煤基胶体特征及其在多孔介质中的运移行为

采集了长焰煤粉并提取其中的胶体,用激光粒度仪、红外光谱仪、扫描电镜和Zeta电位仪对煤基胶体的特征进行了定性和定量表征,研究了煤基胶体在石英砂的多孔介质柱中的运移特征及p H值、阳离子等环境因子的影响。结果表明,该方法提取煤基胶体的实测粒径与理论计算粒径基本吻合,煤基胶体表面具有丰富的褶皱和极其丰富的孔隙结构并呈片状,煤基胶体的化学组成以芳香烃为主,在试验范围内,煤基胶体的Zeta电位在-34.0~-21.2 e V,随p H值升高而下降。溶液p H=7时,煤基胶体在多孔介质中的运移能力最强,c/c0为0.664,增加p H值或降低p H值,运移能力下降。Ca离子对煤基在多孔介质中的运移具有明显的抑制作用,当离子强度IS(Ca Cl2)由0.001 mmol/L增加到0.1 mmol/L时,胶体悬液c/c0从0.569降至0.129。     

春季沙尘过程对华东高山背景区域颗粒物中水溶性无机离子的影响

于2014年3—5月在国家大气背景监测福建武夷山站采集了PM2.5及PM2.5~10样品,利用离子色谱对其中的水溶性组分进行分析,并同步收集气象因子及污染物质量浓度数据,结合后向气流轨迹,分离出受沙尘影响的样品,探讨了春季沙尘过程华东高山背景区域颗粒物中水溶性组分的特征.结果表明,春季武夷山背景点沙尘影响期间颗粒物质量浓度及各水溶性离子浓度均比非沙尘期高,在粗粒子中表现更为明显;沙尘期间NO-3在粗粒子中明显富集,NO-3浓度显著升高;受沙尘影响,粗粒子中阳离子与阴离子的当量浓度比及NO2的二次转化率均明显升高.     

宝鸡市街道尘埃磁学特征空间分布及环境意义

对宝鸡市街道尘埃样品进行详细系统环境磁学实验分析并结合扫描电子显微镜研究表明,宝鸡市街道尘埃中磁性矿物含量高,主要的磁性矿物为多畴和假单畴的低矫顽力亚铁磁性矿物,同时含有少量的赤铁矿等高矫顽力的硬磁性矿物.污染来源主要以工业和交通等人为污染为主.街道尘埃的磁学特征表现出一定的空间变化规律揭示出污染的空间分布,划分为6个主要区域:A(创新路到高新八路区域)和B(东风路和马营路区域),磁性物质含量整体很高,揭示污染相对较重,污染源主要为"工业+交通";C区(火炬路到医康区域)磁性物质含量相对较高,是中度污染的区域,污染源主要为"交通";D(经二路与人民路区域)、E(清姜路和姜谭路西部区域)和F(陈仓区虢镇),磁性物质含量相对较低,揭示轻度污染,污染源主要为"交通".     

添加协效剂的灵石煤自燃阻化剂的研究

为了防止煤的自燃,采用双氧水氧化升温实验,对灵石肥煤在不同阻化剂下的阻化效果进行了研究。利用阻化时间变化率判定阻化效果。结果表明,添加氧化铝厂赤泥作为协效物质的协效阻化剂有效抑制了煤样的氧化升温,提高了阻化效果,阻化时间变化率达50.78%,为灵石肥煤最佳新型协效阻化剂。新型阻化剂原料廉价易得、反应条件温和、制备过程简单、环境友好,且实现了尾矿废渣的综合利用。     

我国煤矿生产与安全投入的计量分析

煤炭生产活动中既有市场产出又有安全输出,而煤炭生产和安全投入之间的关系反映了经济发展和职业安全之间的关系。在近二十年国内煤矿生产数据的基础上,分析煤炭生产和安全之间长期的相互作用关系,根据多元统计回归分析,建立了煤炭生产模型,并使用Eviews软件进行了脉冲曲线分析和方差分解分析。最后基于分析结果,对我国煤矿生产和安全投入现状提出了改进意见。     

公众对煤矿区地质灾害的感知与适应行为研究

煤矿区的地质灾害较为常见,而且随着开采时间的推移地质灾害问题日益严重。公众对煤矿区地质灾害的感知与适应行为直接与他们的生命财产相关,同时还关系到政策法规的制定。通过对煤矿区公众的问卷调查发现,公众对地质灾害的严重程度和灾害原因感知是比较准确的,但仍有相当比例的公众选择采取无效的紧急适应行为,有近三分之一的公众没有考虑采用迁移的适应行为。公众对煤矿区地质灾害适应行为的背后涉及利益相关方的博弈。     

