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21.
对玄武湖实施清淤引水、藻华治理、种群恢复等措施前后的水体数据进行分析,结果表明:清淤引水工程可短时间内降低沉积物中污染物浓度,缓解水体富营养化程度,但从长期效果分析,水体中的营养盐含量并未显著改善.藻华治理能在短期内有效抑制水体中的蓝藻水华,治理后水体各项指标均有提升,水生植物种群得以恢复,是短期改善水体水质的有效方式.在种群恢复阶段与往年相比,水体各项指标均有所改善,持续时间更长,是一种理想的湖泊治理方法.  相似文献   
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中国多数红树林陆地边缘存在着大量的养虾池塘。这些养虾池塘可通过:(1)换塘外排废水,(2)清塘直排污泥影响周围的红树林。本研究共包含两个实验,来探讨这两种类型的排污对秋茄幼苗生长的影响。实验一模拟虾池常规换塘情况,研究换塘废水对秋茄幼苗生长的影响。实验二设置四种虾池清塘污泥沉积厚度(0 cm,2 cm,4 cm,8 cm),研究虾池清塘污泥的累积效应对秋茄幼苗生长的影响。结果如下:在5,15和25三种盐度下,虾池换塘废水未对秋茄生长指标造成显著影响;而清塘污泥对秋茄生长的影响与其沉积厚度有关,大多数生长参数在污泥沉积厚度为4 cm时呈现最大值。秋茄幼苗在适量的沉积厚度下加速了生长,且本实验秋茄幼苗对虾池清塘污泥的耐受性为沉积厚度8 cm。  相似文献   
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珠江磨刀门水道咸潮上溯加剧的原因   总被引:1,自引:0,他引:1  
对磨刀门水道不同年份地形资料和多年枯季潮位资料进行了对比分析,结果表明:大规模的河床采砂,引起磨刀门上游河段河床大幅下切,河道深泓平均加深0.59~2.25 m,河槽容积平均增加8.91×106~12.11×106m3,使该河段枯季潮差增大,进潮量增加,潮汐动力增强,导致咸水界向上游河段推移;口门围垦整治后,磨刀门口门区由众多岛屿环抱而成的内海区变成人工导堤控制的"一主一支"两条水道,水域面积减少了80%,河槽容积减少了40%,深槽趋于顺直加深,使口门区的"调淡"作用消失,这是咸潮上溯的重要原因;根据多年水文频率分析,发生严重咸潮灾害时,西、北江枯季流量并非都是枯水流量,因此枯季上游来水量变化并不是近年来咸潮灾害加剧的主要原因。  相似文献   
25.
Conservation and management of coastal lagoons envisage direct human intervention. To prevent siltation and to preserve the hydrodynamics features of the lagoon system, the inner channels undergo regular maintenance dredging.  相似文献   
26.
Coastal lagoons are ephemeral habitats whose conservation requires human intervention, such as maintenance dredging of inner channels. Dredging can reduce the abundance of benthic species due to the removal of individuals with the sediment, modify sediment properties, and resuspend fine sediment, nutrients and pollutants, which can lead to eutrophication, hypoxic events and increasing toxicity. Both direct effects in the dredged channel and possible indirect effects in surrounding shallow areas could be expected. This study assesses the effects of the channel maintenance dredging, performed between October 2004 and August 2005, on the invertebrate assemblages both in channels and adjacent ponds in the northern Adriatic coastal lagoon of Pialassa Baiona. The lagoon is affected by eutrophication, chemical and thermal pollution from wastewater treatment and power plants. Three impacted sites were located in the dredged channel and three in the adjacent interconnected shallow water ponds, while three non-impacted sites were located in a channel and in a pond far from the dredged area. Replicate samples were collected from each site one time before and one time after the dredging operations. Despite the extent of the intervention, effects of the dredging on macrobenthic assemblages were detected only within the dredged channel, while in the surrounding ponds no clear and unequivocal effects were found. In particular the dredging could have promoted the increase of the abundance of the polychaete Streblospio shrubsolii in the southern and central parts of the dredged channel and the increase in abundance of the amphipod Corophium insidiosum in the northern side, compared to the controls. Instead, species diversity was reduced in the central and northern parts of the dredged channel. These effects on the macrobenthic invertebrate assemblages could be related to the observed changes of sediment characteristics, contamination and toxicity. Overall, direct effects on benthic assemblages in the dredged channels were more detectable than the possible secondary effects in the surrounding shallow ponds, where the higher spatial heterogeneity can mask any relevant effects.  相似文献   
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在疏浚工程检测中的多波束数据后处理方法研究   总被引:1,自引:1,他引:1  
在对多波束测深系统实际测量数据进行数据后处理时,由于采用不同的网格化处理方法,可能会使测量结果产生较大差异。通过对不同的网格化处理方法测量结果的影响分析,介绍了一种全新的网格化处理思路,在疏浚工程检测中,面对大量、密集的多波束测深数据,能更好地满足检测目的,使其能有效的指导疏浚工程施工或为工程竣工验收提供有力依据。  相似文献   
29.
日照港煤码头浚深工程回淤分析   总被引:3,自引:0,他引:3  
采用水动力学三维数学模型对日照港煤码头水域的水动力因素进行了计算,并在此基础上对煤码头浚深工程实施后港池和航道回淤进行了计算分析.计算结果与实测结果比较表明:文中模型较好地重演日照港煤码头水域潮流场,对于港池与航道的回淤分析合理可靠.  相似文献   
30.
The aim of this study was to investigate the effect of dredging intensity on the physical and biological recovery times of the seabed following marine aggregate dredging. Two areas of seabed, previously subject to, respectively, relatively high and lower levels of dredging intensity, were identified on the Hastings Shingle Bank. Two reference areas were also selected for comparative purposes. All four sites were monitored annually over the period 2001–2004, using a combination of acoustic, video and grab sampling techniques. Since the site was last dredged in 1996, this was intended to provide a sequence of data 5–8 years after cessation of dredging. However, an unexpected resumption of dredging within the high intensity site, during 2002 and 2003, allowed an additional assessment of the immediate effects and aftermath of renewed dredging at the seabed. The early stages of recovery could then be assessed after dredging ceased in 2003. Results from both dredged sites provide a useful insight into the early and latter stages of physical and biological recovery. A comparison of recent and historic dredge track features provided evidence of track erosion. However, tracks were still visible 8 years after the cessation of dredging. Within the high dredging intensity site, recolonisation was relatively rapid after the cessation of dredging in 2003. Rather than indicating a full recovery, we suggest that this initial ‘colonization community’ may enter a transition phase before eventually reaching equilibrium. This hypothesis is supported by results from the low intensity site, where biological recovery was judged to have taken 7 years. Further monitoring is needed in order to test this. An alternative explanation is that the rapid recovery may be explained by the settlement of large numbers of Sabellaria spinulosa. As the resumption of dredging within the high intensity site limited our assessment of longer-term recovery it is not yet possible to assume that a 7-year biological recovery period will be applicable to other, more intensively dredged areas at this or more distant locations.  相似文献   
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