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811.
The fatigue assessment plays an increasing role for the offshore structural safety. Many fatigue assessment methods have been developed for this purpose. Among those methods, the time domain method is regarded as the most accurate method but less adopted in practice due to time consuming. In order to improve the efficiency of the time domain method, an innovative block partition and equivalence method of the wave scatter diagram is developed for offshore structural fatigue assessment. After the wave scatter diagram is partitioned into several blocks, the newly developed method, involves determination of the equivalent wave height, wave period and occurrence probability of the representative sea states based on modified energy equivalent principle. The equivalent wave period of the representative sea state is calculated via the spectral moment formula in which the equivalent spectral moments of zero and second order are obtained based on the weighted averaging principle. Combining with the determined wave period, the equivalent significant wave height can be determined by reversing the wave spectrum integral formula, where the equivalent wave energy of a divided block of the wave scatter diagram is modified by introducing a factor to compensate the effect of low- and high-amplitude cycles fatigue damage. The equivalent occurrence probability is equal to the summation of the original sea states’ occurrence probability within the divided block. The developed method has the advantage of preserving the stochastic characteristics of the short term sea states within the divided block during determining the representative sea state. At the same time the newly developed method has no limitation on block partition and can be applied on different offshore structure. Two structural models, a fixed mono-pile platform and a floating semi-submersible platform, are demonstrated in the numerical examples. Results indicate that the newly developed method is robust, computationally affordable, and accurate within engineering expectations. 相似文献
812.
现代黄河三角洲附近海域表层沉积物地球化学分区 总被引:1,自引:1,他引:0
对取自现代黄河三角洲附近海域的表层沉积物样品进行粒度分析和地球化学元素分析。研究表明,沉积物类型主要为砂质粉砂和粉砂,表层沉积物粒度由近岸向渤海东部大致为由粗变细再变粗的趋势,研究区大部分化学元素的含量和分布受沉积物粒度控制作用明显,即"元素的粒度控制律"。运用Q型聚类法对研究区表层沉积物常微量元素进行分析,并将其划分为3个地球化学分区,Ⅰ区主要集中在渤海中部海区,该区化学元素含量高。Ⅱ区主要集中在莱州湾,常微量元素含量比Ⅰ区稍低。Ⅲ区化学元素含量最低,根据地理位置不同又可分为3个亚区。3个分区反映了不同物源和水动力环境对研究区沉积物分布的影响。 相似文献
813.
The automated detection and mapping of landslides from Very High Resolution (VHR) images present several challenges related to the heterogeneity of landslide sizes, shapes and soil surface characteristics. However, a common geomorphological characteristic of landslides is to be organized with a series of embedded and scaled features. These properties motivated the use of a multiresolution image analysis approach for their detection. In this work, we propose a hybrid segmentation/classification region-based method, devoted to this specific issue. The method, which uses images of the same area at various spatial resolutions (Medium to Very High Resolution), relies on a recently introduced top-down hierarchical framework. In the specific context of landslide analysis, two main novelties are introduced to enrich this framework. The first novelty consists of using non-spectral information, obtained from Digital Terrain Model (DTM), as a priori knowledge for the guidance of the segmentation/classification process. The second novelty consists of using a new domain adaptation strategy, that allows to reduce the expert’s interaction when handling large image datasets. Experiments performed on satellite images acquired over terrains affected by landslides demonstrate the efficiency of the proposed method with different hierarchical levels of detail addressing various operational needs. 相似文献
814.
815.
The Yalu Tsangpo River basin is a typical semi-arid and cold region in the Qinghai-Tibet Plateau, where significant climate change has been detected in the past decades. The objective of this paper is to demonstrate how the regional vegetation, especially the typical plant types, responds to the climate changes. In this study, the model of gravity center has been firstly introduced to analyze the spatial-temporal relationship between NDVI and climate factors considering the time-lag effect. The results show that the vegetation grown has been positively influenced by the rainfall and precipitation both in moving tracks of gravity center and time-lag effect especially for the growing season during the past thirteen years. The herbs and shrubs are inclined to be influenced by the change of rainfall and temperature, which is indicated by larger positive correlation coefficients at the 0.05 confidence level and shorter lagging time. For the soil moisture, the significantly negative relationship of NDV-PDI indicates that the growth and productivity of the vegetation are closely related to the short-term soil water, with the correlation coefficients reaching the maximum value of o.81 at Lag 0-1. Among the typicalvegetation types of plateau, the shrubs of low mountain, steppe and meadow are more sensitive to the change of soil moisture with coefficients of -0.95, -0.93, -0.92, respectively. These findings reveal that the spatial and temporal heterogeneity between NDVI and climatic factors are of great ecological significance and practical value for the protection of eco-environment in Qinghai-Tibet Plateau. 相似文献
816.
