溶發 的英文怎麼說

中文拼音 [róng]
溶發 英文
ablate
  • : 動詞(溶化; 溶解) dissolve
  • : 名詞(頭發) hair
  1. Methods the antioxidant of 75 % ethanolic extract and organic solvent extracts, water extracts and polysaccharids from acanthus ilicifolins l. was detected by flow - injection chemiluminescence, to evaluate the ability of scavenge h2o2

    方法採用流動注射化學光法,研究該植物75 %乙醇提取物及其有機劑萃取分離部分、水提取物及多糖對過氧化氫( h2o2 )的清除作用。
  2. Corrosion reactions, with metal dissolution, can occur in both basic and acidic solutions.

    使金屬解的腐蝕反應,可以在堿性也可以在酸性液中生。
  3. The adduct is isolated by evaporating the solvent and any low-boiling concomitants at low temperatures of the order of about-100 to -20℃.

    在-100-20的低溫下,將劑和低沸點成分蒸掉而分離出加合物。
  4. In the early 1960s a worldwide aerosol band was discovered in the lower stratosphere at 17-24km.

    在六十年代初期,在17-24公里平流層下部現世界范圍氣膠帶。
  5. Salinity exists in oceanic atmosphere at aerosol form. usually, seacrafts need desalted air, for example, air for combustion and cooling, airiness of communication cabin and electron cabin, etc. now, lots of large naval ships are equipped with gas turbines both home and abroad

    海洋大氣中含有鹽分且以氣膠形式存在,海洋艦船的進氣往往有除鹽要求,例如艦船動機燃燒用和冷卻用的進氣、通訊電子艙的進氣等。
  6. We have invented a technique to extract the humoral fluid from the amphioxus branchiostoma belcheri tsingtauense

    我們現文昌魚體液出現補體樣的血活性。
  7. The formation of carbonate reservior is controlled by the overlaid c - p strata and the intensity of karstification which was related to the palaeo geomorphy and palaeodrainage system

    下古生界碳酸鹽巖裂縫蝕型儲集層的育特徵以有無上古覆蓋是巖溶發育的前提;古地貌、古水系控制巖溶發育強度。
  8. The first is the depression karst development pattern from dissolution of karst hill during indo - chinese epoch which is the key period for forming space of the reservoir

    其中印支早燕山期裸露巖丘(梁)窪地型巖溶發育模式,是儲集空間形成的重要時期。
  9. Water invasion bursten out during the railway - tunnel construction is usually the mainly problem in constructing or operating, also which brings surface water to exhaustion and pollutes environment or effects ecology, etc. the geleshan tunnel which crosses through guan - yin gorge anticline which trend is near south north, is located between tuanjie village and jingkou village of the shapingba zone, chongqing city, which is belongs to the inducting segment of yu - huai railway. the guan - yin gorge anticline appears to ridge and slot interlacing in land form, and is composed of clastic rock and carbonate rock from jurassic xintiangou group to triassic

    歌樂山隧道位於渝懷線引入段重慶市沙坪壩區團結村至井口村之間,隧道穿越近南北向的觀音峽背斜,地貌上表現為脊、槽相間,觀音峽背斜由侏羅系新田溝組至三疊系下統碎屑巖和碳酸鹽巖組成,歌樂山頂大部分出露可巖地層,地表巖溶發育,有大量泉水和暗河出口,並修建有多個中小型水庫、大量池塘和水井。
  10. The paper takes an example of condensed gas feild in qianmiqiao buried - hills. based on the research of formation and development of the buried - hills, three important subjects in the research are discussed with the application of advanced technical and methods ( namely, balanced cross sections, analysis of carbon isotope, mensuration of reservoir fluid inclusion ) : ( 1 ) the development of karstification and characters of reservoir in ordovician ; ( 2 ) lower tertiary ( es3 ) source in the depression nearby ; ( 3 ) the hydrocarbon generation history, migration phase and reservoir formation history

