half-saturated 中文意思是什麼
half-saturated
解釋
半飽和的-
The air is half saturated.
空氣處於半飽和狀態。 -
Integral equations of vertical vibration ofan elastic circular plate on a fluid - saturated poroelastic half space
多孔飽和半空間上彈性圓板垂直振動的積分方程 -
The displacement field of dislocation on the half - space of two - phase saturated medium
兩相飽和介質半無限空間位錯位移場 -
The main achievements could be summarized as follows : 1 ) the dynamic response of the saturated, porous, elastic half - space is studied in this paper, and saturated soil is taken as elastic two - phase media
現將本文的主要工作簡單介紹如下：本文以飽和土為研究對象，在兩相介質為彈性介質等一些條件假定下，進行了飽和彈性半空間動力響應問題的研究。 -
In the dissertation, a systematic study on the 3 - d dynamic responding of transversely isotropic saturated half - space / layered saturated strata produced by harmonic loading and seismic loading and dynamic interaction of saturated soils - foundation ( circular plate ) based on biot ' s theory for fluid - saturated porous media and the model of elastic half - space
本文基於biot兩相介質波動理論，採用橫觀各向同性飽和半空間及橫觀各向同性飽和有限層地基模型，對飽和地基的三維動力響應及橫觀各向同性飽和地基?基礎（板）的動力相互作用進行了系統研究。 -
Fourthly, the solutions for non - axisymmetical dynamic responding of elastic circular plate ( thin and thick plate ) rested on transversely isotropic saturated half - space / layered ground subjected to arbitrary harmonic loading are presented. under the contact conditions, the problem leads to a pair of dual integral equations which describs the mixed boundary - value problem
首先建立直角坐標系下波動問題的狀態方程，經雙重fo吐er變換求解狀態方程后得到傳遞矩陣:利用遞矩陣給出直角坐標系下層狀橫觀各向同性飽和地基在任意分佈簡諧荷載作用下穩態動力響應的一般解。 -
Furthermore, the dual integral equations can be reduced to the fredholm integral equations of the second kind and solved by numerical procedure. at the end of this chapter, the numerical analysis for dynamic interaction characters of saturated half - space / layered ground and circular plate is evaluated. finally, the solutions for 3 - d dynamic responding of elastic rect
基於橫觀各向同性飽和半空間/有限層地基非軸對稱波動方程的通解，按混合邊值問題建立飽和地基與彈性圓板非軸對稱動力相互作用的積分方程，求解積分方程后得到橫觀各向同性飽和地基上圓板非軸對稱動力響應的一般解，並分析了飽和地基上圓薄板和中厚板振動的若干特徵。 -
As the weather grew warmer it was not sensibly worn away by the water ， nor broken up and floated off as in rivers ， but ， though it was completely melted for half a rod in width about the shore ， the middle was merely honeycombed and saturated with water ， so that you could put your foot through it when six inches thick ； but by the next day evening ， perhaps ， after a warm rain followed by fog ， it would have wholly disappeared ， all gone off with the fog ， spirited away
因為天氣更溫暖了，它不再給水沖掉，也不像河裡的冰那樣地浮動，雖然沿岸半桿闊的地方都已經溶化，可是湖心的依然像蜂房一樣，飽和著水，六英寸深的時候，還可以用你的腳穿過去；可是第二天晚上，也許在一陣溫暖的雨和緊跟著的大霧之後，它就全部消失，跟著霧一起走掉，迅速而神秘地給帶走了。 -
Using the displacement functions and the technique of double fourier transform, the governing differential equations for transversely isotropic saturated poroelastic media are easily solved and, the fourier transformed stress and displacement solutions coorespondingly are obtained. then, under the boundary conditions, the analytical solutions for half - space are presented
藉助位移函數及雙重fourier變換，研究了直角坐標系下橫觀各向同性飽和土的動力響應問題，得到了飽和半空間體在任意分佈的表面諧振荷載作用下穩態響應的一般解。 -
Methods 1 mr1 hybridoma was cultured in hollow fibre system. culture supernatant was harvested, then precipitated by half - saturated ammonia sulphate. mfm was purified by deae - sephacel ion exchange chromatography. mri concentration was measured by elisa
硫酸錢半飽和沉澱， oeae陰離子交換層析分離純化抗co40l單克隆抗體mri 。 pbs透析后， 505一隊ge檢測純化抗體的純度， eusa測定抗體濃度。 -
Abstract : the secular equations of rayleigh waves in a poroelastic half - space soil are developed by analyzing dynamic equation and continuous equation of poroelastic soil. ravleigh surface wave dispersion characteristics and its displacement as well as liquid pressure distributions in saturated half - space soil are discussed
文摘:通過對飽和土中波的運動方程及連續方程分析，推導了飽和土中瑞利波特徵方程，討論了半空間飽和土中瑞利波波速度的彌散特性，以及位移和孔壓分佈情況
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