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1)  sea water chlority
海水气度
2)  seawater temperature
海水温度
1.
Physical and mathematical models are established in order to analyze and calculate the influence of seawater temperature and bubble distribution on conductivity characteristic of ship wake.
为了对水面舰船尾流的电导率特性受海水温度和气泡分布的综合影响进行理论分析和计算,在建立物理模型和数学模型时,对于具有垂直温度梯度的海水中水面舰船的气泡尾流,假设检测尾流的电导率探头极间的气泡分别呈任意分布和均匀分布,获得了海水温度、气泡半径、气泡数密度及气泡分布方式对非尾流区海水电导率与尾流电导率之差δK的综合影响规律。
3)  seawater salinity
海水盐度
1.
Effect of the seawater salinity on the nitrification-denitrification via nitrite pathway;
海水盐度对短程硝化反硝化的影响
2.
The influence of seawater salinity,pH,temperature and ammonia nitrogen loading on the shortcut nitrification of simulated sewage was studied.
采用SBR工艺处理模拟海水冲厕污水,研究了海水盐度、pH值、温度、氨氮负荷对模拟海水冲厕污水短程硝化的影响。
3.
Experiments were conducted under different seawater salinity conditions to investigate such as the rule of low and middle concentration organics degrading velocity and removal,activated sludge settling characteristics and effect of the temperature on organics degrading velocity when seawater was 20% of the total domestic wastewater.
海水盐度降低了有机物的降解速率和去除率,但两种浓度污水的出水CODcr浓度均在30~70mg/L之间,远远低于国家污水综合排放二级标准(GB8978-1996)。
4)  effluent [英]['efluənt]  [美]['ɛfluənt]
海水浓度
1.
The impact of sea-water concentration on biologicaloxidation effluent treatment;
海水浓度对生物接触氧化法处理废水的影响
5)  sea water density
海水密度
1.
Striving to get the maximum cargo carrying capacity and to acquire great economic benefit by use of variations of sea water density in harbours is worth considering by captains and ship operators under the circumstances of sailing safely through shallow waters.
我国沿海河口港较多,利用港区的海水密度变化,在保证船舶安全通过浅水区的前提下,争取最大载货量,提高经济效益,值得引起广大船长和驾驶人员重视。
2.
The existent difference between geodetic leveling and tide station is investigated, and this difference comes from the sea level slope, and the sea level slope mechanism caused by ocean current, air pressure and breaking wave is analyzed, the geoid disturbance computed by three dimensional distribution of sea water density is prese.
进一步讨论了大地水准的测量精度 ,指出了大地 (几何 )水准与沿海验潮资料的不符是由于海面的倾斜 ;分析了海面倾斜的机理 ,其中包括海流、海水密度分布、气压、台风引起的破碎波等的作用 ;提出了用海水异常密度的三维分布计算大地水准面的扰动 ,实质上它反映了海面的倾斜 ,该量占大地水准测量结果的 73% ,这进一步说明密度的异常乃是我国沿海海面倾斜的主要原
6)  Seawater density
海水密度
1.
The calculation method of seawater density by the multi-angle and polarized information was advanced here.
提出一种利用多角度偏振信息计算海水密度的方法,从多角度遥感与偏振光遥感的角度,找出海水的偏振特性与海水密度之间的函数关系,利用海水偏振特性与海水折射率特性对海水密度进行计算,扩展现有遥感应用的领域,同时为海洋基本参数反演开拓新思路。
2.
Using TOPEX/ Poseidon satellite altimeter data, and seawater temperature and salinity estimated from WOA98 model, we calculated sea level height variation caused by seawater density change in multi layers.
基于TOPEX/Poseidon卫星测高资料,采用WOA98海水温度及盐度模型,计算了多层海水密度变化引起的海面高变化。
补充资料:海水增养殖(见海水养殖、海水增殖)


海水增养殖(见海水养殖、海水增殖)
marine aquaculture

_一一’‘~’‘以,’日y以.1日乙川髦增养殖(~ne aquacultu祀’见海水养殖·海水
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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