氧化增重法测试硫化矿石低温氧化性参数优化

为更合理地选择硫化矿石低温氧化速率测定所用氧化增重法的测试条件,减小试验误差,采用室内试验、误差分析等方法探讨环境湿度、矿样初始含水率和预氧化时间等因素对氧化增重法测量结果的影响,完善氧化增重法的理论依据和测试条件。结果表明,初始含水率对5天增重率无显著性影响;把初始含水率设为6%,可使各亲水性不同的试验矿样处于相同水分环境下;设定试验时间为9天,其中矿样制备时间4天,测量时间5天,可提高试验数据精确度,节省时间并且符合实际;用体积增重率取代质量增重率,可使理论更正确,测试结果更合理。     

不同堆积型式硫化矿石堆积体温度场数值模拟

基于有限元数值方法,研究硫化矿石堆积体温度场的空间分布规律,建立硫化矿石堆积体温度场数值模型。利用该模型,计算了不同堆积型式的硫化矿石堆积体温度场演化规律,按照结构堆积型式分为:三角形堆积体和梯形堆积体。计算结果表明,硫化矿石堆积体温度分布受堆积型式影响显著:对于靠侧壁呈三角形的堆积型式,温度场关于侧壁角点和坡面中点连线对称分布;对于平面地基上梯形的堆积型式,温度场并不完全关于过形心点垂线对称分布。在两种型式的堆积过程中堆积体内最高温度值基本相同,而在后期堆放过程中,采用梯形堆积型式的最高温度值较三角形堆积型式的计算结果偏低。     

延迟焦化装置冷焦热水罐硫化氢含量超标的治理

对延迟焦化装置冷焦热水罐溢出气体中硫化氢含量超标原因进行了分析,采取了工艺改进措施,使超标问题得以解决,并提出了彻底解决硫化氢含量超标问题的建议.     

沉积有机质分子地球化学应用于古气候古环境研究

自从上世纪八十年代以来,沉积有机质分子地球化学在古气候古环境研究中发挥了其它学科不可替代的作用。与传统的第四纪地质地球化学研究方法相比,分子有机地球化学在古生态系统恢复与古生产率评估、古大气二氧化碳分压与古温度确定等领域提供了更为精细的信息。文章主要总结与评述了沉积有机质分子及其碳／氢同位素地球化学技术近三十年来在上述领域的主要进展。     

CaO对城市生活垃圾原位水蒸气气化制备富氢燃气的影响

为高效资源化利用城市生活垃圾,提出了一种城市生活垃圾原位水蒸气气化制备富氢燃气方法. 在城市生活垃圾原位水蒸气气化过程中添加CaO,对CO₂进行高温吸收,促进H₂产生. 考察了n(Ca)/n(C)(CaO与垃圾原料中碳元素的摩尔比)、反应温度及垃圾含水率等因素对H₂产率以及气化特性的影响. 结果表明:随着n(Ca)/n(C)由0增至1.5,φ(H₂)和H₂产率(以w计)分别由25.89%、10.86g/kg增至45.90%、31.56g/kg;水蒸气的引入提高了CaO的碳酸化反应活性,促进了H₂的产生,但当含水率高于39.45%时,则会降低产气品质;反应温度高于750℃时,虽能强化城市生活垃圾、焦油的热分解等反应产生更多的H₂,但不利于CaO的碳酸化反应,最佳的操作温度为700～750℃;对固体残留物进行XRD和SEM分析可知,反应温度高于750℃会降低CaO的活性,不利于CaO对CO₂的吸收. 以CaO为添加剂的城市生活垃圾原位水蒸气气化制备富氢燃气是一种有效的城市生活垃圾资源化利用方式.      

Removing carbonyl sulfide with metal-modified activated carbon

A Cu-Co-K/activated carbon (AC) adsorbent has been developed for the removal of carbonyl sulfide (COS). The effects of COS concentration, reaction temperature and relative humidity were closely examined. A breakthrough of 33.23 mg COS·g⁻¹ adsorbent at 60°C, under 30% relative humidity and in presence of 1.0% oxygen was exhibited in the Cu-Co-K/AC adsorbent prepared. Competitive adsorption studies for COS in the presence of CS₂, and H₂S were also conducted. TPD analysis was used to identify sulfur-containing products on the carbon surface, and the results indicated that H₂S, COS and SO₂ were all evident in the effluent gas generated from the exhausted Cu-Co-K/AC. Structure of the activated carbon samples has been characterized using nitrogen adsorption, and their surface chemical structures were also determined with X-ray photoelectron spectroscopy (XPS). It turns out that the modification with Cu(OH)₂CO₃-CoPcS-KOH can significantly improve the COS removal capacity, forming SO42− species simultaneously. Regeneration of the spent activated carbon sorbents by thermal desorption has also been explored.     

