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salinity
相关语句
  盐度
    NEW PROGRESS IN REDEFINITION OF SALINITY——THE PRACTICAL SALINITY SCALE 1978
    电导盐度定义的新进展—实用盐度标度定义(1978)
短句来源
    RELATIONSHIP OF SALINITY VARIATION WITH TIDES AND PRECIPITATION IN THE WATERS SURROUNDING QINGLAN HARBOR
    清澜港附近盐度变化与潮汐降水的关系
短句来源
    A PRELIMINARY ANALYSIS OF DISTRIBUTION FEATURES AND VARIATION SITUATION OF SALINITY IN THE SOUTHERN OF HUANGHAI SEA AND NORTHERN OF EAST CHINA SEA
    黄海南部和东海北部海区盐度分布与变化状况的初步分析
短句来源
    FINITE DIFFERENCE METHOD FOR K_H/U CALCULATED FROM THE SURFACE SALINITY DATA
    由盐度资料计算K_H/U的有限差分法
短句来源
    The Numerical Solutions of the Problem of Two-dimension Diffusion of Salinity for Hangzhou Bay (Ⅱ)
    杭州湾二维盐度扩散问题的数值解(Ⅱ)
短句来源
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    TAIWAN WARM WATER CURRENT IN SUMMER-A SECTIONAL ANALYSIS OF DATA OF TEMPERATURE AND SALINITY NORTH OF TAIWAN IN JULY, 1981
    夏季的台湾暖流水——对1981年7月台湾以北断面温资料的初步分析
短句来源
    Temperature and Salinity Characteristics of the Kuroshio at Section E
    E断面上黑潮温、特征
短句来源
    THE MODIFICATION TO SOME HYDROGRAPHIC FACTORS CALCULATION AFTER MAKING USE OF PRACTICAL SALINITY SCALE,1978 AND THE NEW INTERNATIONAL EQUATION OF STATE OF SEA WATER,1980
    1978年国际实用标、1980年国际海水状态方程的使用,给海洋水文计算中可能带来的修正
短句来源
    DISTRIBUTION CHARACTERISTICS OF TEMPERATURE, SALINITY AND DENSITY IN THE CONTINENTAL SHELF OFF EAST GUANGDONG DURING JULY 1987
    1987年7月粤东陆架区温、、密度跃层的分布特征
短句来源
    Features of Temperature-Salinity of the Tsushima Warm Current in the East China Sea in Summer and Differences of its Salinity in the Summers of 1987 and 1989
    夏季对马暖流“东海段”的温-特征及1987年和1989年夏季的度差异
短句来源
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  含盐度
    Stepwise Regression Analysis of Power Factors Affecting Deposition Quantity and Salinity in Beach Water Area of Eastern Nanhui
    影响南汇东滩水域的积泥量和含盐度的动力因子逐步回归分析
短句来源
    Systematic analysis of sediment samples from the coastal area of Jiangsu and Zhejang Provinces has revealed that the contents of trace elements of B, Sr, Rb and the ratios of B/Ga, Sr/Ba, Rb/K and the ratio of Ca/Ca+Fe in sedimentary phosphate increase gradually with the increase of water salinity.
    对海岸带沉积样品进行系统分析,表明微量元素B的含量与B/Ga比值、Sr的含量与Sr/Ba比值、Rb的含量与Rb/K比值,以及沉积磷酸盐中Ca/Ca+Fe比值,随水体含盐度增加,而含量与比值逐渐增大。
短句来源
    The majority of external sporopollen is Pinus ,and Polyopdiaceae comes next,then the herb does the lowest. (4)The sporopollen assemblage of mangrove indicates its ecological environment,and reflectes tropical marine monsoon climate,temperature,precipitation,salinity,organic content and so on. The sporopollen assemblage indicated the temperature of 21~25℃,precipitation of 1 400~2 000 mm,salinity of 4 6‰~27 6‰,and organic content of 3%~5%.
    (4)红树林孢粉组合能很好指示其生态环境,反映热带季风海洋气候,温度、降水、含盐度、有机质含量等,指示年均气温21~25℃、降水量1400~2000mm,土壤含盐度4.6%~27.8%,有机质3%~5%的生态环境。
短句来源
  “salinity”译为未确定词的双语例句
    A quasi-three-dimensional numerical prediction model of salinity structure in Bohai Sea and Huanghai Sea
    A quasi-three-dimensional numerical prediction model of salinity structure in Bohai Sea and Huanghai Sea
短句来源
    Salinity Intrusion Study in Metro Manila Arca
    菲律宾大马尼拉地区海水入侵研究分析
短句来源
    THE SITUATION AND ANALYSIS OF SALINITY INTRUSION IN COASTAL AREAS,CHINA
    中国沿海地区海水入侵现状与分析
短句来源
    Study on the intrusion of coastal low salinity water in the west of southern Huanghai Sea during spring and summer
    春夏季南黄海西部沿岸低盐水入侵温跃层现象的研究
短句来源
    The pCO_2 distribution in lower salinity region was mainly influenced by the biological activities at the side of freshwater in Yangtze estuary.
    长江口春季表层水的pCO_2分布存在着较大的不均匀性,低盐的长江淡水区生物活动应是低盐区表层pCO_2分布的主要影响因素。
短句来源
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  salinity
popularis increased markedly over the increase of the duration of exposure to salinity, and culminated after 28 days of salt stress.
      
