河道沉積物 的英文怎麼說

中文拼音 [dàochén]
河道沉積物 英文
stream-channel deposit
  • : 1 (天然的和人工的大水道) river 2 (指銀河系) the milky way system; the galaxy 3 (特指黃河) t...
  • : Ⅰ名詞(道路) road; way; route; path 2 (水流通過的途徑) channel; course 3 (方向; 方法; 道理) ...
  • : Ⅰ動詞1 (沉沒; 墜落) sink 2 (沉下 多指抽象事物) keep down; lower 3 [方言] (停止) rest Ⅱ形容...
  • : Ⅰ動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
  • : 名詞1 (東西) thing; matter; object 2 (指自己以外的人或與己相對的環境) other people; the outsi...
  • 河道 : river course; streamway; covalency; runway; cut; river channel河道變遷 channel change; migration ...
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. Small alluvial fans at mouths of wet weather drainage ways also are commonly intermixed indistinguishably.

    潮濕氣侯地區出口處的小沖扇,其的混合通常也難以區別。
  2. Sediment begins to choke the channel's opening.

    開始淤塞口。
  3. The main sedimentary microfacies are submerged distributary channel, debouch bar, submerged natural levee and flood - plain splay. the research shows that the physical property of subermerged distributary channel sandbodies are the best and debouch bar comes second

    長4 + 52長62油層砂體的微相類型主要有水下分流口壩、水下天然堤和水下決口扇等,其中水下分流砂體的性相對最好,其次為口壩砂體。
  4. From sedimentology symbol such as rock assembled, sediment gradus, sandstone grading analysis, protogene sedimentary structure, ichnofossile and logging facies etc and palaeoenvironment background, it is confirmed that shen84 - an12block s34 segment is braid river delta system, not fan delta system ( abrupt slope ). then it can be more partition as braid river delta plain sedimentary assembled, delta front sedimentary assembled and prodelta sedimentary assembled on core and log assembled. and delta plain sedimentary assembled can be identified four microfacies : braided distributary channel, crevasse splay, overbank deposits and interdistributary bay

    微相研究是儲層非均質性研究的基礎,研究區有豐富的巖芯資料和測井資料,通過巖石組合、韻律,砂巖粒度分析、構造、古生遺跡和測井相等學標志,結合古環境背景,確定沈84 ?安12塊s _ 3 ~ 4段為辮狀三角洲體系,而不是前人所認為的扇三角洲(陡坡型)體系,在巖芯和測井組合上可進一步劃分為辮狀三角洲平原組合、三角洲前緣組合和前三角洲組合,其中三角洲平原組合又可識別出辮狀分流、決口扇、分流邊部和分流間灣四種微相類型;三角洲前緣組合識別出水下分流、水下分流邊部和分流口壩三種微相。
  5. 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模式,水下分流口壩是有利的微相;儲層性差,儲層巖石的孔隙類型主要有粒間孔、粒間(內)溶孔及少量晶間微孔;影響蓬萊鎮組氣藏儲層孔隙結構及儲集性的因素有巖相、巖性條件及成巖作用;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。
  6. The author presume the original physiognomy of jiuzhai valley, and acknowledged changhai valley was a surface - water with uniform waterpower, the rize valley was a branch of it but the inequality rise of lithosphere, the deposit of earthquake landslides debris flows and falling or glacier blocked the river - way, furthermore, the flow water with high content of ca ( hco3 ) 2, so tufa dyke formed and evolvement the present dyke of lakes the present physiognomy formed on the base of those 2

    由於地震、滑坡、泥石流引起的堆和冰川作用形成的冰磧堵塞,再加上構造運動造成地殼的不均勻抬升,九寨溝的這種獨特的地質環境以及高含ca ( hco _ 3 ) _ 2的巖溶水流作用下,為caco _ 3創造條件,的caco _ 3加高、連接最終形成灰華堤壩,使湖泊的形成成為可能。
  7. According to the abundance well logging, mud logging and core analysis data, gaotaizi reservoir has been classified into four sand group with the principle of cycle comparison and classified control. based on the detailed study of lithologic character, sedimentary structure, paleontologic fossils, depositional sequence, rock association and logging data, the microfacies of the studied area are divided into such seven types : subaqueous distributary channel microfacies ; river mouth bar microfacies ; subaqueous interdistributary channel microfacies ; subaqueous crevasse channel microfacies ; subaqueous natural barrier microfacies ; distal bar microfacies ; delta front sheet sand microfacies. the characteristic of each sedimentary microfacies are described detailedly

