Thermal cracking of waste printed wiring boards for mechanical recycling by using residual steam preprocessing

Mechanical waste-processing methods, which combine crushing and separation processes for the recovery of valuable materials, have been widely applied in waste printed wiring board (PWB) treatment. However, both the high impact toughness and the tensile and flexural strengths of whole PWB with a laminated structure result in great energy consumption and severe abrasion of the cutters during multi-level crushing. In addition, the high temperatures occurring in continual crushing probably cause the decomposition of the polymer matrix. A thermal-crack method using residual steam as the heating medium has been developed to pre-treat waste PWBs. This treatment reduces the mechanical strength in order to improve the recovery rate of valuable materials in subsequent mechanical recycling. The changes of the PWBs’ macro-mechanical properties were studied to evaluate thermal expansion impacts associated with changes in temperature, and the dynamic dislocation micro-structures were observed to identify the fracture mechanism. The results showed that thermal cracking with steam at the temperature of 500 K can effectively attenuate the mechanical properties of waste PWBs, by reducing the impact, tensile and flexural strengths respectively, by 59.2%, 49.3% and 51.4%, compared to untreated PWB. Thermal expansion can also facilitate the separation of copper from glass fiber by reducing peel resistance by 95.4% at 500 K. It was revealed that the flexural fracture was a transverse cracking caused by concentrated stress when the heating temperature was less than 500 K, and shifted to a vertical cracking after exceeding 500 K.     

海藻酸钠/锆@钙水凝胶的制备及其对磷的吸附研究

利用简便的方法制备了一种新型的海藻酸钠/锆@钙(SA/Zr@Ca)水凝胶材料,采用SEM、XRD对该材料进行了表征,并通过拟合吸附等温模型及吸附动力学模型,结合XPS和Zeta电位分析,研究了该材料对磷酸盐吸附的性能和机理.结果表明,该材料为非晶态的无定型材料.在溶液初始pH为2～7时,SA/Zr@Ca对磷酸盐(以PO...     

Biochemical properties of beryllium potentially relevant to its carcinogenicity†

The carcinogenicity of beryllium to several animal species is well established and evidence exists which strongly suggests that this is the case in human exposure. In this review several biochemical properties of the metallocarcinogen are considered including, the causation of cell transformation, and infidelity of DNA synthesis, inhibition of cell division and enzyme induction, and interference with regulatory mechanisms controlling gene expression. These effects are discussed in relation to beryllium chemistry, cellular accumulation mechanisms and distribution to subcellular organdies and molecular targets. It is suggested that the ultimate location and interactions of the metal ion in cell nuclei and its selective inhibition of certain protein phosphorylation reactions in particular are the biochemical effects potentially most relevant to induction of beryllium carcinogenesis.     

Polycyclic aromatic hydrocarbons in surface sediments held in experimental mesocosms

Sediment was collected from three locations along a pollution gradient in Narragansett Bay and transplanted to controlled mesocosms. Total hydrocarbons and eleven individual polycyclic aromatic hydrocarbons (PAHs) were measured in these sediments over a period of 394 days. Total hydrocarbon concentrations increased in the “relatively uncontaminated”; (Rhode Island Sound) sediment that was held in the mesocosms, but did not change in the two other sediments. The concentrations of four PAHs: naphthalene, 2‐methyl naphthalene, 1‐methyl naphthalene and biphenyl, decreased in the “contaminated”; (Providence River) sediment during the experiment and the calculated half‐lives for these compounds were 287, 353, 321 and 333 days, respectively.     

黄土丘陵区生物结皮对土壤物理属性的影响

生物结皮在干旱、半干旱地区广泛发育。迄今,有关生物结皮发育过程中土壤物理属性的响应仍不明确。论文采用野外调查与室内分析相结合的方法,定量研究不同生物量生物结皮对土壤物理属性的影响。结果表明:①生物结皮的发育能够细化土壤,当生物结皮由初期藻结皮演替至60%~80%苔藓结皮时(5等级),生物结皮层粗砂粒含量降低了86%;②随着生物结皮生物量的增加,生物结皮层土壤容重和硬度较初期分别降低了15%和68%,田间持水量和孔隙度分别增加了36%和14%;生物结皮层粘结力是下层土壤的6~7倍;③生物结皮的发育对土壤物理属性的影响与生物量有关,当苔藓生物量达2.91±0.12 g/dm²时,其土壤物理属性基本稳定。研究结果为揭示生物结皮抗侵蚀机理提供了科学参考。     

废TFT-LCD面板中主要元素溶出特性

以废TFT-LCD面板破碎料为研究对象,在使用XRF（X射线荧光光谱分析仪）分析其主要元素组成以及采用ICP-AES测试不同酸体系下主要元素浓度的基础上,研究了不同酸体系下主要元素的溶出特性. 结果表明:废TFT-LCD面板由Si、Al、Sr和In等10余种元素组成,其主要组成元素在不同酸体系下的溶出特性存在明显差异,这与其赋存形态有密切关系. In在各种酸体系下溶出浓度变化较小,为283～306 mgL. Fe的溶出特性与In相似,是主要伴随离子. Al和Sr易在浓盐酸体系下溶出. As在含有浓硝酸的体系下溶出率较高,最高溶出率为100%,而在无浓硝酸体系下的溶出率最低值仅为293%. Zn、Ti、Cu、Sn和Cr在各酸体系下的溶出浓度均较低(均低于1 mgL),不宜回收.      

