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间歇式沥青搅拌设备称量系统设计 总被引:3,自引:4,他引:3
余建辉 《筑路机械与施工机械化》2004,21(7):17-18
从沥青搅拌设备供料系统到称量系统机构及控制系统设计,全面阐述了影响沥青搅拌设备称量精度的因素及在实际应用中的合理解决办法,并提出沥青搅拌设备称量精度指标要求. 相似文献
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立柱是大面积基坑水平支撑体系的重要组成部分,而在基坑围护设计施工时,采用型钢结合水泥土搅拌桩作为立柱桩的情况较为少见。为此,介绍了某SMW工法桩围护基坑工程中,型钢结合水泥土搅拌桩作为立柱桩的应用情况,以期为类似工程提供一定参考。 相似文献
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John H. Simpson J.A. Mattias Green Tom P. Rippeth Thomas R. Osborn W. Alex M. Nimmo-Smith 《Journal of Marine Systems》2009,77(4):428
We report on an intensive campaign in the summer of 2006 to observe turbulent energy dissipation in the vicinity of a tidal mixing front which separates well mixed and seasonally stratified regimes in the western Irish Sea. The rate of turbulent dissipation ε was observed on a section across the front by a combination of vertical profiles with the FLY dissipation profiler and horizontal profiles by shear sensors mounted on an AUV (Autosub). Mean flow conditions and stratification were obtained from a bed mounted ADCP and a vertical chain of thermistors on a mooring. During an Autosub mission of 60 h, the vehicle, moving at a speed of ~ 1.2 m s− 1, completed 10 useable frontal crossings between end points which were allowed to move with the mean flow. The results were combined with parallel measurements of the vertical profile of ε which were made using FLY for periods of up to 13 h at positions along the Autosub track. The two data sets, which show a satisfactory degree of consistency, were combined to elucidate the space–time variation of dissipation in the frontal zone. Using harmonic analysis, the spatial structure of dissipation was separated from the strong time dependent signal at the M4 tidal frequency to yield a picture of the cross-frontal distribution of energy dissipation. A complementary picture of the frontal velocity field was obtained from a moored ADCP and estimates of the mean velocity derived from the thermal wind using the observed density distribution. which indicated the presence of a strong (0.2 m s− 1) jet-like flow in the high gradient region of the front. Under neap tidal conditions, mean dissipation varied across the section by 3 orders of magnitude exceeding 10− 2 W m− 3 near the seabed in the mixed regime and decreasing to 10− 5 W m− 3. in the strongly stratified interior regime. The spatial pattern of dissipation is consistent in general form with the predictions of models of tidal mixing and does not reflect any strong influence by the frontal jet. 相似文献
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We use hydrographic, current, and microstructure measurements, and tide-forced ocean models, to estimate benthic and interfacial mixing impacting the evolution of a bottom-trapped outflow of dense shelf water from the Drygalski Trough in the northwestern Ross Sea. During summer 2003 an energetic outflow was observed from the outer shelf ( 500 m isobath) to the 1600 m isobath on the continental slope. Outflow thickness was as great as 200 m, and mean speeds were 0.6 m s− 1 relative to background currents exceeding 1 m s− 1 that were primarily tidal in origin. No outflow was detected on the slope in winter 2004, although a thin layer of dense shelf water was present on the outer shelf. When the outflow was well-developed, the estimated benthic stress was of order one Pascal and the bulk Froude number over the upper slope exceeded one. Diapycnal scalar diffusivity (Kz) values in the transition region at the top of the outflow, estimated from Thorpe-scale analysis of potential density and measurements of microscale temperature gradient from sensors attached to the CTD rosette, were of order 10− 3−10− 2 m2 s− 1. For two cases where the upper outflow boundary was particularly sharply defined, entrainment rate we was estimated from Kz and bulk outflow parameters to be 10− 3 m s− 1 ( 100 m day− 1). A tide-forced, three-dimensional primitive equation ocean model with Mellor-Yamada level 2.5 turbulence closure scheme for diapycnal mixing yields results consistent with a significant tidal role in mixing associated with benthic stress and shear within the stratified ocean interior. 相似文献
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针对海相软土含水量大、粘粒含量高的特点,采用水泥土湿喷桩复合地基处理方式。通过对湿喷桩处理段的大量检测结果进行统计分析,得出的一些结论对于高速公路的软基处理具有实际意义。 相似文献
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Stig Skreslet Terje Doksr⊘d Morten Frogh Morten Krogstad Ketil Olsen 《Coastal management》2013,41(2):141-152
A simple numerical model was applied to distinguish permanently oxygenated marine sill basins from periodically anoxic basins in Nordland County, northern Norway. Input data are sill depth, width of the tidal channel, sea surface area, and tidal range. The model produces a Topography Tidal Factor (TTF) that seems to be an adequate index correlating with empirical field data when sills have saddle depths <30 m. The depth of the pycnocline, and the oxygen concentration of the basin water increases logarithmically with the calculated TTF value toward an asymptotic level. At TTF ≥0.02 basins are mostly well-oxygenated and have a permanent fauna of epibenthic and hyperbenthic animals. Basins with TTF <0.02 may become anoxic each autumn, which permanently prevents establishment of communities with multi-annual sessile benthos. Low oxygen concentration may also cause seasonal variation in the occurrence of motile species. In tidal channels, the abundance of bivalves and fish, as well as the biodiversity in general, probably increases with TTF. The applied method may be universally valid in regions shaped by glacial erosion but needs to be further developed by more detailed studies. 相似文献