TiO2光电催化中光生电子降解对苯醌的行为研究

通过施加外加偏压把TiO2/Ti薄膜阳极产生的光生电子转移到阴极,并对其在阴极的电化学行为进行了研究.用水杨酸探针法对阴极溶液中产生的活性氧自由基进行了检测,探讨了pH值、恒电流值和连接类型等因素对阴极室溶液中对苯醌降解效果的影响.实验结果表明,在酸性条件下,转移至阴极的光生电子可将溶液中的溶解氧还原生成H2O2,再进而生成·OH;在pH值为2.0、恒电流为3.5mA和阳离子膜作为反应器双室连接类型的条件下,在60min内,阴极溶液中对苯醌的降解率可达到82.3%.     

Hydrogen production from food wastes and gas post-treatment by CO2 adsorption

The production of H₂ by biological means, although still far from being a commercially viable proposition, offers great promise for the future. Purification of the biogas obtained may lead to the production of highly concentrated H₂ streams appropriate for industrial application. This research work evaluates the dark fermentation of food wastes and assesses the possibility of adsorbing CO₂ from the gas stream by means of a low cost biomass-based adsorbent. The reactor used was a completely stirred tank reactor run at different hydraulic retention times (HRTs) while the concentration of solids of the feeding stream was kept constant. The results obtained demonstrate that the H₂ yields from the fermentation of food wastes were affected by modifications in the hydraulic retention time (HRT) due to incomplete hydrolysis. The decrease in the duration of fermentation had a negative effect on the conversion of the substrate into soluble products. This resulted in a lower amount of soluble substrate being available for metabolisation by H₂ producing microflora leading to a reduction in specific H₂ production.Adsorption of CO₂ from a gas stream generated from the dark fermentation process was successfully carried out. The data obtained demonstrate that the column filled with biomass-derived activated carbon resulted in a high degree of hydrogen purification. Co-adsorption of H₂S onto the activated carbon also took place, there being no evidence of H₂S present in the bio-H₂ exiting the column. Nevertheless, the concentration of H₂S was very low, and this co-adsorption did not affect the CO₂ capture capacity of the activated carbon.     

氢气爆炸特性研究

本文研究、总结了氢气与空气(氢气与氧气)的混合物的爆炸特性.即氢气在空气中,在比较低燃烧界限的情况下,只有向上的传播和非常少的超压可以观测得到.正因为氢气的这种特性,将氢应用于科技将极大地推进社会进步,氢燃料将成为一种主要的能源.然而,氢技术应用的成功与否主要取决于氢使用的安全性.所以,必须掌握实际使用时氢气燃烧的性能.本文在日本过去十年实验数据的基础上,通过实验研究了氢气与空气混合物的燃点.研究了氢气、氧气混合物经氮气稀释后,按化学当量比例将不同浓度的氢气与空气进行混合,并得出了低温下的爆炸压力特性.随后,分别讨论了在初始压力下一致的情况下,试管直径相同的状况下,氢气与空气混合浓度相同的情况下,这三种爆轰传播限制之间的关系.得出了在空气中直接点燃的发生爆轰的最小试管直径,最小的装药量之间的关系,进行了爆轰危险性分级.最后,文章概括比较了氢与其他燃料的燃烧特性,评估了氢气燃烧过程中的危险与安全因素.     

STABLE HYDROGEN AND OXYGEN ISOTOPE COMPOSITION OF PRECIPITATION IN NORTHEASTERN COLORADO1

ABSTRACT: Where data are available, hydrologic studies may use precipitation's stable oxygen and hydrogen isotope composition to investigate streamflow, ground water/surface water interaction, and ground water recharge. Paleoclimate studies utilize the δ¹⁸O_{precipitation}‐T_air relationship, in conjunction with lake sediments, fossils, or old ground waters, for example, to estimate pale‐otemperatures. Ecological studies utilize precipitation and soil water isotope composition to track moisture uptake in plants, and to trace species migration patterns. Such studies require that the isotopic composition of precipitation be known. Oxygen‐18 (δ¹⁸O) and deuterium (δ²H) data for precipitation are lacking in the semi‐arid portion of the north‐central U.S. Great Plains, and thus there is a need to establish additional meteoric water lines as isotope input functions across the region, as well as to develop better understanding of the isotopic climate linkages that control oxygen and hydrogen isotope ratios in precipitation. This study determined the δ¹⁸O and δ²H composition of precipitation in the Pawnee Grasslands of northeastern Colorado from 1994 through 1998 using archived National Atmospheric Deposition Program samples. The resulting local water line follows the relationship δ²H = 7.86 δ¹⁸O‐7.66, and the data show a δ¹⁸O_weekly ‐ T_weekly relationship of δ¹⁸O = 0.560‐T (°C)‐18.8.