This paper presents a brief review of the results on the interaction between waves and muddy bottom obtained during the last decade including the results obtained by the author at the Coastal Engineering Laboratory of Tianjin University. 相似文献
Crustal structures of nine broad tectonic units in China, except the Tarim craton, are derived from 18 seismic refraction
profiles including 12 geoscience transects. Abundances of 63 major, trace and rare earth elements in the upper crust in East
China are estimated. The estimates are based on sampling of 11 451 individual rock samples over an area of 950 000 km2, from which 905 large composite samples are prepared and analyzed by 13 methods. The middle, lower and total crust compositions
of East China are also estimated from studies of exposed crustal cross sections and granulite xenoliths and by correlation
of seismic data with lithologies. All the tectonic units except the Tarim craton and the Qinling orogen show a four-layered
crustal structure, consisting of the upper, middle, upper lower, and lowermost crusts. P-wave velocities of the bulk lower
crust and total crust are 6.8–7.0 and 6:4–6.5 km/s, respectively. They are slower by 0.2–0.4 km/s than the global averages. The bulk lower crust is suggested to be
intermediate with 58% SiO2 in East China. The results contrast with generally accepted global models of mafic lower crusi. The proposed total crust
composition in East China is also more evolved than previous estimates and characterized by SiO2=64%, a significant negative Eu anomaly (Eu/Eu* = 0.80), deficits in Sr and transition metals, a near-arc magma La/Nd ratio
(3.0), and a calculatedμ(238U/204Pb) value of 5. In addition, it has the following ratios of element pairs exhibiting similar compatibility, which are identical
or close to the primitive mantle values: Zr/Hf=37, Nb/Ta=17.5, Ba/Th=87, K/Pb=0.12x104, Rb/Cs=25, Ba/Rb=8.94, Sn/Sm=0.31, Se/Cd=1.64, La/ As=10.3, Ce/Sb=271, Pb/Bi=57, Rb/TI=177, Er/Ag=52, Cu/Au=3.2×104, Sm/Mo=7.5, Nd/W=40, CI/Li=10.8, F/Nd=21.9, and La/B=1.8.
Project supported by the National Natural Science Foundation of China (Grant Nos. 49625305, 49573183, 49673184, 49794043),
the State Comission of Education, the Ministry of Geology and Mineral Resources of China (Grant No. 850514), the Open Laboratory
of Constitution, Interaction and Dynamics of the Crust-Mantle System, and the Alexander-von-Humboldt Foundation of Germany. 相似文献
This study was conducted to evaluate the effect of replacing soybean meal (SBM) by low protein floc meal (LPFM; 24% CP) in tilapia diets on growth performance, feed utilization and fish chemical composition. Three isonitrogenous and isocaloric diets were formulated; control diet (C; without LPFM), FM 25 (25% of SBM protein was substituted by LPFM) and FM 50 (50% of SBM protein was substituted by LPFM). Nine 55l circular plastic tanks were stocked by 12 fish to form three experimental groups. No differences in tilapia performance were observed between the control and the FM 25 diet. Chemical composition of fish did not differ significantly among treatments except for protein and selenium contents where the highest values were recorded in the control treatment. The highest mineral content was recorded in floc collected from the control tanks, while calcium content showed its highest value in floc collected from FM 50 effluent. These data indicate that replacing soybean meal with LPFM up to 25%, had no negative effect on growth performance and potentially may improve the system sustainability. Meanwhile, the adverse effect of more inclusion of LPFM in tilapia diet may be attributed to the higher content of ash. In other word, minerals seem to cause more energy utilization in fish fed floc meal since it is needed to maintain osmotic homeostasis.
A series of axi-symmetry models using finite element analyses were performed to investigate the behavior of circular footings
over reinforced sand under static and dynamic loading. Geogrid was modeled as an elastic element and the soil was modeled
using hardening soil model which use an elasto-plastic hyperbolic stress–strain relation. Several parameters including number
of geogrid layers, depth to the first geogrid layer, spacing between layers and load amplitude of dynamic loading are selected
in this paper to investigate the influence of these parameters on the performance of reinforced systems under both static
and dynamic loads. The numerical studies demonstrated that the presence of geogrid in sand makes the relationship between
contact pressure and settlement of reinforced system nearly linear until reaching the failure stage. The rate of footing settlement
decreases as the number of loading cycles increases and the optimum values of the depth of first geogrid layer and spacing
between layers is found 20% of the footing diameter. Some significant observations on the performance of footing-geogrid systems
with change of the values of parametric study are presented in this paper. 相似文献