北上山地 的英文怎麼說

中文拼音 [běishàngshānde]
北上山地 英文
kitakami sanchi
  • 上 : 上名詞[語言學] （指上聲） falling-rising tone
  • 山 : 名詞1 （地面形成的高聳的部分） hill; mountain 2 （形狀像山的東西） anything resembling a mountain...
  • 北上 : proceed northward; go north
  1. They are jinfo mountain in nanchuan county ( natural protection section ), wuling mountain in qianjiang county ( national emphases forest demonstration county which forest cover rate is beyond 50 % ) and zhongliang mountain in beibei county ( artificial destruction is very grave ). some main land use patterns i. e. woodland, garden, infield, abandon infield, shrub and grassplot are selected in those three sample sites. four aspects on soil fertility index of karst environment under different land use patterns in these three sample sites, are revealed in this paper, by using the field test, indoor measure and analysis, outdoor experiment and field investigation, and the knowledge and technique of soil, ecology, physics and chemistry etc. they are physical characteristic ( effective soil thickness, organic layer thickness, soil texture, water - stable aggregate and soil water etc. ), chemical fertility ( organism, omni - n, omni - p, omni - k, alkali - nitrogen, available p, available k and rapid available k etc. ), soil animalcule ( bacteria, fungi, actinomyces and their grosses ) and soil - seed - pool ( plant community diversity index ) in karst ecosystem

    本研究以重慶市的南川金佛山（自然保護區） 、黔江武陵山（國家重點退耕還林示範縣，森林覆蓋率50以上）和北碚中梁山（遭人為破壞嚴重）典型巖溶區為對象，選擇了幾種重要的利用方式，包括林地、果園、耕地、棄耕地和灌草坡，採用野外巖溶生態調查和室內試驗測量分析相結合的方法，以不同土地利用方式巖溶土壤肥力為重點，對不同土地利用方式土壤肥力特徵進行量化分析，找出巖溶土壤肥力差異的主要方面及其根本原因，論文主要從土壤剖面物理退化指標（有效土層厚度、有機質層厚度、質地、團聚體、水分含量等） ，化學肥力退化指標（有機質、全n 、全p 、全k 、堿解n 、速效p和速效k等） ，樣地土壤微生物指標（細菌、真菌、放線菌數量及總量）以及樣地土壤種子庫植物群落多樣性等4個方面對重慶典型巖溶區的土壤肥力特徵進行了較為詳細的分析研究，為巖溶地區士壤資源的合理利用及結構的調控管理提供依據。
  2. Moisture, temperature, season and forest type, on the occurrence of agarics are extensively discussed in this dissertation. finally, several suggestions for long - term and sustainable research of agarics are given

    可見武夷山地區的菌物區系，處于東西相聯，南北貫通的位置上，從區系成分看也是溫熱兩帶俱全。
  3. In the burren there is a region of bare carboniferous limestone containing arctic - alpine plants which survived from the last glaciation

    Burren有一個只有石碳紀石灰石的地區，那裡有從上個冰期生活下來的北極高山植物。
  4. The general route of the great indian peninsula railway is as follows : - leaving bombay, it passes through salcette, crossing to the continent opposite tannah, goes over the chain of the western ghauts, runs thence north - east as far as burhampoor, skirts the nearly independent territory of bundelcund, ascends to allahabad, turns thence eastwardly, meeting the ganges at benares, then departs from the river a little, and, descending south - eastward by burdivan and the french town of chandernagor, has its terminus at calcutta

    火車離開孟買島穿過薩爾賽特島，進入位於塔那前面的大陸腹地，穿過西高止山脈向東北直達布爾漢普爾，再穿過差不多可以算是獨立的本德爾汗德上邦的領地，北上到阿拉哈巴德，再向東進，在貝拿勒斯與恆河相遇，然後離開恆河不遠向東南下行經過布德萬和法屬殖民地昌德納戈爾直奔終點站加爾各答。
  5. Many large - scale tourism projects have be located in the investment zone, such as jinyinhu international golf course, oriental horse racing ground, wuhan water country tourism project invested by hangzhou songcheng group, canadian caribbean sea water land, dalian haichang ocean polar world, hubei shengshan happy world, boquan jingde temple and zoumaling international scene park

