Ni/Fe双金属对PCE脱氯影响因素研究

以四氯乙烯(PCE)为目标污染物, 利用批试验研究Ni/Fe双金属对氯代烃脱氯的影响因素.结果表明: (1)当参加反应的Ni/Fe双金属分别为10 g和20 g时, 反应速率常数k_obs分别为0.047 7 h-1和0.097 0 h-1, 说明增加参加反应的Ni/Fe双金属的质量可提高脱氯速率; (2)当粒度分别为20~ 40目、40~ 65目和80~ 100目时, k_obs分别为0.047 7 h-1, 0.059‥ 8 h-1和0.088 6 h-1, 说明选用Ni/Fe双金属颗粒越小脱氯速率越快; (3)当Ni/Fe质量比分别为0.024%, 0.048%和0.072%时, 所得k_obs分别为0.047 7 h-1, 0.066 2 h-1和0.073 4 h-1, 说明Ni/Fe双金属系统中Ni/Fe质量比越高脱氯效果越好, 但最优Ni/Fe质量比还有待于进一步研究.      

纳米镍/铁去除四氯乙烯的影响因素

氯代烃是地下水中最常检出的有机污染物之一,传统的处理方法需要很长时间与经费。近年来随着铁还原技术的发展,纳米铁和纳米双金属也是一个活跃的研究领域。本文利用批实验的研究方法以四氯乙烯(PCE)为目标污染物,研究纳米镍/铁在去除PCE过程中的影响因素。实验结果表明,暴露后的纳米Ni/Fe脱氯速率比不暴露时速率降低约4倍;反应温度是影响反应速率的一个重要因素之一,每升高10℃,反应速率常数kSA提高2~3倍;在一定范围内,Ni/Fe质量比越高,越利于脱氯反应的快速进行,当Ni/Fe的质量百分比为8%左右时,对氯代烃脱氯速率最快;反应液中的溶解…     

纳米镍/铁去除氯代烃影响因素的探讨

氯代烃是地下水中最常检出的有机污染物之一,传统的处理方法去除率很低。近年来随着铁还原技术的发展,纳米铁和纳米双金属也成为一个活跃的研究领域。利用批实验的研究方法以四氯乙烯(PCE)和四氯化碳(CT)为目标污染物,研究纳米镍/铁在去除PCE过程中的影响因素。实验结果表明,在碱性条件下,纳米Ni/Fe对PCE脱氯速率比在酸性和中性条件下脱氯速率更快;纳米Ni/Fe对初始浓度为6·51mg/L的PCE溶液脱氯速率是对初始浓度为20·56mg/L的PCE溶液脱氯速率的1·8倍;对于氯代程度相同的CT和PCE,对CT的脱氯速率明显快于对PCE。     

纳米镍-铁去除四氯乙烯的影响因素

氯代烃是地下水中最常检出的有机污染物之一,传统的处理方法需要很长时间与大量经费。本文利用批实验的研究方法以四氯乙烯(PCE)为目标污染物,研究纳米镍铁在去除PCE过程中的影响因素。实验结果表明,暴露后的纳米镍铁脱氯速率比不暴露时速率降低约4倍;反应温度是影响反应速率的重要因素之一,每升高10℃,反应速率常数kSA提高2～3倍;在一定范围内,镍/铁质量比越高,越利于脱氯反应的快速进行,镍/铁的质量比为8%左右时,对氯代烃脱氯速率最快;反应液中的溶解氧不利于纳米颗粒对氯代烃的降解。     

零价铁降解水中氯代烃的实验室研究

由于氯代有机溶剂的大量使用和使用氯气对饮用水消毒 ,致使四氯化碳 (CT)和四氯乙烯 (PCE)成为地下水和饮用水中常见的污染物 .利用廉价铁屑对CT和PCE进行还原性脱氯 ,对其动力学过程进行初步研究 ,并对影响反应速率的因素进行探讨 .结果表明 ,零价铁对氯代烃有明显的脱氯作用 ,相同氯代程度的烷烃和烯烃 ,烷烃的脱氯速度快 ,反应符合一级反应动力学方程 ,反应是准一级反应 ,反应速率受到传质速率即零价铁比表面积的影响 .     

天然地下水环境四氯乙烯的强化生物降解

采用批实验方法, 以天然地下水为基础培养液, 利用在实验室条件下培养驯化的微生物, 以醋酸作为共代谢基质, 加入酵母粉提供氮源, 研究了四氯乙烯(PCE) 的降解效果.研究表明, 通过强化影响PCE降解的某些因素, 在20℃的地下水环境中, PCE可以很快转化为三氯乙烯(TCE), 并可以进一步转化为二氯乙烯(DCEs), 但没有检测到DCEs的脱氯产物.PCE的脱氯速率为0.1848d-1, 半衰期为3.75d.亦研究了低温环境下PCE的降解效果.结果表明, 在低温环境下, PCE也可以发生生物降解, 但是脱氯速率相对较慢, 为0.0761d-1, 半衰期为9.11d, 且终产物为TCE.      

