水域類型 的英文怎麼說

中文拼音 [shuǐlèixíng]
水域類型 英文
type of water area
  • : 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...
  • : 名詞(在一定疆界內的地方; 疆域) land within certain boundaries; territory; region
  • : Ⅰ名1 (許多相似或相同的事物的綜合; 種類) class; category; kind; type 2 (姓氏) a surname Ⅱ動詞...
  • 水域 : waters; body of water; water area; horn; territorial waters; -limnion
  • 類型 : type; mold; form; cut類型論 theory of types; 類型語句 [計算機] type statements
  1. The essay discusses the serious situations of water pollution from small tankers due to quality of rubber hoses during oil operations. it emphasizes on paying more attention to the supervision of hoses qulity, usage and management in accordance with the law and technologic specifications. which will be useful for deepening management of safety and antipollution

    上油作業過程中,由於小油輪橡膠輸油軟管的質量等問題造成污染的嚴峻形勢,從法律、技術規范入手,強調重視對輸油軟管的質量、使用、管理三個方面進行監督檢查,無疑是對安全和防污染管理的深化,對現場監管具有一定的指導作用。
  2. Abstract : the essay discusses the serious situations of water pollution from small tankers due to quality of rubber hoses during oil operations. it emphasizes on paying more attention to the supervision of hoses qulity, usage and management in accordance with the law and technologic specifications. which will be useful for deepening management of safety and antipollution

    文摘:就上油作業過程中,由於小油輪橡膠輸油軟管的質量等問題造成污染的嚴峻形勢,從法律、技術規范入手,強調重視對輸油軟管的質量、使用、管理三個方面進行監督檢查,無疑是對安全和防污染管理的深化,對現場監管具有一定的指導作用。
  3. Through the analysis on the discrepancy between the indexes of land use and landscape structure of both the periods, the change of the eco - environment caused by the causations of both the nature and the human activities is pointed out that the total area of the studying region is somewhat reduced ; the alkali - saline land therein is utilized for fishery breeding ; a part of the unused land and water area are basified ; the sorts of landscape are rich and uniform and serious fragmentations are locally occurred

    通過分析兩期土地利用及景觀結構指數之間的差異性,指出由自然和人為原因引起的生態環境的變化:研究區總面積有所減少,鹽堿地改良後用于了魚蝦養殖,部分未利用地和鹽堿化,區景觀豐富且均勻,局部破碎嚴重。
  4. The land occupied in the process of urbanization is divided into cropland, garden plot, woodland, grass / rangeland, water area, wilderness. according to the characteristic of land occupation in the process of urbanization, the ecological loss of land is environmental loss, land restoration costs and available ecological loss

    本文將城鎮化進程中佔用的土地分為耕地、園地、林地、牧草地、、未利用地六種,根據城鎮化進程中佔用土地造成土地生態損失的特點,將土地生態系統的生態損失分為有效生態損失、環境損失、恢復費用三部分。
  5. Through studying it is shown that in chagan sag, the geothermal gradients in the center are higher than those around the sag margin and major factors influencing the characteristics of temperature field distribution are the property of geotectogenesis and the differences in tectonic portion, lithology and underground water behaviour ; there are three types of mudstone compaction, i. e. normal compaction, undercompacition and overcomepaction ; there are two pressure systems in sandstone reservoirs, i. e. normal pressure and negative pressure systems and the strata ' s being uplifted and denuded is the key factor leading to the formation of the negative pressure system in reservoir ; and the distinctive temperature - pressure field characteristics in the sag are possessed of important petroleum geological significance in hydrocarbon source maturity, hydrocarbon generation, widening on oil and gas exploration domain and selecting exploration targets, etc

