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表层水的英文

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"表层水"怎么读用"表层水"造句

英文翻译手机手机版

  • superficial water
  • surface water
  • top water

例句与用法

  • Don ' t walk through desert puddles , mud holes , or disturb surface water in any way
    不要以任何方式穿过沙漠里的水坑和泥坑,或搅动表层水
  • Dynamic changes and modeling of nitrogen in paddy field surface water after application with different doses of urea
    施用尿素稻田表层水氮素的动态变化及模式表征
  • 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
    特别添加的竹盐成份和凡士林,含有天然的防裂保湿因子,加强皮肤表层水份,防止皮肤干裂和预防冻疮产生。
  • 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
    靠近小河口地区,如俄勒冈州海岸,当风把低盐度的表层水向海洋方向吹时,涌升现象就会出现。这时,下面寒冷的、涌升上来的海水就暴露了出来。
  • 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
    结果表明: ( 1 )上海郊区中小河流氮磷和有机污染十分突出,河流表层水凯氏氮、总磷和cod _ ( cr )指标均数倍于类水的最大允许值。
  • 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
    本文首先根据几种典型下垫面条件下的土壤表层( 1 - 1m )的土壤温湿度资料,采用统计分布、功率谱分析、滤波等方法分析典型下垫面条件下土壤表层水热分布特征及其相互作用。
  • ( 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 )在盛夏高温季节,水流滞缓的小河流表层水和底层水的氮磷指标存在明显分异:底层水nh _ 4 ~ + ,水溶态磷和总反应态磷( trp )含量高于表层水;而表层水no _ 3 ~ -和no _ 2 ~ -含量高于底层水;表层水的ph和do高于底层水。
  • 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
    通过对流式细胞计测量的细胞荧光结果来看,在秋季的p3 、 e7整个混合层、 e6站40米层,春季的p2站均发现有两群不同色素含量的聚球藻( high一pe和low一pe )共存现象,极有可能分别属于不同品系,春季共存站位位置比秋季时更靠外,表明在秋季p3 、 e7等站位的共存是季节性现象,可能与此季节黑潮次表层水沿陆架坡涌升入侵到中陆架有关,水团的运动及混合使从外海迁移而来的high一pe与近岸的low一pe得以共存,在春季,由于长江冲淡水的日渐强盛,在中陆架区的共存区域有所外移。
  • 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
    其区域性形成的原因主要可能是因为各海区对冬季风异常的响应方式不同,强冬季风使得黑潮与我国近海海洋过多散热,海温降低;在西北太平洋暖池北部,强冬季风引起西风异常,从而引发异常气旋性环流,海水辐合下沉加热其表层以下海水,同时异常环流使得更多东侧异常暖水向西加热其表层水;在黑潮与亲潮交汇处的升温也主要是由于强冬季风导致的流场异常,海水辐合下沉升温。
  • ( 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 )据“箱式模型”估算年度平均南海表层水通量约为8 . 364 10 ~ 6t s的净输出,表层之下水体约有有8 . 229 10 ~ 6t s的净输入;同时到达表层溶解态无机氮、活性磷酸盐和活性硅酸盐总量中约有78 、 71和80随颗粒物质下沉到深海;其中未被分解而进入海底沉积物的颗粒态氮、磷和硅仅占由表层沉降深海颗粒态氮、磷和硅的2 . 9 、 2 . 0和8 . 2 。
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