生物基质对煤渣改良地下渗滤系统脱氮效果的影响

地下渗滤系统(SWIS)对硝化、反硝化过程调控不灵活,导致其对氮的去除效果不够理想。组建了两套SWIS装置(1#装置:65～80cm段没有生物基质;2~#装置:65～80cm段添加生物基质),对沿程氮素、硝化和反硝化作用强度及氮还原酶活性进行分析。结果表明,两套装置均表现为硝化反应主要发生在20～60cm段,反硝化反应主要发生在60～80cm段。2~#装置的反硝化作用明显强于1#装置,因此其TN去除率高于1~#装置。硝化作用强度随深度增加而递减,反硝化作用强度随深度增加而递增。硝酸盐还原酶(NAR)活性随深度的增加而逐渐减弱,亚硝酸盐还原酶(NIR)活性随深度的增加先减弱后又增强。主要原因是2~#装置中添加了干化污泥作为生物基质,为反硝化作用补充了碳源,增强了脱氮能力。     

爆炸冲击波作用下圆形通风设施的动态破坏特性

为了研究瓦斯爆炸对通风设施造成的严重破坏及其导致的通风系统紊乱与灾情迅速扩展问题,基于LS-DYNA有限元软件,模拟研究巷道中瓦斯爆炸冲击波作用下圆形通风设施的动态破坏特性,分析应力、应变、速度、位移的动态特征及其破坏过程,并对圆形通风设施动态破坏机理进行初步探索。研究结果表明:爆炸冲击波作用下,圆形通风设施正、反面出现压应力与拉应力分布圆环,且压应力与拉应力峰值处于在外部受约束边界径向圆环附近区域与圆心位置,应变、速度和位移最大值均分布在次区域;爆炸冲击波作用下,通风设施表面形成多圈的正向和反向的应变相互交替,呈现W型的褶皱变形;爆炸冲击波作用下,环向裂纹集中在受约束的边界区域附近,发生脆性破坏,其他区域会出现较多的径向裂纹,可发生韧性破坏,整个断裂过程是脆性与韧性断裂的混合型断裂。     

基于CREAM和贝叶斯网络的空管人误概率预测方法

针对研究管制人因可靠性时存在的模糊性和片面性问题,采用认知可靠性与失误分析方法（CREAM）中的扩展预测法,计算10项管制通用任务的人误概率;在此基础上,以管制行为形成因子作为根节点构建贝叶斯网络,建立其与情景控制模式的不确定关系模型,对管制员在多任务中的人误概率进行预测。研究结果表明:在由相同评判者给出行为形成因子影响效应的前提下,由CREAM扩展预测法和构建贝叶斯网络的方法预测得到的多数任务的人误概率差异较大,从方法的客观性、合理性和适用性角度分析,贝叶斯网络在研究该问题时更具优势。     

消毒水使用对汽车VOC检测结果的影响

以84消毒液为例,研究其对皮革、塑料、发泡、地毯、密封条几种典型汽车材料的袋子法VOC检测结果的影响。经过实验结果分析:84消毒液直接喷在样品上对袋子法VOC检测结果存在影响;84消毒液喷在用PE缠绕膜包装的样品上对袋子法VOC检测结果无影响。     

新型污染物风险防范国际实践及其对中国的启示

随着重化工业的快速发展和各类化学品的大量使用,一些新型污染物对中国居民和生态环境的危害正逐步显现并日趋严重。如何进一步完善中国新型污染物的风险防范体系,是中国生态环境治理面临的重要问题。发达国家新型污染物的风险防范工作启动较早,对中国完善新型污染物风险防范体系具有重要的借鉴意义。本文从制度建设、体制机制、评估监测、科学研究等方面比较国内外新型污染物风险防范实践的异同,立足我国国情,发现国内实践还需加强之处。在此基础上,提出国际新型污染物风险防范实践对中国的启示。     

Sulfur cycle as an electron mediator between carbon and nitrate in a constructed wetland microcosm

