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81.
Structural design of buried pipelines for severe earthquakes 总被引:1,自引:0,他引:1
In order to realistically assess the seismic risk of a pipeline system, the accurate estimate of the pipe strains which depend upon structural details, pipe material, properties of the surrounding soil, the nature of the propagating wave, etc. is critical. Emphasis in this study, therefore has been placed on the analysis of a structural strain for several types of piping elements unique to the buried pipeline and also the provision of a simplified design formula which can be used practically. The purpose of this study is (a) to define the slippage factor in order to estimate the decrease in pipe strain resulting from the slippage effect, (b) to propose a simplified method to evaluate the plastic deformation of the pipeline for severe earthquakes, and (c) to derive a practical design formula for the structural strains of bent pipes. 相似文献
82.
青藏高原中部降水稳定同位素变化与季风活动 总被引:14,自引:2,他引:14
根据1998年夏季中日GAME/Tibet项目在青藏高原中部进行的降水中稳定同位素研究结果以及相关的气象观测资料,分析了青藏高原中部夏季降水中δ^18O的变化规律。研究结果发现,青藏高原中部夏季降水中δ^18O的波动与大规模天气活动有关,而不是地方性的气象条件。该地区降水中δ^18O对水汽来源的变化以及水汽的输送过程十分敏感。夏季伴随西南季风进入高原南部的水汽形成的降水中δ^18O较低,而且季风活动越强,降水中δ^18O也越来低。从青藏高原北部而来的水汽或地方蒸发水汽形成的降水,其δ^18O值较高。 相似文献
83.
The far-infrared extinction spectra of fused silica grains with the size range from 1.8 m to 60 Å were measured. The spectra depend clearly on the grain size. For large grain sizes (from 1.8 m to 400 Å) the spectra show almost the –2 dependence ( is the wavelength), which resembles that of the bulk material. For fine grains (70 and 60 Å) the spectra are less steep, the wavelength dependence being –1. This grain size dependence of extinction spectra agrees essentially with the prediction of Seki and Yamamoto. 相似文献
84.
Bacterial biomass and production rate were measured in the surface (0–100 m) and mesopelagic layers (100–1,000 m) in the subarctic Pacific and the Bering Sea between July–September, 1997. Depth profiles were determined at stations occupied in oceanic domains including the subarctic gyres (western, Bering Sea, and Gulf of Alaska) and a boundary region south of the gyres. In the surface layer (0–100 m), both bacterial biomass and production were generally high in the western and Bering Sea gyres, with the tendency of decrease toward east. This geographic pattern was consistent with the dominant regime of phytoplankton biomass at the time of our survey. A significant portion of variation in bacterial production was explained by the concentration of chlorophyll a (r
2 = 0.340, n = 60, P < 0.001) and, to the greater extent, by the concentration of semilabile total organic carbon (SL-TOC = TOC at a given depth—TOC at 1,000 m, r
2 = 0.488, n = 59, P < 0.0001). Temperature significantly improved the regression model: temperature and chlorophyll jointly explained 60% of variation in bacterial production. These results support the hypothesis that bacteiral growth is largely regulated by the combination of temperature and the supply of dissolved organic carbon in subarctic surface waters. In the mesopelagic layer (100–1,000 m), the geographic pattern of bacterial production was strikingly different from the surface phytoplankton distribution: the production was high in the boundary region where the phytoplankton biomass was lowest. Bacterial growth appeared to be largely controlled by the supply of organic carbon, as indicated by the strong dependency of bacterial production on SL-TOC (r
2 = 0.753, n = 75, P < 0.0001). The spatial uncoupling between surface phytoplankton and mesopelagic bacterial production suggests that the supply rate of labile dissolved organic carbon in the mesopelagic zone does not simply reflect the magnitude of the particulate organic carbon flux in the subarctic Pacific. 相似文献
85.
The concentrations of total bacteria, bacterial aggregates and so-called heterotrophic bacteria were compared and discussed with special reference to the watermasses that vertically layered at the western North Pacific central region and the subarctic Pacific region.The concentrations of bacterial aggregates, having cells more than 25, were considerably uniform throughout the ocean depths. This was also shown indirectly by the measurements of size spectrum and organic constituents of particles, especially in the subsurface and deep watermasses. The so-called heterotrophic bacteria decreased in their concentration in deeper watermass, and the decrease was not obvious within each watermass but obvious among watermasses. 相似文献
86.
Extinction measurements were made for three kinds of amorphous carbon grains in the range 2100 -340 m. Absolute values of extinction coefficients from different sources vary by almost constant factors. Wavelength dependences of extinction curves show a –1 or less steep fall off, against a –2 or steeper fall off of graphite grains. Small humps are found around 6.3, 8, 13.3 and 90 m, although their origins are not yet clear. The infrared properties of amorphous carbon grains suggest that they could supply a significant amount of far-infrared emission noted in recent astronomical observations. 相似文献
87.