    研究表明,查干凹陷中心的地溫梯度高於凹陷邊緣,大地構造性質及所處構造部位、巖性與地下活動的差異是影響凹陷地溫場分佈特徵的主要因素;泥巖壓實存在正常壓實、欠壓實和過壓實三種,砂巖儲層段壓力可分為正常和負壓兩個系統,地層抬升剝蝕是導致儲層負壓系統形成的主導因素;凹陷獨特的溫壓場特徵對烴源巖成熟、油氣生成、油氣勘探領的擴大及勘探方向的選擇等具有重要的油氣地質意義。
  6. The paper concludes that the changing rate of ndvi of rain forest in tropic is the smallest, the changing curve is smooth, while the changing rate of ndvi of the deciduous broad leaf forest in warm - temperate zone is the largest the change of ndvi is the most conspicuous in winter and spring ( especially in april ) while is not conspicuous in summer and autumn by analyzing the change of ndvi along latitude using the ndvi value of different vegetation types along the same longitude. the vegetation index from warm temperate zone to semitropical zone has obvious transition, while other areas have no distinct change by analyzing the change of ndvi from temperate zone to semitropical zone to tropical zone using ndvi averagejn the same time it is concluded that the sink value in the beginning of the year 1995 is from the influence of the monsoon in east of china by analyzing the ndvi curve of several typical needle leaf forests. the relation between ndvi value and temperature is conspicuous while the relation of precipitation is less or not by analyzing the relation between ndvi and temperature and precipitation finally it can get the conclusion that the change of river area is the smallest, the change of sienna area is the greatest by analyzing two phases of tm data in 1987 and 1997 with rs technic

    利用從同一經度的不同森林ndvi值分析,沿緯度方向ndvi變化可得出, ndvi在冬春季變化最明顯(尤其是在4月份最大) ,而在夏季和秋季變化不明顯。利用ndvi均值進行分析,從暖溫帶到亞熱帶到熱帶的變化情況發現,從暖溫帶到亞熱帶ndvi指數形成明顯的階躍,而其它區沒有太大的變化,同時對幾種典的針葉林曲線分析可知其年初的凹值源自於我國東部季風的影響。利用ndvi數據分析其與月均溫度與降的相關性得出與溫度相關性較為顯著,而與降相關性不顯著或無相關性。
  7. The content of the study as follow : 1 to choice the ship form, mainly ship ' s overall size ; draft, according to design of shanghai deep - water port and development of container ; 2. to deside the date of width ; depth ; path ; tract and sinkage through simulator tests ; 3. to replenish and modify some date for channel design to very large container vessels in " design code of general layout for sea port " 4. to study ship ' s turning area ; ship ' s stop distance the new and special content of the study as follow : 1. statistics of path at the channel given by difference operators with the affections certain wind. currents. seas and other influences shows the path really needed under certain condition

    並可在各航道和的通航安全評估及操船方法,航跡帶寬度,航道寬度,航跡帶分佈,船舶各種航行狀態時的下沉量研究中應用。本課題研究的內容: ( 1 )根據洋山深港設計規劃和集裝箱船舶的發展趨勢,通過研究、分析、比較,選擇最合適的船,尤其是船舶主尺度和船舶吃。 ( 2 )在大量模擬研究情況下,得出進港航道所需的航道寬度和深度。
  8. On the other hand, by meticulous diagnosis functions, such as signature analysis, trend analysis, spectrum analysis, the fault classification, position, severity and trend about the high - pressure getting rid of squama while running can be discovered and forecasted

    另外,該系統的精密診斷功能,包括歷史數據回放分析、趨勢分析、時分析、頻譜分析,能對泵的故障、部位、嚴重程度以及發展趨勢進行分析和預測。
  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演化史和油氣生成史,並結合區內構造發育特徵,探討油氣在區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,並結合孔隙演化特徵,探討儲集條件在油氣聚集成藏中的作用;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,對可能存在的油氣藏進行了分,並試圖從油氣的生成與運移、儲集條件、保存條件等方面,動態地綜合評價石炭系?下三疊統油氣成藏條件,並結合構造演化特徵,預測其油氣藏和成藏模式。
  10. According to the types, height and fireproof grade of the buildings, four basic ringed arrangements are brought up, namely the ringed arrangemensts of branch lines, the ringed arrangements of cross mains, the ringed arrangements of feed mains and the ringed arrangements of fire waterhead. on the basis of analyzing the means, characteristic and applicability of the four basic ringed arrangements, several practicality ringed arrangements are brought up, namely the ringed arrangements of branch lines and cross mains, the ringed arrangements of cross mains and feed mains, the ringed arrangements of branch lines and feed mains, the vertical ringed arrangements of feed mains and the ringed arrangements of sprinkler system in the abnormity buildings

    根據建築物的、高度和防火等級等因素,提出配支管環狀、配幹管環狀、立管環狀和消防源環狀這四種基本環狀形式,分析了四種環狀管網的環狀布置方法、特點和適用性。在此基礎上又提出了支管與干管環狀、干管與立管環狀、支管與立管環狀、立管豎向環狀以及不規則區環狀等幾種實用的環狀形式。
  11. With advantageous water, soil and organisms resources, the dadiwan culture, the yangshao culture, the longshan culture and the xiashang culture developed, original settling - down dry farming culture formed gradually, which laid sound foundation for agriculture civilization in the weihe valley ; among which, land use of arable farming was replaced largely by pastoral farming in the mixed area of agriculture and animal husbandry in north weihe region between 4 000 - 3 000 a b. p., because of dry and cold weather resulted in environment deterioration and soil degradation. at the beginning of 3 100 a b. p.,