    論文以千米橋潛山凝析氣藏為例,在研究潛山形成演化基礎上,採用先進技術手段(平衡剖面技術、碳同位素分析、儲層流體包裹體測定) ,討論了該潛山油氣藏研究中三個重要問題: ( 1 )古巖溶發育與奧陶系儲層特徵; ( 2 )臨近凹陷下第三系油氣源: ( 3 )油氣生成史與運移期次以及成藏歷史。
  11. First, on the base of investigating geleshan geologic environments, the author carefully analyzes them, studies their water storage structure, discusses the relationship of underground water dynamic changes and tunnel drainage by desiccation ; secondly, the author makes the dynamic analysis, regression analysis, routine hydrochemistry analysis, isotope analysis, so draws to guan - yin gorge anticlire east and west slot ' s karst developing features, alternated conditions underground water and supplying drain ways ; thirdly, by stating the fissuring ' s surveying data, the author calculates the seeping tensor

    作者在進行歌樂山地質環境調查的基礎上,仔細分析了大量觀測資料,研究其儲水構造,掌握地下水動態變化與隧道施工涌水的關系,及補給受降雨的影響情況。對隧道周圍的地下水進行動態分析、回歸分析、常規水化學分析以及同位素分析,得出觀音峽背斜東西翼槽谷的巖溶發育特徵,及地下水的循環交替條件、補給排泄途徑;統計分析裂隙測量數據,計算滲透張量。
  12. This paper summarizes seven kinds of geological factors advantageous for karstification, such as the lithology, the strata framework, the geological strature, the paleo - relief, the paleo - climate, the former pore space system and the later reconstruction in embedding period

    摘要分析了巖溶發育的7種地質因素,即巖性、地層結構、地質構造、佔地貌、古氣候、先存孔洞系統以及埋藏期的後期改造等。
  13. Besides lithological characters and geological structures, the karst development and groundwater in the area are affected by neotectonic movement and fossil karst

    區內巖溶發育和地下水賦存除受巖性、地質構造的控制外,還受新構造運動和古蝕的影響。
  14. Regularity of karst growth on the left bank of shuibuya dam and its permeability analysis

    水布埡大壩左岸巖溶發育規律及滲透性分析
  15. Because gray rock characteristic is asymmetric, the growth of rock dissolve is jolly unbalanced, harbour state of groundwater is very complicated, under the similar geological condition evaluation and optimization of groundwater resource is also difficult, until now there is no scientific solution to this kind of problem

    由於灰巖的地質特性為非均質,巖溶發育極不均衡,地下水的蓄存狀況極為復雜,因此類似地質條件下的地下水資源評價和優化管理難度是非常大的,目前國內外尚無很好的辦法解決此類問題。
  16. In terms of the regional perspective, the distribution characteristics of ground collapse are controlled by topography and geomorphology, geological structures, groundwater, karst development level, covering layers and human engineering activities

    從區域上看,地面塌陷的分佈特徵受地形地貌、地質構造、地下水作用特徵、巖溶發育程度、覆蓋層條件和人類工程活動等的控制。
  17. Vertical zonation of karstification and its engineering geological significance

    溶發育垂直分帶及其工程地質意義
  18. This results are very useful for the predicting mining damage and dividing the damage duty in the southern china where there are plentiful under water and karst growth

    研究結論為南方巖溶發育地區開采損害預計和責任認定提供了依據。
  19. Based on the karst development pattern, groundwater enrichment pattern, and recharge, runoff and discharge conditions of groundwater, the karst areas distributed in the peripheral area of the basin is divided into 9 systems which are further divided into 25 subsystems

    在研究盆地周邊巖溶發育規律,地下水富集規律,地下水的補給、徑流、排泄條件的基礎上,將周邊巖區劃分為9個巖水系統,進一步劃分為25個巖水子系統。
  20. So it is difficult to forecast the karst collapse ’ s time and place. on the other hand, we can evaluate the possibility of karst collapse by surveying the enigeering geology particularly. in other words, prevention and drawing building ’ s layout decide by the stability of karst collapse

    但是,根據當地的巖溶發育程度,則可以通過詳細的工程地質調查,來評價巖塌陷生的可能性大小,即巖塌陷的穩定性,尋找潛伏的巖洞穴,作為防治塌陷及制訂工程建設規劃的依據。
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