利用扫描电镜技术研究纳米Ni-Fe颗粒对四氯化碳快速脱氯的机理

纳米铁具有高的比表面积和高反应活性,能快速将氯代烯烃还原成无毒氯离子、乙烯和乙烷,但对于氯代烷烃的脱氯仍能产生大量的氯代中间或最终产物,可以通过合成制得纳米双金属提高脱氯速率和减少氯代中间产物。本文利用扫描电镜测得实验室制备的纳米Ni-Fe(2%,质量分数)颗粒直径为20~60 nm,通过批实验方式对纳米Ni-Fe降解四氯化碳的反应动力学性质、产物、持久性能和反应机理进行了探讨。结果表明,纳米Ni-Fe体系主要最终产物为42%CH4和17%CH2Cl2。与铸铁屑和纳米铁相比,纳米Ni-Fe由于催化脱氯加氢,显著提高了氯代烃脱氯速率,同时降低了有毒氯代产物的产量,且Ni作为催化剂不会进入水体引起二次污染。纳米Ni-Fe颗粒在空气中具有很好的稳定性,虽然降解四氯化碳的最终产物CH4与纳米Pd-Fe相比少13%,但由于价格便宜,有望在工程上应用于氯代有机化合物水土污染治理。     

零价铁降解水中氢代烃的实验室研究

由于氯代有机溶剂的大量使用的使用氯气对饮用水消毒，致使四氯化碳（CT）和四氯乙烯（PCE）成为地下水和饮用水中常见的污染物，利用廉价铁屑对CT和PCE进行还原性脱氯，对其动力学过程进步初步研究，并对影响反应速率的因素进行探讨。结果表明，零价铁对氯代烃有明显的脱氯作用，相同氯代程度的烷烃和烯烃，烷烃的脱氯速度快，反应符合一级反应动力学方程，反应是准一级反应，反应速率受到传质速率即零价铁比表面积的影响。     

不同基质共代谢降解地下水中四氯乙烯的研究

文中以甲醇、乙醇、甲酸盐、乙酸盐、乳酸盐和葡萄糖作为共代谢基质,利用某污水处理厂厌氧池中的污水(泥)作为接种物,对厌氧微生物进行培养和驯化,降解四氯乙烯(PCE)。实验结果表明,在厌氧污水(泥)和土壤混合环境下培养的微生物,以COD为培养指标,11d可培养成熟。6种基质均能使PCE还原脱氯降解成三氯乙烯(TCE)和1,1-二氯乙烯(1,1-DCE),PCE的降解均符合一级反应动力学方程,反应速率常数大小依次为K乙酸盐>K葡萄糖>K乳酸盐>K乙醇>K甲酸盐>K甲醇,其中乙酸盐是最有效的共代谢基质,其反应速率常数为0·6632d-1。     

硫化亚铁矿物的生物合成及其对六溴环十二烷的还原脱溴研究

选用两种不同的硫酸盐还原菌(一种是嗜酸性硫酸盐还原菌Desulfosporosinus sp.,另一种是嗜中性硫酸盐还原菌Desulfomicrobium baculatum)合成了两种硫化亚铁(FeS)矿物,并采用BET、SEM、XRD、XPS对其进行表征。结果显示,嗜酸性硫酸盐还原菌合成的FeS矿物(S-FeS)比表面积为13.35 m2/g,铁硫原子比为0.91,表面活性组分FeS相对含量是63.6%;嗜中性硫酸盐还原菌合成的FeS矿物(Z-FeS)比表面积为7.64 m2/g,铁硫原子比为0.84,表面活性组分FeS相对含量为77.2%;两种FeS矿物的主要成分均为不定形FeS和结晶程度较差的四方硫铁矿。通过批处理实验,研究了这两种FeS矿物对六溴环十二烷(HBCD)的还原脱溴效果。结果显示,两种FeS体系下HBCD的还原脱溴反应均遵循假一级反应动力学;反应速率常数随着FeS浓度的增加而增加,当FeS的浓度从0.3 g/L增加至1.2 g/L时,S-FeS和Z-FeS转化HBCD的反应速率常数分别从0.0049 h–1增至0.3194 h–1和0.3868 h–1;反应体系p H值(4~8)的变化极大地影响FeS对HBCD的还原脱溴效率;两种FeS均能还原转化HBCD的三种主要同分异构体,转化率大小依次为β-HBCDγ-HBCDα-HBCD;在两种FeS反应体系中均检测出四溴环十二碳烯(C12H18Br4)、二溴环十二碳二烯(C12H18Br2)和环十二碳三烯(C12H18)等HBCD还原脱溴的中间产物(GC-MS方法鉴定),由此推测S-FeS和Z-FeS还原脱溴HBCD的途径均为逐步邻位双脱溴。以上研究结果表明,两种不同类型硫酸盐还原菌合成的FeS矿物均具有还原脱溴HBCD的能力,并且它们的还原脱溴的能力和机制差异不大。     

The terrestrial fauna of the Late Triassic Pant-y-ffynnon Quarry fissures,South Wales,UK and a new species of Clevosaurus (Lepidosauria: Rhynchocephalia)

Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.     

Définition d'une limite multicritère ; stratigraphie du passage Campanien–Maastrichtien du site géologique de Tercis (Landes,SW France)Definition of a multi-criteria boundary; stratigraphy of the Campanian–Maastrichtian interval of the geological site at Tercis (Landes,SW France)

Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.     

The effect of water on accessory phase solubility in subaluminous and peralkaline granitic melts

The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H₂O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H₂O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.     

Quaternary stresses revealed by calcite twinning inversion: insights from observations in the Savonnières underground quarry (eastern France)

Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ₁ roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).     

NONMETALS DEPOSITS

正20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.)     

MATHEMATICAL GEOLOGY

正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology,     

PROSPECTING EXPLORATION

正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.)     

STRUCTURAL GEOLOGY

正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se-     

STRUCTURAL GEOLOGY

正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with