海雲關 的英文怎麼說
中文拼音 [hǎiyúnguān]
海雲關
英文
hai van pass-
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1參25However, the rumor of his being the illegitimate son of the station s biggest shareholder yan yue hin kwan hoi shan makes a stir in the industry
當他叱吒風雲之際，忽傳出他乃是大股東甄汝軒關海山的私生子，此事震撼整個播音界。Hanhaixingyun bbs secondhand market of university of science and technology of china closed up
科大瀚海星雲bbs二手市場版宣告關閉。The main relative systems of heavy - hard rainfall in northeast plateau are western pacific subtropical high, south asia high, low latitude systems, upper level jet ( ulj ), low level greater wind speed axes, westerly trough and plateau trough, low level vortex, cold frontal, occluded front in qinghai lake, mesoscale low pressure, heat low - pressure in qinghai, shear line and convergence line, mesoscale cloud cluster, etc. the west subsidiary model of south asia high is the main circulation type of heavy - hard rainfall in this area
3 、西太平洋副高、南亞高壓、低緯系統、高空急流、低空大風速軸；西風槽和高原槽、低渦、冷鋒、青海湖錮囚鋒以及中尺度低壓、青海熱低壓、切變線與輻合線、中尺度雲團等系統是高原東北部地區大到暴雨的主要相關系統。 100hpa上的南亞高壓中心強度加強，位置東西擺動預示高原地區將有降水產生，中心強度減弱，降水過程結束。南亞高壓西部副型是高原東北部地區大到暴雨的主要流型。A group of well - known businessmen gathered here from tiejun jewelry, zhenwei collections, liuhe hall, feicui lot, hong changyu carving, min ren fu ; a number of cultural organizations have settled here such as haidian federation of literature and art, zhongguancun club and the chamber of calligraphy and paintings of the beijing federation of industry and commerce
鐵軍珠寶、真唯藏、六合堂、翡翠緣、鴻昌玉雕、民仁福等一批知名商家雲集於此；海淀文聯、 《中關村》俱樂部、北京市工商聯書畫會等一批文化組織落戶於此。The yacht always leads us through difficulties, as in the poem " hard is the way of the world " by li bai, " i ll set my cloud - white sail and cross the sea which raves.
鳴帆將帶領我們跨過重重難關，正如李白行路難一詩描述：長風破浪會有時，直掛雲帆濟滄海The neogene is a key stage of terrestrial environmental evolution in yunnan. three stratigraphic sections including luhe ( late miocene ), yangyi and longling ( late pliocene ) were selected to reconstruct vertical landscape of paleovegetation in these areas, based on palynological data. according to principle of the coexistence approach, seven quantitative paleoclimatic parameters of each deposit area were obtained by using meteorological data ( 1951 - 1980 ) of the distribution area of extant taxa found each palynoflora in china
晚第三紀是雲南地區環境演變過程中的關鍵地質歷史時段，本論文以晚第三紀晚中新世（呂合） 、晚上新世（羊邑和龍陵）地層中的孢粉為研究對象，結合同層位大化石植物證據，參照現代植被，恢復了雲南三個化石出產地區的古植被垂直分佈景觀，並定性地描述了古氣候；同時運用共存分析方法（ theco - existenceapproach ）定量化地重建了三個地區的古氣候參數值；初步推測了沉積地可能的古海拔。“ hoist the greatest sail to the blue sea : a manchurian scholar guan jixin and his research work ”. shenyang : studies of manchu nationality, no. 3, 2001, serial no. 64. pp. 58 - 63
「直掛雲帆濟滄海：當代滿族學人關紀新的學術軌跡」 ， 《滿族研究》 2001年3月號，第58 ~ 63頁。沈陽。The interannual and decadal variability of precipitation for yunnan province in rainy season and its relationship with tropical upper layer heat content
