平原河网地区滨岸带外来植物入侵现状及影响研究——以上海青浦区为例

河流滨岸带作为一种典型的开放系统,在受到外界干扰的条件下极易被外来植物所入侵并受到严重影响。以上海青浦区为例,通过对河流滨岸带生态系统入侵植物分布及现状调查,以及对两种入侵植物：白花三叶草（Trifolium repens）和加拿大一枝黄花（Solidago canadensis）群落的物种多样性及其土壤特性的实证研究,探讨外来植物入侵对河流滨岸带生态系统造成的影响。结果表明：目前该地区河流滨岸带外来入侵植物共有14科24种,其科、种数分别占到该生态系统所有植物的48．3％与26．1％。入侵植物白花三叶草与加拿大一枝黄花在春、秋两季均显著降低了河流滨岸带植物群落的物种多样性。此外,两种人侵植物也对当地河流滨岸及土壤特性造成了不同程度的影响,其中对土壤含水量、pH值的影响最为显著。该研究填补了平原河网地区河流滨岸带生态系统外来植物入侵研究的空白,有助于今后开展对该生态系统的评价、恢复及管理工作。     

矿区周围稻米重金属积累及健康风险分析

选用杂交稻、常规稻和糯稻3个水稻品系共21个水稻品种在广东大宝山矿区周围重金属污染土壤中进行大田试验,研究Cu、Zn、Pb、As和Cd 5种重金属元素在不同水稻品种(品系)稻米中的积累状况,并进行健康风险评价分析。结果表明,供试水稻稻米中Cd和Pb超标率很高,分别为100%和71.43%;Cu和As超标现象不严重,超标率分别为4.76%和14.29%;Zn含量均不超标。供试水稻品系中常规稻和糯稻稻米对Cu、Zn、Pb、Cd的积累能力较高,杂交稻则较低;但杂交稻稻米对As的积累能力高于其他2个品系。稻米中Cu、Zn、Pb、As和Cd含量与稻谷生物量均呈负相关关系,其中Pb含量与稻谷生物量呈显著负相关。供试水稻稻米对5种重金属的富集能力由高到低排序为Cd>Zn>Cu>As>Pb。本研究表明供试土壤中Cd和Pb对人体健康存在比较严重的潜在威胁,Cu、Zn和As对人体健康的潜在危害较小,应重点关注大宝山矿区稻米Cd和Pb的重金属污染问题及其对人体健康的潜在危害。     

常熟地区农户庭院植物多样性与配置模式

选择常熟地区代表性乡村,对农户庭院植物多样性和配置模式进行研究,分析其植物物种组成和多样性,并利用TW INSPAN分类方法,研究了庭院植物配置类型与模式。结果表明:在对281个户级庭院调查中,170户庭院中栽种植物,111户庭院中无任何绿化,共栽种植物151种(含变种、栽培品种),隶属58科116属;庭院植物配置可划分为4种庭院类型和10种配置模式;植物的层次结构对于多样性指数影响较大,植物配置模式的结构越丰富、复杂,其物种多样性指数越高。认为观赏性植物成为庭院的主体植物,观赏功能成为庭院植物的主要功能;庭院内有效绿化面积不足,单位面积植物生态效益较低;乡土植物景观建设与物种多样性保护有待于进一步加强。     

河谷型城市城乡结合部景观格局空间尺度效应分析——以兰州市西固区土地利用格局为例

以兰州市西固区土地利用格局为例,利用2005年SPOT5遥感影像和正射航空影像数据,选取14个常用的景观指数,从景观水平和类型水平2个方面分析景观指数随尺度变化的基本规律,采用200m×200m正方形将研究区土地利用数据切分成规则格网,计算每个格网的多样性指数,通过半方差分析研究西固区多样性空间结构特征。结果表明:10m是西固区土地利用景观的本征观测尺度;研究区景观类型和景观格局特征随尺度增大变化显著,体现出一定的尺度依赖性;各乡(镇、街道)的景观指数呈现出城市中心—城乡交错带—乡村的分异特征,梯度变化明显;西固区多样性空间分布属于中等强度空间相关,高值区主要分布于黄河沿岸。     

生物炭负载氧化石墨烯对离子型稀土矿区土壤中重金属的阻控效应

以脐橙皮渣和天然石墨为原料,采用改进Hummer-共热解法制备了生物炭负载氧化石墨烯(BGO)材料,利用土壤钝化实验考察了 BGO复合材料对稀土矿区土壤重金属形态的影响,土柱淋溶实验探讨了淋滤液重金属含量变化特征以及土壤重金属垂向迁移规律,确定了淋溶条件下重金属的累积释放模型.结果表明,添加BGO复合材料提高了土壤pH...     

