岳山 的英文怎麼說
中文拼音 [yuèshān]
岳山
英文
takeyama-
Industry : it has five solely - owned enterprises of carbon, thermal power, light steel, pressure vessel and wall body material and six enterprises with participating shares of shandong dongyue chemical industry co., ltd, printing center of newspaper office in the middle part of shandong, sida electric, plough textile company, xinquan cast iron co., ltd, laiwu kaiyuan wanxi company
工業：擁有炭素、熱電、輕鋼、壓力容器、墻體材料等5個獨資企業，山東東岳化工股份公司、魯中晨報印務中心、思達電氣、北斗星紡織公司、鑫泉鑄鐵有限公司、萊蕪開源萬鑫公司等6家參股企業。Abstract : soil incubation experiments were conducted in lab to delineate the effect of soil temperature and soil water content on soil respirations in broad - leaved / korean pine forest ( mountain dark brown forest soil ), dark coniferous forest ( mountain brown coniferous forest soil ) and erman ' s birch forest ( mountain soddy forest soil ) in changbai mountain in september 2001. the soil water content was adjusted to five different levels ( 9, 21, 30, 37 and 43 ) by adding certain amount of water into the soil cylinders, and the soil sample was incubated at 0, 5, 15, 25 and 35 for 24 h the results indicated that in broad - leaved / korean pine forest the soil respiration rate was positively correlated to soil temperature from 0 to 35. soil respiration rate increased with increase of soil water content within the limits of 21 to 37, while it decreased with soil water content when water content was over the range. the result suggested the interactive effects of temperature and water content on soil respiration. there were significant differences in soil respiration among the various forest types. the soil respiration rate was highest in broad - leaved / korean pine forest, middle in erman ' s birch forest and the lowest in dark coniferous forest. the optimal soil temperature and soil water content for soil respiration was 35 and 37 in broad - leaved / korean pine forest, 25 and 21 in dark coniferous forest, and 35 and 37 in erman ' s birch forest. because the forests of broad - leaved / korean pine, dark coniferous and erman ' s birch are distributed at different altitudes, the soil temperature had 4 - 5 variation in different forest types during the same period. thus, the soil respiration rates measured in brown pine mountain soil were lower than those in dark brown forest and those measured in mountain grass forest soil were higher than those in brown pine mountain soil
文摘:為了研究土壤溫度和土壤含水量對闊葉紅松林（山地暗棕壤） 、雲冷杉暗針葉林（山地棕針葉林土壤）和岳樺林（生草森林土）的土壤呼吸的影響，於2001年9月在長白山進行了土壤實驗.利用增加土壤樣柱的含水量，將土壤含水量分為9 ， 、 21 、 30 、 37和43 5個等級，土壤樣品分別在0 、 5 、 15 、 25和35的溫度下保持24小時.闊葉紅松林土壤在0 （ 35范圍內，土壤呼吸速率與溫度呈正相關.在一定的含水量范圍內（ 21 （ 37 ） ，土壤呼吸隨含水量的增加而升高，當含水量超出該范圍，土壤呼吸速率則隨含水量的變化而降低.土壤溫度和水分對土壤呼吸作用存在明顯的交互作用.不同森林類型土壤呼吸作用強弱存在顯著差異，大小順序為闊葉紅松林>岳樺林>雲冷杉暗針葉林.紅松闊葉林土壤呼吸作用的最佳條件是土壤溫度35 ，含水量37 ;雲冷杉暗針葉林下的山地棕色針葉土壤呼吸作用的最佳條件是25 ， 21 ;岳樺林土壤呼吸作用的最佳條件是35 ，含水量37 .但是，由於長白山闊葉紅松林，雲冷杉林和岳樺林處在不同的海拔帶上，同期不同森林類型土壤溫度各不相同，相差4 ~ 5 ，所以野外所測的同期的山地棕色針葉林土呼吸速率應低於暗棕色森林土呼吸速率，山地生草森林土呼吸速率應高於山地棕色針葉林土的呼吸速率.圖2表1參25Soil incubation experiments were conducted in lab to delineate the effect of soil temperature and soil water content on soil respirations in broad - leaved / korean pine forest ( mountain dark brown forest soil ), dark coniferous forest ( mountain brown coniferous forest soil ) and ermans birch forest ( mountain soddy forest soil ) in changbai mountain in september 2001. the soil water content was adjusted to five different levels ( 9, 21, 30, 37 and 43 ) by adding certain amount of water into the soil cylinders, and the