粒間孔隙性 的英文怎麼說

中文拼音 [jiānkǒngxìng]
粒間孔隙性 英文
granular porosity
  • : Ⅰ名 (小圓珠形或小碎塊形物) small particles; grain; granule; pellet Ⅱ量詞(用於粒狀物)
  • : 間Ⅰ名詞1 (中間) between; among 2 (一定的空間或時間里) with a definite time or space 3 (一間...
  • : 名詞1 (縫隙; 裂縫) crack; chink; crevice 2 (空閑) gap; interval 3 (漏洞; 機會) loophole; op...
  • : Ⅰ名詞1 (性格) nature; character; disposition 2 (性能; 性質) property; quality 3 (性別) sex ...
  • 孔隙性 : porosity
  1. As an advanced materials preparation technology, spray - deposition has shown remarkable superiority in producing large - sized alloys and metal matrix composites. however, the spray deposeted preforms usually contain a certain quantity of porosity. besides, the oxide films on the surface of the particles lead to week metallurgic conjunction between the particles. in order to obtain an ideal structure and performance, the porous preforms need further densifying and plastical forming. in this paper, a new technology named wedge pressing was used to densify spray - deposeted 5a06 aluminium alloy, in which the large deformation can be obtained through the sum - up of local deformation and multi - step small deformation. this method can also solved the problems in traditional processing and greatly decreased the producing cost. what ’ s more, the reserch on the wedge pressing desification rules about the large - sized spray deposeted preforms was significant it was vital not only to the further densification of the prefoums but also to the further research on plastical deforming the research was also benefit to the industrialization an the application of the spray deposeted porous materials

    坩堝移動式噴射沉積技術作為一種先進的材料制備新技術,在制備大尺寸合金及金屬基復合材料方面具有顯著的優越。然而噴射沉積坯件特別是大型坯件通常存在一定量的,顆表面存在一定量的氧化膜,顆未能完全達到良好的冶金結合狀態,因此需要進行后續緻密化和塑變形才能獲得理想的組織和能。本文採用一種新型的楔形壓制工藝,即通過局部變形、多道次小變形累積實現大變形的緻密化加工方法,對噴射沉積多坯料進行后續緻密化和塑變形,很好地解決了傳統加工工藝的難題,大大降低了生產成本。
  2. The result is that this gas pool has simple structure, only forms a little nose - like structure at the district of fenghuangshan ; this pool belongs to delta front sub - facies sedimentary model, the underwater distributary channel and mouth bar is the better sedimentary microfacies ; the physical property of the reservoir is poor, the type of pore of the reservoir rock mostly are intergranular pore, intergranular solution hole and little are intercrystalline micropore ; the influential factors of pore structure and physical property are lithofacies, lithologic character and diagenesis ; the off - take potentia of all the testing well are deadly shortness, the wells have the worth of industrial recovery only under the condition of going through sand fracturing, and in the early of binging into production, the oil and sheath pressure drop rapidly, the production of the well drop rapidly

    研究認為該氣藏構造簡單,只在鳳凰山形成了一個小型的鼻狀構造;屬於三角洲前緣亞相沉積模式,水下分流河道和河口壩是有利的沉積微相;儲層物差,儲層巖石的類型主要有(內)溶及少量晶;影響蓬萊鎮組氣藏儲層結構及儲集的因素有巖相、巖條件及成巖作用;所有測試井自然產能都極低,必須經加砂壓裂后才有工業開采價值,且投產初期,油套壓下降較快,氣井產量下降迅速。
  3. Stereoscan photographs showed that both the inner and outer coating membranes of sapcus were formed by different size and shape micro particles of coating materials, which were closely stacked at random