Advanced treatment of biologically pretreated coal gasification wastewater by a novel heterogeneous Fenton oxidation process

Sewage sludge from a biological wastewater treatment plant was converted into sewage sludge based activated carbon(SBAC) with Zn Cl2 as activation agent, which was used as a support for ferric oxides to form a catalyst(Fe Ox/SBAC) by a simple impregnation method.The new material was then used to improve the performance of Fenton oxidation of real biologically pretreated coal gasification wastewater(CGW). The results indicated that the prepared Fe Ox/SBAC significantly enhanced the pollutant removal performance in the Fenton process, so that the treated wastewater was more biodegradable and less toxic. The best performance was obtained over a wide p H range from 2 to 7, temperature 30°C, 15 mg/L of H2O2 and 1 g/L of catalyst, and the treated effluent concentrations of COD, total phenols,BOD5 and TOC all met the discharge limits in China. Meanwhile, on the basis of significant inhibition by a radical scavenger in the heterogeneous Fenton process as well as the evolution of FT-IR spectra of pollutant-saturated Fe Ox/BAC with and without H2O2, it was deduced that the catalytic activity was responsible for generating hydroxyl radicals, and a possible reaction pathway and interface mechanism were proposed. Moreover, Fe Ox/SBAC showed superior stability over five successive oxidation runs. Thus, heterogeneous Fenton oxidation of biologically pretreated CGW by Fe Ox/SBAC, with the advantages of being economical, efficient and sustainable, holds promise for engineering application.     

煤矸石-土壤混合基质对小白菜生长的影响及Pb迁移规律

盆栽试验研究了施用不同量煤矸石(0%、13%、26%、40%、53%)对贫瘠土壤改良的效果和对小白菜生长品质的影响。结果表明:(1)混合基质中Pb的迁移能力较差,小白菜中Pb积累量与植物体生物量具有正相关关系;(2)小白菜的发芽率、根系长度、地面以上株高和生物量等均在煤矸石施入比例为26%时达到最佳,发芽率、地面以上株高和干重分别增加23%、23.05%和20.62%;施入煤矸石超过40%时将导致各项指标有所下降;(3)采用单因子污染指数法进行食品质量评价,加入煤矸石量分别为0%、13%和26%时,产品污染指数分别为0.69、0.79和0.93,属于清洁水平;而加入煤矸石量为40%和53%时,污染指数分别为1.12(轻污染水平)和1.38(轻污染水平)。煤矸石可增加植物生长过程所需营养物质而作为贫瘠土壤的改良剂,实现煤矸石资源化并改善矿区生态环境。     

金华市街道灰尘磁化率时空变化研究

对不同时空条件下的金华市二环以内的街道灰尘样品的磁化率进行了研究.结果表明,金华市街道灰尘磁化率均值349.67×10-8 m3/kg,冬、春、夏各个季节的平均值:322.55×10-8 m3/kg、358.16×10-8 m3/kg和368.31×10-8 m3/kg,指示了其均具有磁性增强效应,且其值相近;春、夏两个季节街道灰尘磁化率的高值区分布结构相似,模型参数分析表明,区域因素为影响其值的主因;街道灰尘磁化率高值区与城区工业区大体吻合分布,工业区是主要的区域因素。     

Heterogeneous uptake of nitrogen dioxide on Chinese mineral dust

Mineral dust is one of the major aerosols in the atmosphere. To assess its impact on trace atmospheric gases, in this work we present a laboratory study of the effect of temperature on the heterogeneous reaction of NO₂ on the surface of ambient Chinese dust over the temperature range from 258 to 313 K. The results suggest that nitrogen dioxide could mainly be adsorbed on these types of Chinese mineral dust reversibly with little temperature dependence. Similar to a previous study on NO₂ uptake on mineral aerosols, the uptake coefficients are mainly on the order of 10^− 6 for the Chinese dust, when BET areas are taken into account. HONO was observed as a product, and its formation and decomposition on Chinese mineral dust during the uptake processes were also studied. The complete dataset from this study was compiled with previous literature determinations. Atmospheric implications of the heterogeneous reaction between NO₂ and mineral dust are also discussed, in an effort to understand this important heterogeneous process.