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231.
印辉  魏梅 《环境科技》2005,18(4):21-23
将污染治理和综合利用作为一个整体考虑,利用“厌氧+UASB+好氧”工艺处理酒糟废水,各项指标均取得了较好的处理效果:同时通过回收沼气获得了一定的经济效益。找到了一条技术先进、运行可靠、经济可行的治理工艺路线。  相似文献   
232.
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.  相似文献   
233.
Carbon Management in Agricultural Soils   总被引:11,自引:0,他引:11  
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.  相似文献   
234.
铜陵市硫酸渣的综合利用   总被引:9,自引:1,他引:9  
铜陵市的硫酸渣经过磁化焙烧—球磨—磁选,可以生产出含铁品位为64.13%、没有硫酸渣任何残余特征的优质铁精矿粉.  相似文献   
235.
在土地利用方式改变、能源消耗持续增长、人口膨胀的共同作用下,城市热岛效应日趋显著。大气细颗粒物(PM2.5)污染不断加剧,对城市热岛强度也产生了一定的影响。利用地面空气质量监测站点的逐小时PM2.5污染监测数据、气象监测站点的日均数据和MODIS地表温度数据,结合土地利用类型,划分城郊气象站点和地表温度采样点,分别计算北京市日均PM2.5浓度、冠层城市热岛强度和地表城市热岛强度,并计算地表城市热岛强度指数,得出热岛强度空间分布图。经过对PM2.5与冠层城市热岛强度、地表城市热岛强度及其空间分布的相关性分析,得出以下结论:(1)北京市地表城市热岛强度的月、季间变化明显,主要受土地覆盖类型影响,夏季高于冬季,冠层城市热岛强度的月、季间变化较小;(2)PM2.5质量浓度与冠层城市热岛强度、地表城市热岛强度均呈显著负相关,相关系数分别为?0.5199和?0.6115;(3)昼间地表城市热岛强度与PM2.5质量浓度的相关性高于夜间;(4)PM2.5质量浓度变化对地表城市热岛的空间分布有着显著的影响。随着PM2.5质量浓度的增加,强热岛空间范围向城区缩减。  相似文献   
236.
在污泥焚烧项目环境监理过程中,通过核算钙硫摩尔比考察或佐证二氧化硫的去除能力及效果.根据钙硫比核算需要收集项目相关生产报表,并对污泥焚烧过程中的钙硫摩尔比进行核算.通过对钙硫比的合理性进行分析,进而考察污泥焚烧过程中二氧化硫产生情况及达标排放情况,提升环境监理工作深度.数据来源为企业实际生产报表,分析方法为钙硫元素摩尔量理论反应值、质量平衡、热量平衡.通过实际数据核算分析发现,污泥焚烧项目中的钙硫元素摩尔比明显低于理论设计值,污泥中硫在焚烧过程中转化成SO2的比例约为64.52%.  相似文献   
237.
搭建了蜂窝湿式静电除尘实验台,研究了不同清灰方式下湿式静电除尘的放电特性、除尘效率、分级效率.结果发现,喷淋清灰方式对颗粒物脱除效率最高,溢流清灰方式其次.为了避免喷淋产生的水雾对除尘效率的不稳定影响,着重研究了溢流清灰方式下,湿式静电除尘器比收尘面积、运行电压、烟气初始浓度对除尘效率的影响.研究表明,提高比收尘面积和运行电压均可使除尘效率增加,通过观察颗粒物分级脱除效率发现,粒径段在0.5~1μm之间的颗粒物脱除效率较低.当烟气含尘浓度达到较高值(442.85 mg·m~(-3))时,除尘器仍可保持较高的除尘效率.  相似文献   
238.
