仿骨盐吸附剂的合成及其在脱除重金属方面的应用

本文通过对比固态CaHPO4直接水解法和高浓度化学沉淀法,在低饱和状态下合成了羟基磷灰石.通过等离子发射光谱(ICP)、X射线衍射(XRD)、红外光谱(IR)、热重(TG)以及扫描电镜(SEM)对其进行了表征,考察了其在脱除重金属方面的应用.结果表明:所得产物的组成和形貌均与人骨相似,为缺钙的碳酸盐型羟基磷灰石;其对高浓度的Hg2+、Pb2+、Cd2+、Cr3+和低浓度的Pb2+、Cd2+、Cr3+有较强的吸附,对Cr2O72-和AsO33-则没有吸附作用.     

塔里木盆地塔中I号坡折带中上奥陶统台缘礁滩体储层主控地质因素分析

中晚奥陶世塔中I号坡折带处于台地边缘相带的礁滩镶边体系中,发育了多个礁(丘)、滩的沉积旋回组合,总厚达100~300m,其单个旋回的礁、滩体皆为有利的油气储集体。研究表明,该区礁滩体岩性、岩相的组合是储层发育的重要基础;礁型岩性地貌隆起和海平面相对变化所控制的成岩早期暴露溶蚀是控制储层发育分布的主要因素;多期油气运聚及其伴随的埋藏溶蚀作用的改造改善了礁滩体储层孔隙的储集性能;后期构造破裂作用增加了礁滩体储层的连通性和渗透能力。     

Thermal simulation experiment on the hydrocarbon regeneration of marine carbonate source rock

Hydrocarbon regeneration of marine carbonate source rock was simulated with thermal experiments in a laboratory. The results reveal that hydrocarbon regeneration does not simply continue the primary hydrocarbon generation process, and that, for marine carbonate source rock, discontinuous hydrocarbon generation differs greatly from the continuous generation. Several different features of hydrocarbon regeneration were observed in the experiments. First, the liquid hydrocarbon generation peak was always observed no matter what the initial maturity of the sample was. Moreover, the maturity and the liquid hydrocarbon yield corresponding to the peak varied with the sample’s initial maturity. Second, the hydrocarbon regeneration started earlier than the continuous one. In the experiments, the hydrocarbon could be re-generated when the sample maturity did not rise to any great extent. Third, the accumulative hydrocarbon-generating quantity during discontinuous generation was always more than that during continuous generation. And the hydrocarbon-generating quantity varied with the discontinuous generation history. Chemical kinetic analysis suggests that discontinuous hydrocarbon generation should not only be explained by the parallel reaction mechanism but also by the consecutive reaction mechanism which has been ignored in the traditional chemical kinetic model for continuous hydrocarbon generation.     

Main controlling factors of distribution and genetics of marine reservoirs in China

Marine reservoirs are mainly made up of clastics and carbonate reservoirs, which are distributed widely in central Tarim, Sichuan, Ordos basins from the Pre-Cambrian to Cenozoic, mainly in Palaeozoic. Marine clastic reservoirs are developed in foreshore and nearshore, tidal flat and delta environment. The sedimentary facies are important controlling factors for reservoir quality. Compaction, pressolution and cementation are factors of decreasing porosity, and low palaeo-temperature gradient, early emplacement of oil and gas and dissolution are favorable for preservation of pore. Carbonate reservoirs are divided into reef and bank, karst, dolomite and fracture reservoirs. Dolomitization, dissolution, TSR and fracture are important factors of controlling carbonate reservoirs＇ quality.     

电池联接方式对燃料电池/燃气轮机混合动力系统性能影响

为了研究不同电池联接方式对混合动力系统性能的影响,应用模块化建模的方法建立了混合动力系统模型.利用该模型分析了电池的燃料和氧化剂都采用串联以及燃料串联氧化剂并联2种不同电池联接模式下燃料电池及整个混合动力系统性能的变化.将所有电池都并联的联接方式作为参考,不同联接方式的结果与参考工况进行了比较.结果表明,将电池的燃料和氧化剂都串联后电池堆可以被更好地冷却,电池堆内的温度分布更加均匀,系统的特性会有明显改善.     

怎样给孩子补钙？

1．钙剂不可与植物性的食物同吃。植物性的食物多数都含有草酸盐、碳酸盐、磷酸盐等盐类，会和钙相结合而妨碍钙的吸收。     

海南岛西北岸三万年前后浅海相地层的发现及其意义

在海南岛西北部神尖沿岸地区,广泛出露一套富含海相化石的粉细砂—砾石沉积层,组成了高达20米左右的沿岸台地。该地层中所含化石组合主要有海扇、曼氐孔楯海胆、舌骨牡蛎和个体很大的盖虫。根据岩性、沉积相及~(14)C年代数据可知,在距今三万年前后,这里是一个环境比较稳定的热带浅海湾。海水的温度比现在高。我国其它沿海地区,在0—-27米也普遍存在三万年前后的海相沉积层。不同的是,海南岛西北岸三万年前后的海相层,因受后期火山作用而被抬升至高于现代海面20米左右。