海水帶 的英文怎麼說

中文拼音 [hǎishuǐdài]
海水帶 英文
belt of sea
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  • 海水 : seawater; brine; the sea海水剝蝕 [地質學] marine denudation; 海水淡化 desalination of sea water; ...
  1. Surrounded by sugar - white beaches, an electric - blue lagoon, and some of the clearest water on the planet, bora - bora is home to hundreds of species of tropical fish

    波拉波拉島有著白糖似的沙灘，鐵藍色的礁湖，還有世界上最清澈的海水，是數百種熱帶魚類的產地。
  2. Suitable for clean water, sea water, chemical liquid carrying acid and alkali, and general mushy slurry ( medium viscosity 100 centipoise, solid content below 30 % )

    適用於清水、海水及帶有酸、堿度的化工介質液體和帶有一般糊狀的漿料（介質粘度100厘珀、含固量可達30 %以下） 。
  3. If water in the coral reef area is contaminated by poisonous algae or dinoflagellates containing ciguatoxin, the small fish might carry the ciguatoxin due to consumption of these poisonous algae or dinoflagellates. if a larger fish then eats these small fish, the poison will likewise be accumulated in the larger fish s body. the larger the fish, the larger the amount of toxin it contains

    假使海水受帶有雪卡毒素的單細胞海藻類生物所污染，當海洋中的小魚吃下了海藻，毒素便會積聚在其體內，若大魚吃下這些小魚，毒素在大魚體內積聚更多，故此越重越大的海魚含毒量越高。
  4. Benthic foraminifer fauna, ams14c dating and acoustic sub - bottom profile was analyzed in the core ey02 - 2 and ey02 - 1 drilled from the muddy deposit in the middle southern yellow sea and the mid - shelf of north east china sea. considering the results of core qc2 ? dz4 and the standard oxygen isotope curves, we discussed the late - quaterenary paleo - environment evolution, benthic foraminifer fauna, paleo - climate, the climate events and water mass in postglacial period, average sedimentation rates, paleo - water depth, origin of sediments, average sea level rise rate in the shelf of south yellow sea and east china sea. at last we discussed the condition of sea level rise in the east china, green house effect and the protection of coastal zone

    本文根據南黃海中部泥質區和東海中陸架的兩個鉆孔巖芯的古生物、 ams ~ （ 14 ） c測年、淺地層剖面等，參考qc _ 2 、 dz _ 4成果及標準氧同位素曲線探討了黃東海陸架晚第四紀古環境演化、底棲動物群特徵、古氣候、冰後期以來氣候事件、古水團、沉積速率、古水深、沉積物源、海平面平均上升率，討論目前中國東部海平面上升的狀況、溫室效應及海岸帶保護。
  5. Apple pieces apple dices ; cherries in syrup no stem, no stone ; cherries in syrup stem, whole ; baby - apples in syrup stem, whole ; canned mushroom ; fruit cocktails in syrup ; canned apple solid pack ; canned yellow peaches in syrup ; canned white peaches in syrup ; canned apricot in syrup ; canned grape in syrup ; canned pear halves in syrup

    糖水酸櫻桃去把，去核;蘑菇罐頭;什錦水果罐頭;干裝蘋果;糖水海棠帶把，整粒;糖水黃桃罐頭;糖水杏;糖水葡萄去核去皮;糖水洋梨;蘆筍罐頭;茄汁鯖魚;煙熏貽貝
  6. In middle and late periods of the early permian, the pre - caspian areas rose successively, the climate became dry, and the environment turned to be supratidal zone ( evaporitic environment ), resulting in the spread sedimentation of salts and the formation of the salt sediment group ( the upper part of the lower permian ) which consists mainly of halite and anhydrite

    早二疊世中後期由於持續構造抬升，盆地氣候變得乾旱，海水變淺，潮上帶蒸發環境發育，以致這一時期廣泛發育鹽類沉積，形成含鹽層系，主要由鹽巖和硬石膏層構成，並形成許多大小不等的鹽丘構造。
  7. It includes open marine water, intertidal mudflats, mangal, and a small area of freshwater habitat

    區內有開闊的海水生境潮間帶泥灘紅樹林及小片淡水生境。
  8. During the winter dry season, the kuroshio oceanic current brings warm water of high salinity from the pacific through the luzon strait