    高吸水樹脂包膜尿素的內外膜均是由大小不一形狀不規則的包膜材料微無序緊密堆積,並由膠粘劑填充空膠聯而成,包膜疊層和疊層內有微小,它們是尿素溶出的通道。
  4. The variations in trace element contents and ratios may hold up a mirror to the lake - level fluctuations and climatic changes, which, in turn, have exerted a direct and important effect on the sequence stratigraphic development. collectively, the reservoir rocks from the yanchang formation consist dominantly of the delta front subfacies subaqueous distributary channel and channel - mouth bar microfacies and delta plain subfacies subaerial distributary channel microfacies fine - grained feldspar sandstones and siltstones. the reservoir rocks have been subjected to three stages of diagenetic and porosity evolution : ( 1 ) the porosity reduction by the mechanical compaction and chemical pressure solution during the early diagenetic stage ; ( 2 ) the porosity increase by the dissolution during the a substage of the late diagenetic stage, and ( 3 ) the porosity reduction by the cementation and filling during the b substage of the late diagenetic stage

    系統的儲層特徵研究表明,該區延長組儲層成因類型主要為三角洲前緣水下分流河道、河口砂壩及三角洲平原水上分流河道微相細長石砂巖、粉砂巖;儲層巖石經歷了壓實,膠結,溶蝕等成巖作用,歷經早成巖機械壓實和化學壓溶縮小期、晚成巖a亞期溶蝕作用擴大期及晚成巖a亞期( b亞期)膠結充填縮小期三個成巖-演化階段;儲層物總體上具有較低滲、低滲的特點,類型主要為、殘余內溶、晶及晶,裂縫不發育,儲集巖排驅壓力和中值壓力較高,結構類型以細小-微,微細喉-微喉型為主。
  5. Considering the viscous interaction between the kernel and the air inside the grain the paper shows the dynamic tortuosity function in grain. considering the thermal exchanges between the kernel and the air the paper shows the dynamic permeability function in grain

    考慮準多介質聲傳播中存在空氣與顆的粘滯力和慣力,推導出準多介質中動態曲折度函數表達式。
  6. The paper divided turbidite fan in deep water from long source into braided channel microfacies, inter - braided channel microfacies, medium fan over - belt microfacies, and external fan subfacies, and divided slump turbidite which related with delta into medium fan subfacies and external fan subfacies, and summed up 15 kinds of marking of subfacies and microfacies classification. at the same time, it formed a series of effective technology of analyzing turbidite source at the base of studying region geological which combined with analyzing the content change of terrigenous debris, with the found of logging facies, and with the ancient terrestrial magnetism test and other technology means under the guidance of three - dimensional model of turbidite which has been founded already and the flat surface feature of microfacies

    將遠源深水濁積扇劃分為辮狀水道微相、辮狀水道微相、中扇過渡帶微相和外扇亞相;將與三角洲有關的滑塌濁積扇劃分為中扇和外扇兩個亞相,並總結了濁積巖沉積劃分各種亞相、微相類型的十四種標志,分別為:巖石類型、層理類型、砂巖單層厚度、度結構特徵(度中值、分選、概率曲線) 、生物化石、儲層物度、滲透率) 、泥巖隔層特徵(泥巖單層厚度、層數、顏色) 、鮑瑪層序組合和自然電位曲線特徵。
  7. 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按成因、形態及大小可劃分為溶蝕、溶蝕洞、大型洞穴、風化裂、構造裂等5類,構成5種質有別的儲層,即洞穴型儲層、風化裂型儲層、構造裂型儲層、臺緣灘相顆灰巖溶蝕型儲層和地表殘積物裂(洞)型儲層。
  8. The model shows that : 1 ) structure of the stabilized soil from silt is formed by hydrates, which are generated by hardening agent hydration, wrapping and cementing soil particles and filling pores among the particles ; 2 ) structure of the stabilized soil formed from clayey soil is formed by the hydrates wrapping and cementing clay particle groups, filling pores among the groups, and squeezing and filling pores in the groups

