表層水 的英文怎麼說
中文拼音 [biǎocéngshuǐ]
表層水
英文
superficial water- 表 : Ⅰ名詞1 (外面;外表) outside; surface; external 2 (中表親戚) the relationship between the child...
- 層 : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
- 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...
- 表層 : skin layer; superficial coat; veneer; surface; sexine; bloom; supercrust; surface layer表層沉積 [...
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The bamboo salt specially added into the product contains natural anti - chapping and moistening elements so as to strengthen skin ' s water supply and prevent skin dryness and chilblain growth
特別添加的竹鹽成份和凡士林,含有天然的防裂保濕因子,加強皮膚表層水份,防止皮膚乾裂和預防凍瘡產生。For a time, surface and subsurface current are in opposite directions ; flow is seaward at the surface and landward near the bottom
在一個時期,表層和次表層的水流方向相反;表層水流向外海方向流動,靠近底層的水流則向陸地方向流動。For a time, surface and subsurface currents are in opposite directions ; flow is seaward at the surface and landward nearthe bottom
譯為:有一個時期,表層和次表層的水流方向相反,表層水流向外海方向流動,靠近底層的水流則向陸地方向流動。However it seems that the distribution and abundance of euphausia superba was related to the cold water mass exist at 30 - 100 m, and with the confluence area between the high and the low chi a centers at 25 m depth
調查期間大磷蝦的分佈與表層水溫、鹽度及葉綠素的關系不明顯,但似乎與30 - 100m處的冷水團和25m深度處的葉綠素高值中心和低值中心的交匯區有關。Dynamic changes and modeling of nitrogen in paddy field surface water after application with different doses of urea
施用尿素稻田表層水氮素的動態變化及模式表徵Road and airfield surface characteristics - test methods - part 3 : measurement of pavement surface horizontal drainability
道路和機場表面特徵.試驗方法.第3部分:路面表層水平排水能力的測量The condition of profiles in outer station did n ' t change much in spring cruise, but showed more variable in near - shore stations when observed in different time. fluorescent characteristic per cell can be obtained by flowcytometric analysis. based on fluorescence data of synechococcus of all stations, two distinctly pigment - containing cell types coexisting can be found in some stations of east china sea, which located in all depth of p3, mixlayer of e7, 40 - meter depth of e6 of autumn cruise and in mixlayer of p2 of spring cruise
通過對流式細胞計測量的細胞熒光結果來看,在秋季的p3 、 e7整個混合層、 e6站40米層,春季的p2站均發現有兩群不同色素含量的聚球藻( high一pe和low一pe )共存現象,極有可能分別屬于不同品系,春季共存站位位置比秋季時更靠外,表明在秋季p3 、 e7等站位的共存是季節性現象,可能與此季節黑潮次表層水沿陸架坡涌升入侵到中陸架有關,水團的運動及混合使從外海遷移而來的high一pe與近岸的low一pe得以共存,在春季,由於長江沖淡水的日漸強盛,在中陸架區的共存區域有所外移。Don ' t walk through desert puddles, mud holes, or disturb surface water in any way
不要以任何方式穿過沙漠里的水坑和泥坑,或攪動表層水。Near small river, as along the oregon coast, upwelling can occur when winds move the low - salinity surface layer seaward and the cold, upwelled waters underneath are exposed
靠近小河口地區,如俄勒岡州海岸,當風把低鹽度的表層水向海洋方向吹時,涌升現象就會出現。這時,下面寒冷的、涌升上來的海水就暴露了出來。Water quality of the middle and small creeks in xianghuaqiao town, suburban shanghai has been monitored for more than one year. it indicates that : ( 1 ) the creeks are under heavy eutropic condition, with high loadings of nitrogen, phosphorus and organic pollutants
結果表明: ( 1 )上海郊區中小河流氮磷和有機污染十分突出,河流表層水凱氏氮、總磷和cod _ ( cr )指標均數倍于類水的最大允許值。In this paper, on the basis of observed data, spatial - temporal variation characteristics of soil temperature and soil moisture. soil temperature effects on soil water movement are studied for several kinds of typical underlying surface by using statistics, spectrum, filtering wave methods
