水成演化 的英文怎麼說

中文拼音 [shuǐchéngyǎnhuà]
水成演化 英文
hydromorphic evolution
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  • : 動詞1 (演變; 演化) develop; evolve 2 (發揮) deduce; elaborate 3 (依照程式練習或計算) drill;...
  • 演化 : evolution
  1. With the developments of molecular biology and bioinformatics, it is possible to elucidate the phylogenetic evolutionary relationship of cruciferae at the molecular level

    隨著分子生物學和生物信息學的發展,從分子平闡明十字花科植物系統關系為可能。
  2. Based on field research and the dynamic analysis of remote sensing data of different time ( 1987 tm, 1996 tm and 2000 china - brazil earth resource satellite ccd ), using multi - information of research area ( including data of geology, geography, hydrology, meteorology, economy, human culture and dem ) and existing research results, the dissertation discusses drive factors of desertification and the relationships between drive factors and desertification with the help of gis tool and some mathematical methods such as probability, statistics, curvilinear estimation, logical analysis and analytic hierarchy process

    論文在對研究區土地荒漠現狀野外調研和不同時相( 1987tm 、 1996tm和2000ccd )遙感圖像土地荒漠信息提取和變分析的基礎上,結合研究區已有的多元信息基礎資料及研究果(包括地質、地理、多時期的文氣象、經濟、人文以及dem數據等) ,運用gis強大的空間分析功能和概率統計、曲線估計、邏輯分析、主分分析、層次分析等數學方法綜合研究了土地荒漠與各驅動因子之間的相關關系,揭示了研究區土地荒漠的主要驅動因素,探討了荒漠動態規律。
  3. Benthic foraminifer fauna, ams14c dating and acoustic sub - bottom profile was analyzed in the core ey02 - 2 and ey02 - 1 drilled from the muddy deposit in the middle southern yellow sea and the mid - shelf of north east china sea. considering the results of core qc2 ? dz4 and the standard oxygen isotope curves, we discussed the late - quaterenary paleo - environment evolution, benthic foraminifer fauna, paleo - climate, the climate events and water mass in postglacial period, average sedimentation rates, paleo - water depth, origin of sediments, average sea level rise rate in the shelf of south yellow sea and east china sea. at last we discussed the condition of sea level rise in the east china, green house effect and the protection of coastal zone

    本文根據南黃海中部泥質區和東海中陸架的兩個鉆孔巖芯的古生物、 ams ~ ( 14 ) c測年、淺地層剖面等,參考qc _ 2 、 dz _ 4果及標準氧同位素曲線探討了黃東海陸架晚第四紀古環境、底棲動物群特徵、古氣候、冰後期以來氣候事件、古團、沉積速率、古深、沉積物源、海平面平均上升率,討論目前中國東部海平面上升的狀況、溫室效應及海岸帶保護。
  4. Some researchers have made study on this subject, such as the generation and evolution of frazil ice, shore ice, bottom ice, ice cover and ice jam, the resistance of freeze - up river, flow capacity and variation of water stage

    國內外一些學者通過原型觀測,試驗和數值模擬的方法對內冰,岸冰,底冰,冰蓋和冰塞的生變,封凍河道的阻力、過流能力和位變等有關問題進行了研究。
  5. Abstract : based on the synthetical data from the remote images, geological section, geomorphologic landscape, ancient water system evolution and surface feature spectrum etc, the study indicates that there is an undersand lake in the northern peripberal belt of qarhan salt lakes of qaidam basin

    文摘:根據地球衛星遙感影象、地物波譜測定以及地貌景觀、古和地面地質調查等資料的綜合研究表明,柴達木盆地察爾汗鹽湖礦區北部外圍地帶存在一種新的因類型的鹽湖? ?沙下鹽湖。
  6. Fungi form mycorrhizae in plant roots and the hyphae take in carbon from plants through their epidermal cells and move mineral nutrients and water from soil to their epidermal cells ; this symbiosis is of high importance in studying biodiversity conservation, the origins and evolution of terrestrial plant, the rehabilitation and reconstruction of degenerated ecosystems, agriculture, horticulture and forestry

    真菌在植物根系形菌根后,菌絲通過根的皮層細胞獲取植物提供的碳源,同時將礦物營養和從土壤轉運到皮層細胞,這種共生過程的研究在生物多樣性的保護、陸生植物的起源與、退生態系統的修復與重建以及農業、林業和園藝業的應用具有重要的意義。
  7. This thesis explores origin of dwelling south anhui province from history, phyle, new confucianism, geography, geomantic omen ; analyses reason of development and exist of south anhui province from factor of economy, transportation and situation. continue is memorize of history