soil sample was incubated at 0, 5, 15, 25 and 35 for 24 h the results indicated that in broad - leaved / korean pine forest the soil respiration rate was positively correlated to soil temperature from 0 to 35. soil respiration rate increased with increase of soil water content within the limits of 21 to 37, while it decreased with soil water content when water content was over the range. the result suggested the interactive effects of temperature and water content on soil respiration. there were significant differences in soil respiration among the various forest types. the soil respiration rate was highest in broad - leaved / korean pine forest, middle in ermans birch forest and the lowest in dark coniferous forest. the optimal soil temperature and soil water content for soil respiration was 35 and 37 in broad - leaved / korean pine forest, 25 and 21 in dark coniferous forest, and 35 and 37 in ermans birch forest. because the forests of broad - leaved / korean pine, dark coniferous and ermans birch are distributed at different altitudes, the soil temperature had 4 - 5 variation in different forest types during the same period. thus, the soil respiration rates measured in brown pine mountain soil were lower than those in dark brown forest and those measured in mountain grass forest soil were higher than those in brown pine mountain soil
為了研究土壤溫度和土壤含水量對闊葉紅松林（山地暗棕壤） 、雲冷杉暗針葉林（山地棕針葉林土壤）和岳樺林（生草森林土）的土壤呼吸的影響，於2001年9月在長白山進行了土壤實驗.利用增加土壤樣柱的含水量，將土壤含水量分為9 ， 、 21 、 30 、 37和43 5個等級，土壤樣品分別在0 、 5 、 15 、 25和35的溫度下保持24小時.闊葉紅松林土壤在0 （ 35范圍內，土壤呼吸速率與溫度呈正相關.在一定的含水量范圍內（ 21 （ 37 ） ，土壤呼吸隨含水量的增加而升高，當含水量超出該范圍，土壤呼吸速率則隨含水量的變化而降低.土壤溫度和水分對土壤呼吸作用存在明顯的交互作用.不同森林類型土壤呼吸作用強弱存在顯著差異，大小順序為闊葉紅松林>岳樺林>雲冷杉暗針葉林.紅松闊葉林土壤呼吸作用的最佳條件是土壤溫度35 ，含水量37 ;雲冷杉暗針葉林下的山地棕色針葉土壤呼吸作用的最佳條件是25 ， 21 ;岳樺林土壤呼吸作用的最佳條件是35 ，含水量37 .但是，由於長白山闊葉紅松林，雲冷杉林和岳樺林處在不同的海拔帶上，同期不同森林類型土壤溫度各不相同，相差4 ~ 5 ，所以野外所測的同期的山地棕色針葉林土呼吸速率應低於暗棕色森林土呼吸速率，山地生草森林土呼吸速率應高於山地棕色針葉林土的呼吸速率.圖2表1參25The study results on hydrocarbon preserving conditions have suggest ed that influenced by latter tectonic movements, especially by the yanshan ~ himalayan tectonic movement, obviously different hydrocarbon preserving conditions occur between the eastern and the western parts bounded by the qiyue mountain. the whole lower paleozoic hydrocarbon enclosing and preserving conditions for the shizhu synclinorium - fangdoushan antici inorium to the west of qiyueshan mountain have the advantage over those of the qiyueshan antici inorium - lichuan synclinorium to the east of qiyue mountain
通過油氣保存條件的研究認為：受後期構造運動的影響，尤其是燕山期?喜山期構造運動的影響，造成區內以齊岳山為界東西油氣保存條件存在明顯差異，齊岳山以西的石柱復向斜?方斗山復背斜下古生界油氣整體封存條件明顯優于齊岳山以東的齊岳山復背斜?利川復向斜。Firstly, thesis has been analysed the enterprise present situation, the problem that exists aspect has pointed out the enterprise in the selection in objective market and competitor analyses and positioning etc
論文是以山東光岳轉向節總廠營銷戰略規劃為主線，按照提出問題、分析問題、解決問題的邏輯思路展開。For example, tai mountain is called " east yue " as it is the easternmost one of the five
如泰山是五嶽中最東的一座，因而名為東岳。Hunan, hengshan city two major advantage of the integration of resources will certainly attract the world " from the oil, " jia, diners gathered jugaku ancestor worship food culture
湘菜、衡山我市二大優勢資源的整合，一定會招攬天下「油領」賈商、食客雲集壽岳祭拜飲食文化先祖。I companies in western china anqing city zen one hill - - il foothills, 1997 from anhui province investment group, yuexi county utilities group jointly established. 5 million yuan of registered capital. hydroelectric power generation companies to mainly installed two 1, 000 kw, the average years of 5 million kilowatt hours of electricity. annual profit since its founding companies, year over taxes 150, 000 yuan or more
