微藻对水网藻在水体修复中的胁迫作用研究

通过单独与混合培养实验,结果显示在适宜营养水平下,水网藻对氮、磷有较强的富集吸收能力;而来自微藻生长竞争的压力会促使水网藻对营养物的生态幅变窄,满足其最佳生长所需要的PO43-P从0.085mg/L降低为0.024mg/L;并且其富集磷的能力也大为降低。在利用水网藻进行富营养化水体修复或净化水质时,这种生物之间的抑制现象必须引起重视。     

南方涝渍地区退田还渔的一个实例分析

以江汉平原四湖涝渍地区的一个经围湖造田形成的典型农业微域为研究对象,在对其土壤和作物生长状况进行调查的基础上,探讨了退田还渔的必要性与具体方案。结果表明,对小型湖泊通过围湖造田所形成的农业微域,在人工排水和土地平整不充分的情况下,其地貌和土壤还残留有原有湖泊的影响,处于原湖泊低处的土壤表现出明显的沼泽化和严重潜育化的特征。在该地区种植水稻产量比正常地区减产达16%～26.8%。利用数量化理论Ⅰ确定了该地区适宜退田还渔的具体位置和面积。按照这一方案实施的结果,该地区从1997～2001年的5年中精养鱼塘面积增加9倍,养鱼的效益比种植水稻高5～10倍,还减轻了该地区夏季和冬季的排水压力。     

铁路建设对动物生态行为的影响与控制策略

从动物生境的破坏与污染两方面分析了铁路建设对动物生态行为的影响，并从铁路的路线选择、防噪减噪、设置动物通道、加强管理等方面论述了其控制对策。     

土地荒漠化的成因、危害及防治对策

土地荒漠化是指在干旱、半干旱和某些半湿润、湿润地区,由于气候变化和人类活动等各种因素所造成的土地退化,它使土地生物和经济生产潜力减少,甚至基本丧失.我国是全球荒漠化面积较大、分布较广、危害较严重的国家之一.近年来由于采取了一系列有效的治理措施,荒漠化和沙化整体扩展的趋势已得到初步遏制,但形势依然严峻.     

3种重金属对青萍毒害的研究

对水体中主要的3种重金属(铜、镉、铅)对青萍抗氧化酶系统的几种酶,包括过氧化物酶(POD)、超氧化物歧化酶(SOD)、过氧化氢酶(CAT)的活性,丙二醛(MDA)的含量,可溶性蛋白含量及叶绿体色素含量等指标的影响进行了研究.研究表明青萍对镉污染反应最为敏感,对铜的反应相对缓和一些;青萍在铅的胁迫下表现出无序的状态.因此,青萍不适合应用于重金属镉污染的富营养化水体的治理和生态修复中.     

荷兰浅水湖的生态恢复实践

湖泊的富营养化导致了湖泊生态系统的失衡。要使湖泊获得生态恢复,只通过控制入湖的营养负荷是不够的。荷兰的实践证明,外部营养负荷的大量减少并没有带来预期的恢复效果,而通过湖泊的换水和生物控制,湖泊的透明度、水生植物等得到了迅速改善。根据荷兰方面提供的资料,介绍了荷兰通过换水和生物控制进行浅水湖的生态恢复实践和取得的经验。     

阴山北麓丘陵区林草建设与生态恢复--以固阳县忽鸡沟乡小六分子村为例

针对阴山北麓生态环境特点和主要环境问题，以固阳县忽鸡沟乡大六分子村为基点，应用恢复生态学的基本理论和生态经济学原理，以恢复生态系统良性循环为目标，通过实施以林草建设为核心的一系列植被恢复与重建措施，使遭受破坏的生态系统逐步得到恢复并步入良性循环的轨道，为阴山北麓广大地区生态恢复探索一条切实可行的有效途径。     

渭河流域生态环境对野鸭数量分布的影响

环境是动物生存的基础，人类的活动对环境所造成的影响，直接导致动物种群数量的变动。通过渭河咸阳段气候、水质、水域面积、植物等环境因素的改变对野鸭数量分布影响的调查，表明环境的恶化导致了动物的生存受到威胁，数量减少，分布区域缩小。随着环境保护意识的增强，渭河流域的水土流失，水质污染、退耕还草等环境问题逐渐得到解决，动物的生活环境不断得到改善，其种群数量、分布范围随之增加。     

COLD WATER PATCHES IN WARM STREAMS: PHYSICOCHEMICAL CHARACTERISTICS AND THE INFLUENCE OF SHADING1

ABSTRACT: Discrete cold water patches within the surface waters of summer warm streams afford potential thermal refuge for cold water fishes during periods of heat stress. This analysis focused on reach scale heterogeneity in water temperatures as influenced by local influx of cooler subsurface waters. Using field thermal probes and recording thermistors, we identified and characterized cold water patches (at least 3°C colder than ambient streamflow temperatures) potentially serving as thermal refugia for cold water fishes. Among 37 study sites within alluvial valleys of the Grande Ronde basin in northeastern Oregon, we identified cold water patches associated with side channels, alcoves, lateral seeps, and floodplain spring brooks. These types differed with regard to within floodplain position, area, spatial thermal range, substrate, and availability of cover for fish. Experimental shading cooled daily maximum temperatures of surface waters within cold water patches 2 to 4°C, indicating a strong influence of riparian vegetation on the expression of cold water patch thermal characteristics. Strong vertical temperature gradients associated with heating of surface layers of cold water patches exposed to solar radiation, superimposed upon vertical gradients in dissolved oxygen, can partially restrict suitable refuge volumes for stream salmonids within cold water patches.     

PROFILE: Hungry Water: Effects of Dams and Gravel Mining on River Channels

/ Rivers transport sediment from eroding uplands to depositional areas near sea level. If the continuity of sediment transport is interrupted by dams or removal of sediment from the channel by gravel mining, the flow may become sediment-starved (hungry water) and prone to erode the channel bed and banks, producing channel incision (downcutting), coarsening of bed material, and loss of spawning gravels for salmon and trout (as smaller gravels are transported without replacement from upstream). Gravel is artificially added to the River Rhine to prevent further incision and to many other rivers in attempts to restore spawning habitat. It is possible to pass incoming sediment through some small reservoirs, thereby maintaining the continuity of sediment transport through the system. Damming and mining have reduced sediment delivery from rivers to many coastal areas, leading to accelerated beach erosion. Sand and gravel are mined for construction aggregate from river channel and floodplains. In-channel mining commonly causes incision, which may propagate up- and downstream of the mine, undermining bridges, inducing channel instability, and lowering alluvial water tables. Floodplain gravel pits have the potential to become wildlife habitat upon reclamation, but may be captured by the active channel and thereby become instream pits. Management of sand and gravel in rivers must be done on a regional basis, restoring the continuity of sediment transport where possible and encouraging alternatives to river-derived aggregate sources.KEY WORDS: Dams; Aquatic habitat; Sediment transport; Erosion; Sedimentation; Gravel mining