Latest precambrian (Cadomian) zircon ages, Nd isotopic systematics and P-T evolution of granitoid orthogneisses of the Erzgebirge, Saxony and Czech Republic

Single zircons from two orthogneiss complexes, the Grey Gneiss and Red Gneiss, the lowermost tectonic units in the Erzgebirge, were dated. The grey Freiberg Gneiss is of igneous origin and has a ²⁰⁷Pb/²⁰⁶Pb emplacement age of 550±7 Ma. A quartz monzonite from Lauenstein contains idiomorphic zircons with a mean ²⁰⁷Pb/²⁰⁶Pb age of 555±7 Ma as well as xenocrysts ranging in age between 850 and 1910 Ma. Red gneisses from the central Erzgebirge contain complex zircon populations, including numerous xenocrysts up to 2464 Ma in age. The youngest, idiomorphic, zircons in all samples yielded uniform ²⁰⁷Pb/²⁰⁶Pb ages between 550±9 and 554±10 Ma. Nd isotopic data support the interpretation of crustal anatexis for the origin of both units. _Nd(t) values for the grey gneisses are –7.5 and –6.0 respectively, (mean crustal residence ages of 1.7–1.8 Ga). The red gneisses have a wider range in _Nd(t) values from –7.7 to –2.8 (T _DM ages of 1.4–1.8 Ga). The zircon ages document a distinct late Proterozoic phase of granitoid magmatism, similar in age to granitoids in the Lusatian block farther north-east. However, Palaeozoic deformation as well as medium pressure metamorphism ( 8 kbar/600–650° C) are identical in both gneiss units and distinguish these rocks from the Lusatian granitoids. The grey and red gneisses were overthrust by units with abundant high-pressure relicts and a contrasting P-T evolution. Zircon xenocryst and Nd model ages in the range 1000–1700 Ma are similar to those in granitoid rocks of Lusatia and the West-Sudetes, and document a pre-Cadomian basement in parts of east-central Europe that, chronologically, has similarities with the Sveconorwegian domain in the Baltic Shield.     

钝顶螺旋藻突变株FBL的生理特性

利用倍频Ｎｄ：ＹＡＧ激光（λ＝５３２ｎｍ,ｐ＝５００ｍＷ,Ｓ＝１６０ｍＷ／ｃｍ＾２）对钝顶螺旋藻进行诱变处理,辐照１０ｍｉｎ,经分离获得藻丝开矿变成直形的钝顶螺旋突变株ＦＢＬ。对该变株ＦＢＬ的生长特性、藻多糖、氨基酸、β－胡萝卜素、叶绿素ａ等生化组成的研究。结果表明：与出发株相比,突变株ＦＢＬ生长速度加快;β－胡萝卜素含量提高２２．３％;藻多糖提高４２．０％;氨基酸增幅５．２％,氨基酸的组成比例发     

应用水滑石实时合成分离模拟核素钕

应用水滑石实时合成的方法从高放废液中分离模拟放射性核素钕,通过酸碱滴定、单因素试验及X-射线衍射(XRD)研究确定了最佳分离条件,用红外光谱(FT-IR)、扫描电镜(SEM)、透射电镜(TEM)等对合成的含钕水滑石的结构、形貌进行了分析. 结果表明:模拟放射性核素钕的最佳分离条件,初始ρ(Nd3+)为150 mg/L,pH为10,n(Mg)/［n(Al)+n(Nd)］为3,在该条件下5次平行试验钕的去除率平均值为96.40%,并且钕嵌入到了水滑石的晶格中,合成的含钕水滑石形貌大多为层状六边形;含钕水滑石煅烧产物主要为尖晶石,煅烧产物中未见氧化钕相,表明嵌入到水滑石晶格中的钕在煅烧后仍存在于尖晶石的晶体结构中.      

稀土元素钕对菲律宾蛤仔金属硫蛋白的诱导效应

稀土元素能否诱导海洋生物合成MTs(金属硫蛋白),将影响到MTs对海水重金属的指示作用. 以菲律宾蛤仔(Ruditapes philippinarum)为试验动物,采用含稀土Nd3+的人工海水对其进行暴露培养,测定蛤仔鳃部和内脏中MTs含量随暴露剂量和时间的变化. 结果表明,Nd3+暴露能够增加蛤仔体内MTs含量. ρ(Nd3+)为0.1～10 μg/L时能明显促进蛤仔鳃和内脏MTs的合成;蛤仔在ρ(Nd3+)为1 μg/L下暴露培养7 d,内脏MTs含量达到最高水平;同时,光谱扫描及SDS-PAGE分析表明,Nd3+诱导的蛤仔内脏中MTs在258 nm处有特征吸收峰,主要以二聚体和三聚体的形式存在,分子质量分别为13.0和18.1 ku.      

