介于正常对照与盐胁迫处理之间。研究表明,叶面喷施80mg/L S3307能够有效缓解盐胁迫对大豆的伤害,且这种缓解作用与叶片细胞膜伤害、光合色素含量以及根、茎和叶内部组织结构改变有关,叶面喷施S3307可能是生产上提高大豆耐盐性的一种有效措施。     

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.     

Role of rhizosphere mechanisms in Cd uptake by various wheat cultivars

In each wheat type, cultivars have different propensities to accumulate Cd in their grains, likely depending on Cd uptake by roots and/or Cd distribution in the plant. This study investigates the processes in the root–soil interface and their role in high or low grain Cd accumulation. Twenty-four cultivars of spring bread, winter bread, durum, and spelt wheat with different grain Cd accumulation levels were investigated regarding removal of Cd from soil, pH, Cd and organic acids in root exudates, and cation-exchange capacity of roots (rootCEC). In addition, we investigated ¹⁰⁹Cd uptake from a nutrient solution resembling soil solution. The removal of Cd from the rhizosphere soil increased, likely due to increased rootCEC with increased grain Cd accumulation propensity, except in spring bread wheat. The ¹⁰⁹Cd uptake from solution did not differ between high and low grain Cd accumulators. If the soil Cd concentration was elevated, rootCEC increased, as did pH, and succinic acid levels in the exudates, while lactic and citric acid levels in root exudates decreased. This work indicates that high grain Cd accumulators take up more Cd from soil than do low accumulators. But not by a different capacity to take up Cd from soil solution. The higher rootCEC in high accumulating cultivars may influence the release of Cd from the soil particles.     

不同耕作方式对陇中旱农区春小麦和豌豆根系空间分布及产量的影响

依托陇中旱农区长期的保护性耕作定位试验,对不同耕作方式下春小麦和豌豆根系空间分布特征及作物产量进行研究,以探索耕作措施影响作物产量的机制.结果表明: 随着生育期的推进,春小麦和豌豆的总根长、根表面积呈先增后减的趋势,开花期达到最大;春小麦根系苗期以0～10 cm最多,花期、成熟期10～30 cm最多;而豌豆根系苗期和成熟期均以0～10 cm最多,花期10～30 cm最多.免耕秸秆覆盖和免耕覆膜增加了根长和根表面积,春小麦和豌豆各生育时期的根长较传统耕作增加了35.9%～92.6%,根表面积增加了43.2%～162.4%.免耕秸秆覆盖和免耕覆膜优化了春小麦和豌豆根系分布,与传统耕作相比,增加了春小麦和豌豆苗期0～10 cm土层根长和根表面积分布比例,花期和成熟期深层次根系分布也显著增加,免耕秸秆覆盖在开花期30～80 cm土层根长和根表面积的分布比例分别比传统耕作提高了3.3%和9.7%.春小麦各生育期的总根长、根表面积与产量呈显著正相关,豌豆各生育期的总根长与豌豆产量呈极显著正相关.免耕秸秆覆盖和免耕覆膜较传统耕作春小麦和豌豆产量增加23.4%～38.7%,水分利用效率提高了13.7%～28.5%.在陇中旱农区,免耕秸秆覆盖和免耕覆膜可以增加作物根长和根表面积,优化了根系在土壤中的空间分布,增强作物根层吸收能力,从而提高作物产量和水分高效利用.     

Rooting patterns in near-isogenic lines of spring wheat for dwarfism

The effects of Rht alleles on root growth and distribution in isogenic lines of spring wheat (Triticum aestivum L.) are described under different environmental conditions. Above-ground biomass, root length, root dry-weight and their distribution along the soil profile were measured by destructive sampling for growth of aerial biomass and extraction of soil cores containing roots. Field experiments were conducted under non-limiting water and nutritional conditions during two consecutive years, using an early and a late sowing date each year.Dwarfing genes significantly reduced plant height and above-ground biomass at anthesis. In addition, stem mass ratio also was reduced with increases in the allelic dosage. Conversely, total root length and root dry-weight per unit area at anthesis were increased with decreased plant height, therefore, root mass ratio tended to be negatively correlated with plant height. Differences in distribution of root length and root dry-weight through the soil profile among lines were largely confined to the upper soil layers (i.e. the top 30 cm).Differences in root dry-weight were more important than in root length, so that the dwarf line had the highest root mass per unit root length. Furthermore, a significant positive correlation between the root mass ratio and stem mass per unit stem length was found. It is suggested that increases in root mass per unit root length associated with Rht alleles are evidencing a surplus of photoassimilates during stem elongation which are used for thickening the roots due to the lack of alternative sinks. Agronomic implications of this effect are discussed.     

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。     

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.     

间作模式下冬小麦与春玉米根系的时空分布规律

采用大口径土钻对间作种植模式下冬小麦与春玉米根系进行取样,分析了两种作物根系的空间分布及动态变化规律．结果表明：间作冬小麦根系在空间上呈幂函数递减规律,间作春玉米根系呈指数递减规律．采用多元线性回归建立间作冬小麦和春玉米根系质量密度（R）的二维空间分布函数,经验证,两种作物根系质量密度的二维分布函数均可反映作物根系的实际生长状况．     

咸水灌溉条件下土壤水盐分布特征

通过设置3种灌水量水平（100%ET_c、80%ET_c、60%ET_c）和3种灌水水质水平（0.7、3和6 g·L^-1）,研究了咸水灌溉条件下春小麦120 cm土层内水分动态和盐分累积特征.结果表明：水分在农田土壤中的分布主要受灌水量和土壤质地的影响,充分灌溉使水分存贮在较深土层中,而非充分灌溉则使水分存贮在表层;在相同灌水量的条件下,土体内的盐分积累程度随着灌溉水矿化度的增大而加剧;在相同矿化度条件下,土体内的盐分含量及积盐深度随着灌水量的增加而增大.在作物整个生育期内,连续使用咸水灌溉将导致土壤积盐,且非充分灌溉较充分灌溉更易使土壤表层积盐.