    該模型認為:粉土固化土結構是由固化劑水化物充分包裹膠結土顆和填充土顆而構成;黏土固化土結構是通過固化劑水化物包裹膠結土團、填充土團、擠壓填充土團而構成。
  9. The paper analyzed sedimentary characteristics and depositional environment in t1f3 this region firstly, and on the grounds of establishing logical deposit pattern gave emphasis to make a study of distributing laws and spreading traits of the oolitic beach. because diagenesis is a vitally dominating factor that influenced oolitic beach reservoir nature in the region, the master diagenetic events of the reservoir in the lengthy geological history, as well as the influence to the pore abundance, was made a study of. the diagenetic stages and sequences were divided and the pore evolve pattern was established in the paper

    本論文首先分析了研究區飛三段的沉積特徵與沉積環境,在合理建立沉積相模式的基礎上重點研究了鮞灘(壩)的分佈規律和空展布特點;成巖作用是影響本區鮞灘儲集至關重要的控制因素,論文詳細研究了儲層在漫長地質歷史過程中所經歷的主要成巖事件及其對發育的影響,劃分了成巖階段與成巖演化次序,建立了演化模式並以建南構造為例進行了成巖相展布研究的嘗試;最後還在鮞灘儲層基本特徵研究的基礎上對飛三段儲層進行綜合評價與預測。
  10. Beginning with the analysis of the effects, which are brought by the application of only one kind of pore - former and some other operating factors ( such as sintering temperature, warmth retaining time and so on ), on the properties of the beads, e. g., porosity, strength, size distribution of the beads and pores size, etc., these effects are discussed in detail and the relationship between the factors is studied thoroughly. the use of mpf ( multi - pore - former ) is introduced for the first time, which is of the most importance and significance in this paper

    研究從造劑選用和燒結過程對顆率、機械強度、徑分佈及度分佈的影響入手,找出了造劑的種類及含量、燒結溫度以及保溫時等因素對最終所得產品顆能影響及它們之的相互關系,並首次提出將造劑復配使用來對填充法加以改進,無需擴處理,即能直接制備宏徑、高強度、小度、比表面大的多玻璃載體顆
  11. However, the spray deposited preforms usually contain more than 10vol. % porosity that is a great disadvantage for the mechanical properties. in order to prepare full density products of high mechanical performance, the porous preforms must suffer densification process

    然而噴射沉積材料通常存在一定量的,顆表面存在一定厚度的氧化膜,顆未能完全達到良好的冶金結合狀態,因此需要進行后續緻密化才能獲得理想的組織和能。
  12. This is the direct reason of bad reservoir property of sandstone, especially lower permeability. the influence and control factors of reservoirs include : deposition, diagenesis and tectogenesis. the deposition is the basic factor, it control the shape and distribution of sand body, and influence the type and the intensity of the diagenesis ; the diagenesis is the key factor, it control the process of pore evolvement, so the diagenesis control the sandstone ' s storage space and reservoir quality directly ; the fracture of the tectogenesis formation could improve the porosity and permeability of sandstone

    其中沉積作用是基礎,控制了儲集砂體的形態特徵和分佈范圍,同時由於不同沉積類型砂體在碎屑成分組成、泥質含量、顆度、砂體厚度、砂體內部的非均質介質的物理化學質等方面不盡相同,從而也影響著砂巖所經歷的成巖作用路徑、類型和強度,因此沉積作用是控制儲層發育的主導因素;成巖作用是關鍵,直接決定了砂巖的演化過程,從而決定了儲層內部儲集空特徵和儲集能;而構造作用形成的裂縫對改善砂巖的儲滲能具有一定作用。
  13. The laws between the composition, structure, quality of materials of lc - hpc is studied by means of sem, mip, and so on testing measures. the reaction of hydration and filling effect of mineral admixture not only reduces the proportion of pore of structure and sizes and odds directional crystal of the unfavorable crystal phases such as ch but also leads to the mining of pore size, so it the effect improves the weak structure of interface transition area

    應用sem 、 mip等測試手段,研究lc - hpc組分、結構與能之的影響規律,礦物摻合料的活、填充等效應,降低了混凝土結構率,細化了徑,減小了ch晶尺寸及定向結晶幾率,從而改善界面薄弱過渡區結構。
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