Numerical Simulations of the Transparency of Waterfront Bodies

Measured field data was used to analyze the factors which influence the transparency of the Nei River and to develop a multi-factor correlation for the transparency. A 2-D unsteady model which coupled analyses of the water flow, water quality, suspended sediments, and Chl-a was developed to simulate the changes in the transparency for various conditions. The model was then used to forecast the transparency of the Nei River. The suspended sediment concentration （SSC） was found to be the most important factor influencing the transparency, with high concentrations of CODMn and Chl-a also reducing the transparency to some extent. The transparency model is stable and precise, with relative errors between measured and calculated values of less than 15%. With the environmental scheduling schemes, the Nei River transparency can be significantly improved with a mean transparency in high-water years of 69.3 cm, normal-water years of 70.8 cm, and low-water years of 69.8 cm.     

塔里木盆地库车坳陷砂岩型铀矿成矿潜力分析

库车坳陷位于塔里木盆地北缘,新近系库车组出露面积广,沉积厚度大,为客观认识塔里木盆地库车坳陷新近系库车组的成矿潜力,通过对成矿地质条件分析认为,上新统库车组发育以河流相为主的一套杂(红)色陆相碎屑岩系,具有有利的泥-砂-泥结构; 构造抬升控制着砂岩型铀成矿作用的发生,成为地层中铀活化、淋滤的有利通道; 盆地北缘蚀源区的下元古界绿片岩,下二叠统火山岩及凝灰岩和华力西中、晚期花岗岩体提供丰富的铀源; 具有完善的地下水动力系统,补-径-排体系完善; 铀成矿与含油气构造具有空间上的一致性,油气参与了铀成矿,发育的深大断裂沟通了深部烃源岩与上部圈闭,盆地深部油气逸散的有利地带,为砂岩型铀矿成矿提供了还原障; 同时盆地具有有利的地形地貌条件。由此推断,塔里木盆地库车坳陷砂岩型铀矿成矿条件较好,可作为有利的勘查目标区。     

塔西南昆仑山前地区晚白垩世沉积演化

为阐明塔里木盆地昆仑山前地区晚白垩世沉积演化,以野外实测剖面为基础,结合样品分析测试,综合井下资料分析,结果表明:昆仑山前地区上白垩统自下而上可分为库克拜组、乌依塔克组、依格孜牙组及吐依洛克组,其中,库克拜组可分为"下红上绿"两段,下红段为棕红色砂泥岩、上绿段为灰绿色泥岩夹灰岩,乌依塔克组和吐依洛克组岩性类似,均为红色的含膏砂泥岩,依格孜牙组以"红灰岩"为特征。各组地层自西向东均有减薄趋势。上白垩统沉积时期发生2次大规模的海侵-海退,每个组段发育有典型而又相对单一的沉积相类型,自下而上发育辫状河三角洲(库克拜组)-潮上蒸发砂泥坪(乌依塔克组)-碳酸盐岩台地(依格孜牙组)-潮上蒸发砂泥坪(吐依洛克组)。