Magnetotelluric resistivity modeling for 3D characterization of geothermal reservoirs in the Western side of Mt. Aso, SW Japan 总被引:1,自引:1,他引:1
Hisafumi Asaue Katsuaki Koike Toru Yoshinaga Shinichi Takakura 《Journal of Applied Geophysics》2006,58(4):296
Geothermal reservoirs are usually located at a depth range of 2 to 5 km, so to efficiently utilize such resources an advanced prospecting method is needed to detect these deep geologic structures. This study aimed to three-dimensionally characterize geothermal reservoirs by a combination of Magnetotelluric (MT) survey, inversion analysis of apparent resistivity, and interpolation of the resistivity data obtained. The western side of Mt. Aso crater, southwest Japan, was chosen as the case study area. Three hot springs exist there and a fault is assumed to go in the direction connecting them. A MT survey was carried out at 26 sites and the data processed by a remote reference method to reduce artificial noises. Based on skewness and Mohr circle analyses of the impedance tensor, the local geologic structure at each site could be approximated as horizontally layered and therefore, a one-dimensional inversion analysis was applied to the MT raw data. The resultant resistivity column data were then interpolated by the three-dimensional optimization principle method. The resistivity distributions obtained clarified continuous conductors with especially low resistivity (less than 10 Ω·m) at the hot springs along the fault. Because the resistivity decreases largely with an abundance of clay minerals, the conductors could be considered to correspond with the cap rocks. Thus, two geothermal reservoirs, whose shapes were estimated to be pillar, were detected under the cap rocks in an elevation range of − 1000 to − 3000 m. By comparing the resistivity distributions with the temperature distributions based on fluid-flow calculations at a steady state using FEM, the validity of the location and dimension of the estimated reservoirs were confirmed. 相似文献
88.
Three-dimensional distribution analysis of phosphorus content of limestone through a combination of geostatistics and artificial neural network 总被引:1,自引:0,他引:1
One of the factors that determines the suitability of limestone for industrial use and its commercial value is phosphorus
(P) content, i.e., the weight percentage of phosphorus contained in small quantities of limestone. Because P content changes
locally, geostatistical techniques including semivariogram, ordinary kriging, and conditional indicator sequential simulation
were used in this study to identify the spatial correlation of P content and to estimate its three-dimensional distribution
in an open-pit mine. The P content data at 43,000 points of five different bench levels were analyzed. It was found that the
horizontal semivariograms produced by using the data at the same bench level show anisotropic behavior and are represented
by the sum of two spherical models with different ranges and sills. The twelve vertical semivariograms were also constructed
from P content in boring cores. After these semivariograms were classified into four types, a multilayered neural network
was applied to clarify the horizontal distribution of each one. One of the twelve semivariograms was assigned to an arbitrary
grid point in the study area by the criterion that its type is the same as the one estimated at the point and the borehole
site producing the semivariogram is the nearest to the point. With this technique, ordinary kriging combined with the semivariogram
of borehole data provided a proper estimation of P content in the depth direction. 相似文献
89.
Diurnal and inter-monthly variation of land surface heat fluxes over the central Tibetan Plateau area 总被引:4,自引:1,他引:3
Y. Ma S. Fan H. Ishikawa O. Tsukamoto T. Yao T. Koike H. Zuo Z. Hu Z. Su 《Theoretical and Applied Climatology》2005,80(2-4):259-273
Summary The energy and water cycle over the Tibetan Plateau play an important role in the Asian monsoon system, which in turn is a major component of both the energy and water cycles of the global climate system. Using field observational data observed from the GAME/Tibet (GEWEX (Global Energy and Water cycle Experiment) Asian Monsoon Experiment on the Tibetan Plateau) and the CAMP/Tibet (CEOP (Coordinated Enhanced Observing Period) Asia-Australia Monsoon Project (CAMP) on the Tibetan Plateau), some results on the local surface energy partitioning (diurnal variation, inter-monthly variation and vertical variation etc.) are presented in this study.The study on the regional surface energy partitioning is of paramount importance over heterogeneous landscape of the Tibetan Plateau and it is also one of the main scientific objectives of the GAME/Tibet and the CAMP/Tibet. Therefore, the regional distributions and their inter-monthly variations of surface heat fluxes (net radiation flux, soil heat flux, sensible heat flux and latent heat flux) are also derived by combining NOAA-14/AVHRR data with field observations. The derived results were validated by using the ground truth, and it shows that the derived regional distributions and their inter-monthly variations of land surface heat fluxes are reasonable by using the method proposed in this study. Further improvement of the method and its applying field were also discussed. 相似文献
90.
Environmental studies require multivariate data such as chemical concentrations with space-time coordinates. There are two
general conditions related to such data: the existence of correlations among the coregionalized variables and the differences
in numbers of data which occur because of insufficient data caused by measurement error or bad weather conditions. This study
proposes geostatistical techniques for space-time multivariate modeling that take into consideration these correlations and
data absences. These techniques consist of suitable modeling of semivariograms and cross-semivariograms for quantifying correlation
structures among multivariables and of extending standardized ordinary cokriging. The tensor product cubic smoothing surface
method is used for space-time semivariogram modeling. These methods are applied to the chemical component data of the Ariake
Sea, a typical closed sea in southwest Japan. In order to clarify environmental changes in the Ariake Sea, the concentration
data of four nutritive salts (NO2–N, NO3–N, NH4–N, and PO4–P) at 38 stations over 25 years are used as environmental indicators. For each of the kinds of data, there are spaces and
times for which there is no data available. The effectiveness of the modeling of space-time semivariograms and the high estimation
capability of the extended cokriging are demonstrated by cross-validation. Compared with ordinary kriging for a single variable,
multivariate space-time standardized ordinary cokriging can provide a more detailed concentration map of nutritive salts and
while elucidating their temporal changes over sparsely spaced data areas. In the space-time models by ordinary kriging, on
the other hand, smooth trends are obvious. 相似文献