euphratica leaves exhibited a higher capacity to exclude salt in a longer period of increasing salinity, thus limited salt-induced lipid peroxide and MP, which contributed to membrane integrity maintenance and salt tolerance of P.
      
(herb species) to variations in water and salinity stress were studied in the hyper-arid environment of the Tarim River in China.
      
canadensis seeds have a wide tolerance for different values of pH, salinity and soil moisture.
      
The results of seed germination under various environmental stresses and investigation of soil conditions indicate that well-aerated, slightly acidic soils with low salinity are suitable for the growth of S.
      
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Foraminifera and ostracods were identified from more then 400 bottom samples taken from the East China Sea. As shown by the results of the qualitative and quantitative micropaleontological analyses, the basic factor controlling the distribution of the foraminiferal and ostracod assemblages is water depth and offshore distance, although water temperature, currents and salinity have strong influence on their distribution. These general distribution patterns have been complicated by occurences of Late Pleistocene...

Foraminifera and ostracods were identified from more then 400 bottom samples taken from the East China Sea. As shown by the results of the qualitative and quantitative micropaleontological analyses, the basic factor controlling the distribution of the foraminiferal and ostracod assemblages is water depth and offshore distance, although water temperature, currents and salinity have strong influence on their distribution. These general distribution patterns have been complicated by occurences of Late Pleistocene relict fauna. Six benthic foraminiferal assemblages, each representative of increasing water depth and salinity, were recognized from estuaries to Ryukyu trench: 1. Ammonia convexidorsa-Epistominella naraensis assemblage-estuaries: 2. Ammonia beccarii var.-Elphidium advenum assemblage-water depth<55m.; 3. Bolivina cochei-Ammonia compressiuscula assemblage-50-100m.; 4. Textularia pseudocarinata-Cibicides margaritifera assemblage-100-150m.; 5. Cassidulima spp. assemblage-150-700m.; 6. Lagena spp. assemblage-700-2000m.; Accordingly, G ostracod assemblages may be distinguished as follows: 1. Albileberis sinensis assemblage-estuaries; 2. Leguminocytkereis hodgii assemblage;-<50m.; 3. Munseyella-Cytheropteron assemblage-50100m.; 4. Bairdia-Cytherelloidea assemblage-100-150m.; 5. Krithe producta assemblage-150-2000m.. There are two groups of planktonic foraminiferal species occuring in the East China Sea bottom sediments: eurythermal species such as Globigerina bulloides, Globigerina iuiniueloba and G. pumilio, and warm water species such as Orbulina universa, Globoroialia menardii. The warm water planktonic foraminifera are absent in region with water depth less than 50m., but are partly present in 50-100m. depth region and abundant beyond the 100m. isobath, thus indicating the infuence of the Kuroshio warm water current. The test size of planktonic foraminifera, the ratio of planktonic specimens to total foraminiferal mumber, as well as the ratio of ostracod to foraminiferal number increase generally with distances from coastline to trench.

