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以3种海岛植被修复典型植物木麻黄(Casuarina equisetifolia)、夹竹桃(Nerium indicum)和台湾相思(Acacia confusa)为实验材料,通过对培养基质及植株叶片施加不同浓度的盐溶液,研究不同植物的耐盐能力,筛选耐盐树种.主要结论如下:(1)根据植株生长状况,木麻黄植株的根、叶均可耐受质量浓度3.0%的盐胁迫;夹竹桃植株可耐质量浓度1.0%以下的根系盐胁迫和质量浓度3.0%以下的叶片盐胁迫;台湾相思植株可耐浓度质量2.0%以下的根系盐胁迫和质量浓度0.6%以下的叶片盐胁迫;(2)综合研究结果显示,3种植株耐盐能力为木麻黄夹竹桃台湾相思;(3)植物的生长状态、成活率和株高增长率指标可以很好的指示植株受盐害程度及耐盐能力,可结合赋值法对区域植被耐盐能力进行简单快速的调查;(4)在土壤含盐量较高和受海洋飞沫影响较大的滨海地带开展植被修复时,推荐木麻黄为优先树种;但在土壤含盐量较低的干旱地带,推荐夹竹桃作为先锋品种. 相似文献
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海岛植被破坏严重,而适生物种少的问题已严重影响到海岛植被修复研究工作。本研究通过测定海坛岛和大屿共30种植物的夏季日间光合特性、水分利用效率和比叶面积,为海岛水土流失区生态修复过程中适生植物的筛选提供重要的理论依据。研究结果表明,在海坛岛和大屿的共有种中,仅台湾相思(Acacia confusa)和海桐(Pittosporum tobira)在不同样地的水分利用效率存在差异(p 0.05);滨柃(Eurya emarginata)的原生种和栽培种的水分利用效率没有差异(p 0.05),而海桐的水分利用效率则存在明显的差异(p 0.05)。不同植物的光合参数和比叶面积具有一定的差异,以适应不同的环境。根据水分利用效率进行聚类分析,将30种植物分成3类。其中,夹竹桃(Nerium oleander)、台湾相思、翠芦莉(Ruellia brittoniana)和滨旋花(Calystegia soldanella)等水分利用效率较高,表现出对海岛环境较强的适应能力。因此,将光合特性作为海岛适生物种筛选的指标具有借鉴意义。 相似文献
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2016年4月对厦门无居民海岛猴屿开展了植被和土壤调查,采用全岛调查的方法查清全岛植物种类及生长状况,采用样方调查的方法分析比较人工恢复林和次生林物种多样性和土壤肥力特征,以期为无居民海岛生态修复提供借鉴.结果表明,全岛共有乔木5科5属6种,灌木有10科12属13种,草本植物有21科39属40种.由于被海包围、面积狭小、地形简单,物种传播速度慢,猴屿生物多样性较低,猴屿人工恢复林物种多样性与次生林差异不显著.人工恢复林土壤肥力显著低于次生林,植物生长及其产生的凋落物可以促进土壤肥力的改善.海岛普遍风大、缺水,植被恢复应选用适应海岛环境能力强的物种.猴屿植被破坏导致生态位缺失,进而造成马缨丹生物入侵,影响海岛生态系统稳定性. 相似文献
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海岛独特的自然环境制约了植物的生长，但同时也自然筛选了一批适应能力较强的海岛植物种类。文章采用线路调查和典型样地调查相结合的方法，对平潭岛群中的塘屿、东庠岛、大练岛等海岛临海荒坡山地植被进行实地调查。通过了解平潭周边典型海岛的植被种类、分布及群落结构，分析平潭典型海岛的植被特征，指出风、干旱、盐害及土壤等环境因子是影响平潭周边典型海岛植被生长的制约因素，并针对这几个制约因素，结合调查结果从植物品种筛选、植被配置、修复技术等方面提出困难立地条件的海岛植被修复对策，为相近区位的植被生态修复提供借鉴。 相似文献
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为了探讨台湾相思群落生长发育与气候特征的关系,选用11个位于大屿靠海一侧不同地点的台湾相思群落研究对象。通过2016年4—12月对台湾相思标记枝条的生长状况进行长期监测。观测结果表明:11个样点受盐害叶片占比为1.16%~51.48%,受虫害叶片占比为30.27%~59.78%。植株大多受到盐害与虫害的干扰,花数量和花蕾数量处于一个较低的水平。由植物生长状况与气候特征的相关性结果可知,风向和风力随月份变化而变化,12月风力最高达5.93m/s。月份和风向与受盐害叶片占比、受虫害叶片占比均呈现极显著相关性。在开展海岛植被生态修复时,需要注重冬季养护、病虫害防治和筛选抗风、耐盐雾的海岛适生物种。 相似文献
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海洋盐分主要通过地下水入侵、浪花飞溅、盐雾等方式对滨海植物的根、茎和叶产生影响。采用长势良好2年生夹竹桃（Nerium indicum），分别设置对照0%、0.3%、0.6%、1%、2%、3%多个浓度梯度，开展根系和叶片耐盐实验。盐胁迫处理13周后正常浇水4周。在盐胁迫末期及正常浇水后测定叶片净光合速率（Pn）、蒸腾速率（Tr）、气孔导度（Gs）、水分利用率（WUE）等光合指标；同时测定细胞膜透性、叶片饱和水分亏缺（WSD）等理化指标。结果表明：根系盐胁迫和叶片盐胁迫均会影响夹竹桃植株形态和生长，根系盐胁迫≥1.0%时，夹竹桃植株生长状态向着小于2的趋势发生不可逆下降；叶片盐胁迫≤3.0%时，夹竹桃生长状态普遍大于2。根系盐胁迫极显著降低夹竹桃叶片Pn、Tr和Gs；叶片盐胁迫对夹竹桃植株的Pn和WUE影响极显著，对Tr和Gs无显著影响。夹竹桃Tr与Gs之间极显著相关；高浓度根系盐胁迫下，气孔因素对夹竹桃光合影响较为显著。叶片盐胁迫下，夹竹桃细胞膜透性和WSD变化不显著，高浓度根系盐胁迫下，夹竹桃细胞膜透性和WSD发生不可逆改变；这与生长状态和光合特性的结果可以很好对应，说明膜系统受损反过来影响夹竹桃生长和光合作用。总体上，夹竹桃可耐受3.0%以下的叶片盐胁迫和1.0%以下的根系盐胁迫。将根系和叶片耐盐特性分别研究，可以更好地为夹竹桃在滨海生态和植被修复应用中提供理论指导。 相似文献
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通过样方法和样线法对大兔屿进行植物资源调查,其主要的植被类型是亚热带常绿阔叶林、灌草丛。有维管植物69科,139属,152种。蕨类3科,3属,3种;裸子植物3科,3属,3种;被子植物63科,133属,146种。乔木20科,27属,30种;灌木31科,44属,46种,草本和藤本30科,68属,74种。其中,原生植物125种,外来植物27种,入侵植物10种,无珍稀濒危植物。植被群落的植物区系组成中,属的分析表明,大兔屿植物以热带、亚热带成分为主。种子植物属划分为12个分布区类型及其变型,其中成分最多的是泛热带分布及其变型,为区系总数的35.29%。群落以高位芽植物占主要优势,为46.71%。人工栽培的台湾相思林、马尾松林及木麻黄林总的覆盖率却高达80%。最后针对海岛特色景观的营造,对大兔屿植物资源的保护和利用提出相关的建议。 相似文献