稀土Nd改性纳米TiO2-NTs/SnO2-Sb电极的制备、结构及性能

采用溶剂热法制备了稀土Nd掺杂TiO2-NTs/SnO2-Sb电极,以苯酚作为典型有机物,考察了电极组成、结构与电极电催化效能的关系,实验结果表明,Nd的掺杂量对电极电催化性能有较大的影响,当前驱液中Nd/Sn原子摩尔百分比为3%时,电极的电催化活性最佳,对苯酚浓度及TOC的降解速率较空白电极（Nd0%）提高了60%及52%。利用SEM及XRD分析方法对所制备的电极进行了形貌及晶形结构的表征,并计算了电极表面SnO2晶胞参数以及平均粒径,结果显示,适量地掺杂Nd元素后,电极表面更加致密,SnO2平均粒径变小。通过XPS分析电极表面元素组成,并计算电极表面吸附氧含量,结果表明,由于Nd元素的存在,降低了涂层中晶格氧（Olat）的含量,减弱了电子的吸引作用,促使了Sn4+周围电子云密度升高,从而电极表面Sn元素特征衍射峰表现为向低结合能方向偏移。与空白电极（Nd0%）相比,改性后的电极（Nd3%）涂层表面Sb含量下降,且吸附氧（Oads）含量上升,为空白电极的1.6倍。EPR测试结果进一步证实了改性后电极性能提高的机制,Nd元素的引入,增加了电极涂层表面氧空位的浓度,使得电极涂层表面各元素的化学环境发生改变。掺杂改性后,电极的析氧电位以及产羟基自由基能力均得以提升,从而促使电极催化活性大大增强。     

Geochronology and geochemistry of eclogites from the Mariánské Lázne Complex, Czech Republic: Implications for Variscan orogenesis

The Mariánské Lázn complex (MLC) is located in the Bohemian Massif along the north-western margin of the Teplá-Barrandian microplate and consists of metagabbro, amphibolite and eclogite, with subordinate amounts of serpentinite, felsic gneiss and calcsilicate rocks. The MLC is interpreted as a metaophiolite complex that marks the suture zone between the Saxothuringian rocks to the north-west and the Teplá-Barrandian microplate to the south-east. Sm-Nd geochronology of garnet-omphacite pairs from two eclogite samples yields ages of 377±7, and 367±4 Ma. Samples of eclogite and amphibolite do not define a whole rock Sm-Nd isochron, even though there is a large range in Sm/Nd ratio, implying that the suite of samples may not be cogenetic. Eclogites do not have correlated _Nd values and initial ⁸⁷Sr/⁸⁶Sr ratios. Five of the eight eclogite samples have high _Nd values (+10.2 to +7.1) consistent with derivation from a MORB-like source, but variable ⁸⁷Sr/⁸⁶Sr ratios (0.7033 to 0.7059) which probably reflect hydrothermal seawater alteration. Three other eclogite samples have lower _Nd values (+ 5.4 to –0.8) and widely variable ⁸⁷Sr/⁸⁶Sr ratios (0.7033 to 0.7096). Such low _Nd values are inconsistent with derivation from a MORB, source and may reflect a subduction or oceanic island basalt component in their source. The MLC is an important petrotectonic element in the Bohemian Massif, providing evidence for Cambro-Ordovician formation of oceanic crust and interaction with seawater, Late Devonian (Frasnian-Famennian) high- and medium-pressure metamorphism related to closure of a Saxothuringian ocean basin, Early Carboniferous (Viséan) thrusting of the Teplá terrane over Saxothuringian rocks and Late Viséan extension.     

淹水条件对不同土壤中稀土元素钕形态分布的影响

以旱作条件为参照,研究淹水条件对钕形态分布的影响.结果表明,淹水条件对内源钕B1态(水溶态、可交换态与碳酸盐结合)、B2态(铁锰氧化物结合态)和B3态(有机质及硫化物结合态)的分布无显著影响.对于外源钕,淹水条件使B1和B3态浓度增加,而B2态浓度则因土壤性质而异,中性土壤中浓度稳定,酸性和碱性土壤中浓度分别增高和降低,其机制有待进一步研究;淹水条件对黄红壤和黄褐土中外源钕无显著影响,而砂姜黑土则相反;两种条件下,3种土壤中B2和B3态浓度顺序相同,B2态浓度顺序为:黄红壤黄褐土砂姜黑土,B3态浓度顺序为:砂姜黑土黄褐土黄红壤,而B1态在黄红壤中浓度最大;外源钕有进入残渣态的趋势,但并不明显,且不同土壤的各形态对残渣态的贡献不同.