全球变暖、构造运动与沙漠化

采用统计分析与综合分析方法 ,研究了全球变暖、构造活动、地球 (以及月球和行星 )轨道效应、太阳活动等对降水的影响。认为构造活动、地震、气候变暖与降水或洪涝灾害有一定关系 ;地球的轨道效应是地球气候变化的重要因素 ,从而与旱涝相关 ;月球行星轨道效应和太阳活动均与旱涝有明显的对应关系。气候变冷和构造活动变弱是沙漠化的主要原因 ,人类活动则加速了沙漠化的进程     

宁强碳质球粒陨石的岩石、矿物特征研究

宁强碳质球粒陨石的结构复杂,有粒状、斑状和炉条状等结构。球粒分为玻璃质和晶质两种。聚合体含量丰富、形态各异,有钢性和塑性两种聚合体。目前已查明的矿物有20余种,主要是镁橄榄石、贵橄榄石、烦火辉石、普通辉石和黄长石类矿物等。在宁强陨石中出现罕见的方解石、白云石。不透明矿物有陨硫铁、铁纹石—镍纹石、镍铁矿、磁铁矿和非晶质碳质。Fe/SiO_2为0.71—0.72,SiO_2/MgO为1.37—1.40。根据化学及矿物特征,该陨石应属C_2群。     

Mapping and compositional analysis of mare basalts in the Aristarchus region of the Moon using Clementine data

The process of accurately defining and outlining mare basalt units is necessary for constraining the stratigraphy and ages of basalt units,which are used to determine the duration and the flux of lunar volcanism.We use a combination of Clementine’s five-band ultraviolet/visible data and TiO2and FeO abundance distribution maps to define homogenous mare basalt units and characterize their compositional variations(with maturity)in the Aristarchus region.With 20 groups of distinct mare basaltic soils identified using the method in this paper,six additional spectrally defined areas and five basaltic units are constructed,and their mineralogic quantization values provide new constraints on their temporal and spatial evolution.Our results indicate that the Aristarchus region has diverse basalt units and a complex history of volcanic evolution.We also demonstrate that the techniques,from which spectrally distinct mare basalts can be mapped,performed well in this study and can be confidently expanded to other mare regions of the Moon.     

混合暴露条件下刺参(Apostichopus japonicus)对重金属的富集与释放特征

应用双箱动力学模型模拟了刺参在Pb、Zn、Cu、Cd、Cr、Hg和As 7种重金属混合暴露条件下,呼吸树、消化道和体壁组织对重金属的生物富集与释放实验。结果表明:(1)重金属在刺参组织器官中的富集具有选择性,理论平衡状态下,As、Cd、Cr在各组织的含量分布(CAmax):呼吸树消化道体壁,Cu、Zn分布规律(CAmax):消化道呼吸树体壁,Hg、Pb分布规律(CAmax):体壁呼吸树消化道。(2)刺参对不同重金属的富集系数存在显著差异(P0.05),呼吸树组织对Cr离子富集系数最高2298.2,其次是Cu、Cd离子,其BCF均在1500以上,Hg、Pb、Zn和As离子在呼吸树中的富集系数较低。体壁对Cu离子的富集系数最高为1560.7,对As离子富集系数最低52.7。消化道对Cu离子富集系数最高6037,对As离子富集系数最低为87.9。