First evidence of unicellular glands in the general epidermis of terrestrial reptiles

The general integument of reptiles is traditionally defined as being dry, but we report here the discovery of unicellular mucoid glands (UCMG) in the dorsal skin of lizards of the genus Phelsuma (Gekkonidae). To this end, the skin of these lizards and of some others for comparison was studied by scanning electron microscopy and transmission electron microscopy. These photographs showed that the development and function of the UCMGs are related to the skin's sloughing cycle. The UCMGs differentiate at scattered locations from Oberh?utchen cells of the inner (new) epidermal generation, above the differentiating beta-keratin layer. While the inner generation matures, the UCMG increases in size; unlike the surrounding Oberh?utchen cells, it does not develop the spinules that characterize gecko skin. When, upon sloughing, the inner generation becomes the new outer generation, and the Oberh?utchen forms the skin surface, the UCMGs, several per scale, dot the surface as mucus-inflated "blebs" projecting from the surrounding spinulate Oberh?utchen, each nesting in a shallow pit of the underlying beta-keratin. On the surface, the UCMGs rupture and the mucus appears to dissipate in cords, flowing over the tips of the spinules, and incorporating minute foreign bodies. It is concluded that, due to the low wettability of the spinulate surface (derived from the spacing of the spinules), the cords brush off easily, with the mucus functioning as a cleaning agent.     

Hydrological Connectivity Between Headwater Streams and Downstream Waters: How Science Can Inform Policy1

Abstract: In January 2001, the U.S. Supreme Court ruled that the U.S. Army Corps of Engineers exceeded its statutory authority by asserting Clean Water Act (CWA) jurisdiction over non‐navigable, isolated, intrastate waters based solely on their use by migratory birds. The Supreme Court’s majority opinion addressed broader issues of CWA jurisdiction by implying that the CWA intended some “connection” to navigability and that isolated waters need a “significant nexus” to navigable waters to be jurisdictional. Subsequent to this decision (SWANCC), there have been many lawsuits challenging CWA jurisdiction, many of which are focused on headwater, intermittent, and ephemeral streams. To inform the legal and policy debate surrounding this issue, we present information on the geographic distribution of headwater streams and intermittent and ephemeral streams throughout the U.S., summarize major findings from the scientific literature in considering hydrological connectivity between headwater streams and downstream waters, and relate the scientific information presented to policy issues surrounding the scope of waters protected under the CWA. Headwater streams comprise approximately 53% (2,900,000 km) of the total stream length in the U.S., excluding Alaska, and intermittent and ephemeral streams comprise approximately 59% (3,200,000 km) of the total stream length and approximately 50% (1,460,000 km) of the headwater stream length in the U.S., excluding Alaska. Hillslopes, headwater streams, and downstream waters are best described as individual elements of integrated hydrological systems. Hydrological connectivity allows for the exchange of mass, momentum, energy, and organisms longitudinally, laterally, vertically, and temporally between headwater streams and downstream waters. Via hydrological connectivity, headwater, intermittent and ephemeral streams cumulatively contribute to the functional integrity of downstream waters; hydrologically and ecologically, they are a part of the tributary system. As this debate continues, scientific input from multiple fields will be important for policymaking at the federal, state, and local levels and to inform water resource management regardless of the level at which those decisions are being made. Strengthening the interface between science, policy, and public participation is critical if we are going to achieve effective water resource management.     

鄱阳湖典型湿地沉水植物的分布格局及其水环境影响因子

沉水植物是湖泊湿地生态系统中关键组分,调查研究沉水植物分布格局及其水环境影响因子,对于沉水植被的恢复与重建具有重要的指导意义。2013年5月初期分别对鄱阳湖典型湿地区域中有沉水植物的25个样地进行群落结构调查,采用系统取样方法对沉水植物进行调查采样并监测水环境因子,在野外调查的基础上运用GIS软件制作鄱阳湖典型区域沉水植物的生物量分布图,并采用主成分分析(PCA)和典范对应分析(CCA)方法分析其主要影响因子。结果表明:鄱阳湖湿地沉水植物以苦草(Vallisneria natans)为广布种,其中蚌湖及白沙湖以黑藻(Hydrilla verticillata)为优势种,白沙洲及乐安河龙口段以苦草为优势种,伴生种主要有金鱼藻(Ceratophyllum demersum)、马来眼子菜(Potamogeton malaianus)、菹草(P.crispus)、小茨藻(Najas minor)、大茨藻(N.marina)、刺苦草(V.spinulosa)和水车前(Ottelia alismoides)等。采用双向指示种分析法将研究区沉水植物分为6个群落;5月初大部分沉水植物尚处于生长季初期,生物量相对较低,仅菹草的生物量较大;沉水植物与浮叶植物共存现象明显。主成分分析(PCA)结果显示,第一主成分中水深、总磷和溶解氧等因子的系数值较大,第二主成分中pH值、化学需氧量和水体透明度等因子的系数值较大,是影响沉水植物分布的关键因子;典范对应分析(CCA)结果显示,水深、总磷和总氮对苦草和黑藻的影响显著,水体透明度是马来眼子菜的主要影响因子。     

