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1)  Suspend sediments
悬浮态泥沙
2)  suspended sediment
悬浮泥沙
1.
Experimental study on reflected spectrum and estimating amount of suspended sediment;
悬浮泥沙反射光谱特性和泥沙量估算试验研究
2.
Observations of the size and settling velocity distributions of suspended sediment in the Zhujiang River Estuary during dry season;
枯季珠江河口悬浮泥沙絮凝沉降特征的观测与分析
3.
Remote sensing of suspended sediments in China east coastal waters from SeaWiFS data;
运用Sea WiFS遥感数据探测中国东部沿海悬浮泥沙浓度的研究
3)  suspended sand
悬浮泥沙
1.
We establish the retrieval model of surface suspended sand with the volume concentration of surface suspended sand and field data of spectral reflectance,moreover, we retrieve the volume concentration of .
本文以江苏沿海辐射沙洲中的西洋为研究区,通过实测的表层悬浮泥沙体积浓度和光谱反射率数据,建立表层悬沙反演模型,以Landsat-5影像各波段反射率为原数据反演研究区表层悬沙体积浓度;在此基础上探讨不同的表层悬沙浓度对影像各波段光谱的贡献,并在遥感反演水深时,去除悬沙浓度的光谱贡献以提高水深反演精度。
4)  Suspended sediments
悬浮泥沙
1.
It is to be able to autornatically and continually observe and estimate the real-time concentrations profiles of suspended sediments in water and dynamic changing process.
本文介绍了一种新型的水文观测设备-“ASSM-Ⅱ型声学悬浮泥沙观测系统”,它可以自动、连续和长时间地实时观测水中悬浮泥沙浓度分布和动态变化过程。
2.
The suspended sediments are a major issue which we have to face in the process of controlling Yellow River.
悬浮泥沙一直是黄河治理过程中面临的一个重大问题,在黄河泥沙物理和数学模型的开发等方面都取得了一定的进展,但是通用模式和高精度的模式一直还未建立起来,因此现阶段提高定量的精度已经成为众多研究水体泥沙学者的研究目标。
5)  sediment resuspension
泥沙再悬浮
1.
Based on data observed in the South Passage in of the Changjiang Estuary March and July1997,the variance of particulate heavy metal concentration during sediment resuspension was studied.
基于1997年3月9日和7月27日长江口南槽定点连续观测资料,分析了河口泥沙再悬浮对重金属元素的影响。
6)  suspension power
泥沙悬浮功
1.
The relationship between k_t and effective Reynolds number R_(em) was analyzed according to the data obtained from laboratory test and the variation law of the characteristics of k_t,e_s and suspension power E_s following the changes of suspension concentration were further .
通过应用室内水槽平衡输沙试验实测数据,分析了紊动能转化率kt与有效雷诺数Rem之间关系,并探讨了紊动能转化率kt、泥沙悬浮效率系数es和泥沙悬浮功Es等表述能量的三大特征值随含沙浓度的变化规律,得出了在高含沙水流(Sv≥0。
补充资料:单线态-单线态能量转移
分子式:
CAS号:

性质:处于电子激发单线态的能量给体,通过激发能的转移使能量受体处于激发单线态的过程。

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