溶解作用 的英文怎麼說

中文拼音 [róngjiězuòyòng]
溶解作用 英文
dissolution
  • : 動詞(溶化; 溶解) dissolve
  • : 解動詞(解送) send under guard
  • : Ⅰ動詞1 (使用) use; employ; apply 2 (多用於否定: 需要) need 3 (敬辭: 吃; 喝) eat; drink Ⅱ名...
  • 溶解 : dissolve; dissolution; solution; lysis; solvus; resolution; decomposition; resolving; solving; fu...
  1. The sedimentation is the foundation, affecting the basic pattern of the reservoir, and the sedimentary facies zones beneficial to the formation and evolution of the reservoir includes platform edge bank facies, introplatform point beach facies and acclivity sedimentary facies, etc. ; the diagenesis is the key factor, determining the pattern and scope of the final distribution of the reservoir and being of great influence on reservoir structure, and the diagenesis of promoting the formation of storage rooms is mainly the dissolution occurred during hypergene stage and burial stage ; and the tectonism is the condition of influencing the connectivity among various reservoir bodies and among the storage rooms within a single reservoir body

    該套儲層是在4億年左右的地質歷史中,由沉積、成巖和構造相互影響而形成的最終成果:其中沉積是基礎,影響著儲層的基本形態,有利於儲層形成與演化的沉積相為臺地邊緣灘、臺內點灘和上斜坡等沉積相帶;成巖是關鍵,決定了儲層的最終分佈形態和范圍,對儲層結構的影響至關重要,促進儲集空間形成的成巖主要有表生期和埋藏期的溶解作用;構造是條件,影響著各儲集體之間以及單一儲集體內部儲集空間的連通情況。
  2. The degradation or assimilation of fatty materials is often restricted because of their relative insolubility.

    脂肪物質因其度低,分和吸收常受限制。
  3. For electrodeposition by dc methods, the metals deposite uninterrupted and the particles were also embeded uninterrupted into the coatings ; for electrodeposition by pc method, the particles with biggish volume were desorbed from the coatings and returned to the electrolyte again owing to the presence of pulse interval ; for electrodeposition by prc method, the particles carried positive charges are much more easy to desorb from the coatings owing to the effecf of reverse pulse current combined with pulse interval, in addition, the reverse pulse current also could dissovle the metals, further accelerates the desorption of particles, thus the particles size embeded in the coatings by prc method is the least

    直流電沉積時,基質金屬的沉積連續進行,粒子在電極表面不間斷嵌入鍍層;單脈沖電沉積由於脈沖間歇的存在使得具有較大體積的粒子會脫附,重新回到液中;採周期換向脈沖時,反向脈沖電流使表面荷正電的較大的粒子更易從電極表面脫附,同時,反向脈沖電流對基質金屬的溶解作用,也會促進粒子的脫附,因此鍍層中復合粒子尺寸最小。隨著鍍層中粒子復合量的增加,三種鍍層的晶粒都明顯細化,說明al _ 2o _ 3的存在阻止了晶粒的長大,提高了電沉積過程中晶核的形成速率。
  4. Sulfid also can be regarded as a marker of the action of sulfur bacteria. 8 ) based on research results, author postulated that early generation of hydrocarbons is closely related to the action of sulfur bacteria. many kind of algae such as dinoflagellates, diatom, prynesiophytes etc have rich biological lipids which has lower polymerization

    6 、從未熟一低熟源巖生烴組分及其演化、可有機質轉化生烴等方面,探討了未熟一低熟油的形成機制,提出本區未熟一低熟油氣的形成是低活化能的富氫腐泥組分受到硫細菌早期低溫降的結果。
  5. Despite this solution, the volume of accumulated oceanic pelagic carbonate is staggering because of the size of the oceans.

    盡管有這種溶解作用,但由於海洋的巨大體積,深海碳酸鹽的堆積量仍然是令人驚愕的。
  6. Brown yellow or red brown molding powder, has weak special smell, can dissolve in water and ethanol, not dissolve in ethyl ether and chloroform, good stability, no stimulate, has strong extermination effect to bacteria, virus, epiphyte, mildew and sporule. application

    由於pvpp的高分子量和交聯結構,不於水但遇水能迅速將水引入,促使其網路結構膨脹產生崩,所以pvpp是醫藥上廣泛應於片劑顆粒劑及膠囊劑的崩劑填充劑。
  7. 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酶的水和其他蛋白( gef 、 gap 、 gdi )的調節下發生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。
  8. The diageneses which are constructive to the reservoirs are mainly dolomitization and burial dissolution

    對儲層起建設性的成巖主要有白雲石化、埋藏溶解作用
  9. To sum up, the algae - rich carbonate of foreslope facies can form all kinds of bitumen - associated dissolved pores after experiencing burial dissolution, so it can have good capability of bearing oil and gas

