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921.
梁子湖湿地植物多样性现状与评价 总被引:18,自引:0,他引:18
根据1999~2001年的野外调查数据,研究了湖北梁子湖湿地浮游藻类和高等植物多样性资源.结果表明,该湿地常见浮游藻类73种,隶属于7门58属(绿藻28种,硅藻19种,蓝藻14种,金藻4种,裸藻3种,甲藻3种,隐藻2种);高等植物282种,隶属于72科183属(苔藓8种,蕨类9种,裸子植物3种,被子植物262种),其中国家重点保护野生植物5种.浮游藻类密度和生物量均值分别为(1163.79913.51)104cell/L和6.1342.737mg/L,叶绿素a含量12.754.98mg/L,浮游藻类表层日生产量1.18~2.29mgO2/(Ld).水生植被繁茂,可划分为12个群丛,群丛单位面积生物量为6.443kg/m2;水生植被覆盖率54.27%,单位面积生物量为3.496kg/m2,在同类湖泊中处于中等水平;植被种类复杂,以沉水植物微齿眼子菜(Potamogeton maackianus)和金鱼藻(Ceratophyllum demersum)为优势群落.该湖泊总体上属中营养型水体,仍保持草型湖状态. 相似文献
922.
构建湿地中试系统基质剖面微生物活性的研究 总被引:33,自引:2,他引:31
对稳定运行的复合垂直流构建湿地中试系统基质进行分层采样,测定微生物数量,生物量氮,酶活性,硝化作用,反硝化作用以及呼吸作用等各项指标.结果表明,上行流和下行流池0~10cm的基质层中好氧微生物数量高出30~55cm的层面1~2个数量级;反硝化细菌除下行流池0~10cm的层面外其他基质层数量都达到107个/g干土以上.0~20cm的基质层中脲酶活性明显高于30~55cm的层面;而0~10cm的层面中脱氢酶活性明显高出10~55cm的层面2~5倍.硝化反硝化作用广泛存在于基质中,硝化作用表现出一定的空间规律,0~10cm的基质硝化作用强度要比40~55cm层面的高出20%;反硝化作用的空间差别很小,其作用率最低也达到85.5%. 相似文献
923.
Mubarak A. Khan S. Shehrzade M. Sarwar U. Chowdhury M. M. Rahman 《Journal of Polymers and the Environment》2001,9(3):115-124
Jute yarns were grafted with a single impregnating monomer 1,6-hexanediol diacrylate (HDDA) in order to improve the physicomechanical properties. Jute yarns soaked for different soaking times (3, 5, 10, and 30 minutes) in HDDA+MeOH solutions at different proportions (1–10% HDDA in MeOH [v/v] along with photoinitiator Darocur-1664 [3%]) were cured under UV lamp at different UV radiation intensities (two, four, six, and eight passes). Concentration of monomer, soaking time, and intensity of UV radiation were optimized with extent of mechanical properties such as tensile strength, elongation at break, and modulus. Enhanced tensile strength (67%), modulus (108%), and polymer loading (11%) were achieved with 5% HDDA concentration, 5-minute soaking time, fourth pass of UV radiation. To further improve the mechanical properties, the jute yarns were pretreated with UV radiation (5, 10, 15, 30, and 50 passes) and treated with optimized monomer concentration (5%). UV-pretreated samples showed the enhanced properties. The tensile strength and modulus increase up to 84% and 132%, respectively, than that of virgin jute yarn. An experiment involving water absorption capacity shows that water uptake by treated samples was much lower than that of the untreated samples. During the weathering test, treated yarns exhibited less loss of mechanical properties than untreated yarns. 相似文献
924.
A Coupled Land-Surface and Dry Deposition Model and Comparison to Field Measurements of Surface Heat,Moisture, and Ozone Fluxes 总被引:1,自引:0,他引:1
Pleim Jonathan E. Xiu Aijun Finkelstein Peter L. Otte Tanya L. 《Water, Air, & Soil Pollution: Focus》2001,1(5-6):243-252
We have developed a coupled land-surface and drydeposition model for realistic treatment of surface fluxes ofheat, moisture, and chemical dry deposition within acomprehensive air quality modelling system. A new land-surfacemodel (LSM) with explicit treatment of soil moisture andevapotranspiration and an indirect soil moisture nudging schemehas been added to a mesoscale meteorology model. The new drydeposition model uses the same aerodynamic and bulk stomatalresistances computed for evapotranspiration in the LSM. Thisprovides consistent land-surface and boundary layer propertiesacross the meteorological and chemical components of the system. The coupled dry deposition model also has the advantage of beingable to respond to changing soil moisture and vegetationconditions. Modelled surface fluxes of sensible and latent heatas well as ozone dry deposition velocities were compared to twofield experiments: a soybean field in Kentucky during summer 1995and a mixed forest in the Adirondacks of New York in July 1998.(on assignment to the National Exposure Research Laboratory, U.S. Environmental Protection Agency) (author for correspondence, e-mail(on assignment to the National Exposure Research Laboratory, U.S. Environmental Protection Agency) 相似文献
925.
