锶盐废渣含硫状态分析及硫含量的测定

锶盐废渣中硫的状态及含量不同其作用大不相同,有的呈现活性导致膨胀破坏,而有的则表现为惰性,因此有必要了解硫的存在状态及含量。分析表明锶盐废渣中硫主要以硫酸盐硫(SO3)和硫化物硫(S2-)两种形式存在。选择硫酸钡重量法和碘量法进行化学测定,然后用X-射线能谱仪进行元素定性分析;并将化学分析和仪器测定两种方法进行对比。结果表明,X-射线能谱法可以快捷、方便地探测锶渣所含各种元素,但不能确定元素的价态;化学分析方法可得到相对准确的元素含量;用硫酸钡重量法和碘量法联合测定锶渣中的硫含量,与X-射线能谱法相比,偏差仅为0.37%。     

Virtual phosphorus ore requirement of Japanese economy

Phosphorus is indispensable for agricultural production. Hence, the consumption of imported food indirectly implies the import of phosphorus resources. The global consumption of agricultural products depends on a small number of ore-producing countries. For sustainable management of phosphorus resources, the global supply and demand network should be clarified. In this study, we propose the virtual phosphorus ore requirement as a new indicator of the direct and indirect phosphorus requirements for our society. The virtual phosphorus ore requirement indicates the direct and indirect demands for phosphorus ore transformed into agricultural products and fertilizer. In this study, the virtual phosphorus ore requirement was evaluated for the Japanese economy in 2005. Importantly, the results show that our society requires twice as much phosphorus ore as the domestic demand for fertilizer production. The phosphorus contained in “eaten” agricultural products was only 12% of virtual phosphorus ore requirement.     

浙江建德块状硫化物矿床地球化学特征及其成因意义

浙江建德块状硫化物矿床，以Cu＞Zn＞Ph为特征。鉴于Cu、Ph和Zn三元素的地球化学行为和海底喷流作用的固有特性，它们在横向上和纵向上均具独特的分带性，显示出旋回结构。对黄铁矿中特征元素元素比值、成矿温度以及铅同位素组成等方面的研究表明，该矿床乃同生沉积作用的产物，而非岩浆热液成矿。     

Impact of microbial communities from tropical soils on the mobilization of trace metals during dissolution of cinnabar ore

Biodissolution experiments on cinnabar ore(mercury sulphide and other sulphide minerals,such as pyrite) were performed with microorganisms extracted directly from soil. These experiments were carried out in closed systems under aerobic and anaerobic conditions with 2 different soils sampled in French Guyana. The two main objectives of this study were(1) to quantify the ability of microorganisms to mobilize metals(Fe, Al, Hg) during the dissolution of cinnabar ore, and(2) to identify the links between the type and chemical properties of soils, environmental parameters such as season and the strategies developed by indigenous microorganisms extracted from tropical natural soils to mobilize metals.Results indicate that microbial communities extracted directly from various soils are able to(1) survive in the presence of cinnabar ore, as indicated by consumption of carbon sources and,(2) leach Hg from cinnabar in oxic and anoxic dissolution experiments via the acidification of the medium and the production of low molecular mass organic acids(LMMOAs). The dissolution rate of cinnabar in aerobic conditions with microbial communities ranged from 4.8 × 10~(-4) to 2.6 × 10~(-3) μmol/m~2/day and was independent of the metabolites released by the microorganisms. In addition, these results suggest an indirect action by the microorganisms in the cinnabar dissolution. Additionally, because iron is a key element in the dynamics of Hg, microbes were stimulated by the presence of this metal,and microbes released LMMOAs that leached iron from iron-bearing minerals, such as pyrite and oxy-hydroxide of iron, in the mixed cinnabar ore.     

鞍山市铁矿景观格局变化的遥感调查

采用1997和2007年2个时相的卫星遥感数据,对鞍山市城区周边铁矿典型景观类型的面积及其10年来的变化进行了遥感调查和分析。结果表明,国有矿山采矿场的面积相对稳定,边界无明显变化,民营矿山采矿场面积增加明显。采矿场面积变化与开采方式有关,国有矿山采用深凹露天开采,对地表破坏较轻,民营矿山采用山坡露天开采,对地表破坏较严重。排岩场的总面积有所增加,个别矿区增加明显。复垦绿地有大幅度增加,但仍低于排岩场扩张的速度。     

北武夷下汪家铜多金属矿床地质特征及成因分析

下汪家铜多金属矿床形成于燕山晚期，成矿流体主要来自岩浆期后热液，断裂和岩浆岩是两大重要的成矿条件。控矿构造为北北东向断裂。成矿流体和主要矿质均源于地球深部，以上地幔或壳幔混合带为主，与燕山晚期富碱岩浆活动密切相关。下汪家铜多金属矿床成因上的分析，对该区下一步的找矿工作具有指导意义。     

利用铜矿尾砂研制低强度可控性填料

利用铜矿尾砂、粉煤灰、水泥以及加气剂等,混合搅拌成泥浆体,振动成型,制备出低强度可控性填料(CLSM).试验表明:以水泥12.9％、铜矿尾砂(细集料)22.6％、加气剂3.2％、粉煤灰12.9％等工业废弃物,加水48.4％,固液比控制在(14～15):(15～16)之间,制得的CLSM制品,抗压强度0.35～2.00 ...     

厂坝铅锌矿床中钠长石岩的成因探讨

厂坝铅锌矿床中钠长石岩的产状、常量元素、微量元素、稀土元素和放射性同位素等地质地球化学特征表明．该岩石为中泥盆统成矿流体在海底沉积和交代围岩形成的典型热液沉积岩——钠长石岩，其物质来自矿体的下状沉积地层柱和海水。该沉积岩在后期的强烈变质改造过程中，发生了重结晶作用。     

层控矿床的成岩成矿

本文从成岩分异,成岩交代,自生、脱水、泄水、压实、挤压、扩散和胶结作用等方面,论述层控矿床的成岩成矿作用。     

与玢岩铁矿有关的两类蚀变再认识

长江下游陆相火山岩地区分布着规模巨大的玢岩铁矿及其有关蚀变岩石,铁矿形成后普遍受到古风化淋滤和剥蚀作用的影响,并在浸蚀面上堆积的火山碎屑岩层的底部,发育有含铁矿石和蚀变岩石角砾的碎屑岩层。在此基础上又生成一套直接受火山作用控制的蚀变,称为火山蚀变,它在火山碎屑岩中分布很广泛,其中有黄铁矿化、黄铜矿化、明矾石化、硬石膏化、叶腊石化、硅化、高岭土化和水云母化等。上述两类蚀变是不同时期不同地质作用的结果,在成因上没有直接关系。