溶洞孔隙 的英文怎麼說
中文拼音 [róngdòngkǒngxì]
溶洞孔隙
英文
cavern porosity-
Cavernous porosity can take the equidimensional form of vugs or follow channels, but the void dimensions are measurable in meters.
溶洞孔隙可呈等尺度的溶孔形態，或者呈溶溝形態，但空間大小是以米度量的。The intense eluviation and weathering of soil with groundwater and run - off result in the enhancing of capacity of transference of some elements, such as si, al, fe, mn. the chemical reactions of the colloid particles in the soil water make those crannies or holes filled by some epigenetic clay minerals and quartz. then a great deal of white reticulate clay comes into being in the quaternary laterite of the dongting basin
地下水和地表水強烈的淋溶作用使土壤中硅鋁鐵錳等元素的遷移能力增強，土壤膠體粒子之間的化學反應，使得這些孔隙空間在後期逐漸被次生黏土礦物和石英所充填，最終，在洞庭盆地第四系紅土地層中形成大量的蠕蟲狀和根狀白色網紋。The diageneses which are destructive to the reservoirs are mainly the filling of minerals in secondary pores, the fissures and the dissolved caverns
對儲層起到破壞作用的主要是充填作用，表現為次生溶蝕孔隙、裂縫、溶洞中充填自生礦物，它們的包裹體測溫數據證明充填作用發生在埋藏時期。The favorable reservoir spaces in the carbonate rock could be divided into five types according to their origin, configuration and size, i. e., solution fissure, solution hole, cave, erosional fissure and structural fissure, which form five different reservoirs including cave - type reservoir, erosional fracture reservoir, structural fissure reservoir, and solution pore marginal beach grainstone reservoir
而下奧陶統灰巖段儲集和生產油氣的有效儲滲空間按成因、形態及大小可劃分為溶蝕孔隙、溶蝕孔洞、大型洞穴、風化裂隙、構造裂隙等5類，構成5種性質有別的儲層，即洞穴型儲層、風化裂隙型儲層、構造裂隙型儲層、臺緣灘相顆粒灰巖溶蝕孔隙型儲層和地表殘積物裂隙孔隙（洞）型儲層。Seismic wave field feature of ordovician carbonate karst reservoir ( cave, reef, hole, crack and cranny ) in tahe oil field is the difference magnitude diffraction wave over weak reflection amplitude, so, the diffraction wave exact imaging and fidelity amplitude processing is the basic of carbonate karst reservoir study
摘要塔河油田巖溶儲集體（洞穴、礁灘、孔洞、裂縫或裂隙等）的地震波場特徵是弱反射背景之上的強弱不同的繞射波，因此，繞射波準確歸位成像和振幅保持是研究巖溶儲集體的基礎。Observation of drilling cores and casting - sections and the characters of pore structures and permeability of the matrix of the lower - ordovician carbonate in comparing with the lower limit of a reservoir for matrix reveal that the porosity, permeability, maximum pore diameter, saturation and median throat diameter in the matrix with undeveloped fissures, holes and solution pores are far lower than those of a reservoir limit although some micro - pores are developed in the matrix which therefore has no capacity of storing and producing oil - gas
摘要通過鉆井巖心和鑄體薄片觀察，根據下奧陶統灰巖基質的孔滲特徵和孔隙結構特徵，並與基質作為儲層的下限對照裂隙、洞穴和溶蝕孔洞不發育的灰巖基質，發現盡管有微孔隙的發育，但其孔隙度、滲透率、最大孔喉半徑、飽和度、中值喉道半徑等參數值遠低於儲層下限值，基本不具備儲集和生產油氣的意義。The cross - hole electromagnetic wave - penetrating method has particular advantages in detecting ground fracture zones and caves
摘要跨孔電磁波透視在探測地下裂隙帶、溶洞等方面具有獨到之處。The rock mass is made up with rock and cracks, however, in the carst region " s the rock mass also include the hole and cave develop for corrosion. generally, the rock is impermeable, and the permeability of the rock mass depends on the permeability of cracks
巖體是由巖塊及其裂隙組成的，對巖溶地區的巖體尚包括沿結構面發育而成的溶蝕孔、洞，一般來說，巖石的透水性很小，巖體的透水性主要決定於裂隙的滲透性大小。Induced porosity is typified by fracture development as found in some shales and limestones and by the rugs or solution cavities commonly found in limestones
次生孔隙度是以某些頁巖和石灰巖的裂縫和石灰巖中的巖穴和溶洞為代表。分享友人