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141.
Hydrodynamic data and samples of bed sediment were collected from Nara Inlet, a small incised embayment in the Whitsunday Islands, central Great Barrier Reef. Measured tidal currents in the inlet do not exceed 0.2 ms–1 even at spring tides. Swell waves dominate much of the inner shelf of the Great Barrier Reef but are absent from in the inlet due to the presence of a fringing reef at the inlet mouth. On the silty sand floor of the inlet, particle size decreases towards the inlet head. Most of the bed is too coarse to be remobilised by fair‐weather wave and tides, and we predict that bedload sediment transport thresholds are only exceeded in the inlet during cyclones. The observed distribution of bed sediments is consistent with landward dispersal of sediment under storm conditions. Over 20 m of (presumably Holocene) sediments occurs in the inlet and the seismic character of the infill is consistent with the observed textural variation of the modern sediments. We infer that sediment accumulation on the floor of the inlet has been storm dominated throughout much of the Holocene. 相似文献
142.
Large-scale steady-state groundwater flow in atoll carbonate platforms results from temperature and salinity-induced density gradients. Atolls are built on top of a basaltic substrate that provides geothermal heating from beneath. Moreover, they are immersed in the tropical ocean where temperature decreases rapidly with depth. Groundwater circulation in these platforms has long been associated with the geothermal heat flux because it is capable of generating inward and upward flow of oceanic origin water by buoyancy effects. This study shows that hydraulic circulation occurs even in the absence of a geothermal flux because the combination of the cold subsurface ocean waters with the warm surface conditions is sufficient to maintain a convection cell within the carbonate platform. Using a one-dimensional analytical model, validated by more sophisticated two-dimensional simulations, we can investigate the interaction between these two driving forces. The flow rate inside the platform is, in fact, a function of the ratio of the geothermal flux to the temperature gradient in the ocean. It increases with the geothermal flux but decreases with the oceanic temperature gradient. This one-dimensional model also shows that taking salinity effects on density into account increases the flow rates transiting through the platform by a third. 相似文献
143.
Fresh-water lenses are the major sources of water supply in many atoll islands in the Pacific and Indian Oceans, particularly
in dry seasons. Several two- and three-dimensional models are currently available for the simulation of atoll-island aquifers;
however, 2D models cannot include 3D spatial variability of material properties, they must simplify the boundary conditions,
and they cannot correctly simulate pumping wells. In an attempt to overcome these difficulties, a 3D model, SALTFLOW, was
adopted for the simulation of Home Island in the Indian Ocean. This exercise required a discretisation on the order of a few
metres and time steps of a few hours requiring significantly high CPU times. High CPU demand proved to be a difficult challenge
but cannot be considered a serious practical limitation with today's advanced computers. The exhaustive data demands of the
model (e.g., 3D distributions of hydraulic conductivity, porosity, dispersivities, and spatial and temporal variations of
recharge and extraction rates) proved to be more problematical. Although the Home Island data set is unusually comprehensive
by any standards, nonetheless the quality and quantity of the available data proved inadequate to meet the calibration needs
of a highly karstic aquifer system. The Home Island modeling demonstrates the practical limitations of 3D models. It raises
the concern that our ability to develop computer codes capable of simulating complex systems now exceeds our ability to supply
the input data necessary for reliable calibration. Finally, the paper demonstrates the importance of the transient calibration
in reliable simulation of various management options and emphasises that transient calibration should be considered as an
integral part of any similar 2D or 3D modeling.
Electronic Publication 相似文献
144.