    總之,這些富藻的斜坡相碳酸鹽巖經過埋藏溶解作用而形成與瀝青伴生的各種孔,從而使巖層具有較好的含油氣性。
  10. Algae - rich carbonate of cambrian is typical sediment of foreslope facies in sandu and danzhai, eastern guizhou province. after sediment, it experiences many changes of diagenetic environment, and takes place much diagenetic altercation, among which the biggest is salt water dolomilization, and then is compaction, recrystallization, pressure solution, organic dissolution, burial dolomilization, cementation and silicification

    貴州省東部三都丹寨地區中上寒武統富藻碳酸鹽巖是典型的斜坡沉積,其在沉積后漫長的地質歷史時期內,經受了諸多成巖環境的改造,發生了極大的成巖變化,最大的成巖變化為鹹水雲化,其他的成巖有壓實重結晶有機溶解作用埋藏雲化膠結及硅化等。
  11. Burial dissolution mainly developed inside the primary micropores, the partly filled intergranular porosities and the intercrystal porosities, which furthermore formed lots of enlarged pores, intergranular pores, oolimolds

    埋藏溶解作用主要在粒間半充填剩餘縫隙、交代白雲石的晶間孔內進行,這進一步蝕造就了大量超大孔隙、粒間孔、粒內孔、鑄模孔等。
  12. Soil quality - dissolution for the determination of total element contents - part 1 : dissolution with hydrofluoric and perchloric acids

    土壤質量.為測定總元素含量進行的溶解作用.第1部分:使氫氟酸和過氯酸的
  13. Measurement of coating thickness ; determination of the mass per unit area of zinc and tin - coatings on ferrous materials by dissolution of the coating material ; volumetric method

    塗層厚度測量.塗層材料溶解作用測量鐵素體材料上塗
  14. The cementation of laumonite, calcite and chlorite, compact and pressure solution, as well as the dissolution of laumontite, feldspar are also of main factors which affect reservoir properties

    石、綠泥石、濁沸石的膠結、壓實壓和濁沸石、長石的溶解作用也是影響儲集性能的主要因素。
  15. The diagenesis may result in the variations in pore structures of sandstone reservoirs ; the compression and cementation may lead to the decrease in valid primary porosity of sandstones, and the secondary porosity generated by solution may serve as main oil storage spaces

    壓實和膠結降低了砂巖的原生孔隙度,溶解作用產生的次生孔隙成為主要的汕氣儲集空間。
  16. Deep dissolution is the important diagenesis for forming pores because of its fast buried rate and good preservation of organic matter. the difference is that deep dissolution is strong and fills large amount of bitumen in the section of danzhai, which shows they are pores when the oil and gas assembled ; but pores are comparatively less in the section of sandu

    由於斜坡沉積埋藏速度快,較快進入埋藏成巖環境,所以深有機溶解作用是該地區最主要的成孔成巖,所不同的是:丹寨剖面該種較強,而且孔內大部分灌入瀝青,充分說明其是聚集期孔隙而三都剖面這種孔隙相對較少。
  17. Oxidative degradation of partially hydrolyzed polyacrylamide in aqueous solution

    聚丙烯酰胺水液的氧化降研究
  18. Abstract : this paper introduces the principle of limited enzymatic hydrolysis on controlling wheat gluten, the changes in modified gluten ' s functions such as solubility, foaming ability and emulsifying ability, also the application of proteases in hydrolyzing wheat gluten

    文摘:綜述了控制小麥麵筋蛋白限制性酶水的原理、改性后的麵筋蛋白其水性、起泡性、乳化性功能性質的變化以及各種蛋白酶在水麵筋蛋白中的應
  19. The pattern of diagenetic and porosity evolution are established. the primary porosity of the reservoir rocks was 35 %, which was reduced by 21. 7 % by compaction and pressure solution and 8. 2 % by cementation. the secondary pores were produced by organic acids " dissolution during organic matter maturing stage, resulting an increase of porosity by 5 %

    預測本區砂巖原始孔隙度為35 ,經機械壓實和化學壓孔隙度損失了21 . 7 ,后經自生礦物的膠結,孔隙度損失了8 . 2 ,當進入有機質成熟階段,有機酸的溶解作用產生次生孔隙,使孔隙度增加5 ,現今保存的平均孔隙度為10 . 1 。
  20. The results demonstrate that the pingba red residua is a typical in situ chemical weathering crust, and the material sources of the profile are derived from underlying triassic dolomites, the chemical weathering of dolomite can be divided into two stages : " leaching - accumulating trend " and weathering trend ", the stable teconic and whole weathering of dolomite should be the main reason for the development of thick and consecutive red weathering crust overlying dolomite rock in central guizhou

    結果顯示該剖面是下伏基巖白雲巖風化成土並累積的結果,無其他外來物源,是原位風化殼;成土過程具有兩階段模式特徵,即白雲石、方石的蝕酸不物累積和酸不物進一步風化兩個階段;長時期的構造穩定和白雲巖整體是黔中地區白雲巖風化殼土層厚度大、分佈連續的主要制約因素。
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