雲南省雨季降水的年際年代際變化特徵及其與熱帶上層海洋熱含量分佈的關系Its interannual variation ' s main period is about 4 ~ 5a and the 7 ~ 8a ' s period exist too ; the interdecadal variation ' s main period of the australian high is about 15a. the interannual variation of australian high ( aah ) has correct correlation with antarctic oscillation and enso, and the enso ' s 4a period has the most important influence on the aah. ( 2 ) when the ah becomes stronger, the members of the whole aamcs are stronger following it. that is to say, in the years that the ah is stronger ( compared to the weak years of ah ) and on the horizontal circulation, the members of aamcs, including the ah, the cross - equator flow ( cef ) between 100 and 160 e, the south china sea south - west monsoom ( ssm ), the south sea monsoon rough, the tropical easily flow, subtropical high ( sh ), the mei - yu front, the mid - latitude effect, become stronger, and their positions are more southward ; in the meridional - right circulation, there are five circulations including classic monsoon meridional - cirle circulation and hadley circulation that become stronger in the strong years of ah than in the weak years of ah
本文採用ncep ncar再分析月平均的全球海平面氣壓場、高度場、海表溫度場、高雲量和cmap全球降水資料，以及中國160站逐月降水資料，分析了1948 2002年期間澳大利亞高壓（以下簡稱澳高）的年際和年代際變化以及澳高年際變化對亞澳季風環流系統的影響，結果顯示： （ 1 ）澳高存在明顯的年際和年代際變化，澳高年際變化以4 5年的周期變化為主，同時兼有7 8年左右的周期，而澳高的年代際變化則以15年左右的周期變化為主：澳高年際變化同時與南極濤動和enso有正相關，並且enso的4年左右的周期變化對澳高年際變化影響最大。It starts from haihe in the east, and looks at hebei district each other ; it borders on heping district and hexi district from rongji street, xingan road, and south street to south door outer street, weijin road, and weijin south road ; it reaches miyun road, jieyuan west road, and the lateral of chentangzhuang railway in the west and south, and is joined with xiqing district ; it reaches old iron bridge street and north road in the north, and abuts with hongqiao district from west road to xiguan road, qiangzi river, and south canal
東起海河，與河北區相望沿榮吉大街興安路南馬路至南門外大街衛津路和衛津南路，分別與和平區河西區接壤西南至密雲路芥園西道陳塘莊鐵路支線，與西青區相連北抵老鐵橋大街北馬路，沿西馬路至西關大街墻子河南運河，與紅橋區毗鄰。Every day there are 2 - 4 million stems of fresh flowers are traded on the market. some of them have found their way to many cities of china and other countries. in recent years, the importance of the flower trade has been repeatedly stressed by the scientific community and the government of the province
目前，對雲南省的花卉進出口，根據其鮮活特點，海關設立了「綠色通道」 ，採取相應靈活便利措施，做到花卉進出口手續隨到隨驗，節假日和八小時以外的時間實現預約制。1. based on the data of analysis, using theories and methods of mathematical statistics, two of interception models by canopy of picea crassifolia are established as follows : the regression model on the relationship between penetration rainfall ( p, ) inside forest and total rainfall ( p ) outside of forest : pj = 0. 8245p - 1. 372 ( r = 0. 99 ) ; the model on the relationship between interception rate ( ir ) and rainfall : ir = - 10. 7111n ( p ). ( r = 0. 7524 ) the results show that penetration rainfall inside forest increases with total rainfall outside of forest in linearity, and to certain extent, penetration rainfall inside by canopy also increases with total rainfall outside ; the correlations of the interception rate to rainfall and intensity of rainfall are significant and the intercepted rate by canopy of picea crassifrlia is diminished with the increase of rainfall and rainfall intensity, and increase with the increase of canopy density
