1) euphotic zone
真光层
1.
We observed 234Th excess at station BR03 below the euphotic zone,which is possibly due to the intensive reminera-lization of particulate matter.
溶解态、颗粒态及总234Th的放射性在真光层中显著低于母体238U的放射性,总的234Th与238U在水深大于100m时趋于放射性平衡。
2) euphotic depth
真光层深度
1.
Euphotic depth:retrieval from in situ reflectance and application in assessing eutrophication;
真光层深度的遥感反演及其在富营养化评价中的应用
2.
Spatial pattern of euphotic depth and estimation of phytoplankton primary production in Lake Taihu in autumn 2004;
太湖秋季真光层深度空间分布及浮游植物初级生产力的估算
3.
Using 64 stations water quality data collected in Taihu Lake,the spatial distribution of water color parameters and euphotic depth was analyzed,and the potential effect on hygrophyte photosynthesis was discussed.
利用太湖全湖64个采样点的数据,分析了各水色因子及真光层深度的空间分布和变化特征,并探讨了其对水生植物光合作用的影响。
3) euphotic zone depth
真光层深度
1.
Euphotic zone depth (Zeu) is an important water property.
真光层深度(Zeu)是一个描述水质特性的重要参数。
2.
And then,the potential factors,including the suspended solids(SS),chlorophyll a(Chla)and chromomorphic dissolved organic matter(CDOM),and how the factors influence the euphotic zone depth in PAR(Zeu)can be acquired by the empirical algorithms using statistics analysis.
应用统计方法分析了PAR真光层深度的影响因素。
4) optical distortion
光失真<光>
5) formation truth
地层真值
6) digital well logging
煤层真厚
补充资料:偪真
1.逼真,极为相似。
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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