环境因素对芦苇湿地CH4排放的影响 总被引:16,自引:0,他引:16
用封闭式箱法对辽河三角洲芦苇湿地温室气体CH4 排放进行了长期观测 .结果表明 ,CH4 排放有明显的季节变化规律 ,平均通量为 520μg·m-2·h-1.土壤产CH4 活性主要发生在0~5cm土层中 ,并随土层深度的增加而显著下降 .CH4排放受环境因素影响很大 ,土壤氧化还原电位在 -110mV时就有CH4排放 ,其排放量随氧化还原电位的下降而增加 .另外 ,随着淹水深度的增加 ,CH4 排放反而减少 .在测定期内 ,CH4 排放与温度呈明显的正相关 (R2=0196,n=21,P<0.05). 相似文献
926.
自由表面流人工湿地处理超稠油废水 总被引:55,自引:2,他引:53
采用自由表面流芦苇湿地处理超稠油废水。当芦苇床的水力负荷为3.33cm/d时,对于年平均进水COD459.16mg/L,石油类27.65mg/L,BOD5 33.52mg/L,TN13.74mg/L的超稠油废水,该系统的出水指标为COD77.21mg/L,石油类1.42mg/L,BOD53.90mg/L,TN1.60mg/L。去除率分别为:COD83.18%,石油类94.86%,BOD588.37%,TN88.36%,pH值由7.87降至7.77。处理后的超稠油废水对土壤的污染并不明显,对芦苇的生长和材质指标几乎没有影响。可见,自由表面流芦苇湿地深度处理超稠油废水的出水水质稳定,耐冲击负荷强,是一种经济有效的超稠油废水处理新方法。 相似文献
927.
Lauren E. Hay Robert L. Wilby George H. Leavesley 《Journal of the American Water Resources Association》2000,36(2):387-397
ABSTRACT: Simulated daily precipitation, temperature, and runoff time series were compared in three mountainous basins in the United States: (1) the Animas River basin in Colorado, (2) the East Fork of the Carson River basin in Nevada and California, and (3) the Cle Elum River basin in Washington State. Two methods of climate scenario generation were compared: delta change and statistical downscaling. The delta change method uses differences between simulated current and future climate conditions from the Hadley Centre for Climate Prediction and Research (HadCM2) General Circulation Model (GCM) added to observed time series of climate variables. A statistical downscaling (SDS) model was developed for each basin using station data and output from the National Center for Environmental Prediction/National Center for Atmospheric Research (NCEPINCAR) reanalysis regridded to the scale of HadCM2. The SDS model was then used to simulate local climate variables using HadCM2 output for current and future conditions. Surface climate variables from each scenario were used in a precipitation‐runoff model. Results from this study show that, in the basins tested, a precipitation‐runoff model can simulate realistic runoff series for current conditions using statistically down‐scaled NCEP output. But, use of downscaled HadCM2 output for current or future climate assessments are questionable because the GCM does not produce accurate estimates of the surface variables needed for runoff in these regions. Given the uncertainties in the GCMs ability to simulate current conditions based on either the delta change or downscaling approaches, future climate assessments based on either of these approaches must be treated with caution. 相似文献
928.
Joseph S. Stibrich Thomas J. Charles 《Journal of the American Water Resources Association》2000,36(6):1263-1269
ABSTRACT: This paper describes how a hydrologic model proved to be a valuable tool to help interested parties understand impacts to four threatened and endangered fish species in the Upper Colorado River. In 1994, the Ute Water Conservancy District initiated permitting and design of the Plateau Creek pipeline replacement. The project was considered a major Federal action and therefore subject to the National Environmental Policy Act. Under Section 7 of the Endangered Species Act, the U.S. Fish and Wildlife Service (USFWS) entered the process to develop a Biological Opinion (BO) and determined that the project could potentially impact the endangered fish in the 15‐mile reach of the Colorado River. The Section 7 consultation was directed by a Core Committee comprised of stakeholders in the Upper Colorado River watershed. Hydrologic modeling became the evaluation tool for comparing flow reductions to USFWS target recovery flows and defining make‐up flow requirements to meet those targets. The Colorado River Recovery Implementation Program was designated to provide the make‐up flows. The USFWS released a final BO in December 1997, approving diversions through 2015. An Environmental Impact Statement for the project was completed and the Record of Decision was issued by the Bureau of Land Management in early 1998. 相似文献
929.
Thomas C. Winter 《Journal of the American Water Resources Association》2000,36(2):305-311
ABSTRACT: The vulnerability of wetlands to changes in climate depends on their position within hydrologic landscapes. Hydrologic landscapes are defined by the flow characteristics of ground water and surface water and by the interaction of atmospheric water, surface water, and ground water for any given locality or region. Six general hydrologic landscapes are defined; mountainous, plateau and high plain, broad basins of interior drainage, riverine, flat coastal, and hummocky glacial and dune. Assessment of these landscapes indicate that the vulnerability of all wetlands to climate change fall between two extremes: those dependent primarily on precipitation for their water supply are highly vulnerable, and those dependent primarily on discharge from regional ground water flow systems are the least vulnerable, because of the great buffering capacity of large ground water flow systems to climate change. 相似文献
930.