在频域中分别使用Rankine面元法和去奇点Rankine面元法(desingularized-Rankine panel method,简称DRPM)快速求解有航速船舶耐波性问题。使用两种不同的线性化方式:叠模流线性化法(double-body flow,简称DB)和均匀流线性化方法(Neumann-Kelvin,简称NK)计算了Wigley I、Wigley III和S175在有航速时船舶的水动力系数、波浪激励力和运动响应。两种线性化方法的计算结果与试验结果进行了比较,研究表明:使用Rankine面元法和去奇点Rankine面元法计算的结果相差不大,且与NK法相比使用DB法计算的结果和试验值更吻合,尤其是非对角线上交叉耦合水动力系数A35,B35,A53,B53的计算结果。运动响应对于边界条件线性化方式比较敏感,尤其是垂荡运动,在船共振频率附近,运动受到的影响最明显。 相似文献
817.
元胞空间分区及其对GeoCA模型模拟精度的影响 总被引:1,自引:0,他引:1
采用双约束空间聚类方法对元胞空间进行分区,在此基础上对不同的分区分别求取元胞转换规则,从而提高
元胞自动机的模拟精度。以杭州市土地利用变化为例,采用本文提出的基于双约束空间聚类的分区元胞自动机模型对
研究区域2000年—2005年的土地利用变化进行模拟,并利用逐点对比法和Moran I指数对模拟结果进行精度评估。结果
表明:(1)采用双约束空间聚类算法对元胞空间进行分区,可以保证同一分区内的元胞既在空间上邻近,又具有相对一
致的非空间属性信息,分区效果较好;(2)与不分区元胞自动机模型和基于空间聚类的分区元胞自动机模型相比,双约
束空间聚类元胞自动机模型具有较高的模拟精度,尤其是在空间形态和整体结构上具有较好的模拟效果。 相似文献
818.
Partial melting has been shown to be an important mechanism for intracrustal differentiation and granite petrogenesis. However, a series of compositional differences between granitic melt from experiments and natural granites indicate that the processes of crustal differentiation are complex. To shed light on factors that control the processes of crustal differentiation, and then the compositions of granitic magma, a combined study of petrology and geochemistry was carried out for granites (in the forms of granitic veins and parautochthonous granite) from a granulite terrane in the Tongbai orogen, China. These granites are characterized by high SiO2 (>72 wt%) and low FeO and MgO (<4 wt%) with low Na2O/K2O ratios (<0.7). Minerals in these granites show variable microstructures and compositions. Phase equilibrium modelling using P–T pseudosections shows that neither anatectic melts nor fractionated melts match the compositions of the target granites, challenging the conventional paradigm that granites are the crystallized product of pure granitic melts. Based on the microstructural features of minerals in the granites, and a comparison of their compositions with crystallized minerals from anatectic melts and minerals in granulites, the minerals in these granitoids are considered to have three origins. The first is entrained garnets, which show comparable compositions with those in host granulites. The second is early crystallized mineral from melts, which include large plagioclase and K-feldspar (with high Ca contents) crystals as well as a part of biotite whose compositions can be reproduced by crystallization of the anatectic melts. The compositions of other minerals such as small grained plagioclase, K-feldspar and anorthoclase in the granites with low Ca contents are not well reconstructed, so they are considered as the third origin of crystallized products of fractionated melts. The results of mass balance calculation show that the compositions of these granites can be produced by mixing between different proportions of crystallized minerals and fractionated melts with variable amounts of entrained minerals. However, the calculated modal proportions of different crystallized minerals (plagioclase, K-feldspar, biotite and quartz) in the granites are significantly different from those predicted by melt crystallization modelling. Specifically, some rocks have lower modes of biotite and plagioclase, whereas others show lower K-feldspar modes than those produced by melt crystallization. This indicates that the crystallized minerals would be differentially separated from the primary magmas to form the evolved magmas that produce these granites. Therefore, the crystal entrainment and differential melt-crystal separation make important contributions to the composition of the target granites. Compared with leucogranites worldwide, the target granites show comparable compositions. As such, the leucogranites may form through the crystal fractionation of primary granitic magmas at different extents in addition to variable degrees of partial melting. 相似文献
819.
西太平洋暖池区的海气通量及整体交换系数 总被引:3,自引:1,他引:2
根据西太平洋海域弱风、高温、潮湿的大气状态特征,提出了在光滑面存在粘性副层气流中的廓线的层结订正方案。用此模式对西太平洋暖池区TOGACOAREIOP期间,在向阳红5号船(2°S,154°E)获取的海面风、温、湿梯度资料进行了处理。计算结果显示西太平洋暖池区贴水层气流中不稳定层结占50%-80%,其中很不稳定的占10.3%;该海区海气通量和整体交换系数受层结影响远大于受风速的影响;海气通量和整体交换系数随不稳定程度增加而增大,在相同风速下量值可相差4倍以上;其变化范围为0.3×10-3—3.2×10-3。由此可见,层结的影响使它们的变化大于其它海区的结果。在u10=0-10m/s范围内,中性化整体交换系数平均为CDN=1.2×10-3,CHN=1.14×10-3,CEN=1.19×10-3,与Large和Pond(1981,1982)不稳定条件的研究结果相差无几。 相似文献