硫化氢分解制取氢和硫技术的进展

介绍了 H2 S分解制氢和硫的热力学、动力学最新研究成果 ,综述了 H2 S分解制氢和硫的各种工艺技术的新进展 ,并对这些工艺技术进行了分析和评述。 H2 S分解制氢的同时回收硫是一种很有前途的治理废气减轻污染的方法。     

Decomposition of silicate minerals by Bacillus mucilaginosus in liquid culture

The extraction of K⁺ and SiO₂ from silicate minerals by Bacillus mucilaginosus in liquid culture was studied in incubation experiments. B. mucilaginosus was found to dissolve soil minerals and mica and simultaneously release K⁺ and SiO₂ from the crystal lattices. In contrast, the bacterium did not dissolve feldspar. B. mucilaginosus also produced organic acids and polysaccharides during growth. The polysaccharides strongly adsorbed the organic acids and attached to the surface of the mineral, resulting in an area of high concentration of organic acids near the mineral. The polysaccharides also adsorbed SiO₂ and this affected the equilibrium between the mineral and fluid phases and led to the reaction toward SiO₂ and K⁺ solubilization. These two processes led to the decomposition of silicate minerals by the bacterium.     

Profiling of microbial communities in a bioreactor for treating hydrocarbon-sulfide-containing wastewater

A technology of polymerase chain reaction-denaturing gradient gel electrophoresis(PCR-DGGE)was used to profile the structure and dynamic changes of microbial communities in a bioreactor for treating hydrocarbon-sulfide-containing(HSC)wastewater.The results showed that the heterotrophic genus of Acinetobacter and the autotrophic genera of Thiobacillus and Thiomonas could survive well in all of three operating conditions.Some special genera were also observed with changes of micro-ecoenvironment in the rea...     

再论含金硫化物矿物中能否存在负价金问题──答李九玲等同志

本文从讨论金属结合能何以具有表面化学位移的原因开始,从金属团簇的一般性质出发,论证了金属结合能自尺寸大于1nm的团簇到金属微粒再到块体金属具有连续过渡性;金属结合能与粒径R呈正相关;与1／R具线性负相关关系,认为金微粒或团簇具有1．1eV以上的结合能负位移是可能的。并指出李九玲等同志在“评<含金硫化物矿物中不可能存在负价金>”一文中引用的某些衬底材料上的金团簇呈现结合能正位移的数据是由于这些金困簇已与其衬底材料发生了键合作用造成的,它们不能作为否定金属结合能位移与粒径呈正相关的依据。同时,笔者从“化学结合金”在氰化过程中并未被氧化成正离子金判断,它不应是负价金。并由同质并能位移与粒径可具负相关关系推论,“化学结合金”应是合企硫化物矿物中可存在的少量微粒碲金矿、碲金银矿等中的正离子金。笔者强调在讨论企的价态问题时应采用Allred－Rochow电负性数据而非常用的Pauling电负性数据,并再次指出含金硫化物矿物中不可能有负价金存在。     

硫化碱脱除二氧化硫工业烟气的可行性分析

分析了国内外烟气脱硫的研究现状,论述了用硫化碱脱除二氧化硫化工业烟气在理论上和实验上的可能性。     

低温等离子体治理H2S污染的实验研究

低温等离子体技术是一种高效、快速的污染消除技术，国内外都在对其进行广泛而深入的研究。采用脉冲电晕放电等离子体对空气中的硫化氢进行降解研究，探索了、脉冲峰压、脉冲频率、气体流量以及气体初始浓度对净化效果的影响，气体浓度由气相色谱仪测定。结果表明，脉冲电晕放电可以有效消除硫化氢污染，净化率随脉冲峰压和脉冲频率的增加而提高，随气体初始浓度和流量的增加而下降，且在初始浓度360mg／m^2、流量1200mL／min、脉冲峰压30kV、脉冲频率80Hz的条件下，处理后的气体中已检测不到H2S，根据色谱检测限（0．29mg／m^3）计算出的净化率≥99．92％。采用离子色谱对产物进行了定性分析，发现H2S经放电处理后主要产物为SO2和SO3。     

Migration behavior of naturally occurring radionuclides at the Nopal I uranium deposit, Chihuahua, Mexico

Oxidation of pyrite at the Nopal I uranium deposit, Peña Blanca district, Chihuahua, Mexico has resulted in the formation of Fe-oxides/hydroxides. Anomalous U concentrations (i.e. several hundred to several thousand ppm) measured in goethite, hematite, and amorphous Fe-oxyhydroxides in a major fracture that crosscuts the deposit and the absence of U minerals in the fracture suggest that U was retained during secondary mineral growth or sorbed on mineral surfaces. Mobilization and transport of U away from the deposit is suggested by decreasing U concentrations in fracture-infilling materials and in goethite and hematite with distance from the deposit. Greater than unity ²³⁴U/²³⁸U activity ratios measured in fracture-infilling materials indicate relatively recent ( < 1 Ma) U uptake from fluids that carried excess ²³⁴U. Systematic decreases in ²³⁴U/²³⁸U activity ratios of fracture materials with distance from the deposit suggest a multistage mobilization process, such as remobilization of U from ²³⁴U-enriched infill minerals or differential or diminished transport of U-bearing solutions containing excess ²³⁴U.     

一种新型烟气脱硫技术在燃煤锅炉上的扩大试验

介绍了用硫化碱加TFS添加剂进行燃煤锅炉煤气脱硫并副产硫代硫酸钠的中试成果。     

WATER QUALITY PREDICTION WITHIN AN INTERBASIN TRANSFER SYSTEM1

ABSTRACT A methodology for predicting the spatial and temporal levels of conservative water quality constituents within a multibasin water resource system is presented. Dissolved solids, sulfates, and chlorides are the constituents used during this investigation; however, any other conservative ion or mineral can be incorporated into the simulation model. The methodology is tested on the proposed Texas Water System. The water quality model, QNET-I, utilizes monthly canal and river flows and reservoir storage levels calculated by the Texas Water Development Board's systems simulation model. Discharge-concentration relationships are developed for each source of water in the system, including significant waste-water discharges. Reservoirs in the system are assumed to be completely mixed with respect to conservative constituents. A mass balance analysis is performed for each node and each month during the simulation period. The output from the water quality simulation is a table of the concentrations of the conservative water quality constituents at each demand point in the system and in each reservoir and canal for every month the system is in operation. The desired quality of the water at the demand locations is used to determine the economic utility of transporting and mixing water from various sources.