    本文從歷史、新儒學、宗族、地理、風幾個方面來探究皖南民居形的淵源;並從經濟因素、自然因素、交通和區位因素分析皖南村落人居環境的及其這些古村落仍存在的原因。
  8. 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,該區延長組儲層因類型主要為三角洲前緣下分流河道、河口砂壩及三角洲平原上分流河道微相細粒長石砂巖、粉砂巖;儲層巖石經歷了壓實,膠結,溶蝕等巖作用,歷經早巖機械壓實和學壓溶孔隙縮小期、晚巖a亞期溶蝕作用孔隙擴大期及晚巖a亞期( b亞期)膠結充填孔隙縮小期三個巖-孔隙階段;儲層物性總體上具有較低孔滲、低孔滲的特點,孔隙類型主要為粒間溶孔、殘余粒間孔隙、粒內溶孔、晶間孔及晶間溶孔,裂縫不發育,儲集巖排驅壓力和中值壓力較高,孔隙結構類型以細小孔-微孔隙,微細喉-微喉型為主。
  9. In this paper, thermal evolution history of organic matter of the source rocks and hydrocarbon generation history have been researched by tti method, hydrocarbon migration direction and migration times were probed combining with the area structure development feature ; distribution pattern of the main reservoir intervals on lateral and longitudinal have been predicted by researching on development feature and control factors of the reservoir intervals, the actions of reservoir conditions in hydrocarbon accumulation and bearing also were probed combining with pore evolution feature ; the micro - pore feature of regional cap and direct seal in carboniferous - lower triassic in this area have been determined with micro - capillary pressure curve and intrusive mercury curve ; the prospecting districts have been pointed out combining with the hydro - geologic feature, the potential reservoirs were classified according to trap types in this area, the author attempt to evaluate on the hydrocarbon - bearing condition in the str ata of carboniferous ~ lower triassic from hydrocarbon generation and migration reservoir condition, reserved condition etc, and predict the reservoir types and hydrocarbon - bearing patterns combining with the structure evolution. based on above, the author point out that the central block of chenghu - tuditang synclinorium and the southern block of dangyang synclinorium are the advantageous regions for exploration

    本文用tti方法研究了烴源巖有機質的熱史和油氣生史,並結合區內構造發育特徵,探討油氣在區域上的運移方向和在時間上的運移期次;通過對儲集層段的發育特徵和控制因素的研究,預測了本區主要的儲集層段在橫向上和縱向上的分佈規律,並結合孔隙特徵,探討儲集條件在油氣聚集藏中的作用;利用微毛細管壓力曲線法和壓汞法,對石炭系?下三疊統的區域蓋層和直接蓋層的微孔隙特徵進行了定量評價,並結合文地質分佈特徵,指出有利於油氣保存的地區;根據區內存在的各種圈閉類型,對可能存在的油氣藏進行了分類,並試圖從油氣的生與運移、儲集條件、保存條件等方面,動態地綜合評價石炭系?下三疊統油氣藏條件,並結合構造特徵,預測其油氣藏類型和藏模式。
  10. 4 ) the characteristic of tricyclic terpane reflected the source input of algae. the predominance of 4 - methylsterane and dinosterane, and the c _ ( 27 ) - sterane predominance " v " distribution pattern all indicate the great contribution of algae source input. based on the ratio of sterane c2920s / ( 20s + 20r ) and c29 / ( + ), the source rocks can be regarded as typical immature source rocks

    2 、利用豐富的生物標志合物信息,分析解釋了生源構、沉積環境、有機質等特徵,表明德南窪陷主力烴源巖的生源構是以菌藻類微生物為主且含有一定陸生植物輸入的混合生源,沉積環境為半鹹-鹹還原環境,沉積體具有「層狀」特點,表層鹽度高,底層還原性強。
  11. According to the contrast between different maps and the dynamical conditions, the area of bohe lagoon had reduced by 45. 3 % from 1932 to 2000 and human activities in the coastal zone, such as inning, sand dredging and aquiculture, have brought great effects on the coastal system, which has accelerated the barrier erosion and lagoon evolvement

    通過對比分析, 1932 ~ 2000年,博賀?湖面積減少45 . 3 % ,人類活動已為影響該區海岸變的主導因素;灘塗圍墾、海岸采沙與產養殖等人類活動加劇了沙壩海岸的侵蝕後退,且使得?湖面積迅速減少,不斷淤淺萎縮,大大加快了海岸體系的進程。
  12. Using fine paper, brushes and ink, calligraphers have evolved a richly varied tradition of calligraphic styles, which have been handed down from generation to generation

