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排序方式: 共有570条查询结果,搜索用时 218 毫秒
561.
Živana Ninčević Gladan Ivona Marasović Branka Grbec Sanda Skejić Mia Bužančić Grozdan Kušpilić Slavica Matijević Frano Matić 《Estuaries and Coasts》2010,33(2):376-383
Evaluation of a 45-year data set of primary production (PP), a 30-year data set of phytoplankton biomass, and a 51-year data
set of species composition shows an increase of phytoplankton biomass and abundance in the period from the mid-1980s to the
mid-1990s. Phytoplankton biomass showed bimodal seasonal cycles, with winter and spring maxima, which did not change over
the past 30 years. Diatoms were the most abundant functional group and they prevailed during the colder part of the year while
the dinoflagellate contribution to the phytoplankton community increased in the warmer period from May to August. Diatoms
showed a significant negative correlation with sea surface temperature (SST), while dinoflagellates were positively correlated
with SST. An increase of phytoplankton abundance, particularly dinoflagellate, in the period from the mid-1980s to the mid-1990s
coincided with years characterized by a high North Atlantic Oscillation (NAO) index. Primary production and chlorophyll a concentration in the spring period were negatively correlated with the NAO winter (DJFM) index, probably caused by increased
precipitation associated with a low or negative NAO index. PP in winter during the mixing period was positively related to
the NAO winter index associated with higher temperatures and dry conditions which brought more clear days and increased input
of solar radiation. 相似文献
562.
粗颗粒土的应力应变特性及其数学描述研究 总被引:22,自引:3,他引:19
大型三轴试验研究了粗颗粒土的应力应变特性及邓肯-张模型的适用性。试验结果表明粗颗粒土表现出明显的低围压下体胀高围压下体缩的体变性质,邓肯-张模型在描述粗颗粒土的体变特性方面存在不足。基于试验结果提出了新的体变描述公式,在未增加模型参数的条件下提出了邓肯-张模型的改进模型。采用改进模型对多种粗颗粒土三轴试验结果进行了预测,结果初步表明改进模型能够更好地模拟粗粒土的体变特性。 相似文献
563.
台风活动对青藏高原东北侧干旱的影响 总被引:24,自引:11,他引:13
应用1959 ̄1996的青藏高原东北侧58个站历年逐月降水量资料,历年(1950 ̄1996年)逐月西太平洋台风资料及500hPa高度格点资料,分析了台风活动对高原东北侧干旱的影响。结果指出:少台风活动年与干旱环流流型及高原东北侧干旱之间,多台风活动年与多雨环流流型及高原东北侧多雨之间,均存在着对应关系。 相似文献
564.
基于瑞典条分法的应变软化边坡稳定性评价方法 总被引:6,自引:0,他引:6
引入简化的应变协调方程,基于瑞典条分法的基本原理,提出一个新的能够考虑土的剪应力-应变关系的应变软化边坡稳定性简化分析方法。推导了该方法的计算公式,提出了具体算法并编制了计算程序,分析了不同应变软化特性的边坡稳定性。实际应用表明,该方法简单可靠、效率较高,计算所采用的分条数量和初始滑裂面位置对计算结果精度的影响均很小。应变软化边坡的安全系数介于基于峰值强度和残余强度的极限平衡条分法计算结果之间,具体数值不仅取决于土的抗剪强度指标,还与其剪应力-应变关系密切相关。 相似文献
565.
粗粒土与结构接触面三维本构关系及数值模型 总被引:4,自引:1,他引:3
基于试验结果,探讨了粗粒土与结构接触面的三维力学特性,该接触面在三维剪切时两个方向上的剪应力-应变关系表现出较强的耦合特性,但其主剪应变的大小只与主剪应力的大小有关。基于提出的接触面弹塑性损伤理论,建立了描述三维条件下接触面力学特性的本构模型及其数值格式。编制了有关程序,采用该模型对接触面的力学响应进行了预测。预测结果表明,建立的接触面三维本构关系及数值模型是合理和可行的,能够较好地反映包括剪切耦合特性在内的接触面主要力学特性。 相似文献
566.