• Fe(III) accepted the most electrons from organics, followed by NO₃^‒, SO₄^2‒, and O₂. • The electrons accepted by SO₄^2‒ could be stored in the solid AVS, FeS₂-S, and S⁰. • The autotrophic denitrification driven by solid S had two-phase characteristics. • A conceptual model involving electron acceptance, storage, and donation was built. • S cycle transferred electrons between organics and NO₃^‒ with an efficiency of 15%. A constructed wetland microcosm was employed to investigate the sulfur cycle-mediated electron transfer between carbon and nitrate. Sulfate accepted electrons from organics at the average rate of 0.84 mol/(m³·d) through sulfate reduction, which accounted for 20.0% of the electron input rate. The remainder of the electrons derived from organics were accepted by dissolved oxygen (2.6%), nitrate (26.8%), and iron(III) (39.9%). The sulfide produced from sulfate reduction was transformed into acid-volatile sulfide, pyrite, and elemental sulfur, which were deposited in the substratum, storing electrons in the microcosm at the average rate of 0.52 mol/(m³·d). In the presence of nitrate, the acid-volatile and elemental sulfur were oxidized to sulfate, donating electrons at the average rate of 0.14 mol/(m³·d) and driving autotrophic denitrification at the average rate of 0.30 g N/(m³·d). The overall electron transfer efficiency of the sulfur cycle for autotrophic denitrification was 15.3%. A mass balance assessment indicated that approximately 50% of the input sulfur was discharged from the microcosm, and the remainder was removed through deposition (49%) and plant uptake (1%). Dominant sulfate-reducing (i.e., Desulfovirga, Desulforhopalus, Desulfatitalea, and Desulfatirhabdium) and sulfur-oxidizing bacteria (i.e., Thiohalobacter, Thiobacillus, Sulfuritalea, and Sulfurisoma), which jointly fulfilled a sustainable sulfur cycle, were identified. These results improved understanding of electron transfers among carbon, nitrogen, and sulfur cycles in constructed wetlands, and are of engineering significance.     

A novel sigma coordinate system to simulate abrupt changes of underwater terrain in a hydrodynamic model: application to Lake Mead,USA

The sigma (SIG) coordinate system in ocean circulation simulation models results inevitably in horizontal pressure gradient error. This problem also emerges in models of deep lakes or reservoirs with the same characteristics of underwater terrain mutation. SIG coordinates reflect vertical relative stratification but cannot be used to calculate horizontal pressure gradient force in places with drastic topographic changes; this results in vertical water temperature and circulation errors. In deep lakes or reservoirs, differences in water density caused by the temperature difference between upper and lower water bodies is the primary cause of thermal stratification phenomena. Lake Mead was used as a case study on steep topography based on Environmental Fluid Dynamics Code (EFDC) model in this study. SIG coordinates result in close agreement between the calibrated temperature time series at the top and middle water layers, but disparity in the bottom water layer. The error emerges in the horizontal pressure gradient error due to the SIG coordinate transformation. Neither increasing the vertical resolution nor adjusting the horizontal viscosity coefficient resolve this error. We test the sigma-zed (SGZ) coordinate which combines Z coordinate and SIG coordinate as a replacement for the SIG coordinate to find that they effectively reduce the model’s runtime and simulation efficiency. The vertical temperature distribution in SGZ coordinate mode is more accurate than the distribution in SIG coordinate mode. The Navier-Stokes horizontal gradient and advection diffusion equation results under SIG coordinates are very sensitive to the pressure gradient. The replacement also enhances resolution near the thermocline, facilitates reclosing of the water bottom and the equal sigma surface, lends significant advantages in terms of vertical temperature in the simulation for local deep water with steep terrain, and shortens runtime for 0.14 h. SGZ mixed coordinates are recommended in the simulation of deep lakes or reservoirs wherein the underwater topography is large (with abundant continuous deep trenches or reefs).

     

Manganese-modified biochar for highly efficient sorption of cadmium

Environmental Science and Pollution Research - In this study, corn stalk was modified by manganese (Mn) before (MBC1) and after (MBC2) pyrolysis at different temperatures (400~600 °C)...     

粗枝云杉不同径级根系分解过程中4种养分元素的释放特征

植物根系分解是养分元素进入土壤的重要途径之一.为了解径级对根系分解过程中养分元素释放的潜在影响,以川西亚高山针叶林中的粗枝云杉(Picea asperata)为对象,采用原位分解试验,研究云杉3个径级(0-2 mm,2-5 mm和5-10 mm)根系分解过程中钾(K)、钠(Na)、钙(Ca)和镁(Mg)元素的浓度、残留...     

振荡辐射下PMMA 热解与着火过程研究

采用正弦波变化振荡的辐射热流,对热厚PMMA(聚甲基丙烯酸甲酯)的热解和着火过程进行研究,同时采用数值模拟,对实验结果进行验证和补充。结果表明,表面温度和深度温度随着时间而增加,温度由于周期性的辐射而发生振荡,而振荡幅度随着深度的增加而衰减;表面温度与深度温度振荡存在时间延迟;着火时间随着热流振荡周期的增大而减小,主要由于平均热流密度随着周期增大而增大。