    書法家用上乘的紙張,毛筆和墨逐漸了今天迥異的書法風格,而這些形式,就一代傳給一代了。
  13. The main characters of the river - valley landforms are followed : the outstandingly longitudinal range - gorge landforms constitute the unique view of three parallel rivers ; the relative highness difference of the landform is great and the river valley cut deeply ; the formation and evolution of the river - valley landforms are obviously controlled by the geological structure ; the landforms types and the various characters of the landforms combination in the drainage area are prominent ; the geological environment has relatively strong frangibility ; the branches riverhead of the river - valley mostly come from high mountains and lakes, and the river - valleys of the branches along the banks have disproportional distribution

    其河谷地貌的主要特徵有:突出的縱向嶺谷地貌,構了少有的三江併流奇觀;地貌相對高差大,河谷深切;河谷地貌形發育明顯受地質構造控制;流域范圍內地貌類型和地貌組合多樣特徵突出;地質地貌環境具有較強烈的生態脆弱性;河谷支流源多發源於高山湖泊,兩岸支流河谷分佈不均衡。
  14. By means of the technologies of basin modeling, petroleum system, and correlation among chinese and foreign basins, and integrated analysis of the features of evolution of the basin, tectonic transformation, sidmentology, hydrology, and the anatomising of typical gas pools, the paper focused on the poolforming features of the basin, probed into the characteristics of enrichment, distribution and poolforming of oil and gas, and forecasted the favorable areas or belts of exploration

    本文以藏為主線,從前陸盆地形、構造變形、沉積充填、文地質研究出發,以盆地模擬、含油氣系統研究為手段,通過典型氣藏的解剖和藏主控因素分析,以及與國內外前陸盆地藏特徵對比,探討川西前陸盆地油氣富集規律和藏特徵,並預測有利勘探區帶和方向。
  15. This paper studies the evolution of oil, gas and water in hinterland of junggar basin from point of view of hydrogeology. analyzes the mutual action among theta and the effect of formation water on the formation and distribution of oil - gas reservoirs, including applying some ions and characteristic factors of formation water to reflect the closed relations among the preservation conditions of the oil and gas, the closing degree of reservoirs and the oil - gas migration for the purpose of searching for favorable oil - gas accumulation zones by the varied features of formation water

    文地質觀點和角度研究油氣,剖析和油相互作用的關系,掌握地層對油氣藏形和分佈的作用,同時利用地層的某些離子特徵和特徵系數來反映油氣的保存條件、地層的封閉程度、油氣的運移有著密切的關系,旨在利用學的變特徵來尋找有利的油氣聚集帶。
  16. The author points out that the social economy objectively requires the development of hub container ports and analyzes a variety of elements causing the emergence and development of hub container port, which includes the level and scale of hinterland economy, the natural and social factors of the location on which the port is based and the international ranking status of the port

    作者研究了集裝箱樞紐港的特點與形條件,指出集裝箱樞紐港的形既是社會經濟發展對運輸發展的客觀要求,也是集裝箱運輸自身發展的必然結果。它的形和發展的原因是多方面的,港口腹地經濟的平與規模、港口自身的自然條件和城市依託條件、港口在國際航線中的位置等都影響集裝箱樞紐港的形和發展。
  17. Formation and evolution of the shallow ground fresh water and brackish water is correlation with forming time of delta, characters of microtopography, as well as the distributing of present course and channel in alluvial - marine plain

    黃河三角洲地下淡、微鹹分佈與形與黃河河道的變遷、三角洲形的早晚、微地貌特徵及現代河道與渠系分佈等因素密切相關。
  18. Part 1 : first, from the history cause, tell us the forming, evolution and develops of city which are height reliance to natural environment, such as land, fresh water and mineral energy ; second, from the current situation cause, expound the fact this kind of reliance slacken with economic development and innovation of technology

    第一部分:第一,從歷史的緣由角度,闡述了城市的形與發展是對自然環境如土地、淡及礦物能源等環境要素的高度依賴;第二,從現狀的緣由的角度,論述了這種依賴隨著經濟的發展、技術的革新而消弱。
  19. Marine geology is a course in which the material compositions, formation and evolution of lithosphere covered with sea water at present and the formation and distribution of mineral resources are introduced, studying the geological phenomena in the view of oceanography

    本課程主要介紹在現代海覆蓋下巖石圈的物質組、形以及礦產形與分佈規律,從海洋科學的角度分析與研究地質問題。
  20. Make a comprehensive view of all study results about the flood channel, a model of formation and evolution of the flood channels was proposed. according to this model, not all flood channels formed by ebb channels divided by sand spit develop toward death, some of them may be keeping the current situation or transform to the reserve channel with the change of runoff and sediment concentration from upper reach

    用gis方法計算1861 - 2002年新橋道區域的沖淤變,可定量表達漲潮槽在不同時間尺度形規律,結合漲潮槽巖芯沉積物垂向的沉積特性變,可闡明漲潮槽的形機理與過程,並提出不同種類型漲潮槽的形模式。
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