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红树林是具有重要碳汇功能的生态系统,其保护和修复成为海洋领域应对气候变化的重要手段。适宜的生境条件是红树林生态修复成功与否的关键因素,而红树植物物种和种植措施等也决定了修复后生态系统结构和功能的发展。本研究综述了红树林生态修复固碳功能的特点,分析了生境条件、物种和种植措施等因素对红树林生态系统固碳效果的影响,以期为红树林生态修复提供参考。总体上,红树林生态修复促进了有机碳在植物体和土壤中的累积,而在生态修复初期红树植被的固碳能力高于土壤。水文条件、滩涂高程、底质条件、物种、种植密度和种苗来源等关系到修复后红树植物的生长、颗粒态有机物的沉降、有机物的输出和保留、有机质的分解等过程,进而影响生态系统的固碳能力。因此,开展红树林生态修复时选择适宜生境条件的修复地块,合理选择物种和种植措施,在提高植被恢复效果的同时可提高红树林固碳增汇的生态功能。 相似文献
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通过样方法对福建省厦门市大屿岛主要乔木种生态位特征进行分析。结果表明:整个岛屿乔木树种物种多样性较低,其中Shannon-Wiener物种多样性指数为1. 26,Margalef丰富度指数为1. 44,Simpson生态优势度指数为0. 54,Pielou均匀度指数为0. 57。乔木层优势物种是台湾相思(Acacia confusa),其重要值达53. 84%。其次是马尾松(Pinus massoniana)、柠檬桉(Eucalyptus citriodora)和潺槁木姜子(Litsea glutinosa)。生态位特征分析表明台湾相思生态位宽度最大,其Levins和Shannon生态位宽度值分别为19. 00和2. 84。生态位宽度较大的还有马尾松,潺槁木姜子和柠檬桉。台湾相思和马尾松的生态位重叠值最高,为0. 673,其次为台湾相思和潺槁木姜子,其生态位重叠值为0. 633。台湾相思、马尾松、柠檬桉和潺槁木姜子的胸径和冠幅在空间分布中变化趋势相似。综上可知厦门大屿岛乔木树种多样性较低,植物种类简单,优势种相对明显,生态位特征值较小的植物对生境要求较高,整个生态系统较为脆弱。 相似文献
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Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone. 相似文献
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The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics. 相似文献
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《海洋学报(英文版)》2014,(9):F0003-F0003
<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology, 相似文献
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The relationship between the flux of exotic benthic foraminiferal tests (i.e. tests which are supplied from open-sea sources alone) in a tidal inlet and that of bulk sediment was analysed, which can be expressed as two first-order linear equations. According to this relationship, in order to determine net sediment transport directions in the entrance, the test concentration in surficial sediments of the tidal basin can be compared against a ‘ critical level ’. The critical level is determined for the conditions that no net transport of bulk sediment is present within the entrance. If the observed concentration (averaged over the tidal basin) is higher than the simulated critical level, then the net sediment transport is directed to landward. This method is applied to the analysis of net sand transport at Christchurch Harbour, a tidal inlet system located in southern England. In this investigation, concentrations of exotic foraminiferal tests in the surficial sediments of the tidal basin and ebb tidal delta area were obtained from the analysis of sea-bed sediment samples. A series of probable critical levels were calculated based upon the data sets with regard to: (1) sediment discharge from the rivers; (2) magnitude of sediment discharge within the entrance during the ebb; (3) the test concentration outside the harbour; (4) the thickness of the moving layer; and (5) two parameters associated with dispersive processes. The results show that the concentration in the tidal basin sediment is higher than a number of simulated critical concentrations for representative cases. Consequently, the high level of the concentration of exotic benthic foraminiferal tests within the harbour should be explained as a result of landward net transport of sands within the entrance. 相似文献