本文首先根據幾種典型下墊面條件下的土壤表層( 1 - 1m )的土壤溫濕度資料,採用統計分佈、功率譜分析、濾波等方法分析典型下墊面條件下土壤表層水熱分佈特徵及其相互作用。( 4 ) at the height of the summer, the surface and bottom water of the creeks differed in n and p loadings. nh4 +, soluble p and total reactive p in the bottom water were higher than those in the surface ; while no3 - and no2 - in the surface were higher than those in the bottom. such water - quality stratification inevitably resulted from the enhancement of phytoplankton in the surface water and intensified release of nh4 + and p from the sediments
( 4 )在盛夏高溫季節,水流滯緩的小河流表層水和底層水的氮磷指標存在明顯分異:底層水nh _ 4 ~ + ,水溶態磷和總反應態磷( trp )含量高於表層水;而表層水no _ 3 ~ -和no _ 2 ~ -含量高於底層水;表層水的ph和do高於底層水。Genetic analysis shows that it may be caused by the difference of the response of each area to winter monsoon ' s abnormal, the kuroshio and our offshore is influenced mostly by heat flux between the sea and atmosphere, but in the other areas, the abnormal current incited by abnormal wind has decisive effect on the change of the sea temperature, at the same time, air pressure also has some impact on the sea temperature
其區域性形成的原因主要可能是因為各海區對冬季風異常的響應方式不同,強冬季風使得黑潮與我國近海海洋過多散熱,海溫降低;在西北太平洋暖池北部,強冬季風引起西風異常,從而引發異常氣旋性環流,海水輻合下沉加熱其表層以下海水,同時異常環流使得更多東側異常暖水向西加熱其表層水;在黑潮與親潮交匯處的升溫也主要是由於強冬季風導致的流場異常,海水輻合下沉升溫。( 3 ) box model results indicate that the net flux of suface water, flowing into the south china sea, is about 8. 364x 106t / s and the net flux of water, which is under suface water, flows out of the south china sea at about 8. 229x 106t / s on annual average. the quantity of din, reactive phosphate or reactice silicate, which sinked into deep water in the form of particle matter, was about 78, 71 and 80 percent of total quantity of din, reactive phosphate and reactive silicate, which flowed into suface water in any ways. but in these particle matters, ahout2. 9 percent of particle nitrogen, 2. 0 percent of particle phosphor and 8. 2 percent of particle silicon sinked into sediment
( 3 )據「箱式模型」估算年度平均南海表層水通量約為8 . 364 10 ~ 6t s的凈輸出,表層之下水體約有有8 . 229 10 ~ 6t s的凈輸入;同時到達表層溶解態無機氮、活性磷酸鹽和活性硅酸鹽總量中約有78 、 71和80隨顆粒物質下沉到深海;其中未被分解而進入海底沉積物的顆粒態氮、磷和硅僅占由表層沉降深海顆粒態氮、磷和硅的2 . 9 、 2 . 0和8 . 2 。Compared with water temperature and the monthly alternatives of fish was much significant
漁獲種類的季節變化比較明顯,與海洋表層水溫變化有關,種類的月更替率比較高。Both the he and m communities were consisted of species belonging to diverse ecotypes, but temperate species was more dominant in he while
多元回歸分析表明,表層水溫、鹽度是對浮遊動物的分佈、群落劃分較為重要的環境因子。The species composition of fish varied significantly with seasons, particularly high with monthly alternatives, and associated with changes of water temperature
漁獲種類的季節變化比較明顯,種類的月更替率比較高,與海洋表層水溫變化有關。The diverse phytoplankton species inhabiting the ocean ' s surface waters ? which mainly consist of single - celled cyanobacteria, diatoms and other kinds of algae ? form the base of the marine food web
這表層水域里住了各式各樣的浮游植物(以單細胞的藍綠藻、矽藻和其他藻類為主) ,形成了海洋食物網的基礎。With the increase of temperature and biomass, nh4 + and no3 - in the surface water were largely consumed and decreased as a result ; while organic n and particle p increased as the enhancement of suspending biological particles. no2 - in the surface water increased with temperature as nitrifying bacteria became active
隨著氣溫升高和河流表層生物量的增大,表層水nh _ 4 ~ + 、 no _ 3 ~ -因大量消耗而降低;有機氮和顆粒態磷含量因生物顆粒的增加而加大; no _ 2 ~ -也會因硝化細菌活動的加劇而增加。Standard guide for use of hollow - stem augers for geoenvironmental exploration and the installation of subsurface water - quality monitoring devices
亞表層水質檢測裝置安裝和地理環境勘探中空螺旋鉆使用的標準指南分享友人