    一批大型旅遊項目落戶我區，主要有金銀湖國際高爾夫球場、東方馬城、杭州宋城集團武漢水鄉旅遊城項目、加拿大加勒比海水上樂園、大連海昌海洋極地世界、湖北聖山歡樂世界、柏泉景德寺、走馬嶺國際風情園等項目。
  6. Abstract : monthly rainfall data from 1951 to 1995 for june, july and august in 13 meteorological stations of the north china were used for accounting z index and discussing serious flood and drought featureas in these months. serious flood mainly happened in july and august, and sevious drought mainly happened in august. there were more flood in 1950 ' s to 1960 ' s and more drought since 1970 ' s in the north china. meanwhile, the deeper trough which covered the regions from the ural mts. to the balkhash lake play an important role in serious rainstom in rainy season in the north china. there often happened serious flood ( drought ) when the northwester pacific subtropical high was by west and north ( east and south ), and the sea surface temperature in the equatorial central and eastern pacific was mainly in dropping ( raising ) stage

    文摘:利用華北平原地區的13個站點， 45年（ 1951 1995 ）的降水資料，對夏季4個時段（ 6月、 7月、 8月、 6 8月）進行了z指數計算，確定了該地區各個時段的嚴重澇年和嚴重旱年.發現華北地區雨季的嚴重洪澇主要集中在7 ， 8月，嚴重乾旱則主要發生在8月，並可明顯看出由50 60年代的多水期向70年代中期以後的少水期的轉變，另外，烏拉爾山到巴爾喀什湖附近的低壓槽加深和西北太平洋副熱帶高壓的北抬，對華北地區雨季持續性暴雨的產生起著決定性的作用.嚴重洪澇年的夏季（ 6 8月） ，西北太平洋副熱帶高壓偏西、偏北，赤道東太平洋海溫多處于下降階段;嚴重乾旱年西北太平洋副高偏東、偏南，赤道東太平洋海溫則處于上升階段
  7. From the point of view of risk, a index system of risk assessment of winter wheat losses caused by drought was established, including the meanings, token models and estimate methods of risk index of natural water deficiency rate, risk index of yield reduction rate and trending vector coefficient of disaster resistance capability, then on the base of these indices, the comprehensive risk index model of losses caused by drought was established and regionalized. the results indicated : the high risk region included the middle north of shanxi, some of middle of shaanxi and some of hebei in east ; the higher risk region included some of middle of shaanxi, the tangshan region and some of west of hebei ; the moderate risk region included the middle of s

    從風險的角度，建立了冬小麥乾旱災損風險評估的指標體系，包括自然水分虧缺率風險指數、減產率風險指數和抗災性能趨勢向量系數的意義、表徵模式和估算技術方法，在此基礎上構建了災損綜合風險模型，並對模型參數區域化，結果表明：冬小麥乾旱災損高風險區在陜西中北部、山西中部的部分地區和河北滄州的部分地區；較高風險區在山西中部的部分地區、河北的唐山地區和西部的部分地區；中風險區在陜西中部、山西南部、河北滄州的大部分地區；低風險區在陜西中南部、河南中北部、北京市、天津市、河北中南部和山東省。
  8. It is obvious that semi - quantitative was a scientific and practical method in water quality bio - assessment for macro - invertebrate assemblage sampling. ii the calculation of the tolerance value of benthic macro - invertebrate taxa 1. ninety - two samples were obtained from mountain streams in jixi, ningguo, xouning, qimeng and susong counties, anhui province, and plain waterbodies in qinghuaihe river and small water bodies in zijingshan, nanjing city, jiangsu province from 1998 - 2002

    從1998年至2002 ，在位於安徽績溪縣、休寧縣境內的新安江水繫上游支流、寧國縣的青陽河、九華山九華河上游、祁門縣境內的閶江水系和大北河水系以及宿松縣趾風河，南京秦淮河流域和紫金山地區小水體設點採集大型底棲無脊椎動物樣本，共獲92個樣本。
  9. Firstly, based on the basin prototype, the triassic and jurassic mudstone and coal, the main source rocks of the basin, did not develop better in baicheng sag than in the northern thrust belt including keyi structural belt ; secondly, because of the thrusting happened in late cenozoic, the triassic and jurassic source rocks reach to a high to over high maturity and thus generate gas or condensate oil mainly. thirdly, the thrust faults compelled the natural gas to migrate from the north to the south or from the deep to the shallow. as a result, the keyi structural belt and the eastern qiulitage structural belt enriched in natural gas because they were not only located on the migration routines of the natural gas, but also developed simultaneously when the gas migration happened

