云南白秧坪铜银矿床Cu、Ag迁移形式探讨

在野外地质研究的基础上,采用地球化学热力学方法研究了Cu、Ag的迁移形式。研究结果表明,铜在热液中主要以CuCl42-、Cu(H2O)42+、Cu(S2O3)46-、CuS46-、Cu(HS)42-、Cu(SbS3)410-形式迁移;银在热液中主要以AgCl2-、Ag(S2O3)23-、Ag(HS)2-、AgS23-、Ag(SbS3)25-形式迁移。铜银矿床是在含矿热液物理化学条件发生改变的情况下铜银化合物发生解析作用而成。     

Body mass estimations for <Emphasis Type="Italic">Plateosaurus engelhardti</Emphasis> using laser scanning and 3D reconstruction methods

Both body mass and surface area are factors determining the essence of any living organism. This should also hold true for an extinct organism such as a dinosaur. The present report discusses the use of a new 3D laser scanner method to establish body masses and surface areas of an Asian elephant (Zoological Museum of Copenhagen, Denmark) and of Plateosaurus engelhardti, a prosauropod from the Upper Triassic, exhibited at the Paleontological Museum in Tübingen (Germany). This method was used to study the effect that slight changes in body shape had on body mass for P. engelhardti. It was established that body volumes varied between 0.79 m³ (slim version) and 1.14 m³ (robust version), resulting in a presumable body mass of 630 and 912 kg, respectively. The total body surface areas ranged between 8.8 and 10.2 m², of which, in both reconstructions of P. engelhardti, ∼33% account for the thorax area alone. The main difference between the two models is in the tail and hind limb reconstruction. The tail of the slim version has a surface area of 1.98 m², whereas that of the robust version has a surface area of 2.73 m². The body volumes calculated for the slim version were as follows: head 0.006 m³, neck 0.016 m³, fore limbs 0.020 m³, hind limbs 0.08 m³, thoracic cavity 0.533 m³, and tail 0.136 m³. For the robust model, the following volumes were established: 0.01 m³ head, neck 0.026 m³, fore limbs 0.025 m³, hind limbs 0.18 m³, thoracic cavity 0.616 m³, and finally, tail 0.28 m³. Based on these body volumes, scaling equations were used to assess the size that the organs of this extinct dinosaur have.     

海洋费氏弧菌培养条件的研究

以本室保存的一株海洋费氏弧菌作为实验对象,采用单因素试验方法研究培养基起始pH值、盐浓度和摇瓶装液量等因素对菌株生长的影响,利用分光光度法测定其生长曲线,采用均匀设计方法,对该菌的培养基组分进行优化研究,确定其适合的生长条件,结果表明:当培养温度为30℃,通气量为180r/min时,该菌株在20h左右达到生长稳定期,对甘油的利用率要优于葡萄糖,盐浓度在5%以下时生长良好,最适装液量为60mL/250mL,培养液初始pH值为8.0。确定100mL培养基配方为:蛋白胨2g,酵母粉1.0g,氯化铵1.2g,氯化钠0.2g,磷酸二氢钾1.0g,此条件下可以得到最大的生物量。     

垃圾降解过程中脲酶测定条件优化

在土壤脲酶测定方法的基础上,以垃圾填埋场中的填埋垃圾为研究对象,通过单因素试验和正交试验对垃圾降解过程中脲酶活性测定方法进行优化。结果表明,垃圾降解过程中脲酶活性测定最优条件为:垃圾样品风干温度30℃,甲苯0.5mL,10%尿素1mL,0.1mol/LpH5.5柠檬酸钠缓冲液3mL,培养温度及培养时间分别为30℃和24h。优化后的的测定条件RSD小于0.82%,且测定值较传统方法提高30.48%～147.28%,表明该方法精密度高,可行性强。     

西南喀斯特流域枯季地下水电导率特征及水-岩作用分析

受特殊水文地质条件影响,西南喀斯特流域水动力过程与物质循环过程复杂,利用单一水文信息分析该地区水动力过程具有较大难度。地下水电导率受喀斯特水文地质条件影响显著,可以综合反映区域水动力条件与岩性特征。论文选取贵州普定县后寨河流域为研究区,通过野外调查及地下水电导率原位测定,结合流域地形、岩性及落水洞、岩溶泉等岩溶地貌空间分布规律,分析了喀斯特流域枯季地下水电导率空间分布及其受水-岩特征的影响。结果表明,山丘区地下水电导率较低,主要由于喀斯特山区是岩溶裂隙/管道网络发育的强径流区,水-岩接触时间较短。随高程降低,地下水电导率呈现增加趋势,表明地下水流速度减缓,水-岩接触时间变长。地下水电导率受岩性特征影响显著,石灰岩区水-岩作用强烈,易形成较高电导率地下水,平均电导率650 μS/cm,白云岩区水-岩作用减弱,地下水电导率降低,平均值523 μS/cm。     

