东胜砂岩型铀矿微量元素地球化学特征初探

近年来 ,鄂尔多斯盆地在石油和天然气勘查取得重大进展的同时 ,在盆地北部东胜地区也发现了可地浸砂岩型铀矿床 ,标志着我国地浸砂岩型铀矿勘查取得了重要突破。从微量元素地球化学入手 ,初步总结了东胜地区砂岩型铀矿的微量元素地球化学特征 ,与新疆伊犁和中亚典型的层间氧化带型砂岩铀矿进行了对比 ,分析探讨了铀成矿作用 ,认为东胜砂岩型铀矿成矿作用虽与氧化还原过渡带有关 ,也具外生和深源双重性质的微量元素组合 ,不同于单一的外生水成层间氧化带型砂岩铀矿 ,铀成矿过程中有深部物质和含煤层气或油气流体参与。     

我国寻找超大型陆相火山岩型铀矿床的潜力评估

国外早己发现了超大型陆相火山岩型铀矿床 ,但我国迄今尚末找到。我国有广泛分布的陆相火山岩 ,能否找到此类超大型铀矿床 ,这是当前火山岩铀矿地质工作者急待解决的重要课题。本文在剖析了世界上已发现的超大型陆相火山岩型铀矿床的成矿环境和成矿条件及我国大型陆相火山岩型铀矿床成矿特点的基础上 ,对我国陆相火山岩的时空分布规律及我国主要构造火山岩带成矿潜力作了评述 ,综合得出在我国找到超大型陆相火山岩型铀矿床是有可能的 ,并确认赣杭、南岭、燕辽、大兴安岭等构造火山岩带具备形成超大型陆相火山岩型铀矿床的地质条件。上述主要构造火山岩带与其它构造火山 ( -侵入 )岩带交汇重叠部位 ,是最有希望的突破区。     

地浸采铀技术与工艺

地浸采铀是世界上十分先进的采矿技术，其基本原理是对可地浸砂岩型铀矿按一定网度布置工艺钻孔，从注液注孔入地浸液，使地浸液与铀进行充分反应，经铀液孔提出地表，在地表工厂进行萃取铀的过程，地浸法分为酸法和碱法两种，地浸采铀能使低品位砂岩型铀矿成为有工业价值的矿床，由于对环境污染小，已被世界大多数国家广泛采用。但是并非所有的砂岩铀矿都能地浸，只有符合地浸地质-水文评价指标的砂岩铀矿才能地浸。地浸工艺包括钻孔的布置、浸液的配制、地下水的复原和环境保护等方面。我国的地浸采铀于20世纪70年代开始探索，90年代中期开展了大规模的地浸砂岩铀找矿与开采工作，并取得了突破性进展，新疆512矿床是就是利用地浸技术评价与开采的我国第一座大型地浸铀矿山。     

Airborne C1- and C2-halocarbons at four representative sites in Europe

Air concentratiions of trichlorofluoromethane, trichloromethane, tetrachloromethane, 1,1,2-trichloro-1,2,2-trifluoroethane, 1,1,1-trichloroethane, trichloroethene and tetrachloroethene have been determined at four sites: a medium-sized (80, 000 inhabitants), moderately industrialized city in southwest Germany, a mountain forest site in the northern Black Forest, a suburb south of Lisbon at the Atlantic coast of Portugal, and a truly remote oceanic site, the island of Madeira. As expected, there are large differences in the concentrations of those halocarbons which find wide technical applications and have relatively short atmospheric lifetimes; moderate or small differences are found for those with small anthropogenic sources—chloroform and tetrachloromethane. Chloroform tends to be higher at the marine sites, suggesting that it arises from natural sources.     

浙江大桥坞铀矿床铅、氢、氧同位素研究

浙江大桥坞矿床是赣杭火山岩铀成矿带重要的铀矿床之一。本文通过对大桥坞铀矿床铅、氢和氧同位素及前人资料的综合研究,探讨了矿床成矿流体和成矿物质来源。结果表明花岗斑岩、凝灰岩、辉绿岩、矿石中黄铁矿、蚀变围岩中黄铁矿的Pb同位素组成变化较小,可能指示它们具有相似的源区。在铅同位素构造环境判别图解中,铅同位素投影点分布范围较广,但多数集中于地幔和造山带演化线之间,偏向造山带,反映了铅的来源与岩浆活动有关。氢、氧同位素组成显示,成矿流体主要来自大气降水。成矿物质来源于壳幔混合源。     