矿业权集聚、经济增长与区域贫困减缓

本文基于泰尔指数法,计算并测度了中国资源富集区的城乡收入差距与行业(矿业)收入差距,然后结合矿业权集聚度的测度结果和中国资源税改革的变动特征,建立面板数据回归模型,考察了2004—2014年中国资源富集区矿业权集聚与经济增长、贫困减缓的长期关系。本文的主要结论是:资源税对矿业权集聚水平和矿业经济增长具有正向刺激作用,但矿业经济增长并不利于地区经济的整体改进,也不利于区域贫困减缓。资源税低水平征收对"资源诅咒"和"区域贫困"具有传导效应,进而对资源富集区的贫困减缓形成阻滞作用。另外,矿业权集聚对地区贫困的影响存在异质性,异质性揭示了区域资源性收益分配存在的差异。短期来看,矿业权集聚使中央企业惠及更多,是引致"富饶中的贫困"怪圈的重要原因;但长期来看,随着矿业权集聚度的提升,地方政府获得的累积性资源性收益不断上升,渐次增强了地方政府通过社会保障支出实施收入调节的能力,总体上有利于区域贫困的减缓。因此,为实现资源富集区的精准扶贫,资源主管部门在制定减贫措施前,应根据不同区域特点区别对待,短期内应着力于调整资源性收益分配机制,赋予地方更多资源性收益,并加大对社会的保障性支出;长期来看,应探索建立合理有效的资源税体制,促进经济增长方式的多样化,并鼓励科技创新,进一步提高社会群体的受教育程度,从根本上改变区域贫困产生的内生性环境和外生性环境。     

城市河流水质常规评价技术研究

运用综合水质标识指数法,对我国河流水质评价面临的关键技术问题,包括水质评价方法、水质评价项目,水质级别评价,水环境功能区达标评价、水质定性评价、河流及水系整体水质比较、水质随时间和空间变化等作了明确界定,并介绍了在上海河流水质评价中的应用。     

表面活性物质对HPMA阻垢缓蚀性能的影响

表面活性物质的加入可明显提高水解聚马来酸酐(HPMA)的阻垢、缓蚀性能,且不同表面活性物质影响程度不同,通过剩余硬度法测定阻垢性能,静态失重法测定缓蚀性能,从而比较异丙醇、葡萄糖酸钠对HPMA阻垢、缓蚀性能的影响。实验结果表明,异丙醇与HPMA复合使用时效果较好,阻垢率达到 79 0 %,缓蚀率达 70 7%,且阻垢率随Ca2 + 浓度增大而增大。     

城市污水处理厂中水回用初探

以沈阳市污水处理厂实际工程为例 ,提出了中水回用项目的可行性、项目方案及工程投资预测     

浑河环境保护与地下水资源质量的改善

介绍了沈阳市地下水水源地分布状况、浑河沿岸水文地质条件与河水的渗漏、浑河污染对地下水源的影响及2 0 0 2～ 2 0 0 3年浑河治臭工程对地下水环境的影响     

关于积极推进生态城市建设的对策建议

介绍了沈阳市在生态城市建设中的成绩 ,提出积极推进生态城市建设中要切实注重的几个问题———进一步完善森林城市生态规划 ,提高水资源利用率 ,建设节水型社会 ,保护地下水 ,使人民群众喝上安全合格的水 ,提出对策建议。     

活性炭吸附低浓度SO_2烟气的研究

利用水洗再生活性炭吸附法，对模拟火力发电厂烟气及克劳斯炉尾气进行脱除ＳＯ２的试验研究，ＳＯ２脱除率大于９０％．