三峡地区河岸带植物群落的特征及其分类与排序研究

本文以长江三峡干流河岸植物群落为研究对象,对群落的物种组成、物种多样性进行了分析,并利用TWINSPAN和DCA对植物群落进行等级式划分。结果表明:河岸植物区系组成较为复杂,以温带成分为主,有着较高比率的世界分布成分。灌、草丛群落之间的物种多样性差异不显著,但部分草丛的不同层次间存在较大差异。TWINSPAN 和DCA分析显示,河岸植物群落呈现沿湿度梯度方向的分布格局。图2表3参8。     

沈阳地区河岸植被缓冲带对氮、磷的削减效果研究

为充分了解河岸植被缓冲带对地表径流污染物的去除效果, 本研究选取辽宁省沈阳市两条典型河流——浑河与蒲河为对象, 研究其滨水不同河岸植被缓冲带对地表径流氮、磷污染物的削减效果。结果表明: 在6 种河岸植被带中, 人工林草地对氮的削减效果最好, 对总氮、硝态氮和铵态氮的平均削减率分别为47%、36%和31%; 人工林地对磷的削减效果较好, 平均削减率为74%; 而人工林地对氮以及人工草地对磷的削减效果较差。随长度增加, 河岸植被缓冲带对地表径流污染物的削减效果基本呈增强趋势。以上研究结果说明不同河岸植被缓冲带对地表径流中氮、磷的削减各有优点。在对遭受污染的河流进行生态修复时, 应考虑环境污染特点和地表特征, 以充分发挥河岸植被缓冲带对污染物的削减优势。     

废弃农药厂污染场地浅层地下水生态毒性诊断研究

选择大型溞、斜生栅藻、发光菌为试验生物,对某废弃农药厂污染场地4个不同区域土壤剖面浅层地下水编号为CP01、CP02、CP03、CP04的4种水样进行了急性毒性试验,同时对水样进行了化学分析。结果表明,4种水样对大型溞的24h-EC50分别为0.29%、5.12%、0.83%、1.99%;对斜生栅藻的96h-EC50分别为11.04%、50.44%、12.21%、41.66%;对费舍尔弧菌的发光抑制率分别为95%、66%、88%、75%。化学检测结果表明,CP01中的主要污染物为苯系物与少量烷烃、烯烃类多种物质,CP02中的污染物质只有少量二氯甲烷与1,2-二氯乙烷两种物质,CP03、CP04中的主要污染物为苯系物与烷烃多种物质。毒性试验结果与化学检测结果具有较好的相关性,3种试验生物的毒性效应结果相一致。该研究方法简单快速,可以用于污染场地水样污染毒性诊断,快速筛选出敏感区域,同时提供污染物质的联合毒性基础数据,为场地进一步危害识别与风险评估提供依据。     

森林游憩的发展回顾与前景展望

回顾了森林游憩在国外的发展历程,系统讨论了森林公园、自然保护区、风景名胜区在我国森林游憩业中的发展过程与现状,并展望了森林游憩业在我国的前景和发展方向。     

浅谈人文景观在风景名胜区规划中的作用

初步探讨了人文景观在风景名胜区规划中的作用，并对现在的问题进行了讨论。我国具有丰富的人文景观资源，根据其内容的不同分为四大类型，合理地把它们应用到风景名胜区规划中，使其与自然景观和谐地融汇，充分人文景观的作用，对于优美景观的创造和旅游事业的发展都有很大帮助。     

Plant Availability Index by Potassium Exchange Isotherms in Selected Rice Soils of Lesser Himalayas

Potassium (K) exchange isotherms (quantity–intensity technique, Q/I) and K values derived from the Q/I relationship provide information about soil K availability. This investigation was conducted to study Q/I parameters of K, available K extracted by 1 N ammonium acetate (NH₄AOc) (exchangeable K plus solution K), K saturation percentage (K index, %), and the properties of 10 different agricultural soils. In addition, the relationship of mustard plant yield response to the K requirement test based on K exchange isotherms was investigated. The Q/I parameters included readily exchangeable K (ΔK₀), specific K sites (K_X), linear potential buffering capacity (PBC^K), and energy of exchange of K (E_K). The results of x-ray diffraction analysis of the oriented clay fractions indicated that some mixed clay minerals, illite clay minerals, along with chlorite/hydroxy interlayered vermiculite and kaolinite were present in the soils. The soil solution K activity ratio at equilibrium (AR₀) ranged from 8.0 × 10^?4 to 3.1 × 10^?3 (mol L^?1)^0.5. The readily exchangeable K (ΔK₀) was between 0.105 to 0.325 cmol_ckg^?1 soil, which represented an average of 88% of the exchangeable K (K_ex). The soils showed high capacities to maintain the potential of K against depletion, as they represented high linear potential buffering capacities (PBC^K) [13.8 to 50.1 cmol_c kg^?1/(mol L^?1)^0.5. The E_K values for the soils ranged from ?3420 to ?4220 calories M^?1. The percentage of K saturation (K index) ranged from 0.7% to 2.2%. Analysis of variance of the dry matter (DM), K concentrations, and K uptake of mustard plants indicated that there were no significant differences among the adjusted levels of K as determined by the exchange-isotherm curve.     

禽流感相关在线资源

这篇文章对禽流感疫情作出简介后 ,主要介绍了禽流感的新闻常识类网页、预防以及中国有关禽流感法律法规网页、专业资源网站     

Rangeland Monitoring: Water Quality and Riparian Systems

Ecological concepts serve as a foundation for developing a monitoring program to evaluate water quality and associated riparian systems. Ecological concepts used for developing a monitoring plan must be supported by scientific literature and related to streamflow dynamics and channel interactions. These interactions help determine natural or background habitat quality within and along river longitudinal and environmental gradients from mountains through basins in the western United States. In addition stream size, position in the watershed, and flow are related to sediment sorting, channel bank strength, and channel configuration. These relationships determine channel substrate habitat for aquatic organisms and population diversity. These habitat features may be modified by a channel's ability to store and transport sediment and associated pollutants within a watershed's drainage pattern. Sediment supply, delivery, and timing are altered by differences in snowmelt along elevation gradients, runoff from convective storms, water development history, and stream channel succession. Potential impairment of reference or background aquatic habitat in the western United States is generally sediment related and should be greater in basin river segments and during base flow conditions. Impairment sources can be shown to originate in the steep and first order tributaries of foothill and basin watersheds, and not from valley slopes where supply must cross established riparian zones. Water column, substrate disturbance, and channel bank disturbances may alter amount of sediment and bacteria pollution measured in basins and during base flow conditions.