溶解變形作用 的英文怎麼說
中文拼音 [róngjiěbiànxíngzuòyòng]
溶解變形作用
英文
solution deformation-
The unstable solid solution would disintegrate and transform into carbide phases in these systems of sisocso, tisocso and zrsocso, based on the increase of free energy introduced by the effect mechanical alloying. for the system of wsocso, the solid solution had not transformed into tungsten carbides but an amorphous phase, which was different from those systems. the exist of fe in these experiments, which came from the abrasion of ball - milling tool because of the higher hardness of w and w - c solid solution, would induce the crystalline - to - amorphous phase transformation during milling
C50球磨體系中，繼續球磨時，不穩定的固溶體在機械合金化作用下，由於體系能量提高，會發生分解相變，從而可以形成碳化物；對于w扣c50球磨體系， w ? c固溶體具有較高的硬度，磨削不銹鋼質的球磨介質和球磨容器，而引入雜質，其中fe會促使固溶體向非晶相轉變。Rab7 mediates transport of proteins from early endosome to late endosome or fusion of early endosome with late endosome, while rab9 mediates the retransport of m6pr from late endosome to trans - golgi network. the gtp / gdp - binding ability and intrinsic gtpase activity of rab proteins make them exist in rab - gtp or rab - gdp status. the switching of rabs between gtp - bound ( active ) and gdp - bound ( inactive ) forms requires other regulatory proteins, including guanosine exchange factor ( gef ), gdp dissociation inhibitor ( gdi ) and gtpase activating protein ( gap ), and lays the foundations of rab function
Rab蛋白家族成員和其他小g蛋白一樣可以結合gtp gdp ，在自身gtp酶的水解作用和其他蛋白（ gef 、 gap 、 gdi ）的調節作用下發生gtp （活化狀態）和gdp （無活性）結合形式的轉變；同時rab蛋白也在膜結合性（ membrane - bound ）和胞漿可溶性（ cytosolic ）之間變化，一個變化過程對應著一個功能循環，接著rab蛋白回到初始狀態參與下一個循環。Main content in simulation is the spatio - temporal evolution of the set of descriptive variables characterizing tectonic mineralization state under coupling of various processes as following : ( 1 ) variables related to forming and property of ore - forming fluid, such as dissolution rate of minerals ( include metal minerals ) in rock, concentration and saturation of aqueous species in fluid, temperature, pressure, and ionic strength etc. ; ( 2 ) variables related to structural deformation and fluid flow, such as stress, deformation rate, fracture network, porosity, fracture permeability ; ( 3 ) variables related to precipitation and mineralization, such as nucleation rate of gangue and metal minerals, accumulation precipitation of various minerals, etc. ; ( 4 ) spatio - temporal coupling relation of various variables above, such as the coupling relationship between spatio - temporal evolution of fracture permeability and flow and focus of fluid and ore - forming
模擬的主要內容是在各種過程耦合作用下，以下描述構造成礦體系的主要變量的時空演化：與成礦流體的形成和性質有關的變量，如地層中礦物（包括成礦物質）的溶解速率、流體中各組分的濃度與飽和度、流體溫度、壓力、離子強度等；與構造變形和流體運移有關的各變量，如應力與變形速率、巖石孔隙度、構造（斷裂）滲透率等；與沉澱成礦有關的變量，如礦物（金屬礦物和脈石礦物）的成核速率、各礦物的沉澱量等；上述各有關變量間的時空耦合關系，如斷裂滲透率時空演化與流體流動、匯聚和成礦的耦合關系等。( 4 ) which deformation behavior of cementite lamellae in pearlite colonies is closely related to the stress state of cementite which significantly depends on cementite thickness and orientation, especially on cementite thickness. ( 5 ) the lamellar cementite undergoes partial dissolution on the present deformation. the thermodynamical destability of cementite is attributed to a large number of defect in cementite introduced by severe plastic deformation providing evidence for cementite dissolution
而滲碳體的應力狀態主要是與滲碳體的片層厚度和取向密切相關的，其中滲碳體的厚度起決定性作用； （ 5 ）本實驗變形條件下，滲碳體出現了部分溶解的現象，這是由於強烈塑性變形而在滲碳體中引入大量的缺陷導致其處于高能不穩定狀態從而促使了滲碳體溶解。分享友人