偏二甲肼超临界水氧化动力学研究

利用一套连续式超临界水氧化实验装置,以H2O2为氧化剂,在480～550℃、30 MPa条件下,进行了超临界水氧化偏二甲肼实验,建立了COD去除宏观动力学方程.实验结果表明,在超临界条件下,偏二甲肼氧化分解很快,当温度为550℃、压力为30 MPa、停留时间为5.8 s时,COD去除率可高达93.5%以上.偏二甲肼的去除率随反应温度升高、停留时间延长而提高.在H2O2过量50%的情况下,偏二甲肼氧化分解反应对有机物为1.13级,对氧气为0.29级;反应活化能Ea为44.65 kJ·mol-1;指前因子A为4.93×103.     

Detection and quantitation of trace levels of low molecular weight halocarbons (LMHs) associated with commercial sodium humate

Examination of vapor above commercial sodium humate and above 10wt% aqueous humate solution by gas chromatography (GC) revealed the presence of chloroform and trichloroethylene. Further examination of the aqueous humate by the purge and trap procedure confirmed the association of chloroform and trichloroethylene with the humate. GC/mass spectrometry analyses of methylene chloride extract of the humate established the association of LMHs with the humate. Improved headspace capillary GC technique showed that the humate contained not only chloroform, trichloroethylene but several other LMHs in the range 190 to 4000ng·kg^‐1.     

A model algorithm for defining the vertical profile of absolute humidity by ground measurements of humidity

In this study a double model algorithm is developed for the simulation of the vertical profiles of monthly values of absolute humidity. The thrust of the algorithm is that is depends on the use of ground measurements for humidity and is based upon the use of two model relations for altitudes above and below 1 Km respectively. Monthly absolute humidity profiles as estimated using the specially constructed double model algorithm compare well with those calculated with the use of radiosonde data for the time period 1980–1990 (Helliniko station, Southern Greece). In particular the model estimation is very satisfactory at altitudes above the Planetary Boundary Layer and rather satisfying at altitudes below 1 Km. This implies that the model algorithm may be useful in supporting climatological studies in areas where lack of relevant information on the vertical distribution of water vapour is recognised.     

灾害化学的核心原理研究

为完善安全科学原理的内容,促进安全科学的理论发展,基于对安全科学理论体系和灾害化学的研究,提出灾害化学原理的定义及其研究内容。归纳出灾害化学的六个核心原理,即热平衡原理、过程控制原理、平衡移动原理、反应减速原理、条件阻隔原理、质能守恒原理,并分析这些原理的概念和内涵。最后,从本质化安全生产设计、职业安全健康与管理和安全经济效益的角度分析灾害化学原理的应用,并选取具体实例详细阐述了各原理的实用性。     

辽宁省背景地区降水化学特征及其与大气传输的关系

为了解辽宁省背景地区降水化学特征及其与大气传输的关系,于2007年2月─2008年1月在辽中县水文监测站进行了降水化学特征观测,测量项目包括降水pH,电导率和离子浓度. 观测期间降水pH为3.4～7.3,降水量加权平均值为4.6,整体呈酸性. 降水中主要阴离子为SO₄2-和NO₃-,浓度分别为154.3和53.4 μeq/L,二者占阴离子总量的76.8%; 主要阳离子为NH₄+和Ca2+,浓度分别为124.6和89.2 μeq/L,占阳离子总量的70.6%. 利用后向气流轨迹分析了降水气团来源对降水化学的影响,结果表明:在辽宁省及周边地区的局地气团影响下,降水中离子浓度最高;而在起源于东亚地区,经朝鲜半岛到达的南-东南气团影响下,降水次数虽最多,但离子浓度最低.      

太湖北部流域水化学特征及其控制因素

为了解太湖北部流域主要河网区水质受该流域地质状况、岩石和土壤的化学风化作用以及人类活动的影响等方面,对太湖北部流域河网区主要河道水体中的主要离子进行了采样研究。结果表明：太湖北部流域水体中的TDS平均值为355．74mg·L-1,变化范围为276．08--681．54mg·L-1,其中ca2＋和HCO3-是占绝对优势的离子,分别占阳离子和阴离子总量的46．2％和48．9％;其次是Na＋和SO42-,分别占阳离子和阴离子总量的35．9％和27．5％。进而判断出该流域水化学类型是以碳酸盐岩石和蒸发岩来源为主的HCO3-Ca2＋-Na＋型。再从离子的自然起源和人类活动角度分别对水化学类型的控制因素进行分析,一方面利用吉布斯分布模式投点作图得出结论：其离子自然起源的优势机制是岩石的风化作用,而蒸发一结晶和大气降水的输入作用十分微弱,这与该流域的水文、地理、地质背景相一致;另一方面通过SPSS软件的相关关系分析得出结论：NO3-、SO42-、心、ca2＋和Mg2＋的相关性较强,与cl‘也呈正相关,说明水体中这些主要离子都具有共同的来源,其中NO3-的较高含量（平均值为14．74mg·L-1）反映了该流域受人类影响较大。尤其是NO3-与sO42-的相关性达到0．83,再次说明氮污染对该流域水体的酸化和水质变化有较大影响。     