    從盆地構造史研究的角度認為庫車盆地的天然氣主要來源於北部山前沖斷帶： 1受原型盆地構造格局的制約，三疊系侏羅系烴源巖發育的最有利位置不是在拜城凹陷，而是在克依構造帶及其以北的北部山前沖斷帶2晚第三紀以來的逆沖推覆作用使得烴源巖提早進入高過成熟階段，並以產氣和凝析油為主3逆沖推覆作用所產生的北傾逆斷層控制天然氣自下而上自北而南運移，位於運移路線上的克依構造帶和秋里塔格構造帶的東段與烴源巖的排氣期匹配較好，從而使這些地區最富集天然氣。
  10. 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
  11. Since the suggested method makes a significant improvement in wind speed, it is more suitable for wind field estimation over complex terrain than other methods which only concerns the effect of distance. then we calculate the wind change with evaluation, last we can conclude the wind abase the hilly terrain, we find the wind in westward and center plain is much smaller than other area. while the wind in northward hilly area is much bigger with the hilly arising. the wind of chongqing is the biggest period in spring ( april ), the smallest period in winter ( january ), the wind in summer ( july ) is bigger than its in autumn ( october )

    本文利用重慶及其周邊地區的常規氣象站的1951 ? 1980年30年的風速平均資料，針對復雜地形風速診斷，以地理信息系統為數據處理平臺，根據重慶1 ： 25萬dem數據，來獲得重慶市實際復雜地形的高程，提出了一種適合於起伏地形的權重內插方法，通過引入一個表示地形起伏變化程度的因子，構造了一種新的權重函數，來處理復雜地形上的風速，通過與只考慮距因素同反平內插方法比較發現，本方法更適合在起伏地形條件下使用；然後根據經驗公式在地形上進行計算，得出重慶地區起伏地形下的風速分佈；得出重慶市的西部、中部平原地帶風速較小，而北部山區隨海拔高度升高風速也較大；重慶市風速最大時期為四月份，冬季一月份最小，夏季（七月份）大於秋季（十月份） 。
  12. ( 2 ) in southern china, the velocities are near average value. a little low velocities exist in the regions such as zhujiangkou, middle of guangxi, lushan and so on. a little high velocities exist in the middle region lied to the south of yangzi river and to the north of zhujiang river

    東部地區速度變化以低速異常為主：整個華北和東北地區，都呈現pn低速異常，特別是華北盆地區、渤海灣和山西地塹低速異常非常明顯，最小低於7 . 8km / s ；華南地區整體上在平均值上下，在珠江口地區、廣西中部地區、廬山地區波速略微偏低，在長江以南，珠江以北地區中部波速略微偏高。
  13. At the laoshan olympic mountain bike course in beijing sunday on november 20, 2005. no matter where he goes, or how far, us president george w. bush ' s passion for always travels with him and so does his fancy mountain bike

    11月20日下午2點多， 59歲的布希頭戴紅色自行車頭盔身著黑色上衣，配以深藍色短褲出現在北京西部老山的2008年奧運會山地車賽場，酷愛自行車運動的布希，在這里騎一把山地車
  14. The result indicates that from the north to the south, from the east to the west, the seal ability of four caprocks is better and better, the good seal areas of caprock distributes in heiyupao sag and its south. based on the research of the seal mechanism of the faults, this paper researched the vertical seal of t1 and t2 fautlts in binbei region by means of the mudstone content in fault zone and the pressure of fault plane. the result indicates the good seal areas of t2 fault for gas and oil distribute in daqing - anda and their north of binbei region, the good seal areas of t | fault for gas and oil distribute in wuyuer and heiyupao sags of binbei region

    本文通過濱北地區青山口組和嫩一、二段蓋層宏觀發育和微觀封閉能力分析，利用模糊數學綜合評價方法對濱北地區青山口組和嫩一、二段泥巖蓋層的封蓋能力進行了評價，結果表明這四套蓋層封蓋能力從北向南，從東向西逐漸變好。好蓋層封蓋能力區主要分佈於黑魚泡凹陷及其以南地區。在斷層封閉機理研究的基礎上，利用斷層面壓力和斷面填充泥質含量研究了濱北地區t _ 2層和t _ 1層斷層封閉性，結果表明濱北地區t _ 2斷層好的封油氣區位於大慶?安達以北局部地區， t _ 1層斷層好的封油氣區位於烏裕爾、黑魚泡凹陷處。
  15. A popular place to go is mandalay hill. situated a couple of hundred meters above town, it offers an excellent view over the city. there are four staircases, one from each direction

