填埋场中亚硝酸还原酶测定条件的优化

填埋垃圾中的含氮化合物经一系列生物脱氮作用,最终使得填埋场中的氮素得以消减,在这一过程中亚硝酸还原酶起着十分重要的作用。以填埋场中的填埋垃圾为研究对象,在土壤亚硝酸还原酶测定方法的基础上,对亚硝酸还原酶活性测定条件进行了优化。结果表明,填埋垃圾中的亚硝酸还原酶活性测定的最优条件为:垃圾样品风干温度25℃,2mL的1%NaNO2溶液和2.5 mL的1%葡萄糖溶液,抽气5 min,置于25℃的培养箱中培养24 h。优化后的测定条件相对标准偏差(RSD)小于1.27%,表明该方法具有较高的灵敏度和精密度。     

Source apportionment of polycyclic aromatic hydrocarbons in surface soil in Tianjin, China

Principal component analysis and multiple linear regression were applied to apportion sources of polycyclic aromatic hydrocarbons (PAHs) in surface soils of Tianjin, China based on the measured PAH concentrations of 188 surface soil samples. Four principal components were identified representing coal combustion, petroleum, coke oven plus biomass burning, and chemical industry discharge, respectively. The contributions of major sources were quantified as 41% from coal, 20% from petroleum, and 39% from coking and biomass, which are compatible with PAH emissions estimated based on fuel consumption and emission factors. When the study area was divided into three zones with distinctive differences in soil PAH concentration and profile, different source features were unveiled. For the industrialized Tanggu-Hangu zone, the major contributors were cooking (43%), coal (37%) and vehicle exhaust (20%). In rural area, however, in addition to the three main sources, biomass burning was also important (13%). In urban-suburban zone, incineration accounted for one fourth of the total.     

Reassessment of the Ocean-To-Atmosphere Flux of Carbon Monoxide

Carbon monoxide (CO) in the surface sea waters is produced predominantly by photochemical processes, oxidized by micro-organisms and outgassed to the atmosphere. to assess carbon monoxide flux from the oceans to the atmosphere, the photochemical production and microbial oxidation of carbon monoxide in the oceanic mixed-layer was investigated during several oeanographic cruises and in the laboratory. the photoproduction rate of carbon monoxide was found to be well correlated to the concentration of dissolved organic carbon (DOC) in coastal and open ocean surface waters. Taking a global average carbon monoxide production rate of 10 ± 2 nmole litre^-1 (mg DOC hr)^-1 in the surface open ocean water, and 25 ± 7 nmole litre^-1 (mg DOC hr)^-1 in coastal sea water, at cloud-free summer solar noon, the photochemical production of carbon monoxide in the global oceans is estimated to be at a rate of 1200 ± 200 Tg CO y^-1. the microbial carbon monoxide turnover time in the mixed-layer was observed to range from hours in a coastal estuary to 16 days in the Pacific along 1057deg; W in dark incubations. Natural sunlight can largely inhibit the microbial consumption of carbon monoxide in surface water. On a global scale, microbial consumption is responsible for the loss of less than 10% of photochemical produced carbon monoxide in the surface ocean. Field measurements have shown that the net transport of carbon monoxide from the euphotic zone to the underlying deeper ocean water is limited and that the overall life time in surface sea waters is less than 3-4 hours. When combined, these field measurements with the photoproduction and microbial consumption rates obtained, we estimate the oceanic flux to the atmosphere is about 1000 ± 200 Tg CO y^-1, which represents the largest single source of atmospheric carbon monoxide.     

Measurement of the surface charge of ultrafine particles from laser printers and analysis of their electrostatic force

Ultrafine particles (UFPs) released from laser printers are electrostatically charged during the working processes of the devices, and the electrostatic force can obviously influence the dynamics of the particles. Due to the measurement difficulty and scarcity of relevant research, this issue was not reported. This study tried to address this issue through experimental measurement of the surface charge of UFPs and numerical investigation on the influence of electrostatic force on the dynamics of UFPs. A test chamber was set up to collect the UFPs, and the Scanning Electron Microscope was used to observe the morphologies of the UFPs. Based on the particle diameter and surface zeta potential, the surface charge of UFPs was calculated. The measurement results gave that particle emitted from laser printers are negatively charged and the average surface charge of particle emissions for four laser printers is in a range of about ?4.16 × 10^?17 to ?6.07 × 10^?17 C (～?260 to ?379 e). This paper also discussed the influence of electrostatic force on the dynamics of UFPs. According to the numerical investigation, it was found that, in the absence of electric field, the electrostatic force has to be considered when the surface charge is larger than 1 × 10^?16 C and when the UFP is very close to the wall with a distance of less than 0.01 m. These findings will guide constructively in predicting the dispersion and deposition of particles emitted from laser printers.     

