辽宁双台子河口湿地生态水文模拟与调控     

罗先香  张蕊  严登华 《地理研究》2011,30(6):1089-1100

在全球气候变化和人类活动影响下,辽宁省双台子河口湿地出现生态用水不足,水环境恶化,土壤盐渍化和海水倒灌等问题,导致湿地明显退化.为解决湿地生态用水供需矛盾,从流域生态水文学角度出发,运用所构建的生态水文耦合模型,对1981～2005年双台予河口湿地集水区生态水文演变规律进行模拟,结果表明:25年间湿地集水区各生态水文要...  相似文献   

Recycling of oceanic crust and the origin of intraplate volcanism     

A. D. Smith 《Australian Journal of Earth Sciences》2013,60(6-7):675-680

Source models for intraplate volcanism (IPV) include vertical introduction of material from deep in the mantle (plume model), contamination of the shallow mantle (perisphere and continental mantle delamination models) and derivation by selective partial melting of oceanic crust recycled into the depleted mantle (SUMA/streaky mantle models). The plume hypothesis became the ruling model after a flawed interpretation of helium isotope data in the mid 1980s that led to plumes being imposed on models for crustal recycling into the depleted mantle. This incorporation of otherwise competing concepts, is the cause of unnecessary complexity in modern geodynamic models. The plume model cannot explain all manifestations of IPV and a comprehensive explanation can only be found by invoking the alternative options, combined with their tapping by plate tectonic processes.  相似文献   

Ophiolites of Different Tectonic Settings and Mantle Melt Origins     

Yildirim DILEK 《《地质学报》英文版》2013,87(Z1):199-199

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中国滨海河口海湾湿地生态系统研究进展——以长江口为例     

高宇  黄晓荣  张婷婷  王妤  杨刚  庄平 《湿地科学与管理》2016,(4):59-63

在全球气候变化的背景条件下,中国河口海湾生态系统的研究逐渐深入和系统化,研究热点开始关注国际公约中的重要生态敏感区,大大缩短了与国际学术界同类研究的差距。以长江口为例,由于河口海湾地区处于海洋、陆地和河流生态系统相互作用的界面上,具有开放度高、敏感度高、脆弱性高和稳定性低的"三高一低"特征。针对长江口大量滩涂栖息地被围垦和侵占的现状,提出了在长江口受损湿地构建人工替代栖息地进行人工优化的途径。中国河口海湾研究不仅需要开展国际、国内交流,还要广泛争取国际组织的资助和合作,探索跨学科、跨行业、跨地区参与动态保护管理和开发利用,使以长江三角洲为代表的中国滨海河口海湾三角洲地区的保护开发和资源利用实现可持续的生态文明。  相似文献   

Modelling of underwater bubble plumes and gas dissolution with an Eulerian-Lagrangian CFD model     

《Applied Ocean Research》2016

Underwater bubble plumes emerge from subsea releases of gas. They can be studied by mathematical models. Here an Eulerian-Lagrangian CFD model is presented. It accounts for relevant physics including buoyancy, turbulence, gas expansion and gas dissolution. The model is compared against three sets of experiments. There is consistency between model and experiments. Special focus is given to the effect of gas dissolution. It is demonstrated how the choice of mass transfer coefficient strongly affects the amount of gas dissolution. Since it is not apparent which mass transfer correlation is applicable, it is argued that more experimental data is needed.  相似文献   

Oceanographic controls on shallow‐water temperate carbonate sedimentation: Spencer Gulf,South Australia          下载免费PDF全文

Laura G. O'Connell  Noel P. James  Mark Doubell  John F. Middleton  John Luick  David R. Currie  Yvonne Bone 《Sedimentology》2016,63(1):105-135

