SAS/IPPA/AA三元共聚物对碳酸钙阻垢性能的研究

以水为溶剂,过硫酸铵为引发剂,丙烯磺酸钠、异丙烯膦酸和丙烯酸为单体,合成了三元共聚物丙烯磺酸钠/异丙烯膦酸/丙烯酸(SAS/ IPPA/AA),研究了共聚物在不同水质条件下对CaCO3的阻垢性能,探讨了共聚物浓度、pH值、钙离子浓度、碳酸根离子浓度和温度等条件对CaCO3的阻垢性能的影响,结果显示,在共聚物用量为18mg·l-1时,可使阻垢率达到100%.     

湘江江水中重金属转化的主要地球化学因素

研究湘江江水悬浮态和溶解态金属浓度的变化、重金属在沉积物中的赋存形态及对制约湘江江水重金属进入沉积物的地球化学作用结果表明,在湿热的湘江流域气候环境条件下,河流水体中重金属的地球化学作用一方面表现出明显的地带性特征,即Fe/Mn水合氧化物的吸附沉淀作用较强,又受区域地质条件、岩石性质的影响,表现为较强的碳酸盐的地球化学作用,但不同金属的地球化学趋向不同,铅易以碳酸盐形式、铜主要依靠有机质的结合作用进入沉积物。     

Functionalization of nitrogen-doped graphene quantum dot: A sustainable carbon-based catalyst for the production of cyclic carbonate from epoxide and CO2

A series of organic compounds were successfully immobilized on an N-doped graphene quantum dot (N-GQD) to prepare a multifunctional organocatalyst for coupling reaction between CO₂ and propylene oxide (PO). The simultaneous presence of halide ions in conjunction with acidic- and basic-functional groups on the surface of the nanoparticles makes them highly active for the production of propylene carbonate (PC). The effects of variables such as catalyst loading, reaction temperature, and structure of substituents are discussed. The proposed catalysts were characterized by different techniques, including Fourier transform infrared spectroscopy (FTIR), field emission scanning electron microscopy/energy dispersive X-ray microanalysis (FESEM/EDX), thermogravimetric analysis (TGA), elemental analysis, atomic force microscopy (AFM), and ultraviolet–visible (UV-Vis) spectroscopy. Under optimal reaction conditions, 3-bromopropionic acid (BPA) immobilized on N-GQD showed a remarkable activity, affording the highest yield of 98% at 140°C and 10⁶ Pa without any co-catalyst or solvent. These new metal-free catalysts have the advantage of easy separation and reuse several times. Based on the experimental data, a plausible reaction mechanism is suggested, where the hydrogen bonding donors and halogen ion can activate the epoxide, and amine functional groups play a vital role in CO₂ adsorption.     

Carbon Management in Agricultural Soils

World soils have been a major source of enrichment of atmospheric concentration of CO₂ ever since the dawn of settled agriculture, about 10,000 years ago. Historic emission of soil C is estimated at 78 ± 12 Pg out of the total terrestrial emission of 136 ± 55 Pg, and post-industrial fossil fuel emission of 270 ± 30 Pg. Most soils in agricultural ecosystems have lost 50 to 75% of their antecedent soil C pool, with the magnitude of loss ranging from 30 to 60 Mg C/ha. The depletion of soil organic carbon (SOC) pool is exacerbated by soil drainage, plowing, removal of crop residue, biomass burning, subsistence or low-input agriculture, and soil degradation by erosion and other processes. The magnitude of soil C depletion is high in coarse-textured soils (e.g., sandy texture, excessive internal drainage, low activity clays and poor aggregation), prone to soil erosion and other degradative processes. Thus, most agricultural soils contain soil C pool below their ecological potential. Adoption of recommend management practices (e.g., no-till farming with crop residue mulch, incorporation of forages in the rotation cycle, maintaining a positive nutrient balance, use of manure and other biosolids), conversion of agriculturally marginal soils to a perennial land use, and restoration of degraded soils and wetlands can enhance the SOC pool. Cultivation of peatlands and harvesting of peatland moss must be strongly discouraged, and restoration of degraded soils and ecosystems encouraged especially in developing countries. The rate of SOC sequestration is 300 to 500 Kg C/ha/yr under intensive agricultural practices, and 0.8 to 1.0 Mg/ha/yr through restoration of wetlands. In soils with severe depletion of SOC pool, the rate of SOC sequestration with adoption of restorative measures which add a considerable amount of biomass to the soil, and irrigated farming may be 1.0 to 1.5 Mg/ha/yr. Principal mechanisms of soil C sequestration include aggregation, high humification rate of biosolids applied to soil, deep transfer into the sub-soil horizons, formation of secondary carbonates and leaching of bicarbonates into the ground water. The rate of formation of secondary carbonates may be 10 to 15 Kg/ha/yr, and the rate of leaching of bicarbonates with good quality irrigation water may be 0.25 to 1.0 Mg C/ha/yr. The global potential of soil C sequestration is 0.6 to 1.2 Pg C/yr which can off-set about 15% of the fossil fuel emissions.     