电磁辐射职业危害及防护对策

科技飞速发展的今天,射频及微波技术已经广泛应用于国民经济的各个领域,这使得越来越多的从业人员在工作场所受到电磁辐射污染的影响。本文总结归纳了我国电磁辐射职业危害状况,分析了现代企业电磁辐射防护的新特点,并提出企业电磁辐射防护对策。     

How “open” are open spaces: evaluating transformation of open space at residential level in Adelaide – a case study

This paper examines the transformation of open space and how it compares to older residential development. A study has been conducted at the residential level because neighbourhoods have been a basic unit of city design throughout the recent history of urban settlements. Furthermore, the neighbourhood is a more humanly relevant scale of urban development. The method adopted for this research was a comparative urbanism by comparing old and new residential areas. This study found that incremental redevelopment of old residential areas through both re-subdivision and intensification of development on existing allotments has resulted in a progressive loss of open space. However, the study also confirmed that the current supplies of open space across all the study areas (old and new residential areas) are relatively similar. The main difference between the open space supply in older and newer residential areas comes down to the ownership of land (i.e. the proportion of public versus private open space). The study demonstrated that older residential areas with large allotments have experienced a significant loss of private open space – originally from 50%, to current levels of 23–30%. The paper concludes that there is a need for a holistic approach to the provision of public and private open spaces to improve the quality of life at a residential level.     

Release,Dispersion, and Resuspension of Escherichia coli From Direct Fecal Deposits Under Controlled Flows1

Abstract: Water‐quality standards have been placed on fecal indicator organisms such as Escherichia coli in an attempt to limit the concentrations in water bodies. Cattle can be a significant source of bacteria to water systems, particularly when they are allowed direct access to streams. A flume study was conducted to quantify the effect and understand the transport of E. coli from directly deposited cattle manure. Five steady‐state flows, ranging from 0.00683 to 0.0176 m³/s, were studied and loads from a single cowpie exceeded the U.S. Environmental Protection Agency’s recommended water‐quality standards (235 CFU/100 ml) at each flow over the hour study period. Average E. coli concentrations ranged from 10² to 10⁵ CFU/100 ml over the hour sampling period for all flows. High spatial variations in E. coli concentrations were often seen at each sampling time, with higher concentrations typically at the bottom of the flume. E. coli resuspension was initially greater at 0.5 min after deposition, for the lowest flow (10⁵ CFU/m²/s); however, resuspension rates became similar over time, on the order of 10³ CFU/m²/s. This study demonstrates that the concentrations of E. coli can vary over the water column, and therefore grab samples may inaccurately measure bacteria concentrations and loads in streams. In addition, resuspension rates were often high, so the incorporation of this process into water‐quality models is important for bacteria prediction.     

Characterization of Storm Flow Dynamics of Headwater Streams in the South Carolina Lower Coastal Plain1

Epps, Thomas H., Daniel R. Hitchcock, Anand D. Jayakaran, Drake R. Loflin, Thomas M. Williams, and Devendra M. Amatya, 2012. Characterization of Storm Flow Dynamics of Headwater Streams in the South Carolina Lower Coastal Plain. Journal of the American Water Resources Association (JAWRA) 1‐14. DOI: 10.1111/jawr.12000 Abstract: Hydrologic monitoring was conducted in two first‐order lower coastal plain watersheds in South Carolina, United States, a region with increasing growth and land use change. Storm events over a three‐year period were analyzed for direct runoff coefficients (ROC) and the total storm response (TSR) as percent rainfall. ROC calculations utilized an empirical hydrograph separation method that partitioned total streamflow into sustained base flow and direct runoff components. ROC ratios ranged from 0 to 0.32 on the Upper Debidue Creek (UDC) watershed and 0 to 0.57 on Watershed 80 (WS80); TSR results ranged from 0 to 0.93 at UDC and 0.01 to 0.74 at WS80. Variability in event runoff generation was attributed to seasonal trends in water table elevation fluctuation as regulated by evapotranspiration. Groundwater elevation breakpoints for each watershed were identified based on antecedent water table elevation, streamflow, ROCs, and TSRs. These thresholds represent the groundwater elevation above which event runoff generation increased sharply in response to rainfall. For effective coastal land use decision making, baseline watershed hydrology must be understood to serve as a benchmark for management goals, based on both seasonal and event‐based surface and groundwater interactions.     

Modeling Monthly Fluctuations in Submersion Area of a Dammed River Reservoir: A Case Study1

Lu, Haorong, S. Samuel Li, and Jinsong Guo, 2012. Modeling Monthly Fluctuations in Submersion Area of a Dammed River Reservoir: A Case Study. Journal of the American Water Resources Association (JAWRA) 1‐13. DOI: 10.1111/jawr.12003 Abstract: Fluctuations in water submersion of the Three Gorges Reservoir in China have not been explored in spite of their important implications for shoreline erosion and other undesirable consequences. This article aims to quantify the monthly fluctuations in response to changing hydraulic parameters and regional climatic factors. Flow velocity and water levels distributed along the 609‐km long dammed river reservoir are calculated with a one‐dimensional hydrodynamics model. Evaporation of water from the surface of the reservoir is determined using mass transfer‐based methods. Calculated flow velocities and water levels compare well with field data. We show that the water surface slope decreases with rising water level at the dam, and decreases to almost zero during the winter months of water storage when the downstream water level reaches the normal pool level. The submersion area varies between 830 and 1,070 km² over the year or over 20% of the reservoir zone will experience the annual cycle of dry land and partial or complete submersion. These fluctuations are of relevance to shoreline management and to the prevention and restoration of shoreline erosion. Evaporation is estimated to fluctuate between 1,240 and 26,110 tons of water per month per kilometer length of reservoir channel; this can possibly affect the hydrological budget of the reservoir region. The simple methodologies discussed in this article can easily be applied to other dammed river reservoirs for submersion estimates.