培养条件下酵母菌吸附铀的研究

研究在培养条件下对活酵母菌吸附铀的能力作了初步研究。利用偶氮胂Ⅲ作为显色剂采用分光光度法测定铀浓度的变化,结合标准曲线计算生长曲线,对酵母生长的抑制及吸附率。结果表明:酵母菌生长曲线基本符合S型生长曲线模型;低铀浓度、短培养时间时铀对酵母菌生长起促进作用,当铀浓度达到0.6mg/mL时才明显表现为抑制作用;铀浓度对吸附率的影响曲线符合典型的吸附等温线模型,随着铀浓度增大,吸附量总趋势增大;在培养条件下酵母菌对铀的处理以6～10h为佳;在低铀浓度下,铀的吸附可由Langmuir和Freundlich吸附模型模拟。     

Biologische Wirkungen der Bestrahlung mit schweren Ionen

Experiments with accelerated heavy ions may contribute to the understanding of biological radiation action. After outlining the theoretical background experiments are described which were carried out at the UNILAC-machine (Gesellschaft für Schwerionenforschung, Darmstadt, Germany) where ions up to uranium can be accelerated to maximal specific energies of 10 MeV/u. Yeast cells served as biological test systems with the synthesis of ribosomal RNA (r-RNA), colony-forming ability and mutation induction as experimental endpoints. A relationship between action and energy deposition by individual particles can be demonstrated for the inhibition of r-RNA synthesis, in other cases the ion energy plays also an important role indicating that the interaction of δ-electrons from different particles contributes significantly to the biological effect.     

老挝铁矿资源与成矿预测

经资料整理与实地调研:老挝已发现铁矿床(点)42处。重要矿床为万象省(P.Vientiane)万荣(Vangviang)铁矿、川圹省(P.Xiangkhouang)富诺安(Phou.Nhouan)铁矿、万象省(P.Vientiane)帕莱(Pha Lek)铁矿、甘蒙省(P.Khammouan)班农洛(Ban Nonglao)铁矿。重要矿床的矿体呈似层状、脉状产出,矿石质量较好,矿床属接触交代矿床、热液矿床。据地层条件、岩浆岩条件、构造条件、铁矿床(点)的分布情况,老挝划分出琅勃拉邦(Louangphabang)、孟佩(Muang Pek)、桑怒(Xam-Nua)3个成矿预测区。     

与黑色岩系有关矿床研究进展

与黑色岩系有关矿床近年来在国内外研究中都取得了重要进展。黑色岩系不但是许多金属元素的重要来源，而且其本身也具有经济价值，但在开采利用中应注意环境保护。黑色岩系可以形成于还原环境，也可以形成于较为氧化的环境。黑色岩系中的矿床有些与生物作用有关，有些属于后生矿床，有些则与海相火山-喷气活动有关。除了本身含矿外，黑色岩系还可为其它类型金属矿床提供成矿物质或提供有利的成矿条件。     

花岗岩铀地球化学特征新认识——以赣南富城产铀花岗岩体为例

对富城花岗岩U、T h含量分析结果进行的频数统计分析表明富城花岗岩U的均值为8.92×1-0 6、众数为8.0×10-6、中位数为7.03×1-0 6,其概率密度曲线偏向高端呈右偏非对称分布(偏度系数CSK=1.10)。T h的均值、众数和中位数三者一致,分别为25.7×10-6,25.75×10-6,25.8×1-0 6,其概率密度曲线呈对称正态分布(偏度系数CSK=0.11)。核诱发裂变径迹研究查明富城花岗岩中铀有4种存在形式:(1)显微粒状铀矿物(晶质铀矿);(2)以类质同像形式存在于锆石、磷灰石等副矿物之中;(3)均匀分散赋存在造岩矿物晶格之中的结构铀;(4)沿造岩矿物(长石、石英)微裂隙及粒间分布的非结构铀。对富城花岗岩铀配分研究发现,赋存在造岩矿物中均匀分散状的结构铀含量与全岩铀不呈消长关系,而是存在一定的极限值:长石、石英<3×1-0 6,白云母<5×10-6,黑云母<9×10-6。溶浸实验结果表明,富城花岗岩活动性铀浸出率很高(平均值52%),为富城花岗岩具有较大铀成矿潜力提供了佐证。     

The evolution of Müllerian mimicry

It is now 130 years since Fritz Müller proposed an evolutionary explanation for the close similarity of co-existing unpalatable prey species, a phenomenon now known as Müllerian mimicry. Müller's hypothesis was that unpalatable species evolve a similar appearance to reduce the mortality involved in training predators to avoid them, and he backed up his arguments with a mathematical model in which predators attack a fixed number (n) of each distinct unpalatable type in a given season before avoiding them. Here, I review what has since been discovered about Müllerian mimicry and consider in particular its relationship to other forms of mimicry. Müller's specific model of associative learning involving a "fixed n" in a given season has not been supported, and several experiments now suggest that two distinct unpalatable prey types may be just as easy to learn to avoid as one. Nevertheless, Müller's general insight that novel unpalatable forms have higher mortality than common unpalatable forms as a result of predation has been well supported by field experiments. From its inception, there has been a heated debate over the nature of the relationship between Müllerian co-mimics that differ in their level of defence. There is now a growing awareness that this relationship can be mediated by many factors, including synergistic effects between co-mimics that differ in their mode of defence, rates of generalisation among warning signals and concomitant changes in prey density as mimicry evolves. I highlight areas for future enquiry, including the possibility of Müllerian mimicry systems based on profitability rather than unprofitability and the co-evolution of defence.     

