丹江口水库氮磷内源释放对比

利用柱状沉积物采样器在丹江口水库采集不同点位原位柱状沉积物,通过静态培养释放实验及间隙水分子扩散模型两种方法获取沉积物-水界面N和P释放速率,分析水体N和P释放特征.结果表明,不同采样点N和P界面交换速率差异显著.静态培养条件下,5个点位NH_4~+-N和PO_4~(3-)-P释放速率分别为13. 07～24. 88 mg·(m~2·d)~(-1)和3. 06～6. 02 mg·(m~2·d)~(-1);分子扩散模型条件下,5个点位NH_4~+-N和PO_4~(3-)-P释放速率分别为2. 67～7. 25 mg·(m~2·d)~(-1)和0. 04～0. 18 mg·(m~2·d)~(-1). N和P释放速率总体呈北高南低的趋势,支流N和P最低释放速率分别是主库区最高释放速率的1. 48和1. 57倍.两种方法均表明郭家山支流N和P的释放速率最高,具有较大内源N和P释放风险.比较两种方法发现,利用Fick定律计算出的界面N和P释放速率明显小于柱样模拟方法得出的结果,N和P的R/F值分别为3. 43～4. 98和29. 67～72. 88,这表明用分子扩散模型法进行内源释放速率估算时,偏离真实情况较大,而原柱样静态模拟实验则较贴近真实情况.     

2000~2020年天津PM2.5质量浓度演变及驱动因子分析

基于中国大气成分实时追踪数据集、天津气象局和生态环境局长序列PM_2.5质量浓度和气象观测,结合MEIC排放清单和环境模式构建的细颗粒气象条件扩散指数,研究2000～2020年天津地区PM_2.5质量浓度演变规律及驱动因子,以期更科学地分析气象对大气环境影响,为“十四五”期间深度环境治理提供支撑.结果表明,2000～2020年天津PM_2.5质量浓度呈现3个阶段变化,第一阶段2000～2007年,呈现持续地上升,其变化速率为4.58μg·（m³·a）^-1,该阶段排放量的快速增加是主导因素,其作用是气象条件年际波动影响的4倍,排放量增加使得PM_2.5质量浓度增加45.3%;第二阶段为2007～2013年,该阶段PM_2.5质量浓度呈现波动变化,出现了两个浓度峰值年（2007年和2013年）,该阶段排放稳定,气象条件年际波动对PM_2.5质量浓度年际波动产生重要影响,两者相关系数0.81;第三阶段为2013～2020年,PM<...     

脱水污泥薄层干燥特性及动力学模型分析

采用薄层干燥方式进行脱水污泥热干燥的研究,考察了污泥的干燥特性,并引入薄层干燥模型进行数值分析.结果表明, Logarithmic模型比其他模型更适合薄层污泥干燥分析.应用Fick扩散模型,得到80~150℃条件下薄层污泥干燥的有效扩散系数的变化范围为8.486′10-10~4.386′10-9m2/s,并根据Arrhenius经验公式建立温度与扩散系数的关系,得到污泥干燥时水分扩散的活化能为29.56kJ/mol.     

Migration of colloids in discretely fractured porous media: effect of colloidal matrix diffusion

Numerical simulations of colloid transport in discretely fractured porous media were performed to investigate the importance of matrix diffusion of colloids as well as the filtration and remobilization of colloidal particles in both the fractures and porous matrix. To achieve this objective a finite element numerical code entitled COLDIFF was developed. The processes that COLDIFF takes into account include advective-dispersive transport of colloids, filtration and remobilization of colloidal particles in both fractures and porous matrix, and diffusive interactions of colloids between the fractures and porous matrix. Three sets of simulations were conducted to examine the importance of parameters and processes controlling colloid migration. First, a sensitivity analysis was performed using a porous block containing a single fracture to determine the relative importance of various phenomenological coefficients on colloid transport. The primary result of the analysis showed that the porosity of the matrix and the process of colloid filtration in fractures play important roles in controlling colloid migration. Second, simulations were performed to replicate and examine the results of a laboratory column study using a fractured shale saprolite. Results of this analysis showed that the filtration of colloidal particles in the porous matrix can greatly affect the tailing of colloid concentrations after the colloid source was removed. Finally, field-scale simulations were performed to examine the effect of matrix porosity, fracture filtration and fracture remobilization on long-term colloid concentration and migration distance. The field scale simulations indicated that matrix diffusion and fracture filtration can significantly reduce colloid migration distance. Results of all three analyses indicated that in environments where porosity is relatively high and colloidal particles are small enough to diffuse out of fractures, the characteristics of the porous matrix that affect colloid transport become more important than those of the fracture network. Because the properties of the fracture network tend to have greater uncertainty due to difficulties in their measurement relative to those of the porous matrix, prediction uncertainties associated with colloid transport in discretely fractured porous media may be reduced.     