改性粉煤灰协同PSFA处理高度乳化油废水

通过正交实验对改性粉煤灰协同粉煤灰基混凝剂PSFA处理高度乳化油废水的工艺条件进行了优化。实验结果表明:当处理500 mL废水,投加改性粉煤灰25 g,粉煤灰基混凝剂6～8 g,PAM6～9 mL,pH为7.0,搅拌10～15 min的优化条件下,高度乳化油废水中COD、石油类物质的去除率可分别可达85.4%及50.3%。该方法与传统CaCl2+PFS+PAM组合相比,具有处理效果好,沉降速度快,运行费用低等优点。     

污泥龄对LSP & PNR污泥减量新工艺运行效能的影响

通过研究分析污泥龄（SRT）对富磷污水除磷的LSP&PNR污泥减量新工艺运行效果的影响，结果发现，延长污泥龄有利于提高系统的厌氧释磷能力，但不影响其总的除磷率，同时磷的回收比例增大，当SRT=50 d时，磷回收率取得最大值70.4％；LSP&PNR系统污泥龄增加，还有利于污泥产率的降低。试验还发现，排富磷污水除磷的长污泥龄LSP&PNR系统的除磷效率与污泥产率之间不存在制约关系，即系统可以同时获得优异的污泥减量与生物除磷效果，当SRT=50 d时，每降解1 kg COD仅产生0.143 kg污泥，而除磷率达最高值928％；LSP&PNR系统中SRT、DO与SVI之间存在一定的相关性，在供氧充足（DO＝0.8～1.5 mg/L）条件下，SRT增加，SVI越高，但对于SRT为50 d的LSP&PNR系统，稳定运行时没有污泥膨胀之虞。     

污泥龄对LSP & PNR污泥减量新工艺运行效能的影响

通过研究分析污泥龄(SRT)对富磷污水除磷的LSP&PNR污泥减量新工艺运行效果的影响,结果发现,延长污泥龄有利于提高系统的厌氧释磷能力,但不影响其总的除磷率,同时磷的回收比例增大,当SRT=50 d时,磷回收率取得最大值70.4%;LSP&PNR系统污泥龄增加,还有利于污泥产率的降低.试验还发现,排富磷污水除磷的长污泥龄LSP&PNR系统的除磷效率与污泥产率之间不存在制约关系,即系统可以同时获得优异的污泥减量与生物除磷效果,当SRT=50 d时,每降解1 kg COD仅产生0.143 kg污泥,而除磷率达最高值92.8%;LSP&PNR系统中SRT、DO与SVI之间存在一定的相关性,在供氧充足(DO=0.8～1.5 mg/L)条件下,SRT增加,SVI越高,但对于SRT为50 d的LSP&PNR系统,稳定运行时没有污泥膨胀之虞.     

贝纳德效应和地震预报

本文根据海城地震前后重力变化的实测资料提出重力加速度随时间变化的一种简化表示。在重力发生扰动时对贝纳德问题的动力学方程进行求解。计算结果表明,在强地震的孕育期,贝纳德花样的周期变化在一定时间后将自动停止。这个结论的验证可以作为一种新的地震预测方法的理论基础。     

一株对二甲苯降解菌的筛选鉴定及其降解特性

以对二甲苯为惟—碳源和能源,从某石化废水处理厂活性污泥中筛选得到一株对二甲苯降解菌株.生理生化实验、16S rDNA基因鉴定结果表明,该菌属于假单胞杆菌属(Pseudomonas sp.).通过对降解过程的动力学分析可知,该菌对底物的降解过程符合零级动力学特征,在初始对二甲苯质量浓度为800 mg/L时,降解速率常数最大,达18.43 mg/(L·h).在降解温度为30 ℃、废水pH为7.5、摇床转速为150 r/min的条件下,将5 mL菌液投加至32 mL对二甲苯质量浓度分别为840 mg/L和830 mg/L的焦化废水和石化废水中,降解84 h后基本无对二甲苯检出.