天然土壤对水溶液中Pb~(2+)的吸附

以天然土壤为吸附材料,处理水溶液中的Pb2+,研究3种土壤对水溶液中Pb2+的吸附过程并结合土壤的理化性质对吸附规律进行初步分析。结果表明,棕壤和钙层土对Pb2+的吸附能力远大于红壤,3种土壤对Pb2+的吸附动力学曲线与二次动力学方程有较好的拟合性;3种土壤吸附Pb2+的吸附等温线用Langmuir方程描述最为合适,其次是Temkin方程,再次是Frenudlich方程,钙层土对Pb2+的吸附受温度影响较为明显;由实验数据得出的反应热力学参数说明3种土壤对Pb2+的吸附是自发的吸热过程;Pb2+在饱和吸附的土壤表面覆盖率并不高;土壤对Pb2+的吸附能力受各种土壤理化性质的综合影响。     

Ti/SnO2-Sb2O3/β-PbO2阳极消毒处理医院污水

采用热分解+电沉积法制备Ti/SnO2-Sb2O3/β-PbO2作为阳极消毒处理医院污水,初步探讨其杀菌基本原理,并研究了阳极材料、电流密度、电极间距、NaCl电解质浓度对消毒效果的影响。结果表明,以Ti/SnO2-Sb2O3/β-PbO2作为阳极,碳纤维作为阴极,在电流密度为80 A/m2,消毒时间为12 min,电极间距为5 mm,不添加电解质的实验条件下,处理后出水的粪大群肠菌数小于500 cfu/L,符合污水综合排放一级标准(GB8978-1996)。     

羽毛角蛋白海绵材料对亚甲基蓝的吸附去除

以羽毛角蛋白提取后产生的残渣为原料,采用简单物理法制得角蛋白海绵材料,通过扫描电镜和红外光谱对其表观形貌和表面结构进行表征,同时以亚甲基蓝染料作为实验对象,考察制得的海绵材料对其吸附特性和去除效果。结果表明,当吸附平衡时间为1 440 min、亚甲基蓝溶液初始浓度为100 mg/L、海绵材料投加量为0.06 g、反应温度为25℃、溶液pH为7.0时,海绵材料对亚甲基蓝的吸附去除率可达98%以上,同时由Langmuir等温吸附模型拟合结果可知,海绵材料对亚甲基蓝的最大吸附量可达151.5 mg/g。因此,将羽毛角蛋白提取后产生的残渣可制备良好的染料吸附剂,取得良好的环境效益。     

用幼苗法指示污泥和土壤中重金属的植物有效性

利用小麦幼苗与黑麦幼苗研究了污泥和土壤中重金属的植物有效性,并对二者进行了比较。结果表明, 在两种污灌区土壤、四种污泥以及一种污泥施用于两种清洁土壤中,黑麦和小麦测定的Cd,Pb,Cu,Zn,Ni五种重金属有效性的顺序,以及有效性大小的数量级上是一致的;除了在污泥中,二者的茎Pb,Ni及根Zn相关不显著,以及在Lou土中施用污泥后,两种植物各部位相关不好外,在污泥及污泥施于赤红壤各处理中黑麦与小麦相关均匀为极显著。上述结果表明,应用小麦幼苗可以替代黑麦幼苗指标土壤中重金属的植物有效性,但同时也应考虑不同植物间的差异。     

液膜法处理硫普罗宁废水的研究

采用W／O型乳状液膜法提取水溶液中的硫普罗宁,考察了载体、温度、硫普罗宁浓度以及油内比、试剂比、乳水比对提取率的影响,并得出了液膜法提取硫普罗宁的最佳乳液配方：油内比＝1：1,乳水比＝1：2,试剂比＝6－8,载体浓度＝5％,温度20℃,转速＝240－250r.min^-1,其提取率高达90％。     

金华生态建筑的设计

金华生态建筑是自身良性循环的绿色建筑物,有3个特点,即屋顶覆土种植或养殖或设太阳能装置,地下设有以净化生活污水为主要目的沼气净化池,墙体垂直绿化,这三者缺不一可,但可单项利用,它有节土,节水,节能和经济,环境,社会产益协调统一这两大优点。     

浙江省农业生物灾害的现状、趋势及减灾对策

病虫草鼠是农业的主要生物灾害。本文分析了浙江省农业生物灾害的现状和今后农作物重大病虫害的发生趋势,提出了农业有害生物的控制对策。     

Health risk assessment of heavy metals for edible parts of vegetables grown in sewage-irrigated soils in suburbs of Baoding City,China

With the long-term application of wastewater to vegetable production fields, there is concern about potential health risks of heavy metals contaminating the edible parts of vegetables grown in contaminated soils in the suburban areas of Baoding City, China. The average concentration of elemental Zn in sewage-irrigated soil was the highest (153.77 mg kg⁻¹), followed by Pb (38.35 mg kg⁻¹), Cu (35.06 mg kg⁻¹), Ni (29.81 mg kg⁻¹), and Cd (0.22 mg kg⁻¹) which were significantly higher (P < 0.05) than those in the reference soil. The results showed that long-term sewage irrigation had led to a growing accumulation of heavy metals in the soils, especially for Cd, Zn, and Pb. Furthermore, the concentrations of elemental Cd, Zn, and Ni in vegetables (e.g., Beassica pekinensis L., Allium fistulosum L., Spinacia oleracea L.) collected from the wastewater-irrigated soils exceeded the maximum permissible limits, and this also increased the daily intake of metals by food. However, compared with the health risk index of <1 for heavy metals, the ingestion of vegetables from the soils irrigated with sewage effluent posed a low health risk. Nevertheless, heavy metal concentrations should be periodically monitored in vegetables grown in these soils together with the implementation effective remediation technologies to minimize possible impacts on human health.     

Dynamics of aeolian desertification and its driving forces in the Horqin Sandy Land,Northern China

Aeolian desertification is one of the most serious environmental and socioeconomic problems in arid, semi-arid, and dry subhumid zones. Understanding desertification processes and causes is important to provide reasonable and effective control measures for preventing desertification. With satellite remote sensing images as data source to assess the temporal and spatial dynamics of desertification from 1975 to 2010 in the Horqin Sandy Land, dynamic changes of aeolian desertification were detected using the human–machine interactive interpretation method. The driving factors of local desertification were analyzed based on natural and socioeconomic data. The results show that aeolian desertified land in the study area covered 30,199 km² in 2010, accounting for 24.1 % of the study area. The total area of aeolian desertified land obviously expanded from 30,884 km² in 1975 to 32,071 km² in 1990, and gradually decreased to 30,199 km² in 2010; aeolian desertified land represented an increasing trend firstly and then decreased. During the past 35 years, the gravity centers of desertified lands that are classified as extremely severe and severe generally migrated to the northeast, whereas those that are moderate and slight migrated to the northwest. The migration distance of severely desertified land was the largest, which indicated the southern desertified lands were improved during the last few decades. In addition, the climatic variation in the past 35 years has been favorable to desertification in the Horqin Sandy Land. Aeolian desertified land rapidly expanded from 1975 to 1990 under the combined effects of climate changes and unreasonable human activities. After the 1990s, the main driving factors responsible for the decrease in desertification were positive human activities, such as the series of antidesertification and ecological restoration projects.