陸上河流的 的英文怎麼說

中文拼音 [liùshànghéliúde]
陸上河流的 英文
fluvioterrestrial
  • 陸 : 陸數詞（六的大寫） six （used for the numeral 六 on cheques, etc. to avoid mistakes or alterations）
  • 上 : 上名詞[語言學] （指上聲） falling-rising tone
  • 河 : 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...
  • 流 : Ⅰ動1 （液體移動; 流動） flow 2 （移動不定） drift; move; wander 3 （流傳; 傳播） spread 4 （向壞...
  • 的 : 4次方是 The fourth power of 2 is direction
  • 河流 : rivers; stream
  1. The water above the continental shelf is moved by the tides and by estuarine currents.

    潮流和河口流使大陸架上的海水流動。
  2. The depositional environment of the upper paleozoic in the ordos evoluted from the epicontinental sea to the fluvial - delta. the change of the depositional environment and eustacy controlled the main depositional systems in the research area

    上古生界沉積環境演化過程總的是由陸表淺海逐漸變為陸相的河流?三角洲，海平面升降和海水進退控制了區內主要的沉積體系和沉積相類型。
  3. The yanchang formation of upper triassic in north shaanxi is major terrigenous clastic system deposited in fluvial - latchstring environment, under the influence of the llocyclicity factor which include indosinian tectonic, eustacy, sedimentary supplies and the autocyclicity factor. in late triassic, north shaanxi was divided into two parts bounded by zhidan - ganquan - yichuan demarcation line

    陜北地區上三疊統延長組是以河流一湖泊相為特徵的陸源碎屑巖系，當時的陜北地區，以志丹?甘泉?宜川沿線為界，南側以明顯的斜坡向深湖盆地過渡，北部則為一地形平緩的淺水臺地。
  4. Many research such as clay minerals, suspend in the sea, the grain size trend analysis of surface sediment, poc 6 cu and 8 c13 in bottom sediments etc. showed that : the yellow sea warm current divided the south yellow sea into two, the terrestrial material of modern sediment on the west shelf plain mainly came from the modem yellow river suspend carried by the alongshore current, and the sediment difference between the west and east side of yellow sea trough was represented by the sedimentation thickness in postglacial period, sedimentation stratum, and oxygen isotope record

    粘土礦物、碳酸鹽、粗碎屑、海域懸浮體、表層沉積物粒度趨勢分析、 poc c ~ （ 13 ）及底質沉積物的c ~ （ 13 ）等多方面研究表明：以黃海暖流為主導，南黃海堆積陸架平原西側現代沉積物陸源物質主要源於黃海沿岸流攜帶的現代黃河懸移物質，黃海槽東西兩側的沉積差異主要表現在冰消期以來沉積厚度、沉積層序、氧同位素記錄上。
  5. This paper firstly reviews two different kinds of terrestrial erosion ( the mechanical and chemical weathering mechanisms ), discusses their respective roles in providing carbon to the river, and compares the differences between the monsoon and non - monsoon drainage basins in flux and the characteristic of the riverine carbon transport

    首先就機械和化學風化兩種不同的陸地侵蝕機制在提供河流碳源方面所發揮的不同作用作了詳細論述，並比較了季風流域和非季風流域間河流碳輸移在通量及性質上的差異。
  6. The yanchang formation is divided, for the first time, into six third - order sequences, each with an average time duration of about 4. 5 ma. the single sequence is composed of deltaic and lacustrine sandstones, siltstones and mudstones. the subaerial and subaqueous distributary channel and channel - mouth bar sandstone reservoirs are well developed mainly in the lowstand and highland systems tracts

    論文在富縣探區首次應用陸相層序地層學的觀點和方法，把延長組劃分為6個三級層序，平均時限4 . 5ma ，各層序由三角洲與湖泊相砂、泥巖沉積組成，主要在低位體系域和高位體系域發育水下（上）分流河道和河口砂壩砂巖儲層
  7. It has extensive views and between it and the watercourse below is a drop in elevation of approximately 300 meters. added to which, there are prolific updrafts which makes it taiwan s best location for air sports. in holiday periods top gliders flock here and there s a real carnival atmosphere