We present a comprehensive analysis of the dynamics of Veritas family members located in a chaotic strip centeredat 3.174
AU. A total of 600 chaotic members of the family and their clones were integrated for 100 Myr, and the variation of the distance
with respect to the barycenter of the family have been computed forall of them. A simple classification of the prevailing
behaviors hasbeen introduced to help identify typical dynamical patterns and states that could affect an estimate of the upper
bound to the age of the family. We pointed out the importance of the temporary captures in thequasi-stable states, which occur
often enough to affect the statistical analysis of the exits. The results are compatible with the young age (<100 Myr) for
the family of Veritas, but we cannot say precisely how young it really is.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
567.
地理信息系统中时空多维数据可视化技术研究 总被引:23,自引:0,他引:23
将科学可视化技术应用于地理信息系统之中,增强地理信息系统对时空多维数据的显示,处理胆当前的研究热点之一。通过对现有地理数据组织,显示简便概述的基础上,提出一种基于体素的时空多维数据组织方式。并通过二维,三维显示及动画形式的研究,从技术上对科学可视化与地理信息系统的结合进行初步的探索。 相似文献
568.
Gaël Cazes David Fink Alexandru T. Codilean Réka-Hajnalka Fülöp Toshiyuki Fujioka Klaus M. Wilcken 《地球表面变化过程与地形》2020,45(2):424-439
We use cosmogenic 10Be and 26Al in both bedrock and fluvial sediments to investigate controls on erosion rates and sediment supply to river basins at the regional scale in the Kimberley, NW Australia. The area is characterised by lithologically controlled morphologies such as cuestas, isolated mesas and extensive plateaus made of slightly dipping, extensively jointed sandstones. All sampled bedrock surfaces at plateau tops, ridgelines, and in the broader floodplain of major rivers over the region show similar slow lowering rates between 0.17 and 4.88 m.Myr-1, with a mean value of 1.0 ± 0.6 m.Myr-1 (n=15), whilst two bedrock samples collected directly within river-beds record rates that are one to two orders of magnitude higher (14.4 ± 1.5 and 20.9 ± 2.5 m.Myr-1, respectively). Bedrock 26Al/10Be ratios are all compatible with simple, continuous sub-aerial exposure histories. Modern river sediment yield lower 10Be and 26Al concentrations, apparent 10Be basin-wide denudation rates ranging between 1.8 and 7.7 m.Myr-1, with a median value of 2.6 m.Myr-1, more than double the magnitude of bedrock erosion rates. 26Al/10Be ratios of the sediment samples are lower than those obtained for bedrock samples. We propose that these depleted 26Al/10Be ratios can largely be explained by the supply of sediment to river basins from the slab fragmentation and chemical weathering of channel gorge walls and plateau escarpments that result in diluting the cosmogenic nuclide concentration in river sediments measured at the basin outlets. The results of a mass-balance model suggest that ~60–90% of river sediment in the Kimberley results from the breakdown and chemical weathering of retreating vertical sandstone rock-walls in contrast to sediment generated by bedrock weathering and erosion on the plateau tops. This study emphasises the value of analysing two or more isotopes in basin-scale studies using cosmogenic nuclides, especially in slowly eroding post-orogenic settings. © 2019 John Wiley & Sons, Ltd. 相似文献
569.
Tiiu Elbra Petr Schnabl Kristýna Čížková Petr Pruner Šimon Kdýr Jacek Grabowski Daniela Reháková Andrea Svobodová Camille Frau William A.P. Wimbledon 《Studia Geophysica et Geodaetica》2018,62(2):323-338
Palaeo- and rock-magnetic investigations of the St Bertrand’s Spring (Le Ravin de Font de St Bertrand) locality in France were carried out in order to contribute to, and improve, the stratigraphy of the Jurassic-Cretaceous boundary interval. Magnetic susceptibility shows slightly diamagnetic behaviour in the lowermost part of the profile and an increase (paramagnetic) towards its middle and upper parts. Rock-magnetic measurements throughout the section show magnetite as the main magnetic fraction, together with traces of hematite. Additionally, thermal demagnetization indicates the presence of goethite. Our magnetostratigraphy indicates three normal/reversed polarity sequences; possibly encompassing the magnetozones M19r to the M17n. This suggests that the St Bertrand section straddles the Tithonian/Berriasian boundary and reaches the middle Berriasian sensu lato. 相似文献
570.