东海沉积中有孔虫、介形虫定量研究的结果表明:河口、陆架内部、中部、外部、陆坡与海槽,分別具有不同的有孔虫、介形虫组合,它们受水深,水温与盐度等因素控制。

This paper tries to study the prediction of time-space variation of salinity distribution in Yantai-Weihai region of North Yellow sea by adopting the predi- cting model of optimal factorial field. In addition to describe briefly the adopt- ed predicting method, the paper gives the preliminary analysis about the notable factors which influnce the variation of salinity distribution in this region and the predicted results. The tried predicted results show that the absolute error of assembly average...

This paper tries to study the prediction of time-space variation of salinity distribution in Yantai-Weihai region of North Yellow sea by adopting the predi- cting model of optimal factorial field. In addition to describe briefly the adopt- ed predicting method, the paper gives the preliminary analysis about the notable factors which influnce the variation of salinity distribution in this region and the predicted results. The tried predicted results show that the absolute error of assembly average is 0.27‰, the relative predictimg error is about 18%, the nu- mber of stations with the predicting error less than 0.5‰. Makes up 85% of the total number of stations, and the predicted tendency is in keeping more or less with the observed materials.

本文以我国北黄海的烟威渔场为研究对象,采用优选因子场预报模式,对盐度的时空变化进行预报试验。文中对所采用的统计预报方法,作了简要介绍。对影响本海区盐度变化的显著因子及预报结果作了初步分析。预报试验表明:预报的总体平均绝对误差为0.27‰,预报相对误差在18%左右,预报误差小于0.5‰的站数占总站数的85%,预报趋势与实测资料基本一致。

Systematic analysis of sediment samples from the coastal area of Jiangsu and Zhejang Provinces has revealed that the contents of trace elements of B, Sr, Rb and the ratios of B/Ga, Sr/Ba, Rb/K and the ratio of Ca/Ca+Fe in sedimentary phosphate increase gradually with the increase of water salinity.The values of content and ratio of these trace elements, while compared with those from modern lacustrine and marine area, interpose themselves between those of marine and terrigenous environment with closer...

Systematic analysis of sediment samples from the coastal area of Jiangsu and Zhejang Provinces has revealed that the contents of trace elements of B, Sr, Rb and the ratios of B/Ga, Sr/Ba, Rb/K and the ratio of Ca/Ca+Fe in sedimentary phosphate increase gradually with the increase of water salinity.The values of content and ratio of these trace elements, while compared with those from modern lacustrine and marine area, interpose themselves between those of marine and terrigenous environment with closer affinity to the former.It suggests that the geochemical method is available in identification of characteristics of the coastal sediments and can provide evidences in recognition of similar ancient sedimentary formations.

对海岸带沉积样品进行系统分析,表明微量元素B的含量与B/Ga比值、Sr的含量与Sr/Ba比值、Rb的含量与Rb/K比值,以及沉积磷酸盐中Ca/Ca+Fe比值,随水体含盐度增加,而含量与比值逐渐增大。这些微量元素的含量与比值,同现代湖泊和海洋沉积物分析数据对比,系介于海相与陆相之间,但偏于海相。说明用地球化学法区分海岸沉积物特征是有效的,并为认识古代类似沉积层提供依据。关于泥质物中的有关元素的富集与分布,是随着沉积的自然地理环境的变化而变化的。这种变化是决定元素迁移的主要方式,并控制着沉积物内元素的分布。

 
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