环境规制、省际产业转移对污染迁移的空间溢出效应

目前我国正在积极地探寻经济增长高质量发展,生态环境与经济持续、稳定的和谐发展至关重要。虽然政府制定了相关的环境治理政策,但我国环境治理整体效果仍然欠佳。自从分税制改革以来,地方政府为了获得较高经济效益,会放松对环境管理,导致环境治理高投入低成效。同时,由于区域经济发展不平衡导致政府在制定相关环境治理政策时带有区域性特点,迫使高污染高能耗企业迁移至环境规制相对薄弱的地区,由此产生污染迁移的现象。基于此,对2003—2017年30个省区市(港澳台和西藏除外)环境污染总指数的空间溢出效应进行探讨,构建动态空间杜宾模型研究环境规制、省际产业转移对污染迁移的影响。研究结果表明:①环境规制总体上对环境污染具有显著直接效应且存在正向空间溢出效应,当某省环境规制强度增加,环境污染总指数会降低,从而引起污染向相邻省份转移,造成相邻省份的环境污染总指数上升。②省际产业转移整体上对环境污染具有显著直接效应且存在负向空间溢出效应,当某省的产业转移到相邻省份时,会缓解本省环境污染,却加重相邻省份的环境污染程度。这就需要中央政府加强对于各省区市的环境管控,统筹各区域的联防联治机制。产业转移承接省份在招商引资的过程中不仅要考虑本省环境承载能力和环境治理能力,还要考虑入驻企业自身污染排放处理能力,并将污染排放指数纳入筛选条件。同时,产业转移承接省份要引入企业的生产工艺、技术、研发团队等,运用技术溢出效应提升区域环境治理水平。     

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。     

Natech风险研究:现状、理论及展望

由自然灾害引发的工业企业环境安全事故又称为自然灾害诱发的技术事故(Natech).我国是工业大国,重化工业是我国的主导产业之一;同时我国还是世界上自然灾害严重的国家之一,Natech风险不容忽视.开展Natech风险识别、评估和管理研究,有助于我国Natech风险管理体系的完善,防范和降低区域Natech风险.目前,我国Natech风险基础研究尚处于起步阶段,难以支撑我国Natech风险防控实践.本文从Natech风险发生机制、风险评估、风险感知与最大可接受风险水平、风险管理体系等四个方面回顾了国内外Natech风险研究现状,初步梳理了Natech风险的基本理论,并对我国未来Natech风险的研究方向进行了展望,为我国Natech风险研究领域的发展提供参考.     

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)...     

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。     

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...