城市污水排江工程模型试验的研究

对城市污水排江问题进行了模拟试验,通过对水力模型不同试验工况中改变喷嘴个数、射流速度、射流角度和上升管间距条件下的试验结果分析,结合武汉市污水排江工程问题,确定了黄浦路、平湖门尾水排放中的近区多喷口形式的最佳工程参数,实践证明效果良好。     

含油污泥薄层干燥特性及动力学模型分析

采用薄层干燥方式进行含油污泥热干燥的研究,引入薄层干燥模型对含油污泥干燥过程进行模拟,结果表明,Midilli模型比其他模型更适合含油污泥的薄层干燥分析。应用Fick扩散模型,得到80～140℃条件下含油污泥干燥的有效扩散系数变化范围为1.08×10-10～4.22×10-10 m2/s,其值随着温度升高而增大。根据Arrhenius经验公式建立温度与扩散系数的关系,得到含油污泥干燥时水分扩散的活化能为27.26kJ/mol。     

泽泻(Alisma orientale)对全氟化合物的吸收和传输特征-浓度的影响

为探究泽泻(Alisma orientale)对不同浓度全氟化合物(PFASs)的吸收、积累和传输特征,进行了为期3周的水培实验,全氟辛酸和全氟辛烷磺酸的暴露浓度分别为0、5、10、50、100、200、500和1 000μg·L~(-1).结果表明:随着PFASs浓度的增加,根系电导率、根茎中Cu含量、茎叶中Ca含量均降低,但泽泻生长状况良好;植物对PFASs的去除量不断增加(0. 87～116. 50μg),去除率却不断降低(20. 1%～2. 9%).根、茎和叶中PFASs的浓度随着PFASs浓度的增加呈线性增加,且符合Langmuir吸附等温式和Michaelis-menten方程,表明泽泻通过被动扩散的方式吸收PFASs.计算PFOA和PFOS的根、茎和蒸腾流富集系数(RCF、SCF、TSCF),并用限制分配模型对RCF和SCF值进行拟合,发现RCF、SCF、TSCF和限制分配模型准平衡分配系数αpt均随着PFASs浓度的增加而降低,这是由于随着PFASs浓度的增加,达到平衡所需要的水分量增加,达到平衡的时间也变长.     

铁磁流体对煤粒瓦斯解吸性能影响实验研究*

为探究铁磁流体对煤体瓦斯解吸性能的影响,采用水浴恒温吸附解吸系统,开展0.44,0.65,1.14 MPa 3组不同平衡压力下加铁磁流体前后的瓦斯解吸对比实验,根据Langmuir方程经验公式计算瓦斯极限解吸量和初始扩散系数,分析铁磁流体对煤体瓦斯解吸影响的机理。结果表明:在3组不同平衡压力下加入铁磁流体后瓦斯极限解吸量由2.5,10,20 mL/g降低为2.22,3.33,10 mL/g,降低11.2%,66.7%,50%;初始扩散系数由0.997 1,1.629 9,3.888 3 μm2·s降低为0.685 5,0.997 1,2.933 5 μm2·s,降低31.25%,38.82%,24.56%。在铁磁流体的作用下,煤体瓦斯解吸性能得到大幅降低。     

中国低碳城市试点的政策设计逻辑

政策试点是中国国家治理策略体系的重要组成部分,是中国政府遵循“由点到面”逻辑以试验手段制定政策的一种常规性工作方法。低碳城市试点是中国应对气候变化战略的重要组成部分,通过选择不同类型、不同发展阶段、不同资源禀赋的地区开展试点,探索经济增长与碳排放脱钩的模式。现有文献侧重低碳城市建设的内涵、建设模式与路径、温室气体的核算方法、政策手段、峰值研究与达峰路径、效果评估等,有力地支持了低碳城市建设决策,但对于低碳城市试点的政策设计鲜有涉及。本文从政策过程理论、央地关系两个视角,结合府际学习与竞争关系,建构了中国低碳城市政策“试点–扩散”机制与政府行为的分析框架。中国的低碳城市试点具有探索型开拓性、综合型专业性、授权型自主性的特点,结合三批低碳城市试点的文件要求和实践进展,从政策试点的选点、设计、执行、监督和评估五个方面对于中国低碳城市试点进行了系统的梳理分析。相较于经济领域的其他政策试点,低碳城市政策试点具有弱激励弱约束的政策环境。地方政府基于自身的学习能力和领导力,在政策创新方面表现出争先、自主、效仿和守成四种行为特征,并以杭州、深圳、镇江、成都四个表率城市做了实证。政策“试点-扩散”的过程从本质上讲是中国政策创新与扩散的过程,可能在现实中需要往复多次进行,中国已陆续开展的三批低碳城市试点工作就遵循这样的政策逻辑。试点的意义是试出问题、解决问题、积累经验。从前三批试点城市评估结果来看,试点城市在低碳发展目标设定、转型路径探索和低碳发展动力转换等方面与社会的预期仍有差距,为此本文提出了推进低碳城市建设的四点建议:一是激发城市低碳发展的内生动力;二是完善低碳城市试点的科学论证机制;三是建立激励与约束并举的长效机制;四是强化市场公平竞争的政策导向。     

An Experimental Methodology for Monitoring Contaminant Transport Through Geotechnical Centrifuge Models

In this paper, an attempt has been made to highlight an experimental methodology for monitoring contaminant transport through locally available silty soil and commercially available clay in geotechnical centrifuge models, for different compaction states. Use of multiple depth sensors to determine depth distribution of sodium chloride in the soil column has been detailed. The obtained results have been compared with argentometric method. To validate the centrifuge modelling, modelling of models has been used. The test setup developed can simulate contaminant transport mechanisms through the soil mass, which is approximately 10 m deep, over a period of 600 days. R _e and P _e are found to be N times higher in the centrifuge models. These numbers are found to be several orders less than unity. This indicates that laminar flow prevails and the dominating Cl⁻ transport mechanism in centrifuge is diffusion. The study also highlights the fact that the geotechnical centrifuge modelling can be used as a viable alternative to field scale experimentation.