    位於賽嘉的航空園區，座落在一個小山頭上，視野遼闊，和下方平坦的河川地著陸區之間，約有三百公尺的高度落差，加上此地上升氣流旺盛，是國內最佳的航空運動場地，每逢假日，飛行高手匯聚，十分熱鬧。
  8. The sedimentary facies show a depositional evolution from the deep - water sediments through shallow - water sediments to the continental sediments, including alluvial fan, river, lake, delta ( tide - dominated ), barrier coast, shallow sea, deep sea and volcanic debris flow deposits

    在沉積相上，經歷了從深水沉積到淺水直至陸相沉積的演變，發育有沖積扇、河流、湖泊、三角洲（潮汐） 、障壁海岸、淺海、深海和火山碎屑流沉積。
  9. Lakes and ponds are basins of water surrounded by land, whereas rivers and streams are the arteries that move freshwater from land, such as mountain peaks, to the oceans

    湖泊和池塘是被陸地環繞的水盆，而河流和溪水是陸地上淡水流動的要道，比如從山峰到海洋。
  10. The ordos basin is an important terrestrial basin that came into being during mesozoic in our country. the yanchang formation more than one kilometer in thickness is the main oil - bearing beds in the study area. its lithology characteristic indicated that the formation was deposited in fluvial - lacustrine environment

    鄂爾多斯盆地是我國十分重要的中生代內陸盆地，厚逾千米的上三疊統延長組是區內主要的含油巖系，其巖性特徵表現為河流-湖泊相的陸相沉積。
  11. Normally water resources is affected by human activities and climatic change, but it is affected mainly by climatic change in runoff forming regions located in the high and middle mountainous area in the northwestern china. river runoff in the hexi inland arid region all originates from the qilian mt. area and the change of mountainous runoff resulted from global weather warming up and will bring an important effect to the development of society and economy in the hexi region. so the response on mountainous runoff and its changing trends are analyzed on the basis of the measured data of precipitation, air temperature, and discharges observed from some weather and hydrologic stations in the studied area. the results show that seasonal variation of mountainous runoff in the hexi inland region is mainly affected by the river ' s geographical location and supply source, and the yearly change by precipitation and that in the west of the region by air temperature besides precipitation. there are some obviously regional differences in the influences of climatic change on surface runoff in the hexi inland arid region, that is, rivers runoff in the west of the hexi area have been increasing and rivers in the east part have been decreasing, and the rivers runoff in the central part presented slowly increase trend, such as the heihe river, but it is not quite obvious

    一般情況下，水資源的變化主要受氣候變化和人類活動的影響，但在位於我國西北內陸乾旱地區的中高山地帶，徑流的形成主要受前者的影響.甘肅省的河西內陸乾旱區是該省重要的工農業生產和經濟開發區，這里各項社會和經濟活動與出山徑流的變化都有著十分密切的關系.因此，筆者根據有關水文氣象臺站的降水、氣溫和徑流觀測資料，分析了以黑河、昌馬河、西營河等主要河流為代表的河西內陸區出山徑流的變化特徵與規律.結果表明，河西內陸區出山口徑流的季節變化主要受地理位置和河流補給來源的影響，而年際變幅則受山區降水量年際變化及變幅的影響十分明顯.目前，梨園河以西河流水量處于上升階段，梨園河以東的河流則處于下降的階段;以黑河幹流鶯落峽水文站年徑流為代表的走廊中部地區的出山口徑流正處於1990年開始的枯水段的上升段.但總體而言，河西內陸乾旱區出山口徑流的變化相對比較穩定.預計今後若干年內，河西內陸乾旱區東段河流出山口徑流的變化以偏枯為主，中段、西段河流出山口徑流的變化以平水或平水偏豐為主
  12. Chang - 2 oil - bearing beds of the yanchang formation, which is one of the most important oil - producing beds in the area, is mainly composed of braided river deposits with the meandering river existed only in the restricted northwest part of yanchang

    延長地區上三疊統長2油層組是一套發育于淺水臺地背景之下的陸源碎屑巖沉積，以辮狀河河流相沉積為主，曲流河沉積僅在研究區西南角小面積分佈。
  13. Based on existed achievements of the continental river of arid area, the paper system analysis hydro - eco characteristics, hydro - eco changes and watershed changes. a case in tarim river, the paper study hydro - eco characteristics, river evolution, evaluated eco - environment quality, explore ecology water demand, study the rational utilization of water resources in tarim river watershed. the paper is composed of nine chapters, chapter 1 include research background, main research contents, research methods and research, meaning

