長谷田 的英文怎麼說

中文拼音 [zhǎngtián]
長谷田 英文
haseda
  • : 長Ⅰ形容詞1 (年紀較大) older; elder; senior 2 (排行最大) eldest; oldest Ⅱ名詞(領導人) chief;...
  • : 谷名詞1 (兩山或兩塊高地中間的狹長而有出口的地帶) valley; ravine; gorge 2 (姓氏) a surname 3 ...
  • : Ⅰ名詞1. (田地) field; farmland; cropland; land 2. (姓氏) a surname Ⅱ動詞[書面語] (打獵) hunt
  1. The railway, on leaving benares, passed for a while along the valley of the ganges. through the windows of their carriage the travellers had glimpses of the diversified landscape of behar, with its mountains clothed in verdure, its fields of barley, wheat, and corn, its jungles peopled with green alligators, its neat villages, and its still thickly - leaved forests

    從貝拿勒斯出發,鐵路穿過一段恆河山,天氣相當晴朗,窗外顯示出比哈爾千變萬化的美麗景色:青翠的高山,生著大麥小麥和玉米的野,棲居著淺綠色鱷魚的河川和池沼,整整的村莊和四季常青的森林,幾只大象和一些單峰的駱駝正在聖河裡洗澡。
  2. There are bays and beaches and various scenic natural features. thus, it is very popular among campers. walk for about 10 minutes from university kcr station to ma liu shui pier and take a scheduled ferry

    該村位於西貢石屋山北麓,前臨赤門海峽,灣深灘廣,近岸處畦上下,中山泉流,環境極佳,是露營的好去處。
  3. The temple was originally established in 1611 in former kandakitatera - machi ( present chiyoda city ) and was moved to yanaka shimizuzaka area in 1648 and then to the current location in 1680

    16年( 1611 )神北寺町(現千代區)創建后,慶安元年( 1648 )搬遷到中清水坂,后來又于延寶8年( 1680 )搬遷到了現在的地點。
  4. On june 30 governor shintaro ishihara visited kishi memorial sports hall shibuya ward to present president tsunekazu takeda of the japanese olympic committee with tokyo s proposal for hosting the games of the xxxi olympiad in 2016

    6月30日,石原慎太郎市參觀了澀區shibuya ward的kishi紀念體育館,並向日本奧委會joc主席竹恆和提交了東京申辦2016年第31屆奧運會的請求。
  5. Abstract : because the shenfu - dongsheng mine area is located in intermediate of arid and semiarid zone, its ecological environment is very fragile. based on the fragileeco - environmental, the coal mining and construction have brought out some new environmental problems. man - made debris flow problems is the most serious of them which caused by coal mining, construction of railway and highway as wellas exploiting stone. through a great deal of experiments of artificial simulation setting water rushing to two types of slope debris flow and debris flow gully in shenfu - dongsheng mine site, the characteristics is favourable to formation of debris flow ; ( 2 ) the waste gangue is easy to initiate and is main solid material of debris flow in this area ; ( 3 ) the whole debris flow process could be observed through the model simulation experiment of debris flow gully. at present, this experiment method is the best way to analyze debris flow genesis and process

    文摘:神府東勝礦區位於黃土高原北部乾旱半乾旱過度地帶,由於煤的大量開采,誘發了大量的環境問題,尤以人為泥石流最為嚴重.本文以神府-東勝礦區人為泥石流為研究對象,採用人工放水沖刷模擬實驗的方法,分析了坡面型和溝型泥石流源地鬆散體起動、產沙、泥石流過程的特性,所得結論為: ( 1 )放水歷時、強度大,有利於泥石流的形成; ( 2 )棄土石渣易起動,是該區泥石流固體物質的主體; ( 3 )溝道型泥石流放水沖刷模擬實驗,便於觀測泥石流的全過程,坡面型泥石流放水沖刷模擬實驗,利於統計產沙、觀測侵蝕形態
  6. Because the shenfu - dongsheng mine area is located in intermediate of arid and semiarid zone, its ecological environment is very fragile. based on the fragileeco - environmental, the coal mining and construction have brought out some new environmental problems. man - made debris flow problems is the most serious of them which caused by coal mining, construction of railway and highway as wellas exploiting stone. through a great deal of experiments of artificial simulation setting water rushing to two types of slope debris flow and debris flow gully in shenfu - dongsheng mine site, the characteristics is favourable to formation of debris flow ; ( 2 ) the waste gangue is easy to initiate and is main solid material of debris flow in this area ; ( 3 ) the whole debris flow process could be observed through the model simulation experiment of debris flow gully. at present, this experiment method is the best way to analyze debris flow genesis and process

    神府東勝礦區位於黃土高原北部乾旱半乾旱過度地帶,由於煤的大量開采,誘發了大量的環境問題,尤以人為泥石流最為嚴重.本文以神府-東勝礦區人為泥石流為研究對象,採用人工放水沖刷模擬實驗的方法,分析了坡面型和溝型泥石流源地鬆散體起動、產沙、泥石流過程的特性,所得結論為: ( 1 )放水歷時、強度大,有利於泥石流的形成; ( 2 )棄土石渣易起動,是該區泥石流固體物質的主體; ( 3 )溝道型泥石流放水沖刷模擬實驗,便於觀測泥石流的全過程,坡面型泥石流放水沖刷模擬實驗,利於統計產沙、觀測侵蝕形態
分享友人