成都市大气细颗粒物组成和污染特征分析(2012-2013年)   总被引:18,自引:4,他引:14  
陈源  谢绍东  罗彬 《环境科学学报》2016,36(3):1021-1031
为了解成都市大气细颗粒物的污染特征,于2012年5月-2013年5月在成都市城区开展了每6 d采集1次样品的长期颗粒物观测.利用十万分之一分析天平、热光碳分析仪、离子色谱、电感耦合等离子体质谱(ICP-MS)分别分析了颗粒物样品的质量浓度、有机碳/元素碳、水溶性离子、无机元素等,同步收集了污染物在线观测数据、气象数据和卫星遥感数据.结果表明,采样期间,成都市可吸入颗粒物(PM10)和细粒子(PM2.5)浓度颗粒物浓度分别高达(129.7±76.4)和(91.6±54.3) μg·m-3,PM2.5中以二次无机离子(SNA,43.6%)和有机物(OM,31.2%)污染最为突出,其次为土壤组分(Soil,13.8%)、元素碳(EC,5.0%)和微量元素(Trace,0.8%);1月、3月、5月和10月是污染较重的月份.通过比较揭示了不同污染源影响下的典型污染特征.生物质燃烧期间,成都城区PM2.5浓度达214.3 μg·m-3,PM2.5/PM10比达0.89,其中OM贡献增加至57.2%,K+浓度达8.7 μg·m-3,OC/EC比达8.3,SNA比重下降;而沙尘传输期间,PM2.5浓度为122.6 μg·m-3,仅占PM10浓度的0.28,PM2.5中土壤组分比例剧增至77.3%,SNA和无机元素的比重明显下降;静稳天气下PM2.5浓度为261.0 μg·m-3,各组分比重并无明显变化,硝酸盐和铵盐比例稍有增加.  相似文献   
239.
硬脂酸和硅烷偶联剂KH570对氧化钙疏水改性研究   总被引:1,自引:0,他引:1  
为开发事故情况下高浓度毒性有机物污染土壤快速固化/稳定化材料,本文以氧化钙(Ca O)为基材,硬脂酸和硅烷偶联剂KH570为两种改性剂,采用湿法工艺对Ca O粉体进行表面疏水改性,探讨不同工艺条件对改性效果的影响,并对改性后Ca O的形态和结构进行表征.结果表明,硬脂酸改性氧化钙的最佳工艺条件为:硬脂酸添加质量分数5%,改性温度30℃,改性时间30 min;KH570改性Ca O的最佳工艺条件为:KH570添加量0.02 m L·g-1Ca O,改性时间40 min.改性后Ca O的接触角均大于90°.傅里叶红外和扫描电镜分析表明,两种改性剂均以化学吸附的方式包覆在Ca O表面,达到了表面疏水改性的目的.  相似文献   
240.
The present study was undertaken with the objective of studying repeated batch and continuous degradation of chlorpyrifos (O,O-diethyl O-3,5,6-trichloropyridin-2-yl phosphorothioate) using Ca-alginate immobilized cells of Pseudomonas putida isolated from an agricultural soil, and to study the genes and enzymes involved in degradation. The study was carried out to reduce the toxicity of chlorpyrifos by degrading it to less toxic metabolites. Long-term stability of pesticide degradation was studied during repeated batch degradation of chlorpyrifos, which was carried out over a period of 50 days. Immobilized cells were able to show 65% degradation of chlorpyrifos at the end of the 50th cycle with a cell leakage of 112 × 103 cfu mL?1. During continuous treatment, 100% degradation was observed at 100 mL h?1 flow rate with 2% chlorpyrifos, and with 10% concentration of chlorpyrifos 98% and 80% degradation was recorded at 20 mL h?1 and 100 mL h?1 flow rate respectively. The products of degradation detected by liquid chromatography–mass spectrometry analysis were 3,5,6-trichloro-2-pyridinol and chlorpyrifos oxon. Plasmid curing experiments with ethidium bromide indicated that genes responsible for the degradation of chlorpyrifos are present on the chromosome and not on the plasmid. The results of Polymerase chain reaction indicate that a ~890-bp product expected for mpd gene was present in Ps. putida. Enzymatic degradation studies indicated that the enzymes involved in the degradation of chlorpyrifos are membrane-bound. The study indicates that immobilized cells of Ps. putida have the potential to be used in bioremediation of water contaminated with chlorpyrifos.  相似文献   
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