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neap tide相关的网络例句

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与 neap tide 相关的网络例句 [注:此内容来源于网络,仅供参考]

Also thanks all friends, no matter I do know you, thanks you in my life neap tide.

也谢谢所有的朋友,不管我认不认识你,谢谢你们在我人生最低潮。

The result is a smaller difference between high and low tides and is known as a neap tide.

其结果是退潮高,规模较小的差异,是潮流称为小潮。

The simulated hypoxia phenomena develop during the neap tide and disappear during the spring tide.

缺氧现象的发展与减退受潮汐涨落的影响。

Little difference of surface sediment grain size was showed between spring tide and neap tide, and the difference of mean diameter was about 9.7%.

表层沉积物大小潮变化较小,两次采样平均差别为9.7%;沉积物年际变化随大通流量和输沙量的变化而变化。

The result shows:(1) the value of R in situ is higher than 0.8, which is lower than that in lab;(2) the averaged value of relative error in spring tide is higher than that of in neap tide and the value is less than 15%.(3) the particle size is the main factor that influences the precision of OBS, while the biology, the color of particle and water, the air bubble in water have some effect on it.

主要结果有:(1)现场OBS标定R值比室内标定偏低,但也在0.8以上;(2)大潮平均相对误差值变化比小潮大,在悬沙浓度低于1.5kg/立方公尺条件下,大小潮悬沙浓度平均相对误差都在15%以下;(3)悬沙粒径大小是影响OBS观测精度的主要因素,生物、泥沙颜色、水色和水中气泡等因素也对观测结果产生一定影响。

In Jintang Channel, the resuspension flux decreases from spring tide to neap tide; resuspension is caused by strong current speeds, with dispersion also playing an important role in suspended sediment transport and vertical distribution.

根据鸭绿江河口地区的悬沙输运机制分析,平均流作用、斯托克斯漂移效应以及水深与悬沙浓度的潮变化引起的悬沙输送是本区最主要的悬沙输送机制。

The spectrum analysis was applied to analyze the fluctu- ation of flocs diameter during the spring tide and the neap tide.

分析表明,长江口徐六泾处细颗粒泥沙絮凝体粒径存在着明显的变化周期:大潮表层存在7.86h,3.93h和2.95h的变化周期;小潮表层存在8.38h和3.14h的变化周期;大潮底层存在3.33h和1.19h的变化周期。

The temporal change in floes size of fine suspended sediments was measured in Xuliujin of the Changjiang Estuary in June of 2003, by using an in situ laser diffraction particle sizer, the laser in situ scattering and transmissomerty-100(LISST-100). The spectrum analysis was applied to analyze the fluctuation of floes diameter during the spring tide and the neap tide.

2003年6月利用现场激光粒度仪(LISST-100)在不扰动的情况下,获取了长江口徐六泾处悬浮细颗粒泥沙絮凝体的现场粒径系列资料,应用谱分析方法研究了絮凝体粒径在大小潮、表底层的变化规律。

The observation showes that average VC, D,Δp and ω at the surface water during spring tide are 98.0μl/L, 39.8μm, 1173 kg/m^3 and 1.14 mm/s, whereas those during neap tide are 70.8 μl/L, 64.4μm, 919 kg/m^3 and 2.32 mm/s, respectively.

观测结果显示,徐六泾大、小潮表层絮凝体体积浓度、粒径、有效密度和静水沉速的平均值分别为98.0μl/L、39.8μm、1173kg/平方公尺、1.14mm/s和70.8μl/L、64.4μm、919kg/平方公尺,2.32mm/s。

Results show that floes' VC and D at the surface water were closely related to current velocity; and the peaks of VC lag those of the current velocity. The lag variation during ebb and flood tides is 10-30min and 30-50 min, respectively. Current velocity at 50 cm/s is a turning point of D vs. vertical average current velocity, before the point, Dm increases with current velocity, and decreases after the point. Similarly, VC at 75μl/L becomes a critical point in the surface water, below the point, D increases with VC, and above the point, D stabilizes.Δp is D dependent, larger floes have much lower Δp than smaller floes. Both D and Δp of floes affect ω. In the surface water during spring tide and neap tide, a power exponent relationship exists between Δp and D, and ω and D.

研究表明:①长江口徐六泾表层絮凝体体积浓度主要受水流流速影响,再悬浮现象明显,体积浓度过程线滞后流速过程线,落潮期间滞后10-30min,涨潮则滞后30-50min;②小于一定流速时絮凝体平均粒径随流速增大而增大,大于一定流速时絮凝体平均粒径则随流速增大而减小,徐六泾夫、小潮表层絮凝体在50cm/s的垂线平均流速时出现平均粒径与垂线平均流速关系的转折;③徐六注大、小潮表层絮凝体平均粒径在体积浓度75μl/L时出现平均粒径与体积浓度关系的转折,体积浓度小于75μl/L时粒径随体积浓度增加而增大,超过75μl/L时粒径随体积浓度的增加变化不明显;④絮凝体有效密度由粒径大小控制,粒径大,有效密度小,反之亦然,粒径和有效密度共同决定絮凝体静水沉速,有效密度和沉速与平均粒径之间均存在良好的幂指数关系。

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