某石墨矿保护石墨片度的选矿试验研究

石墨片度的大小,对其工业价值有很大的影响。鳞片越大,工业价值越高.所以,石墨矿在选矿过程中,在保证精矿质量的前提下,如何采取措施,保护石墨鳞片,多生产正目产品,以获取最佳的经济效益,是首先要考虑的问题。

坦桑尼亚纳钦圭阿石墨成矿带地质特征及成因初析

纳钦圭阿石墨成矿带位于坦桑尼亚南部林迪—姆特瓦拉地区,近年来发现一系列大型、超大型优质晶质石墨矿,尚未见系统报道。该成矿带东西宽约40 km,南北长约120 km,区域岩性为一套中高变质的片麻岩、片岩、石英岩、大理岩、角闪岩等,局部混合岩化强烈。地层呈NE—NEE向展布,局部平卧褶皱、鞘褶皱等发育,断裂构造以NE向为主,多顺层产出,NW向断层常错断石墨含矿地层。石墨矿体呈层状、似层状产出,发育多层矿体。矿体规模沿走向延伸从500 m~10 km,矿体群宽度100~500 m,单矿体厚度2~100 m。矿石类型以片岩型、片麻岩型为主,在石英岩、大理岩、伟晶岩中常见石墨矿化。围岩与夹石主要有片岩、片麻岩、大理岩、角闪岩等。原矿石墨片径多为0.10~2.40 mm,+100目含量大多大于95%,+50目含量大于67%,精矿石墨片径+100目含量为54%~75%,+50目含量为12%~49%。石墨矿石主量元素具有富铝硅贫钙的特征,根据地球化学原岩恢复图解投点,原岩为一套含碳、富铝的泥砂质沉积建造,可能混入少量火成岩。初步分析认为,纳钦圭阿成矿带晶质石墨矿床成因属于区域变质型矿床,成矿物质来源主要为原岩中的有机碳。

Effects of Carbide Formation in Graphene Growth

Besides carbon solubility, the carbide formation possibility is another important factor to differentiate various substrate materials in graphene growth. A recent experiment indicates that the formation of transition metal carbides （TMCs） can suppress carbon precipitation. In this study, Mo2C, a representative of TMCs, is used to study the effects of carbide formation in graphene growth from first principles. Carbon diffusion in Mo2C bulk turns out to be very difficult and it becomes much easier on the Mo2C（001） surface. Therefore, carbon precipitation suppression and graphene growth can be realized simultaneously. A direction depended diffusion behavior is observed on the Mo2C（101） surface, which makes it less favorable for graphene growth compared to the （001） surface.