Numerical study on the ozone formation inside street canyons using a chemistry box model

Tropospheric ozone is a secondary air pollutant produced in the presence of nitrogen oxides (NO_x),volatile organic compounds (VOCs),and solar radiation.In an urban environment,ground-level vehicular exhaust is the major anthropogenic source of ozone precursors.In the cases of street canyons,pollutant dilution is weakened by the surrounding buildings that creates localized high concentration of NO_x and VOCs,and thus leads to high potential of ozone formation.By considering the major physical and chemica...     

利用化学沉淀法降低焦化废水氨氮浓度的预处理工艺研究

为了有效净化高浓度氨氮工业废水,采用向废水中投加MgCl2·6H2O和Na3PO4·12H2O生成磷酸氨镁沉淀的方法,以去除其中的高浓度氨氮。结果表明,在pH值为9.0,Mg^2＋、NH4^＋、PO4^3-的摩尔比为1.2：1：0.9,反应温度为25℃,反应时间为20 min,沉淀时间为50 min的条件下,氨氮质量浓度可由3 100 mg/l降低到56mg/l,去除率达到98%以上,为后续生化处理创造了条件。     

Spatially distributed modeling of the long-term carbon balance of a boreal landscape

Spatially and temporally distributed information on the sizes of biomass carbon (C) pools (BCPs) and soil C pools (SCPs) is vital for improving our understanding of biosphere-atmosphere C fluxes. Because the sizes of C pools result from the integrated effects of primary production, age-effects, changes in climate, atmospheric CO₂ concentration, N deposition, and disturbances, a modeling scheme that interactively considers these processes is important. We used the InTEC model, driven by various spatio-temporal datasets to simulate the long-term C-balance in a boreal landscape in eastern Canada. Our results suggested that in this boreal landscape, mature coniferous stands had stabilized their productivity and fluctuated as a weak C-sink or C-source depending on the interannual variations in hydrometeorological factors. Disturbed deciduous stands were larger C-sinks (NEP₂₀₀₄ = 150 gC m⁻² yr⁻¹) than undisturbed coniferous stands (e.g. NEP₂₀₀₄ = 8 gC m⁻² yr⁻¹). Wetlands had lower NPP but showed temporally consistent C accumulation patterns. The simulated spatio-temporal patterns of BCPs and SCPs were unique and reflected the integrated effects of climate, plant growth and atmospheric chemistry besides the inherent properties of the C pool themselves. The simulated BCPs and SCPs generally compared well with the biometric estimates (BCPs: r = 0.86, SCPs: r = 0.84). The largest BCP biases were found in recently disturbed stands and the largest SCP biases were seen in locations where moss necro-masses were abundant. Reconstructing C pools and C fluxes in the ecosystem in such a spatio-temporal manner could help reduce the uncertainties in our understanding of terrestrial C-cycle.     

A review of gas-phase chemical mechanisms commonly used in atmospheric chemistry modelling

The atmospheric chemical mechanism is an essential component of airshed models used for investigating the chemical behaviors and impacts of species. Since the first tropospheric chemical mechanism was proposed in the 1960s, various mechanisms including Master Chemical Mechanism (MCM), Carbon Bond Mechanism (CBM), Statewide Air Pollution Research Center (SAPRC) and Regional Atmospheric Chemistry Mechanism (RACM) have been developed for different research purposes. This work summarizes the development and applications of these mechanisms, introduces their compositions and lumping methods, and compares the ways the mechanisms treat radicals with box model simulations. CBM can reproduce urban pollution events with relatively low cost compared to SAPRC and RACM, whereas the chemical behaviors of radicals and the photochemical production of ozone are described in detail in RACM. The photolysis rates of some oxygenated compounds are low in SAPRC07, which may result in underestimation of radical levels. As an explicit chemical mechanism, MCM describes the chemical processes of primary pollutants and their oxidation products in detail. MCM can be used to investigate certain chemical processes; however, due to its large size, it is rarely used in regional model simulations. A box model case study showed that the chemical behavior of OH and HO₂ radicals and the production of ozone were well described by all mechanisms. CBM and SAPRC underestimated the radical levels for different chemical treatments, leading to low ozone production values in both cases. MCM and RACM are widely used in box model studies, while CBM and SAPRC are often selected in regional simulations.