氟化铵制备氟化钙最优条件研究

试验采用氟化铵与石灰石粉、石灰乳反应制取氟化钙,研究了反应温度、物料浓度、物料过量系数等各主要参数变化对氟化钙结晶、过滤速度、氟收率及其含量的影响,摸索出最优反应条件。     

唐山市大气中多环芳烃污染现状研究

通过污染源调查和采集样品分析得出唐山市大气中多环芳烃污染现状，与国内外一些城市相比较，了解目前唐山市大气中多环芳烃污染水平。     

Body fluid analog chlorination: Application to the determination of disinfection byproduct formation kinetics in swimming pool water

Disinfection by-products(DBPs) are formed in swimming pools by the reactions of bather inputs with the disinfectant.Although a wide range of molecules has been identified within DBPs,only few kinetic rates have been reported.This study investigates the kinetics of chlorine consumption,chloroform formation and dichloroacetonitrile formation caused by human releases.Since the flux and main components of human inputs have been determined and formalized through Body Fluid Analogs(BFAs),it is possible to model the DBPs formation kinetics by studying a limited number of precursor molecules.For each parameter the individual contributions of BFA components have been quantified and kinetic rates have been determined,based on reaction mechanisms proposed in the literature.With a molar consumption of 4 mol Cl_2/mol,urea is confirmed as the major chlorine consumer in the BFA because of its high concentration in human releases.The higher reactivity of ammonia is however highlighted.Citric acid is responsible for most of the chloroform produced during BFA chlorination.Chloroform formation is relatively slow with a limiting rate constant determined at 5.50 × 10~(-3) L/mol/sec.L-histidine is the only precursor for dichloroacetonitrile in the BFA.This DBP is rapidly formed and its degradation by hydrolysis and by reaction with hypochlorite shortens its lifetime in the basin.Reaction rates of dichloroacetonitrile formation by L-histidine chlorination have been established based on the latest chlorination mechanisms proposed.Moreover,this study shows that the reactivity toward chlorine differs whether L-histidine is isolated or mixed with BFA components.     

长江口海域生态环境状况及保护对策

为加快推进长江口海域的生态环境保护和修复工作,结合长江经济带大保护,系统总结分析了近20年长江口环境质量和生态监控区的监测结果.结果表明:①长江口海域生态系统长期处于亚健康状态.②长江径流总量呈现波动变化,年均流量无明显的变化,而长江口海域海水环境状况一直较差.③营养盐污染严重,主要污染物是无机氮和活性磷酸盐;浮游生物和底栖生物群落结构不稳定,存在生境破碎化严重、外来生物入侵、赤潮频发、低氧区等诸多生态问题.为加强长江口海域生态环境的保护与修复,建议:①加强顶层设计,推进落实陆海统筹;②科学规划临港产业布局,加强涉海产业的污染管理;③加强污染物入海排放管控,提升海洋环境保护意识;④保障海洋生态建设资金,强化海洋生态保护与建设.      

2009~2018年太湖湖泛强度变化及其影响因素

基于2009~2018年的每年4~10月对太湖湖泛易发区的逐日巡查成果,以及相关太湖气象、水文、水质和水华监测资料的综合分析,揭示了太湖湖泛发生的环境条件及年际差异性特征,分析了影响太湖湖泛强度年际变化的因素及防控途径.结果表明,2009~2018年10 a中太湖共发生大小湖泛事件75次,平均湖泛面积1.35 km²,最大面积9.20 km²,平均持续时间3 d,最长持续16 d;湖泛发生引起了水体有机质、氮和磷等水质指标明显增高;湖泛的发生均在水温20℃以上,发生首日均处在5~9月;年际湖泛强度变化较大,2017年湖泛强度最大,2018年次之,而2014年湖泛强度最小;年际湖泛强度与蓝藻水华强度及5~9月的湖水平均温度显著正相关,而与水体营养盐等指标关系不密切,表明年际气候条件的波动对湖泛情势影响很大;湖泛的形成与河口区蓝藻水华的堆积关系密切：除了5次草源性湖泛外,70次藻源性湖泛均发生在入湖河口附近水域,河口区的底泥污染状况及底泥悬浮状况可能对湖泛的发生具有促进作用.根据形成湖泛的腐烂物质、来源、发生地点和持续时间的不同,可将湖泛分为藻源性湖泛和草源性湖泛这2种类型,藻源性湖泛又可分为港源型、迁移型和原发型这3种.结果表明,控制蓝藻水华强度是降低湖泛风险的根本途径,而避免河口区蓝藻水华过度堆积及厌氧分解的措施,如对蓝藻水华的及时打捞、工程措施形成的局部流场改变、蓝藻水华的离岸打捞工程和滨岸水华堆积区的应急曝气工程,以及河口区的污染底泥疏浚等工程措施,是降低湖泛发生风险的工程措施选项.