淄博市空气污染物变化及其与气象条件的关系

近年来淄博市由于加强了对二氧化硫和粉尘等污染物排放企业脱硫除尘的监管,可吸入颗粒物和二氧化硫浓度呈现逐年下降趋势,而燃煤量和机动车保有量的逐年增加使氮氧化物浓度呈现波动式上升趋势;四季分明的气候条件使淄博市的空气污染程度在一、四季度高于二、三季度;同时污染物浓度和风速、湿度呈负相关,和温度、气压呈正相关。     

La3+-TiO2/斜发沸石光催化剂的制备及其对甲基橙的光催化性能

以钛酸丁酯、La2O3、斜发沸石为原料,采用溶胶-凝胶法制备了La^3＋ -TiO2/斜发沸石光催化剂。利用红外光谱、热重-示差扫描量热、X射线衍射、扫描电子显微镜等方法对所制备的光催化剂进行了表征。以甲基橙为目标物,太阳光为光源,对光催化剂的性能进行了评价。实验结果表明：w（La3＋）=0.5%的光催化剂经400℃热处理3h后对甲基橙的光催化效果最好,甲基橙的降解率达92%;反应温度越高,降解率越高,40℃下反应3h时的降解率达97%;溶液pH为5时,降解率达92%。     

超稠油污水深度处理工艺技术

针对辽河油田超稠油污水的特点设计了处理工艺流程,进行了药剂的筛选,根据各工艺设备的出水水质要求确定了合适的净水剂、除硅剂、阻垢剂的加量,并进行了现场实际应用,外输出水达到锅炉给水指标要求,用于锅炉注汽使用,效果良好,分析了该超稠油污水处理技术的特点和优势,提出了超稠油污水回用锅炉的建议。     

水上公园水体的水供现状及营养功能状态评价

本文论述了天津市水上公园水体的水质现状,并依据有关标准对水体的营养状态,水体的游览景 产养殖,饮水备用水源等功能进行了评价。     

天津市秋季臭氧浓度影响因素及相关关系研究

选择天津市秋季典型重污染时期2005年11月2～7日近地面大气O3、NO、NO2、CO、紫外线(UV)强度和温度等观测数据,研究O3浓度的时间变化特征及其与相关前体物、气象条件的相关关系.结果表明,在观测期间O3浓度存在明显的日变化周期,在13:00～14:00时浓度最大,夜间变化平缓;O3浓度与NO、NO2、NOx和CO等前体物呈较好的负相关关系;温度和UV与O3浓度密切相关,昼间O3与UV呈相同变化趋势,相关系数达0.71,O3浓度变化滞后于UV变化,将O3浓度与前1小时的UV对比分析,相关系数提高到0.81.     

Simplified creation of polyester fabric supported Fe-based MOFs by an industrialized dyeing process: Conditions optimization, photocatalytics activity and polyvinyl alcohol removal

MIL-53(Fe) was successfully prepared and deposited on the surface carboxylated polyester (PET) fiber by an optimized conventional solvothermal or industrialized high temperature pressure exhaustion (HTPE) process to develop a PET fiber supported MIL-53(Fe) photocatalyst ([email protected]) for the degradation of polyvinyl alcohol (PVA) in water under light emitting diode (LED) visible irradiation. On the basis of several characterizations, [email protected] was tested for the photocalytic ability and degradation mechanism. It was found that temperature elevation significantly enhanced the formation and deposition of MIL-53(Fe) with better photocatalytic activity. However, higher temperature than 130°C was not in favor of its photocatalytic activity. Increasing the number of surface carboxyl groups of the modified PET fiber could cause a liner improvement in MIL-53(Fe) loading content and photocatalytic ability. High visible irradiation intensity also dramatically increased photocatalytic ability and PVA degradation efficiency of [email protected] Na₂S₂O₈ was used to replace H₂O₂ as electron acceptor for further promoting PVA degradation in this system. [email protected] prepared by HTPE process showed higher MIL-53(Fe) loading content and slightly lower PVA degradation efficiency than that prepared by solvothermal process at the same conditions. These findings provided a practical strategy for the large-scale production of the supported MIL-53(Fe) as a photocatalyst in the future.     

Formation mechanism of hydrogeochemical characterization of mineral water in Antu County,Changbai Mountain area

Antu County in the Changbai Mountains is an important source of mineral water, but there is a lack of research on the source of groundwater characteristic components, affecting the protection of water resources. This study obtained hydrochemical and isotopic data (28 groups in total, April and September in 2019) by summarizing research and sampling data in order to identify the formation process of characteristics. The formation mechanism of the characteristic components was revealed using geostatistical, isotopic, and hydrogeochemical inversion simulations. The results show that the metasilicic acid is a common component of groundwater water chemistry in the study area. The water body primarily receives stable recharge from low-mineralized precipitation with ages ranging from 27.7 to 38.4 years and recharge elevations ranging from 1160 to 2393 m, providing ample time for water–rock interaction. The dissolution of olivine, pyroxene, albite, and other siliceous minerals is the source of characteristic components, and deep faults and deep basalt heat flow are the key conditions for the formation of metasilicic acid. When low-mineralized precipitation recharges the underground aquifer, it dissolves the silica-aluminate and silicon-containing minerals in the surrounding rocks through the water–rock action under the effect of CO₂, causing a large amount of metasilic acid to dissolve into the groundwater and forming metasilic acid-type mineral water.