    在8500 3100abp全新世大暖期,渭河流、土、生物資源條件優越,人發展了大地灣文化、仰韶文化、龍山文化和夏商文化,逐步形成了原始定居旱作農業文化,從而奠定了渭河流農業文明的基礎,其間在4000刁000ab衛,渭河流北部的農牧交錯帶,由於氣候的逐漸冷干化,導致、土、生物資源退化,造成旱作農業土地利用方式由遊牧業取而代之。
  12. Chapter two explain not only the economics and technologic level of wuhan and shenzhen but also the reasons for the technologic level of wuhan are higher than shenzhen but the economics level of wuhan are lower than shenzhen. chapter three analyze the internal and external factors of the economic development of wuhan and shenzhen. on the basis of above three chapters, the last chapter gives out some suggestion on explicating circumstantially the strategy of the economic development of wuhan and those problems in the course of establishing the method of the economic development of wuhan which should be pay attention to and should be avoided

    第一章除論述經濟發展及其模式的概念、、應分清的三組概念外,還探討了我國的三種區經濟發展模式;武漢與深圳在經濟發展平和科技實力兩方面各有所長,第二章對武漢與深圳經濟、科技進行了比較,並詳盡闡述了武漢科技實力強于深圳但在經濟上卻落後深圳的原因;第三章就經濟發展模式的內在和外在因素,對武漢與深圳經濟發展進行比較分析;聯系前面三章內容,最後一章主要探討武漢發展的優勢、劣勢和原因,詳盡闡述了構築武漢經濟發展模式的策略和在構建武漢經濟發展模式中應避免和注意的問題。
  13. Directed by the advance theories of sequence stratigraphy, reservoir beds sedimentology, seismic stratigraphy and petro - geology, measured by exactitude seismic procession, analysis of seismic facies, analysis of single well lithfacies and sedimentary facies, study of macro and micro character of reservoir and diagenesis, this paper study comprehensively the stratigraphy sequence, the type and distributiong of sedimentary facies, reservoir properties, the diagenesis and the evolution of pores of the 2nd and 3rd parts of pingdiquan formation of permian in wucaiwan - shishugou region in jungan basin. we can optimum seek favourable target area and apply the study results on oil field production in order to solve the difficult questions. we mainly achieve several views as follows : l ) establish the sedimential sequence framework of permian formation in studying area and delimint the jiangjunmiao formation of middle dyas series as lowstand system tract, the lower of the second part to the third part of pingdiquan formation of middle dyas series as transgressive system tract, the upper of the second part to the first part of pingdiquan formation as highstand system tract

    以層序地層學、儲層沉積學、地震地層學、石油地質學的先進理論為指導,以地震資料精細目標處理、地震相分析、單井巖相分析、沉積相分析、宏觀和微觀儲層特徵分析及成巖作用研究為手段,對準噶爾盆地東部五彩灣? ?石樹溝地區二疊系平地泉組二、三段的地層層序、沉積相及展布、儲層物性特徵、成巖作用及孔隙演化進行綜合研究,優選出有利勘探區帶,並將研究結果應用到生產中,解決生產中的難題,主要取得了以下幾點認識:建立了工區內二疊系沉積層序框架,把中二疊統將軍廟組地層劃為低位體系,中二疊統平地泉組二段下部三段地層為進體系,二段上部一段地層為高位體系
  14. It decides the protective objectives for different ecological reserve area based on the study of channel wetlands and survey and analysis of top - grade species ( fishes ) of the yellow river : from the point of the basin, the main ecological protective objectives of the tipper stream are vegetation and forest for conservation of water supply ; soil and water conservation is the main in the middle reaches for vegetation protection and rehabilitation and ; the lower reaches takes types of wetlands protection and wetlands area maintenance as the main, protecting biodiversity and important birds resources