近50余年来南海西沙海域冬季风强度的变率 总被引:3,自引:0,他引:3
采用南海西沙永兴岛海洋观察站1958~1997年12~2月实测的北东向冬季风风速的平均值作为冬季风强度指数 (WMI),与南海北缘滨珊瑚的相应年月份的实测δ18O平均值进行相关分析,得到线性回归方程WMI (m/s) = - 4.913- 2.138δ18O (‰),r = 0.83, n = 40。在计算(后报) 所得的1944~1997年代际变化序列中,WMI在40~60年代呈下降趋势,70年代略有上升,而80~90年代又呈下降趋势。在年际变化序列中,WMI呈显著的下降趋势,所得线性回归方程为WMI = 79.67-0.0377 Year, r = 0.68, n = 54。由斜率看出,WMI每10年平均下降约0.4 m/s。用Daniell功率谱法分析,近54年来WMI的变化存在2.5~7年的周期,与季风的QBO周期为2~2.4年,以及ENSO活动的3~8年周期密切相关。WMI连续下降的趋势是与全球持续变暖相映,南海海域冬季风强度的变化受到了全球变化的制约。 相似文献
145.
Accidental oil spills from ships or rigs and inputs of effluent such as production formation water (PFW) are key perceived threats to tropical biota from industry activities. Scleractinian corals are an important functional component of tropical reefs and the abundance, diversity and resilience of coral communities can be used as an indicator of ecosystem health. In this paper, we report the effects of petroleum products, including water accommodated fractions (WAF) of crude oil, PFW and dispersant (Corexit 9527), on fertilization and larval metamorphosis of the widespread scleractinian coral, Acropora millepora (Ehrenberg, 1834) in laboratory-based assays. At 20% v/v PFW fertilization was inhibited by 25%. This concentration was equivalent 0.0721 mg l−1 total hydrocarbon (THC). In contrast, larval metamorphosis was more sensitive to this effluent, with 98% metamorphosis inhibited at the same concentration. Crude oil WAF did not inhibit fertilization of gametes until dispersant was introduced. Dispersed oil was slightly more toxic to fertilization than dispersant alone, suggesting toxicity to that event may be additive. The minimum concentration of dispersed oil which inhibited fertilization was 0.0325 mg l−1 THC. Larval metamorphosis was more sensitive than fertilization to crude oil. Although crude oil and dispersant inhibited larval metamorphosis individually, this toxicity was magnified when larvae were exposed to combinations of both. Crude oil inhibited metamorphosis at 0.0824 mg l−1 THC and at 0.0325 mg l−1 THC when dispersed in 10% v/v (dispersant/oil). Management of petroleum-related risks to spawning corals should consider not only the occurrence of the annual coral spawning event, but also the subsequent 1–3-week period during which most larval metamorphosis and recruitment occur. 相似文献
146.
ANDREW J. WHEELER MAXIM KOZACHENKO DOUG G. MASSON VEERLE A. I. HUVENNE 《Sedimentology》2008,55(6):1875-1887
The Darwin Mounds are small (up to 70 m in diameter), discrete cold‐water coral banks found at c. 950 m water depth in the northern Rockall Trough, north‐east Atlantic. Formerly described in terms of their genesis, the Darwin Mounds are re‐evaluated here in terms of mound growth processes based on 100 and 410 kHz side‐scan sonar data. The side‐scan sonar coverage is divided into a series of acoustic facies representing increasing current speed and sediment transport/erosion from south to north: pockmark facies, ‘mounds within depressions’ facies, Darwin Mound facies, stippled seabed facies and sand wave facies. Mound morphometric changes are quantified and show a south‐to‐north divergence from an inherited morphology, reflecting the outline of coral‐colonized fluid escape structures, to developed, downstream elongated, elevated mound forms. It is postulated that increasing current speeds and bedload sand transport favour mound growth and development by a process of enhanced sand sedimentation within mounds due to current deceleration by frictional drag around coral colonies. Comparisons are made with similar growth processes attributed to comparably sized cold‐water coral mounds in the Porcupine Seabight, offshore Ireland. 相似文献
147.