陇东高原全新世黄土古土壤沉积序列辐射环境研究

通过对泾河上游陇东高原两个全新世黄土古土壤沉积序列剂量率的分析,发现全新世剖面中剂量率值的变化分别受到了沉积粉尘物质组成的变化和易淋溶元素迁移的影响。前者对剂量率的影响非常微弱;后者的影响相对较大。同时剖面内部剂量率的绝对值变化较小。Fe/Al值的变化也表明了整个全新世黄土古土壤剖面中沉积粉尘的物质组成变化极小,指示了研究区域沉积物源在全新世近万年时间尺度内是相对较稳定的。     

环境污染物浓缩铀诱发雄性机体的生殖毒性研究

在不同水平浓缩铀￣（２３５）ＵＯ＿２Ｆ＿２内污染诱发机体生殖毒性的研究中，观察到浓缩铀可诱发精子畸形，主要呈现双头和无钩精子。浓缩铀诱发精原细胞染色体畸变，则以染色体断片为主，对初级精母细胞可产生染色体断片和易位，出现多价体。浓缩铀可致精子ＤＮＡ链断裂，其断裂片段则可随￣（２３５）ＵＯ＿２Ｆ＿２摄入量的加大而增多，浓缩铀引起遗传物质的损伤，可诱发胎鼠显性致死突变和骨骼畸形增生，而其诱发骨骼畸形的发生率则与睾丸浓缩铀的摄入量呈正相关。     

核探测技术在粤北下庄铀矿田找矿中的应用研究

对粤北下庄铀矿田希望矿床(330矿床)进行了土壤天然热释光、氡气和地面γ能谱三种核探测技术的测量工作,对它们在下庄花岗岩型铀矿田找矿中的应用效果进行了讨论,通过现场测量结果与地质研究成果的比较,初步总结出所测得的异常与矿体之间的空间关系。研究结果表明,这三种探测技术在花岗岩地区进行铀矿的"攻深找盲"有较佳效果。     

Decolorization of Direct Black 22 by Aspergillus ficuum

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Black Sea beaches vulnerability to sea level rise

Integrated Coastal Zone Management (ICZM) aims to promote sustainable management of coastal zones based on ecosystem and holistic management approaches. In this context, policies have to consider the complex interactions that influence the fragile equilibrium of coastal ecosystems. Beaches represent both valuable and vulnerable natural resources because of the various ecosystem services they provide and their sensitivity to climate change and sea level rise.We present the first comprehensive digital record of all Black Sea beaches and provide a rapid assessment of their erosion risk under different scenarios of sea level rise. Through the digitisation of freely available remote-sensed images on the web, we provide broad information on the spatial characteristics and other attributes of all Black Sea beaches (e.g. photo-based visual estimation of the sediment type, presence of coastal defences, urban development). These data have been assembled and stored in full Spatial Data Infrastructure (SDI) – allowing spatial queries, visualisation and data sharing – and are therefore particularly interesting to feed/supply web-GIS portals (coastal atlases) for visualisation purpose, spatial queries or spatial indicators calculations.The resulting Black Sea beaches database contains 1228 beaches, with a total coastline length of 2042 km with an area of 224 km². The majority of the Black Sea beaches have been found to have small widths (61% have maximum widths less than 50 m), whereas 47% of all beaches presented coastal defence schemes, suggesting an already serious beach erosion problem.The erosion risk of the Black Sea beaches was assessed through the comparison of their maximum widths with estimations of the sea level rise-induced retreat by an ensemble of six 1-D analytical and numerical morphodynamic models. Following more than 17,000 experiments using different combinations of wave conditions, beach sediment textures and slopes and 11 scenarios of sea level rise (up to 2 m), the means (best fits) of the lowest and highest projections by the model ensemble were estimated; these were then compared to the maximum widths of the Black Sea beaches. The analysis showed that sea level rise will have highly significant impacts on the Black Sea beaches, as for a 0.5 m sea level rise 56% of all beaches are projected to retreat by 50% of their maximum width. For a 0.82 m sea level rise (the high IPCC estimate for the period 2081–2100) about 41% are projected to retreat by their entire maximum width, whereas for 1 m sea level rise about 51% of all Black Sea beaches are projected to retreat by (drowned or shifted landward by) their entire maximum width, if the high mean of the model ensemble projections is used.Results substantiate the risk of beach erosion as a major environmental problem along the Black Sea coast, which therefore needs to be taken into account in any future coastal management plans, as a matter of urgency. As these scenarios consider only sea level rise, they are considered to be conservative. Although the present results cannot replace detailed studies, the database and projections may assist Black Sea coastal managers and policy makers to rapidly identify beaches with increased risk of erosion, valuate accordingly coastal assets and infrastructure, estimate beach capacity for touristic development purposes, and rapidly assess direct and indirect costs and benefits of beach protection options. They also provide the necessary inputs to advance discussions relevant to the Black Sea ICZM.     

