不同地域天然伊利石表面酸碱特性的比较

利用电位滴定技术和恒定容量表面络合模式表征不同来源天然伊利石的表面酸碱性质。鉴于固体基质在酸量滴定过程中发生溶解，相应的滴定上清液被视为体系空白。考虑到水解铝、硅酸和伊利石表面活性位之间的表面络合或沉淀反应，提出两种表面质子反应模型。对其中的特例，还考虑了表面离子交换反应。模拟程序的拟合结果显示两种模型对水解伊利石体系的滴定行为均可获得满意的描述。相的的表面固有酸度常数表明样品的酸碱性质之间存在一些共性。     

天然水体及生活饮用水中铝的含量及形态分布

采用ＰＣＶ络合比色法和Ｆｅｒｒｏｎ逐时络合比色法，选取３种典型环境中的水体为研究对象；江西德兴铜矿地区的乐安江，白洋淀地区以及从源水，自来水到铝锅煮沸水序列水样，着重分析其中铝的含量及其形态分布，并讨论了铝的含量及其形态的变化对３种典型环境的影响。     

河流沉积物重金属污染质量控制基准的研究 Ⅰ.C-B-T质量三合一方法(Triad)

在综合数据库ＣＥＲＰ－ＤＢＭＳ支持下，利用水体沉积物质量三合一工具，初步建立江西乐安江表层沉积物中重金属污染的质量控制基准。通过将化学分析、毒性鉴定２和底栖群落结构变化三基元集成为一体的三轴图和相应的响应信息判断矩阵，基于现场生物响应的重金属污染的剂量－响应关系。     

机械活化煤气化细渣资源化利用及残碳燃烧反应动力学探究

随着我国煤气化技术的快速发展，气化渣的产生和排放量逐年增加.煤气化细渣的大量堆存，给当地的环境保护造成了巨大的压力，已经成为限制煤化工产业基地可持续发展急需解决的重大问题.本文针对气化细渣中残碳反应活性低和转化难度大的问题，研究了机械活化法对气化渣残碳反应动力学的影响.采用Coats-Redfern法分析了机械活化对残碳反应活化能的作用规律.结果表明，机械活化8 h，残碳燃烧反应活性显著提高，650℃下的活化能由63.2 k J·mol^-1降到28.4 k J·mol^-1.不添加其他化学试剂，1000℃烧制高强度轻质陶粒，其堆积密度为0.867 g·cm^-3，筒压强度为7.67 MPa.相关研究可以为我国气化细渣的资源化利用提供一定的数据和技术基础.     

Transverse distribution of the streamwise velocity for the open-channel flow with floating vegetated islands

Environmental Science and Pollution Research - Floating vegetation islands (FVIs) have been widely utilized in various river ecological restoration projects due to their ability to purify...     

Seasonal and spatial occurrence and distribution of atmospheric polycyclic aromatic hydrocarbons (PAHs) in rural and urban areas of the North Chinese Plain

Passive air sampling (PAS) was employed to study the occurrence of gaseous and particle-bound PAHs in the North Chinese Plain. The averaged concentrations of gaseous and particle-bound PAHs were 485 ± 209 ng/m³ and 267 ± 161 ng/m³, respectively. The PAHs concentrations at urban sites were generally higher than those at rural ones with ratios <1.5 in spring, summer and fall, but differences between them were not significant for the wintertime and annually averaged concentrations. This urban-rural distribution pattern was related to the PAHs emission sources. PAHs spatial variation can be partially (49%) explained by emission with a simple linear regression method. Both the gaseous and particle-bound PAHs were highest in winter and lowest in summer, with winter/summer ratios of 1.8 and 8, respectively. Emission strength was the most important factor for the seasonality.     

DNA同源性分析最终确定新疆中华根瘤菌（Sinorhizobium xinjiangensis）为一独立种

针对S.xinjiangensis分类地位的争议,从新疆再次分离获得34株快生大豆根瘤菌,在16SrDNAPCR-RFLP分析和SDS全细胞蛋白电泳分群的基础上,进行了16SrDNA全序列相似性和DNA同源性分析.所测4个菌株和S.fredii模式菌株USDA205的16SrDNA全序列有很高的相似性.而DNA同源性分析说明新分离的菌株代表与原定的S.xinjiangensis为一个DNA同源群.其模式菌株CCBAU110与S.fredii的2株参比菌株USDA194、2048之间的DNA同源性分别为31.5%和28.7%.S.fredii的模式菌株USDA205与新分离的菌株代表及原定的S.xinjiangensis的模式菌株和2个参比菌株之间的DNA同源性为20.8%～39%,远低于70%.属于种水平上的差异.按照国际细菌分类委员会以DNA同源性≥70%且△Tm≤5℃作为定种的标准,S.xinjiangensis是Sinorhizobium属中不同于S.fredii的一个独立的种.表3参20     

环境规制对城市生态技术扩散效率的影响研究

生态技术扩散是长江经济带生态文明建设的必要环节,也是企业履行环保责任的有效措施。本文以长江经济带110个地级及以上城市为研究对象,采用非径向方向距离函数对城市工业企业生态技术扩散效率进行测算,分别从整体和区域异质性角度实证分析环境规制对城市工业企业生态技术扩散效率的影响及内在机理。结果表明：长江经济带城市环境规制与生态技术扩散效率存在倒“U”形关系,环境规制对生态技术扩散效率还存在多重影响路径,外商直接投资和工业集聚在影响路径中分别起着中介作用,且外商直接投资和工业集聚的链式中介显著。在异质性分析中,发现环境规制、外商直接投资、工业集聚和生态技术扩散效率之间的关系因区域位置不同而存在差异性。为此,依据研究结论及环境规制实施现状提出相应的政策建议,实现长江经济带经济永续绿色发展目标。     

Sorption kinetic characteristics of polybrominated diphenyl ethers on natural soils

Sorption kinetic characteristics of BDE-28 and BDE-47 on five natural soils with different organic carbon fractions were investigated, and could be satisfactorily described by a two (fast and slow)-compartment first-order model with the ratio of rate constants ranged from 9 to 94 times. The fast compartment made a dominant contribution (71% ∼ 94%) to the total sorption amount in the whole process, and accounted for over 90% of the increase in the total sorption amount at initial 5 h. The influence of the slow compartment on the increase in the total sorption amount became principal (above 90%) in the subsequent stage approximately from 9 h or 25 h to the apparent equilibrium at 265 h. The results proposed the different sorption behaviors of the mathematically classified compartments for BDE-28 and BDE-47, which may correspond to the different soil components, such as soil organic fractions with amorphous and condensed structures, respectively.