锑砷钙渣的应用

有色冶炼产生的锑砷钙渣在玻璃瓶生产中的应用 ,理论和实践证明 :用锑砷钙渣代替白砒是可行的。     

微生物诱导碳酸盐沉淀及其在固定重金属领域的应用进展

生物矿化已受到化学、物理、生物、材料、医学、生命及环境等多学科的广泛关注,其中,以尿素为底物的MICP（微生物诱导碳酸盐沉淀）技术是生物矿化领域的研究热点之一.在分析MICP过程中的酶解机理和生物大分子在微生物矿化过程中的作用基础上,通过对重金属离子的矿化产物和碳酸盐矿化菌的成矿因素分析,揭示MICP矿化产物的特征及形成条件.碳酸盐矿化菌主要产生脲酶分解尿素,增加土壤CO₃2-饱和度,其代谢产生的胞外聚合物具有多种功能团组合和键能连接,起着调控生物矿化的作用.MICP技术可用于固定土壤和水体中的Cu、Pb、Zn、Cd、Cr、As等重金属,重金属主要以共沉淀的形式被固定,阴阳离子型重金属以类质同象置换方式分别占据方解石中的CO₃2-位和Ca2+位,从而促使污染土壤中的可交换态重金属向碳酸盐结合态转移.但是,MICP技术主要针对减少重金属的生物可利用性,不能满足以全量来计算的现行土壤环境质量标准,且MICP技术在长期有效性、生物安全性和土壤理化性质等方面存在诸多隐患.因此,由试验条件转向实际应用具有一定挑战.建议寻找更稳定的方法以阻止碳酸盐矿物中的重金属溶出,且有必要将开发高效的土著微生物复合菌剂作为未来MICP研究的方向之一.      

Ca and OH release of ceramsites containing anorthite and gehlenite prepared from waste lime mud

Lime mud is a kind of solid waste in the papermaking industry, which has been a source of serious environmental pollution. Ceramsites containing anorthite and gehlenite were prepared from lime mud and fly ash through the solid state reaction method at 1050°C. The objective of this study was to explore the efficiency of Ca^2 + and OH⁻ release and assess the phosphorus and copper ion removal performance of the ceramsites via batch experiments, X-ray diffraction (XRD) and scanning electron microscopy (SEM). The results show that Ca^2 + and OH⁻ were released from the ceramsites due to the dissolution of anorthite, gehlenite and available lime. It is also concluded that gehlenite had stronger capacity for Ca^2 + and OH⁻ release compared with anorthite. The Ca^2 + release could be fit well by the Avrami kinetic model. Increases of porosity, dosage and temperature were associated with increases in the concentrations of Ca^2 + and OH⁻ released. Under different conditions, the ceramsites could maintain aqueous solutions in alkaline conditions (pH = 9.3–10.9) and the release of Ca^2 + was not affected. The removal rates of phosphorus and copper ions were as high as 96.88% and 96.81%, respectively. The final pH values of both phosphorus and copper ions solutions changed slightly. The reuse of lime mud in the form of ceramsites is an effective strategy.     

Removal of H2S using molten carbonate at high temperature

Gasification is considered to be an effective process for energy conversion from various sources such as coal, biomass, and waste. Cleanup of the hot syngas produced by such a process may improve the thermal efficiency of the overall gasification system. Therefore, the cleanup of hot syngas from biomass gasification using molten carbonate is investigated in bench-scale tests. Molten carbonate acts as an absorbent during desulfurization and dechlorination and as a thermal catalyst for tar cracking. In this study, the performance of molten carbonate for removing H₂S was evaluated. The temperature of the molten carbonate was set within the range from 800 to 1000 °C. It is found that the removal of H₂S is significantly affected by the concentration of CO₂ in the syngas. When only a small percentage of CO₂ is present, desulfurization using molten carbonate is inadequate. However, when carbon elements, such as char and tar, are continuously supplied, H₂S removal can be maintained at a high level.To confirm the performance of the molten carbonate gas-cleaning system, purified biogas was used as a fuel in power generation tests with a molten carbonate fuel cell (MCFC). The fuel cell is a high-performance sensor for detecting gaseous impurities. When purified gas from a gas-cleaning reactor was continuously supplied to the fuel cell, the cell voltage remained stable. Thus, the molten carbonate gas-cleaning reactor was found to afford good gas-cleaning performance.     

外源水对碳酸盐侵蚀速率研究——以桂林毛村地下河为例

本文对桂林毛村地下河流域,进行了野外监测与室内分析研究,详细研究了外源水与岩溶水对碳酸盐岩侵蚀速率差异。研究结果表明,碳酸盐岩在岩溶水与外源水中的侵蚀速率存在较大差异,雨季碳酸盐岩侵蚀速率:外源水外源水补给的岩溶水岩溶水空气;旱季碳酸盐岩溶蚀速率:外源水外源水补给的岩溶水空气岩溶水;外源水中的灰岩侵蚀速率白云岩侵蚀速率;碳酸盐岩试块的侵蚀速率具有明显的季节变化,主要受控于方解石饱和指数、pH值与水动力条件。     

巴里富碳酸盐硫化物尾矿中重金属的赋存状态

本文以广西大厂锡石-硫化物矿区巴里尾矿库的富碳酸盐尾矿(堆放了20余年)作为研究对象,采用BCR三步提取法研究Zn、Cd、Pb和As的化学形态分量以及其总含量在该尾矿铅垂剖面中的分布,并结合尾矿的结构构造、次生和原生矿物成分及其变化等分析,探讨在氧化/酸化条件下富碳酸盐尾矿中重金属的释放机制。研究结果表明:(1)尾矿下层原尾矿中重金属主要以稳定或较稳定的残渣态(As、Pb、Zn、Cd)、氧化物结合态(Pb)及硫化物结合态(Zn、Cd)形式赋存。在酸水淋滤作用下,原尾矿中重金属的释放顺序为Cd≈ZnPbAs;(2)尾矿上部厚层状氧化硬层(厚度1~1.5m)中,Zn、Cd以酸可溶态大量富集,具有较强的迁移性;As、Pb主要以残渣态以及氧化物结合态赋存,其迁移性较差。因此,富含碳酸盐的硫化物尾矿经过氧化作用具有释放多种重金属的潜能。由于这类尾矿中各重金属的赋存状态存在差异性,因此对其迁移性及环境效应须具体分析。