活性黑KN-B染料的生物降解研究

通过试验考察了厌氧条件下活性黑KN-B的生物降解历程,同时对染料的降解动力学及降解机理进行了初步探讨与分析。结果表明:厌氧颗粒污泥可以单独降解活性黑KN-B(以活性黑为单一碳源时,活性黑KN-B的24降解率为43.1%),也可以在以葡萄糖为共基质条件下降解活性黑KN-B;以活性黑KN-B为单一碳源时其降解过程符合一级反应动力学方程,而以葡萄糖为共基质时其降解过程符合二级反应动力学方程;对降解前和降解24h后的降解液采用UV一可见、红外光谱分析,用UV-可见光谱发现活性黑KN-B在可见光区600nm处的吸收峰已消失,并且紫外区309nm处的吸收峰减弱,但255nm处的吸收峰增强,说明活性黑KN-B染料中的偶氮键断裂后生成芳香胺类化合物,这些中间产物可进一步降解。用红外光谱分析,结果与UV-可见光谱分析一致。     

海拉尔盆地地下水铀的分布特征及富集规律

通过采集海拉尔盆地地表水样品12件,地下水样品67件,运用Durov图、等值线图和铀形态计算理论,结合数理统计方法,分析研究区域地下水铀的分布特征和赋存形态,结果表明:海拉尔盆地赫尔洪德凹陷地区主要为HCO₃-Ca·Na型,蹉岗隆起、乌尔逊凹陷和贝尔凹陷地区主要为Cl-Na型和HCO₃-Na型,巴彦山隆起地区主要为HCO₃-Na型,红旗牧场和新宝力格凹陷主要为Cl-Na型.研究区域铀的分布范围为17~425μg/L,平均值为80μg/L,标准偏差为70μg/L,引发了区域地源性地下水铀污染问题.地下水中以UO₂(CO₃)₃^4-和UO₂(CO₃)₂^2-的主要形式存在,与Eh表现的氧化还原环境具有一致性,其中呼伦贝尔湖东南部属于地下水铀成矿有利区域.潜在铀成矿范围属于重碳酸铀酰占优势的HCO₃型含铀地下水,铀酰碳酸盐复合物应占主导地位,铀的溶解与HCO₃^-的增加有关,地下水中的铀存在参与碳酸盐岩和硫酸盐岩的混合溶滤作用的可能性,UO₂(CO₃)₃^4-、UO₂(CO₃)₂^2-、U₄O₉和沥青铀矿等处于饱和状态,总Fe和(Ca²⁺+Mg²⁺)浓度较低,各种水化学指标对铀富集具有指示意义,因此可将其视为潜在铀源的参考依据.     

华南东部主要铀矿区居民室内外氡浓度研究

对华南东部6个铀矿区居民室内外空气氡浓度及其变化规律进行了研究。矿区废渣和坑道口释放出来的氡气对周围大气形成了氡污染,特别是在矿区周围0.5～1.5 km的范围内的污染严重。但是空气中的这种氡污染随离矿区的距离增大而迅速减弱。矿区周围居民室内氡的浓度高,是广东省室内氡浓度平均值的10倍左右。在进行调查的190个居室中,有45个(23%)居室室内氡浓度超过美国环境保护局制定的148 Bq/m3室内氡浓度的上限值。居室中氡浓度的升高,除了受矿区释放出来的氡污染外,更主要是因本地区属高本底辐射区,房基下的土壤、岩石和建筑材料中的铀、镭等放射性元素的含量高,其放射性衰变产生的氡释放出来进入室内。      

Topo萃取铬天青s光度法测定废水中铀

研制了一种测定废水中微量铀的灵敏光度法。在硝酸酸性溶液中 ,用Topo 环己烷萃取铀 ,然后用碳酸铵溶液反萃取铀 ,在CTAB存在下 ,用铬天青s与铀生成蓝色络合物 ,其最大吸收波长在 62 5nm ,摩尔吸光系数达 9 5 0× 10 4。0～ 17μg 2 5mL铀遵守比尔定律。该方法用于测定废水中的铀 ,获得了满意的结果