我公司位於安慶市西部中國禪宗第一山- -司空山麓，一九九七年由安徽省投資集團，岳西縣水電集團共同投資創建.注冊資本500萬人民幣.公司以水電發電為主，裝機兩臺1000千瓦，多年平均水電量500萬千瓦時.公司自創建以來年年贏利，年上繳稅金十五萬元以上The lofty spirit of director yue feng
楓骨凌霜映山紅岳楓導演According to the chinese ancient mythology, when pangu, the ancestor of all things, died, his head turned into mount tai, his belly turned into the central mountain, his left arm turned into the south mountain, his right arm turned into the north mountain and his feet turned into the west mountain
中國古代神話傳說，天地萬物之祖盤古氏死後，頭部化作東岳泰山。據梁人任日方撰的述異記： 「昔，盤古之死也，頭為四岳，目為日月，脂膏為江海，毛發為草木。Because of nanyue mountain ( chang shou - shan ), shek kwu college ( song taizong treason 2003, the national academy of four ), with wang chuan, cai lun, fu li, peng yu - scales, and other celebrities and the birth of the precipitation value xiang cultural uniqueness yanfeng rain, shek kwu jiangshan, anther spring river, xue - ling yue ping, zhu ling shidong, grass white wine bridge home, the west lake night - white lotus, look at the east, and warm peach wave steaming mountain city shigu, hunan, lei sanshui in this intersection and the huang director
因受南嶽衡山（五嶽壽山） 、石鼓書院（宋太宗至道三年，全國四大書院之一）影響，隨著王船山、蔡倫、李芾、彭玉鱗等眾多名人的誕生而沉澱了衡湘文化的精髓，雁峰煙雨、石鼓江山、花藥春溪、岳屏雪嶺、朱陵詩洞、青草橋頭酒白家、西湖夜放白蓮花、細看東州桃浪暖及市內石鼓山下蒸、湘、耒三水在此交匯而名遐三湘。H ua yan ( 1682 - 1756 ), alternatively named qiuyue and nicknamed xinluo hermit. he was good at painting people, mountains and water, and was especially good at flower, bird, grasses and insects
華? （ 1682 1756年） ，福建汀州人，清代著名畫家。字秋岳，號新羅山人。擅畫人物、山水，尤精花鳥、草蟲，自成風貌，為一時之冠。The eastern part of the mural illustrates " setting off on the tour ", while the western part, " returning to his palace "
殿壁繪東岳山神出巡壁畫，名啟蹕回鑾圖。In the south to ancient huizhou, is the grand high mountain huangshan ; and in the north to huangshan, is feida s glorious enterprise
古徽州以南，是黃山的巍峨雄姿黃岳以北，有飛達的煌煌大業。Shandong luyue chemical industry co., ltd. is situated at the foot of taishan mountain
山東魯岳化工有限公司位於馳名中外的泰山西麓，風景秀麗的肥桃之鄉。Join us on a trip to the major tourist spots or sites of historical interests in china such as the tiansha prairie, yangguan checkpoint, hukou fall of.
分別展現天山牧場陽關黃河壺口瀑布圓明園巴音布魯克草原樂山大佛外漢夜景安岳臥佛天壇地壇等大自然的莊麗風光及鬼斧神工。A classical kung fu tv drama produced by hong kong asia tv about the love and hatred between the kung fu practitioners.
明知山有虎，偏向虎山行。劇情峰迴路轉，不是冤家不聚頭，南滄海，北鐵山，一岳擎天決世間。Since 1992, professor tsao has headed the long - term, nation - wide ritual music in china research programme rmcrp. under the support of competitive granting organizations such as the chiang ching - kuo foundation for international scholarly exchange and the research grants council, the rmcrp has completed several large - scale projects
曹本冶教授的主要著述作包括： 《海上白雲觀施食音樂研究》 ， 《武當山道教音樂研究》 ， 《杭州抱撲道院道教音樂》 ， 《溫州平陽柬岳觀道教音樂研究》 ， 《中國道教音樂史略》 ， 《虎山天師道科儀音樂研究》 ，( 2 ) the most favorable region of gas formation lays inside of the shizhu synclinore and in the west of fangdou mountain block. the secondary favorable region is from zichuya region to longjuba region. the adverse region lays qiyue mountain structure including west of it and fangdou mountain structure
成藏的有利區位於石柱復向斜內和方西區塊；成藏的較有利區位於茨竹埡? ?龍駒壩地區；成藏不利區位於齊岳山及其西翼、方斗山等地。Western hubei and eastern chongqing region lays southeast border of sichuan basin with its area about 9500 km2. qiyue mountain anticlinal structure is on the east of it and changjiang river on the west of it
鄂西渝東區位於四川盆地東南緣，齊岳山背斜帶以西，長江以東，面積約9500km ~ 2 。分享友人