1在利用數理統計原理和方法對實測資料進行綜合分析的基礎上，建立了青海雲杉林林冠截留降水模型：林內透過雨量與降雨量回歸模型： p _ i = 0 . 8245p - 1 . 372 （ r = 0 . 99 ） ；林冠的截留率與降雨量的模型： i _ r = - 10 . 711ln （ p ） （ r = 0 . 7524 ） ；分析模型表明：林內透過雨量與降雨量呈良好的線性關系，在一定的降雨量范圍內，林內透過雨量隨降雨量的增加而增加；林冠截留率與降雨量、降雨強度之間也呈良好的關系，林冠截留率隨降雨量和降雨強度的增大而減小，隨郁閉度的增加而增大。Other leading deities include kwan tai ( god of war and the source of righteousness ), pak tai ( supreme emperor of the dark heaven and local patron of the island of cheung chau ) and hung shing ( god of the south seas and a weather prophet )
其他廣為人知的神明有義薄雲天的武聖關帝、號稱玄天上帝的長洲守護神北帝，以及司掌天氣的南海之神洪聖。No. 33 pingan south road shijiazhung
秦皇島市山海關開發區雲南南路2號The historical development of the chinese associations in malaysia, originally known as cheng hoon teng temple in 1673 and lasting until the 21st century, is divided into four periods, which are the beginning period ( 1673 - 1799 ), the inward developing period ( 1800 - 1899 ), the outward developing period ( 1890 - 1945 ), and the comprehensive developing period ( from 1945 till now ). the thesis analyzes not only the historical developing processes of the associations of hokkien pang, cantonese pang, hakka pang, teochew pang, hainanese pang, and so forth, but also those of the localized associations, the lineage associations, the business associations, the cultural associations, the religious associations, the charitable associations, and other associations during each period. it discusses the interaction relation between the chinese associations, and chinese society, malaysian society and chinese society in malaysia
本篇博士論文把從1673年青雲亭的創建開始至21世紀初的馬來西亞華人社團的發展歷史劃分為雛型時期（ 1673 ? 1799年） 、內向發展時期（ 1800 ? 1889年） 、外向發展時期（ 1890年至二戰結束前） 、全面發展時期（二戰后至今） ，按每個時期分別分析福建幫、廣東幫、客家幫、潮州幫、海南幫等各幫派華人社團的歷史發展；分析馬來西亞華人地緣性社團（宗鄉會館） 、血緣性社團（宗親會館） 、業緣性社團、文（學）緣性社團、宗教社團、慈善性社團等各類型華人社團的歷史發展過程；論述在這一歷史發展過程中，馬來西亞華人社團和中國社會、馬來西亞社會、馬來西亞華人社會的互動關系，以及馬來西亞華人社團內部的互動關系，總結幾種互動關系的規律、特點、作用、影響，探討互動理論在研究海外華人社會和華人社團歷史發展時的可行性。The conception of building lianyungang a city centre proper surrounding linghong by the sea
關于建設連雲港市臨洪濱海中心城區的構想Mengla customs authority of yunnan province detected two infringement cases in succession, realizing zero - breakthrough in the number of detected cases in kunming customs district
雲南省勐臘海關連續查獲兩起侵權案件，使昆明關區在知識產權案件查獲方面實現了「零突破」 。However, recently i have received complaints that owing to the serious shortage of public transport services to and from some housing estates in remote locations, such as horizon place in kwai chung, rambler crest in tsing yi and the cliveden in tsuen wan, these housing estates need to apply for operating residents bus services between the estates and the mtr stations. however, such applications have been repeatedly rejected by the government, causing inconvenience to the residents of the estates concerned
然而，本人最近接獲投訴，指部分位於偏遠地區的屋苑，例如葵涌月海灣、青衣藍澄灣及荃灣寶雲匯等，公共交通服務嚴重不足，故此需要開辦居民巴士服務，接載屋苑居民往返地鐵站及屋苑，但開辦有關服務的申請卻屢遭政府拒絕，為該等屋苑的居民帶來不便。分享友人