    本論文在總結乾旱地區內陸河研究已有成果的基礎上，系統分析了乾旱地區內陸河的水文生態特徵、水文生態變化以及流域生態環境變化的基礎上，以我國最大的內陸河?塔里木河為例，初步研究了塔里木河的水文生態特徵、塔里木河的演變及其流域生態環境變化，探討了塔里木河流域的生態需水量，進行了塔里木河流域生態環境質量評價，研究了塔里木河流域水資源的合理開發利用。
  14. Even now, when the continents have been mapped and their interiors made accessible by road, river and air, most of the world ' s people live no more than 200 miles from the sea and relate closely to it

    時至今日，大陸已在地圖上標出，內地已由道路、河流和空中航線溝通，然而世界上大多數的人仍然生活在距離海洋不超過200英里的區域內，並與其保持著密切的關系。
  15. We had said, the bohai sea resembles a big basin, 3 its are being surrounded by land, there are 8 bigger fluvial infuse bohai seas on land, in these 8 rivers, have yellow river of world - renowned of slimy river not only, also have with " small yellow river " famed always decide a river, after collecting the haihe river, infuse bohai sea

    我們已經說過，渤海像個大盆，它的三面都被陸地包圍著，陸地上有8條較大的河流注入渤海，這8條河中，不僅有世界聞名的泥河黃河，也有以「小黃河」聞名的永定河，匯入海河后，注入渤海。
  16. In fact, in many of the continent ' s most fertile river basins, urban sprawl is consuming growing quantities of prime rice - farming land

    事實上，在亞洲大陸許多非常肥沃的江河流域，城市擴張正在吞噬越來越多最適于種植水稻的土地。
  17. It ` s in the middle of henan, shandong, jiangsu, zhejiang, jiangxi, hubei, across yangtze river and thehuaihe river

    分別與河南、山東、江蘇、浙江、江西、湖北接壤，跨長江、淮河流域，緊靠以上海為中心的長江三角洲經濟區，是臨江近海的內陸省份。
  18. The paper puts forward an ecosystem and the consideration of grading management and planning of water used for ecology, approaches to the water resources issues related to 8 important aspects of water and ecologic security, property management of water resources and business accounting, water resources allocation management, management of water resources policies, management of water resources development and utilization, water used for ecology and carrying capacity of water resources, man - built meadows and water saving, protection, management and water use of semi - desert meadows on the border of oasis and puts forward important strategic countermeasures on sustainable development of oasis situated on the downstream of dry endorheic drainage based on the study of orientation and key points of ecological building of the oasis

    摘要在研究乾旱內陸河流域下游綠洲生態建設方向與重點的基礎上，提出了生態系統和生態用水量分級管理和規劃的思想，探討了其所涉及的重要的水安全與生態安全、水資源產權管理與核算、水資源配置管理、水資源政策管理、水資源開發利用管理、生態用水與水資源承載能力、人工草場與節約用水、綠洲邊緣半荒漠草場的保護治理與用水等8個方面的水資源問題，提出了乾旱內陸河流域下游綠洲可持續發展的重大戰略對策。
  19. Based on a comparative study of the social economic development and the water resources characteristics in 13 arid inland basins of north - western china, it is pointed out that oasis will move from lower reach to upper reach in the circumstances of lower water availability per capita and poorer social economic structures

    摘要本文在對中國西北13個內陸河流域水資源稟賦和社會經濟發展狀況進行對比研究的基礎上，指出在人口不斷增長和社會經濟結構不適宜的情況下，人均水資源量的不斷減少，將導致流域內綠洲重心逐漸從下游向中游、上游遷移。
  20. And sedimentary microfacies of the main reservoir sands has been divided according to regional background, lithology or rock texture, sedimentary structure, sedimentary rhythm, grain size analysis, palaeontological assemblage, log and seismic facies. with all the heterogeneity appraisal parameters, the macro - heterogeneity of reservoirs has been evaluated quantitatively

    從區域背景、巖性及巖石結構、沉積構造、沉積韻律、粒度分析、古生物組合、測井相和地震相分析入手，確定了埕島油田館上段儲層為陸相沉積河流亞相，並進一步劃分了館上段儲層主力油砂體的沉積微相。
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