    在黃河河道濕地研究和黃河體內頂級物種(魚)的調查分析基礎上,確定了黃河不同生態保護區的生態保護目標:從流角度而言,黃河上游的主要生態保護目標是植被和源涵養林;中游應以土保持為主,主要是恢復和保護植被;下游以保護濕地和維持濕地面積為重點,保護生物多樣性和重要鳥資源。
  15. The result shows that the area proportions of habitat landscape, industrial landscape, green - land landscape and water area landscape are 29. 57 %, 15. 423 %, 14. 501 % and 5. 98 % respectively in 2000. the number of landscape patch and diversity index of habitation is the highest and the fragmentation index of green - land landscape is the lowest in all landscape types

    結果表明, 2000年各景觀中,居住景觀和工業景觀的斑塊面積比例較大,分別為29 . 57和15 . 423 ,綠地景觀和景觀的比例偏小,分別為14 . 501和5 . 98 ;居住景觀的斑塊數和多樣性指數最大,綠地景觀的破碎度最小。
  16. Using many related documents for reference, the article selects 10 types of the county region ' s economic development, which belongs to 8 categories in ningxia hui autonomous region, and utilizes quantity and graph method to analyze the types of economic development level in 17 counties, which can be classified into advanced type, medium type and backward type

    摘要在借鑒大量文獻的基礎上,選取寧夏回族自治區縣經濟發展的810項指標,並運用量圖分析方法對寧夏區內17個縣市經濟發展平進行分析,排序為先進、中等和落後三種
  17. The evapration of water area is calculated by et0 multiplied by kc ; and then the evapotranspiration estimation models for other categories ( singular underling surface ) are presented ; based on bare soil and dense grass models the evapotranspiration estimation models for partly grass covered surface is presented combined with vegetation fraction data. it is feasible and logical each categories using singular way and mean, the result of regional evapotranspiration over south ningxia is given

    體單獨處理,由參考作物蒸散乘以比例系數直接計算得出體蒸發;建立了4種單一下墊面(裸地區、草地完全覆蓋區、喬木林區、灌叢區)蒸散計算模;對混合下墊面(草地?裸地區)區蒸發(散)計算方法使用裸土和草地完全覆蓋蒸發(散)計算模,然後結合植被覆蓋度給出。
  18. This paper adopts the land use state in2000a ( l : 3 + 104 ), the soil chart ( 1 : 6 + 104 ) and hectometer contour relief map ( include three chongqing area ) of chongqing and geology map ( l : 6 + 104 ) of sichuan province as basic analytical data, measure landscape patches into 7 types including cultivated land, orchard, forestland, unused land, grassland, resident and industry land, water bodies according to land use state basing on land use types, make the landscape map of chongqing karst area by gis software

    本研究是以重慶市1 : 30萬的土地利用現狀圖( 2000年版) 、 1 : 60萬的土壤圖以及重慶市百米等高距的地形圖和四川省(包括重慶市) 1 : 60萬的地質圖作為基本分析圖件。在土地利用的基礎上,依據土地利用現狀劃分了耕地、園地、林地、未利用地、草地、居民工礦用地和7景觀嵌塊體,再藉助于gis軟體生成重慶巖溶區景觀圖。
  19. The results show that : ( 1 ) soil moisture follows a - distribution over the discussed zone of the humid area in summer, but do distribution at the researched zone vicinity of oasis desert area in winter

    結果表明: ( 1 )在研究區不同的下墊面條件下,夏季土壤分在濕潤研究區呈明顯的單峰偏態分佈,且以分佈擬合效果為最好;而在臨近綠洲的沙漠研究區則呈多峰分佈,冬季呈分佈。
  20. Based on an analysis of causes and basic characteristics of drought in north and south areas of china, it is pointed out that drought in north areas, such as the yellow river basin and the huaihe river basin, was characterized by the severe systematic demand - supply contradiction resulted from the shortage of water resources, and successive drought disasters intensified by hot and dry weather, and that drought in south areas was characterized by the occurrence or successive occurrence of dry years due to hot and dry weather and the seasonal water shortage induced by their geographic and climatic features and insufficient water supply capacity

    摘要以區乾旱特徵分析以及乾旱災害應對策略研究為目的,闡述我國南、北方兩種不同地的區乾旱成因和基本特徵,指出黃淮海區的乾旱特徵主要表現在天然資源短缺引發的系統性深度供需矛盾,以及晴熱少雨氣候加劇這種矛盾而產生的持續乾旱災害;南方地區的乾旱特徵主要表現在晴熱少雨氣候導致枯年或連續枯年出現,以及地理氣候特徵和供工程容量不足等因素產生的年內季節性乾旱缺
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