珊瑚骨骼生长有年、月、日周期,能够当作古生物钟来记录地质历史。块状珊瑚骨骼密度条带年周期的发现对后来的珊瑚古气候研究产生了深远的影响,随后又发现世界各热带海域的珊瑚存在多种多样的骨骼密度变化模式,起先常从珊瑚的生长环境中寻找骨骼密度变化的控制因素,但是没有成功,从80年代后期,部分学者试图从珊瑚骨骼构架本身出发、综合考虑环境因素和骨骼密度条带之间的关系来探求骨骼密度变化的机理,并提出了一个可以解释大多数块状珊瑚骨骼密度条带变化模式的骨骼生长模型。块状珊瑚软体层厚度是一个十分重要但至今仍没引起足够重视的珊瑚生长参数,它相对于骨骼线性生长率的变化影响着骨骼密度变化模式。骨骼钙化作用和虫黄藻光合作用的相互关系还存有争议,珊瑚骨骼钙化机理仍在探索中。 相似文献
148.
依据中国早石炭世珊瑚群特征的研究,岩关期珊瑚地理区系可分(一)北方珊瑚大区——中国北方珊瑚区:①兴安珊瑚分区以Ankhelasma和Homalophylites等北美分子为主的单体不具鳞板的珊瑚;②准噶尔珊瑚分区以Kasinela,Hebukephyylum等欧亚分子为主体的单体无鳞板珊瑚。(二)特提斯珊瑚大区——中国南方珊瑚区:①华南珊瑚分区以Cystophrentis-Pseudouralinia为代表的珊瑚群;②西部珊瑚分区以Beichuanophylum-Siphonophylia-Humboldtia为代表的珊瑚群。大塘期珊瑚地理区系可分(一)特提斯珊瑚大区——K.Y.珊瑚区:①北天山—吉中珊瑚分区以Yuanophylum-Gangamophylum-Siphonophylia为代表的珊瑚群;②南部珊瑚分区以Yuanophylum-Keichouphylum为代表的珊瑚群。(二)冈瓦纳珊瑚大区——藏南珊瑚区:①冈底斯—口念青唐古拉珊瑚分区以Rhopalolasma-Mirusophylum为代表的小型单体无鳞板的珊瑚群;②喜马拉雅珊瑚分区以Longiclava-Cumminsia为代表的单体不具鳞 相似文献
149.
在三亚湾环境下四种方法在五种造礁石珊瑚上移植效果的比较 总被引:2,自引:0,他引:2
珊瑚移植一直被认为是增加退化珊瑚礁上珊瑚数量的重要手段之一。为了调查多种珊瑚移植方法和不同珊瑚种类的移植效果,我们选择了已严重退化并仍面临着人类和自然环境胁迫的三亚鹿回头珊瑚礁作为移植地,对5种珊瑚共902个断枝利用4种方法进行了移植。在移植后的10个月,移植珊瑚的存活率为45.5%。移植方法对于不同珊瑚种类具有不同效果,但没有一种方法能够对所有珊瑚的移植效果产生促进作用。虽然对于叶状蔷薇珊瑚(Montipora foliosa)和风信子鹿角珊瑚(Acropora hyacinthus)来说,适合的移植方法能够减缓其死亡速率,但并不能改变其死亡趋势。叶状蔷薇珊瑚和风信子鹿角珊瑚的移植个体呈现出高死亡率和明显的存活组织面积下降,而扁枝滨珊瑚(Porites andrewsi)和丛生盔形珊瑚(Galaxea fascicularis)死亡率和组织部分死亡率则优于前两者。扁枝滨珊瑚和丛生盔形珊瑚仅在一种移植方法中出现了存活组织面积明显增长。鹿角杯形珊瑚(Pocillopora damicornis)是移植珊瑚中唯一一种在所有移植方法上都呈现珊瑚平均存活面积增长的种类。实验结果说明在受到高度胁迫的海域进行珊瑚移植很难取得满意效果,珊瑚种类的选择对胁迫环境下的珊瑚移植效果具有决定性影响,而移植方法只能在部分程度上改善移植效果,但无法弥补鹿回头环境压力对敏感种类胁迫造成的影响。在鹿回头珊瑚礁需首先治理对珊瑚造成胁迫的因子,再进行珊瑚移植,并应优先考虑移植环境耐受性高的珊瑚种类。 相似文献
150.