机械化学法修复柴油污染土壤的效率、产物及影响

针对常规污染土壤修复处理方法存在有毒降解产物、容易产生二次污染等问题,本研究采用行星球磨仪研究了机械化学法（MC）对柴油污染土壤的修复效能,利用GC/MS对柴油烃组分的降解产物进行分析,并采用SEM、XRD、BET、FTIR和TGA等方法对不同处理条件下的土壤样品进行表征.结果表明,MC处理在0.5~4.0 h内对土壤中总石油烃（TPH）的去除率可达95%以上.随着初始TPH浓度和球土质量比的升高,TPH去除率随之提高.采用MC处理后柴油组分降解难度顺序如下：烷烃<烯烃<环烷烃<芳香族化合物.在球磨处理4 h后,未检出有毒有害残留物质.球磨后土壤粒径变小,表面变粗糙,粘土矿物中的硅氧四面体暴露在土壤表面,矿物结构的结晶度逐渐降低,晶体结构逐渐破裂或变形,可在土壤表面形成富电子区域或促使土壤具有更高的反应活性,这是机械化学法高效降解柴油的主要机制.其次,土壤有机质的主要官能团受到破坏,纳米级孔隙容量降低,从而降低了土壤组分的吸附能力,增加了柴油的有效性,也有助于柴油的解吸和机械化学降解.此外,随着球磨时间的增加,土壤有机碳（SOC）含量先增加后下降,但均高于处理前.可见,MC处理可以快速彻底降解土壤中的柴油,且有利于增加土壤有机碳含量,对于石油烃污染土壤修复具有较好的应用潜力.     

莲花湖库区红松水源涵养林土壤水分-物理性质的空间分布特征

运用地统计学对莲花湖库区红松水源涵养林表层土壤水分-物理性质进行了空间异质性分析。研究结果表明: 土壤含水量、土壤密度、毛管孔隙度、非毛管孔隙度等因子均服从对数正态分布;毛管孔隙度最优拟合模型是球状模型,其它因子均为指数模型。土壤含水量、土壤密度、毛管孔隙度和非毛管孔隙度块金值、变程、结构比、分数维和空间自相关系数最大值分别为0.311、0.297、0.192、0.293,6.87 m、10.29 m、8.31 m、8.88 m, 0.690、0.694、0.814、0.707,1.968、1.939、1.937、1.945,0.111、0.200、0.246、0.157。可见以上4个因子空间自相关性均较强,随着空间距离的增大,其相关性逐渐减弱。其中毛管孔隙度均一性程度较高;土壤含水量空间分布形态较复杂,破碎化程度高。     

北京奥运会期间奥运村站空气质量的观测与研究

为了跟踪研究北京2008年奥运会期间奥运村大气污染物浓度的变化,2008年6月1日─9月30日,利用符合国际标准的在线观测仪器,对奥运村站大气中主要污染物进行加强观测. 结果表明:奥运会期间奥运村站大气中φ(NO₂),φ(SO₂),ρ(PM_2.5)和ρ(PM₁₀₎分别比奥运会前(7月1日─8月7日)下降了11.2%,46.7%,57.0%和50.0%;比残奥会后时段(9月20─30日)分别下降了41.7%,31.8%,21.6%和28.6%;与2007年同期相比,奥运会时段的φ(NO₂),φ(O₃),ρ(PM_2.5)和ρ(PM₁₀₎分别下降了38.8%,37.2%,42.1%和68.0%;残奥会时段分别下降了17.8%,27.5%,44.0%和64.1%. 除对污染源严格的控制措施取得了良好的效果外,有利的天气过程也是奥运会期间北京空气质量全面达标的重要原因.      

入田泥沙对黄河三角洲地区土壤物理性状的影响——以小开河引黄灌区为例

为研究人田泥沙对小开河灌区自然土壤的影响,用分析化验和工程测试等方法,分析了引黄泥沙和输沙人田后土壤颗粒组成、容重、孔隙状况等物理性状。结果表明：引黄泥沙中0．02～0．002mm的细粉粒比例最高,平均39-31％。小开河自然土壤中0．05-0．02mm的粗粉粒比例最高,为53．41％,泥沙中细粉粒和粘粒含量明显高于当地土壤。输沙人田使灌区土壤中0．02—0．002mm的细粉粒和〈0．002mm的粘粒比例明显增加,〉0．02mm的颗粒比例下降,虽有效避免了因渠首集中沉沙造成的土壤沙化和生态环境恶化,但增加了土壤的粘重程度。农田耕作在一定程度上增加土壤通气孔隙比例、降低土壤容重,但土壤毛管孔隙度依旧稳定在40％左右,毛管作用旺盛,使土壤通气状况不能满足作物需求。在黄河三角洲地区输沙入田的泥沙处理,应结合当地土壤的基本性质和水盐运动规律配置泥沙,以免增强当地土壤紧实、通透性差的性状。