    曼德勒最負盛名的地方是曼德勒山，海拔高出市區幾百米，是俯瞰市區的最佳位置，東南西北每個方向各有一條階梯通道上山，其中一條在中途可換乘電梯。
  16. Based on the variation of light / heavy mineral components of sedimentary rocks, the typomorphic characteristics of various debris, the cathodoluminescence color of quartzes, the direction of paleocurrent and the extension of sedimentary facies, two source direction of the studied area in carboniferous and permian can be recognized, one is in bayanwusu, wulan ' ge ' er and hetaoyinshan area north of hangjinqi in the north margin of ordos, another is alashan area in the northwest margin of ordos

    在深入研究本區沉積巖輕、重礦物組分的變化、各種巖屑的標型特徵、石英陰極發光顏色、古水流方向及沉積相帶展布等基礎上，認為研究區石炭?二疊紀的物源方向主要有兩個，分別為：北緣杭錦旗以北的巴彥烏蘇、烏蘭格爾及河套陰山地區；以及研究區西北緣的阿拉善地區。
  17. ( 5 ) based on the research of the danxia landform in the northwest of the yunnan province, it analyzes the tourism resource character of the three scenery spots and its exploiting direction, function and assessing mode. it also takes the protecting measures of the tourism resource of the danxia landfonn in the northwest of the yunnan province. ( 6 ) summary and discussion

    第五，在對滇西北丹霞地貌的研究基礎上，分析了本區丹霞地貌的旅遊資源特徵，並對黎明黎光、羅古箐、石寶山的丹霞地貌旅遊資源進行了評價，分析了開發方向、功能、模式和丹霞地貌旅遊資源保護的對策措施等。
  18. Monthly rainfall data from 1951 to 1995 for june, july and august in 13 meteorological stations of the north china were used for accounting z index and discussing serious flood and drought featureas in these months. serious flood mainly happened in july and august, and sevious drought mainly happened in august. there were more flood in 1950 ' s to 1960 ' s and more drought since 1970 ' s in the north china. meanwhile, the deeper trough which covered the regions from the ural mts. to the balkhash lake play an important role in serious rainstom in rainy season in the north china. there often happened serious flood ( drought ) when the northwester pacific subtropical high was by west and north ( east and south ), and the sea surface temperature in the equatorial central and eastern pacific was mainly in dropping ( raising ) stage

    利用華北平原地區的13個站點， 45年（ 1951 1995 ）的降水資料，對夏季4個時段（ 6月、 7月、 8月、 6 8月）進行了z指數計算，確定了該地區各個時段的嚴重澇年和嚴重旱年.發現華北地區雨季的嚴重洪澇主要集中在7 ， 8月，嚴重乾旱則主要發生在8月，並可明顯看出由50 60年代的多水期向70年代中期以後的少水期的轉變，另外，烏拉爾山到巴爾喀什湖附近的低壓槽加深和西北太平洋副熱帶高壓的北抬，對華北地區雨季持續性暴雨的產生起著決定性的作用.嚴重洪澇年的夏季（ 6 8月） ，西北太平洋副熱帶高壓偏西、偏北，赤道東太平洋海溫多處于下降階段;嚴重乾旱年西北太平洋副高偏東、偏南，赤道東太平洋海溫則處于上升階段
  19. Based on the natural conditions and economic status of the hilly area in northern zhejiang, and on the plain ecological concept of traditional housing culture, this paper has studied urban and suburban green settlement of the area, set up an evaluation system for sustainable hilly inhabitancy development objects

    本論文以浙北低山丘陵地區基本住居單位為對象，針對該地區特定的自然條件和發展現狀，以該地區綠色住居研究為突破口，在發掘住居傳統文脈中的樸素生態意識基礎上，從丘陵地域人居環境著眼，確立可持續發展的目標與評價體系。
  20. Considering spatial pattern of stockbreeding industrialization in yunnan province, six stockbreeding industrial belts are divided as : 1 ) the northeast industrial belt on plateau mountain in warm temperate zone and temperate zone ; 2 ) the central industrial belt in warm temperate zone and subtropical zone ; 3 ) the northwest mountain industrial belt in temperate zone and cool temperate zone ; 4 ) the southeast industrial belt in subtropical zone and tropical zone ; 5 ) the south industrial belt in subtropical zone and tropical zone ; 6 ) the southwest industrial belt in warm temperate zone, subtropical zone and tropical zone

    在畜牧產業化發展的區域空間布局上，把全省分為6個畜牧產業帶，即滇東北山原暖溫帶、溫帶畜牧產業帶，滇中亞熱帶、暖溫帶畜牧產業帶，滇西北山地溫帶、寒溫帶畜牧產業帶，滇東南亞熱帶、熱帶畜牧產業帶，滇南亞熱帶、熱帶畜牧產業帶，滇西南亞熱帶、熱帶、暖溫帶畜牧產業帶。
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