    通過研究大量測井、錄井資料和巖芯資料,依據「旋迴對比,分級控制」的原則,把研究區高臺子油層劃分為g 、 g 、 g 、 g四個砂層組。通過對研究區巖性、構造、古生序列、巖石組合及測井曲線特徵進行研究的基礎上,認為研究區高臺子油層屬於三角洲前緣亞相,並將研究區微相劃分為:水下分流口壩、水下分流間、水下決口扇、水下天然堤、遠砂壩、席狀砂等七種微相類型。
  8. The alternative changes of paleoenvironment favored the formation and imbedding of brine, which is the source of salt - water intrusion ; and the paleochannel that formed during regressive of sea level is the path of salt - water intrusion

    海進時期,大面的濱海平原被淹沒,在近海平原窪地滯留的海水經過蒸發、濃縮變為鹵水,成為鹹水入侵的源;海退後陸源碎屑在濱海地區形成了巨厚的古砂層。
  9. Distribution features of grain size of yinxian stream sediments in dali basin

    大理盆地隱仙溪河道沉積物粒度分佈特徵
  10. This was a particularly severe problem in the lower shing mun river in sha tin, but dredging and a bio - remediation project undertaken in 1997 made a huge difference to the smell of the river

    沙田城門下游以往曾有水發出惡臭的問題。政府於1997年治理,在床口進行挖掘污染工程及利用生化處理方法改善質素,難聞氣味已較以前大幅度減少。
  11. Based on the results of the study about the geological background in this area, this paper has discussed about the sedimentation facies marks for the fan delta in baimiao gas field, worked out a detailed proposal about the development of physical simulation experiment about the fan delta, and described in detail the general laws and major controlling factors governing the sedimentation processes of the fan delta. a detailed measurement was made about the experimental results, and a systematic comparison was made relative to the prototypic characteristics. based on the observation and description about the experimental processes and the analyses about the experimental results, this paper has given detailed

    在地質背景研究的基礎上,對白廟氣田扇三角洲相標志進行了論述,在此基礎上,制定了開展扇三角洲理模擬實驗的詳細方案,詳細描述了扇三角洲過程的一般規律及主要控制因素;對實驗結果進行詳細的測量,並與原型特徵進行了系統的對比,根據實驗過程觀察描述和實驗結果分析,詳細劃分了白廟氣田扇三角洲的巖石相類型及微相;分22個砂層組完成了微相尤其是扇三角洲上辮狀展布規律的研究,分不同時期指出了22個砂層組砂體分佈規律,為儲層預測及該地區滾動勘探奠定了基礎,這是本論文的重點內容之一。
  12. Using sedimentary facies analytical and formation inverse technique, the depositional characteristics and distribution of dujiatai formation of this area were described, disclosing that delta front facies and prodelta facies were mainly developed in dujiatai formation. material source are mainly from southern and northeast of the working area. sand types are mainly of delta front subwater distributaries channel sand body, river mouth bar and sheet sand body with large degree of planar variation

    2 .採用相分析及儲層反演預測技術,對新齊14井區杜家臺油層儲層特徵及展布特徵進行了詳細描述,揭示出本區主要目的層杜家臺油層屬t -扇二角洲,發育扇三角洲前緣亞相及前扇三角洲亞相,源主要來自於工區南部及東北部,發育的砂體類型土要為扇三角洲前緣水下分流砂體、口壩砂體及席狀砂砂體。
  13. Moreover, the current development status of sedimentation simulation research in china was demonstrated and five big trends for the future development of sedimentation simulation technologies were analyzed. the geometric similitude, kinematic similitude and kinetic similitude between the lab model and the prototype for sedimentation simulation form the basis of three similitude principles, while three similitude rules, i. e., the suspension similitude rule, the particle movement similitude rule and the riverway distortion similitude rule can be deduced from the three similitude principles, and thee principles and rules are the basic theories for the development of physical simulation about the clastic sedimentation processes

    模擬實驗模型及原型的幾何相似、運動相似、動力相似及其由上述三個相似性原理導出的懸浮相似、顆粒運動相似及變形相似等三個相似準則是開展碎屑過程理模擬的基本原理;在此基礎上,論述了碎屑模擬研究的主要方法?自然模型法和比尺模型法;提出了開展碎屑過程理模擬的主要方法步驟,這是本論文第二章的主要內容。
  14. Increase in runoff in the stream not only will cause a direct impact to the stream biotic communities, it may also affect the water quality in tung chung bay

    增加不僅直接影響的生群落,同時亦會影響東涌灣的水質。
  15. Because the intertidal main channel of the shing mun river suffers from a very weak flow, pollutants have tended to build up in the sediment, leading to low levels of dissolved oxygen

    城門的潮汐水流緩慢,污染容易床淤泥里,引致溶解氧水平下降,水散發出惡臭。
  16. The distribution of the reservoir is controlled by the depositional environment and the faces which are mainly alluvial, delta and river. determined by the diagenesis and the latter reformation, the physical property of the reservoir in general is poor, ranked as class 3 - 4

    儲層分佈則受環境、相控制,主要有沖扇、扇三角洲、砂等砂體,儲油性則受成巖作用及後期改造影響而較差,屬級。
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