    在乾旱的冬季，黑潮海流把高鹹度的溫暖海水由太平洋經呂宋海峽帶入本港。
  9. The shengyuan logistics co., ltd., of taizhou, locate in the middle part of shanghai - guangzhou gold coast zone, the most developed economy area, where there is chinese valve door, and one natural deep water good harbour group undeveloped - damaiyu harbour of yuhuan, zhejiang. landway connects shanghai - fujian speedway

    臺州生源物流有限公司，地處滬穗黃金海岸帶中部，經濟最發達區域，中國閥門之都，國內尚未開發天然深水良港群浙江玉環大麥嶼港，陸上滬閩交速公路連接。
  10. The area around kwun tong s foothills including kowloon bay, was originally a tract of saltpans from which the government revenue was generated through production of salt and collection of taxes from salt - producers. it was said that the original name for kwun tong ( literally means government owned ponds ) was derived from these saltpans, which were similar to ordinary ponds when filled up with seawater and largely owned by the government

    觀塘山麓一帶包括九龍灣在內，原是一片鹽場，而產鹽及向制鹽商徵收稅項便成為當時政府的收入來源。觀塘的原名為官塘，字面解作由官府擁有的池塘。據說，由於注滿海水的鹽場貌似池塘，加上大部分的鹽場均由官府擁有，所以得此名稱。
  11. He wore rough clothes that smacked of the sea.

    他穿著帶有海水氣息的粗布衣裳。
  12. 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1參25
  13. 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 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1參25
  14. Biological activities are also vigorous at the boundaries of freshwater and shelf water, including the boundaries of water masses and the upwelling areas. the sink of co2 is thus further enlarged

    沖淡水帶來了大量的營養鹽，促進了生物活動的發展，必然消耗大量的coz ，使海水成為大氣co :的匯區。
  15. Anne took helen to the water pump in the yard

    安妮把海倫帶到院子的抽水機旁。
  16. If a decadal positive temperature anomaly occurs in the eastern tropical pacific, the atmospheric response excites a anticyclonic wind stress anomaly in the east of australia, which will lead to generate a negative temperature anomaly in the western tropical south pacific

    當熱帶東太平洋的海溫為暖異常，它將激發澳大利亞的東部沿岸的大氣產生反氣旋性風應力異常，在這種風場的作用，下方海水向四周輻散，導致熱帶西南太平洋的溫躍層變淺，產生負的溫度異常。
  17. Hanging on to a plank or astride of a beam for grim life, life - belt round round him, gulping salt water, and that s the last of his nibs till the sharks catch hold of him

    拼死拼活地抓住一塊板子，或跨在一根桁條上，身上纏著救生帶， 161嘴裏灌進海水。這是他最後的掙扎了，直到被鯊魚捉住。
  18. Based on the analysis mentioned above, a conceptual diagram explaining the physical process is put forward : stronger ( weaker ) convective activities in tropical areas stronger upward ( downward ) vertical anomaly stream in tropical areas more ( less ) moisture transports from " key regions " to shandong stronger ( weaker ) hadley and walker circulation stronger ( weaker ) east asian summer monsoon eap ( negative eap ) in 500hpa upward ( downward ) vertical anomaly stream rise in shandong subtropical high abnormally located northward ( southward ) more ( less ) rain in shandong province

    弱季風年與山東夏旱年則相反。通過分析山東夏季降水與東亞夏季風以及大氣環流異常的物理過程，得出了如下物理概念模型:熱帶印度洋以及南海-熱帶西太平洋地區對流加強（減弱）吟熱帶地區垂直上升（下沉）氣流增強崢熱帶印度洋和南海一西太平洋地區水汽輸送通量增加。
  19. Intertidal flat is a place where seawater constantly rises and falls. as a vanguard zone where sea and land interact, the features of intertidal flat are largely on behalf of the characteristics of its own coast

    潮灘是海岸帶中的海水漲落地段，時而出露水面，時而被海水淹沒，它作為海陸交互作用的前鋒地帶，其特徵在很大程度上代表了所在海岸的性質。
  20. Let the invigorating waters bring you into the present moment of a new awakening

    就讓這令人振作的海水馬上帶你進入一個嶄新的意識幻覺吧！
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