No matter whether we consider it from the perspective of historical development or specific conditions of reality, the formation of the concept of human rights, especial- ly its process of playing the realistic role v...No matter whether we consider it from the perspective of historical development or specific conditions of reality, the formation of the concept of human rights, especial- ly its process of playing the realistic role via the concrete realization, has a direct and extremely close relationship with specific cultural values and historical heritages. Therefore, studies of human rights should not just remain at the abstract level of ＂from concept to concept.＂ On the contrary, we should further promote the sound development of the cause of human rights via concretizing this kind of studies.展开更多
In this study, a flume experiment was designed to investigate the characteristics of wave-induced pore water pressure in the soil of a silty seabed with different clay contents, soil layer buried depths and wave heigh...In this study, a flume experiment was designed to investigate the characteristics of wave-induced pore water pressure in the soil of a silty seabed with different clay contents, soil layer buried depths and wave heights respectively. The study showed that water waves propagating over silty seabed can induce significant change of pore water pressure, and the amplitude of pore pressure depends on depth of buried soil layer, clay content and wave height, which are considered as the three influencing factors for pore water pressure change. The pressure will attenuate according to exponential law with increase of soil layer buried depth, and the attenuation being more rapid in those soil layers with higher clay content and greater wave height. The pore pressure in silty seabed increases rapidly in the initial stage of wave action, then decreases gradually to a stable value, depending on the depth of buried soil layer, clay content and wave height. The peak value of pore pressure will increase if clay content or depth of buried soil layer decreases, or wave height increases. The analysis indicated that these soils with 5% clay content and waves with higher wave height produce instability in bed easier, and that the wave energy is mostly dissipated near the surface of soils and 5% clay content in soils can prevent pore pressure from dissipating immediately.展开更多
But in the non-capital market, the practices in some JVs have already broken the rule.For example, Dongfeng Yueda Kia. When it was established, Dongfeng and Yueda held25 percent shareholding respectively and Kia the r...But in the non-capital market, the practices in some JVs have already broken the rule.For example, Dongfeng Yueda Kia. When it was established, Dongfeng and Yueda held25 percent shareholding respectively and Kia the remaining 50 percent. In fact, theforeign side is the holder of the company.展开更多
文摘No matter whether we consider it from the perspective of historical development or specific conditions of reality, the formation of the concept of human rights, especial- ly its process of playing the realistic role via the concrete realization, has a direct and extremely close relationship with specific cultural values and historical heritages. Therefore, studies of human rights should not just remain at the abstract level of ＂from concept to concept.＂ On the contrary, we should further promote the sound development of the cause of human rights via concretizing this kind of studies.
基金financially supported by the National Fundamental Research Program of Ministry of Science & Technology,China (Grant No. 2010CB951202)
文摘In this study, a flume experiment was designed to investigate the characteristics of wave-induced pore water pressure in the soil of a silty seabed with different clay contents, soil layer buried depths and wave heights respectively. The study showed that water waves propagating over silty seabed can induce significant change of pore water pressure, and the amplitude of pore pressure depends on depth of buried soil layer, clay content and wave height, which are considered as the three influencing factors for pore water pressure change. The pressure will attenuate according to exponential law with increase of soil layer buried depth, and the attenuation being more rapid in those soil layers with higher clay content and greater wave height. The pore pressure in silty seabed increases rapidly in the initial stage of wave action, then decreases gradually to a stable value, depending on the depth of buried soil layer, clay content and wave height. The peak value of pore pressure will increase if clay content or depth of buried soil layer decreases, or wave height increases. The analysis indicated that these soils with 5% clay content and waves with higher wave height produce instability in bed easier, and that the wave energy is mostly dissipated near the surface of soils and 5% clay content in soils can prevent pore pressure from dissipating immediately.
文摘But in the non-capital market, the practices in some JVs have already broken the rule.For example, Dongfeng Yueda Kia. When it was established, Dongfeng and Yueda held25 percent shareholding respectively and Kia the remaining 50 percent. In fact, theforeign side is the holder of the company.