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Coastal inundation associated with extreme sea levels is the main factor which leads to the loss of life and property whenever a severe tropical cyclonic storm hits the Indian coasts. The Andhra and Orissa coasts are most vulnerable for coastal inundation due to extreme rise in sea levels associated with tropical cyclones. Loss of life may be minimized if extreme sea levels and associated coastal flooding is predicted well in advance. Keeping this in view, location specific coastal inundation models are developed and applied for the Andhra and Orissa coasts of India. Several numerical experiments are carried out using the data of past severe cyclones that struck these regions. The simulated inland inundation distances are found to be in general agreement with the reported flooding. 相似文献
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Hoi-Soo Jung Kap-Sik Jeong Yong-Shik Chu Sung-Hyun Park Ki-Hyune Kim 《Marine Georesources & Geotechnology》2001,19(3):181-195
Grain size and water content in box-core sediments from the Clarion-Clipperton fracture zone (C-C zone) in the northeast equatorial Pacific were analyzed in detail to understand the downcore variations across a hiatus between Quaternary and Tertiary layers. Grain-size distributions in the topmost core sediments show two modes: a coarse mode (peaked at 50 μm) and a fine mode (at 2-25 μm). The coarse mode disappears gradually with depth accompanied by the dissolution of siliceous fossil tests, whereas the fine mode coarsens due to the formation of authigenic minerals. Water content increases abruptly across a color boundary between an upper pale brown layer and a lower dark brown layer that is the hiatus between Quaternary and Tertiary layers. Abundant smectites and microvoid molds, which are created by the prolonged fossil dissolution in the underlying sediment, are attributed for the abrupt downcore variation of water content. Overall variations in grain size and water content in the topmost core sediments in the western C-C zone are possibly constrained by the dissolution of biogenic siliceous fossils. Variations in geotechnical properties related to these changes must be considered in the design of nodule collectors. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2001,24(1):27-33
This article concerns an interrelation between the sea levels and the western boundary flow near a tectonic boundary in a local zone in the Northwestern Pacific. In this zone, sea level variations at stations located on the coast facing the Pacific are studied to find the interrelation between variations of the Kurosio flow as an index of the distance of the flow axis off a specific coast. The result is discussed after data processing of the monthly means of the sea levels, and a notice is taken of variations caused by active crustal upheavals during a seismic event, a local earthquake. 相似文献