Spencer Gulf is a large (ca 22 000 km²), shallow (<60 m water depth) embayment with active heterozoan carbonate sedimentation. Gulf waters are metahaline (salinities 39 to 47‰) and warm‐temperate (ca 12 to ?28°C) with inverse estuarine circulation. The integrated approach of facies analysis paired with high‐resolution, monthly oceanographic data sets is used to pinpoint controls on sedimentation patterns with more confidence than heretofore possible for temperate systems. Biofragments – mainly bivalves, benthic foraminifera, bryozoans, coralline algae and echinoids – accumulate in five benthic environments: luxuriant seagrass meadows, patchy seagrass sand flats, rhodolith pavements, open gravel/sand plains and muddy seafloors. The biotic diversity of Spencer Gulf is remarkably high, considering the elevated seawater salinities. Echinoids and coralline algae (traditionally considered stenohaline organisms) are ubiquitous. Euphotic zone depth is interpreted as the primary control on environmental distribution, whereas seawater salinity, temperature, hydrodynamics and nutrient availability are viewed as secondary controls. Luxuriant seagrass meadows with carbonate muddy sands dominate brightly lit seafloors where waters have relatively low nutrient concentrations (ca 0 to 1 mg Chl‐a m^?3). Low‐diversity bivalve‐dominated deposits occur in meadows with highest seawater salinities and temperatures (43 to 47‰, up to 28°C). Patchy seagrass sand flats cover less‐illuminated seafloors. Open gravel/sand plains contain coarse bivalve–bryozoan sediments, interpreted as subphotic deposits, in waters with near normal marine salinities and moderate trophic resources (0·5 to 1·6 mg Chl‐a m^?3) to support diverse suspension feeders. Rhodolith pavements (coralline algal gravels) form where seagrass growth is arrested, either because of decreased water clarity due to elevated nutrients and associated phytoplankton growth (0·6 to 2 mg Chl‐a m^?3), or bottom waters that are too energetic for seagrasses (currents up to 2 m sec^?1). Muddy seafloors occur in low‐energy areas below the euphotic zone. The relationships between oceanographic influences and depositional patterns outlined in Spencer Gulf are valuable for environmental interpretations of other recent and ancient (particularly Neogene) high‐salinity and temperate carbonate systems worldwide.  相似文献   

Nitrogen uptake dynamics of a persistent cyanobacterium Cyanothece sp. bloom in Lake St Lucia,South Africa     

《African Journal of Marine Science》2013,35(2):155-161

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Additions to the freshwater ostracod fauna of New Zealand     

Maureen H. Barclay 《新西兰海洋与淡水研究杂志》2013,47(1):67-80

Several species of ostracods, new to New Zealand, are described, including Darwinula sphagna n.sp. and Cypridopsis obstinata n.sp. Limnocythere duffi Hornibrook, 1955 is placed in the genus Gomphocythere Sars, 1924, and a colour variation of Newnhamia fenestrata King, 1855 is discussed.  相似文献   

Adventive occurrence of the fouling serpulid Ficopomatus enigmaticus (Polychaeta) in New Zealand   总被引：1，自引：1，他引：0  

Geoffrey B. Read  Dennis P. Gordon 《新西兰海洋与淡水研究杂志》2013,47(3):269-273

The exotic marine‐fouling polychaete Ficopomatus enigmaticus (Fauvel) is recorded and described from New Zealand. Its sudden occurrence in New Zealand around 1967 was marked by its ecological prominence in estuaries of Whangarei and Auckland Harbours, as a nuisance species on submerged artificial structures including pleasure craft and power station intake pipes.  相似文献   

Microbial activity in natural and organically enriched intertidal sediments near Nelson,New Zealand     

Paul A. Gillespie  A. Lincoln MacKenzie 《新西兰海洋与淡水研究杂志》2013,47(4):471-480

Two measures of microbial activity were used to characterise a variety of sediment habitats in three intertidal inlets in the Nelson region, South Island, New Zealand. Rates of microbial mineralisation potential and epibenthic microalgal production were compared with sediment textures, concentrations of photosynthetic pigments, ATP concentrations, and organic and inorganic nutrients. Baseline ranges for these parameters were established for relatively undisturbed estuarine sites for assessing future environmental deterioration and for comparison with sites affected by organic enrichment. Sediment mineralisation rates were increased more than 1000‐fold by enrichment from a fruit processing plant and microalgal production was enhanced by more than 50‐fold at a site exposed to slaughterhouse wastes. The remaining variables, although often strongly correlated with activity measurements, were not as sensitive as measures of enrichment. Sediment microbial activity measurements are proposed as a means of detecting changes in nutrient status of estuarine environments.  相似文献