...海的高密冷水,可沿大陆坡沉到 海底,并向三大洋底部扩散,实现表层与底层 水的交换 海[海洋]水团 海[海洋]水团 海[海洋]水团(water mass):源地和形成机 制相近,具有相对均匀的物理、化学和 生物特征及大体一致的变化趋势,而与 周围海水存在明显差异的宏大水体 黄...
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warm water mass 暖水团
cold water mass [海洋] 冷水团
water mass identification [环境] 水质辨识
added water mass 附加动水质量 ; 附连水质量
Antarctic Circumpolar Water Mass [海洋] 南极绕极水团
Huanghai Cold Water Mass 黄海冷水团
water-mass continuity 水体连续性
At 1811 ka,the higher paleoproductivity was resulted from the rich-nutrients water mass(the Oyasio and the East China Sea coastal water) inflowing into the Sea of Japan with relative sea-level rise,and the maximum value was observed at 12.611.5 ka.
在1811 ka随着海平面的上升,富营养盐水团(亲潮和东海沿岸流水团)的流入导致古生产力逐渐增大,在12.611.5 ka古生产力达到最大值。
参考来源 - 48ka以来日本海古生产力和古氧化还原环境变化的地球化学记录·2,447,543篇论文数据,部分数据来源于NoteExpress
When the water mass fraction of the substrate is about 45%, its EC can be predicted accurately by both the power function as well as the linear function models.
控制基质质量含水率在45%左右的条件下,用幂函数和线性函数预测基质电导率都获得了较高的精度。
The results show that each water relative content and total water mass on hydro-montmorillonite by the method are inconsistent to them by isothermal adsorption.
结果表明,用该方法得到的水合蒙脱土中各种水分的相对含量及总含水量与等温吸附实验结果相一致。
The features of distribution and transformation of the East China Sea surface water mass are analyzed by using NOAA satellite images and simultaneous hydrographic data.
本文利用NOAA卫星图像处理结果与同期水文观测资料,对东海表层水团的分布和转移特征作了初步分析。
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