常温下基质与时间对ANAMMOX污泥活性保藏影响

采用厌氧氨氧化污泥,通过脱氮效能的测定,研究了常温（15±2）℃下保藏过程中基质添加与保藏时间对污泥活性的影响以及探讨长期保持污泥活性的保藏策略。结果表明,在无营养物添加的情况下,保藏的前45天厌氧氨氧化污泥氮去除速率由0.107 kg/（m3·d）下降到0.025 kg/（m3·d）,其速率下降最快,但是经过6 d培养,污泥的活性可以得到恢复;当保藏365 d后,厌氧氨氧化污泥活性基本消失,即使通过11 d恢复也无明显的厌氧氨氧化特性。说明常温下保藏时间对厌氧氨氧化污泥活性影响显著,随着保藏时间的延长污泥氮去除速率会大幅降低,甚至消失。根据衰减指数模型拟合出常温状态下厌氧氨氧化污泥活性衰减模型为y=0.547×exp（-0.0109×t）。通过定期（15 d）投加营养物,经过150d和365 d保藏后的厌氧氨氧化污泥仍然保持48%和31%的活性。说明定期投加营养物可以有效缓解厌氧氨氧化污泥活性在常温保藏过程中的衰减,适用于厌氧氨氧化污泥常温下长期保藏。     

锰铜复合催化剂常温催化氧化NO

采用浸渍法,以γA1₂O₃为载体制备了常温下对NO具有良好催化氧化活性的Mn-Cu复合催化剂。系统考察催化剂组分、焙烧温度等与催化剂性能的关系,结果显示200℃干燥所得催化剂的活性最好,催化剂15%Mn-24%Cu/Al₂O₃在常温下对NO的催化氧化效率达到50%以上。XRD分析表明,催化剂活性组分为Cu（OH）Cl,且随反应时间延长催化性能下降,其物相由Cu（OH）Cl转变为活性较低的Cu₂（OH）₃Cl相。     

Selenium speciation and localization in chironomids from lakes receiving treated metal mine effluent

A lake system in northern Saskatchewan receiving treated metal mine and mill effluent contains elevated levels of selenium (Se). An important step in the trophic transfer of Se is the bioaccumulation of Se by benthic invertebrates, especially primary consumers serving as a food source for higher trophic level organisms. Chironomids, ubiquitous components of many northern aquatic ecosystems, were sampled at lakes downstream of the milling operation and were found to contain Se concentrations ranging from 7 to 80 mg kg⁻¹ dry weight. For comparison, laboratory-reared Chironomus dilutus were exposed to waterborne selenate, selenite, or seleno-DL-methionine under laboratory conditions at the average total Se concentrations found in lakes near the operation. Similarities in Se localization and speciation in laboratory and field chironomids were observed using synchrotron-based X-ray fluorescence (XRF) imaging and X-ray absorption spectroscopy (XAS). Selenium localized primarily in the head capsule, brain, salivary glands and gut lining, with organic Se species modeled as selenocystine and selenomethionine being the most abundant. Similarities between field chironomids and C. dilutus exposed in the laboratory to waterborne selenomethionine suggest that selenomethionine-like species are most readily accumulated, whether from diet or water.     

海洋大气环境下Q235钢表面氯离子沉积量分布规律研究

目的 研究海洋大气环境下氯离子在Q235钢表面的沉积分布规律。方法 使用便携式X射线荧光光谱仪测试Q235钢在海南岛不同地点大气环境暴露后的表面氯离子沉积，然后采用插值算法绘制氯离子在Q235钢表面沉积分布图和海南岛不同地点氯离子在Q235钢表面平均沉积量分布图，并根据氯离子沉积分布图分析氯离子在Q235钢表面的沉积量分布规律。结果 氯离子在Q235钢表面呈不均匀分布特征。在环境暴露试验前6个月，Q235钢表面氯离子含量逐渐增加；暴露6~12个月，Q235钢表面的氯离子含量总体变化不大。从整个海南岛看，内陆地区氯离子在Q235钢表面的沉积量低，而在沿海环岛区域的沉积量高。在海南岛沿海地区，Q235钢表面氯离子沉积量随季风风向的变化而变化。结论 氯离子在Q235钢表面呈不均匀沉积分布，Q235钢表面氯离子沉积量在海南岛不同地点呈“中间低、两边高”的沉积分布规律，内陆地区沉积量低，而沿海环岛区域沉积量高，并且沿海地区的氯离子沉积易受季风风向的影响。     

Coprecipitation mechanisms of Zn by birnessite formation and its mineralogy under neutral pH conditions

Birnessite (δ-Mn(IV)O₂) is a great manganese (Mn) adsorbent for dissolved divalent metals. In this study, we investigated the coprecipitation mechanism of δ-MnO₂ in the presence of Zn(II) and an oxidizing agent (sodium hypochlorite) under two neutral pH values (6.0 and 7.5). The mineralogical characteristics and Zn–Mn mixed products were compared with simple surface complexation by adsorption modeling and structural analysis. Batch coprecipitation experiments at different Zn/Mn molar ratios showed a Langmuir-type isotherm at pH 6.0, which was similar to the result of adsorption experiments at pH 6.0 and 7.5. X-ray diffraction and X-ray absorption fine structure analysis revealed triple-corner-sharing inner-sphere complexation on the vacant sites was the dominant Zn sorption mechanism on δ-MnO₂ under these experimental conditions. A coprecipitation experiment at pH 6.0 produced some hetaerolite (ZnMn(III)₂O₄) and manganite (γ-Mn(III)OOH), but only at low Zn/Mn molar ratios (< 1). These secondary precipitates disappeared because of crystal dissolution at higher Zn/Mn molar ratios because they were thermodynamically unstable. Woodruffite (ZnMn(IV)₃O₇•2H₂O) was produced in the coprecipitation experiment at pH 7.5 with a high Zn/Mn molar ratio of 5. This resulted in a Brunauer–Emmett–Teller (BET)-type sorption isotherm, in which formation was explained by transformation of the crystalline structure of δ-MnO₂ to a tunnel structure. Our experiments demonstrate that abiotic coprecipitation reactions can induce Zn–Mn compound formation on the δ-MnO₂ surface, and that the pH is an important controlling factor for the crystalline structures and thermodynamic stabilities.