1、

Low viscosity, fast curing, low odor, high index and euphotic index.

低粘度, 固化快, 低气味, 高折射率和透光率.

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2、

Significant linear correlations were found between transparence, PAR attenuation coefficient, euphotic depth and total suspended solid, especially inorganic suspended solid, while chlorophyll a was the most nonsignificant light attenuator.

透明度、PAR衰减系数、真光层深度与悬浮物浓度存在显著性线性相关,并且与悬浮物中无机颗粒物相关性最好,而与叶绿素a、脱镁叶绿素及溶解性有机碳相关性很低。

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3、

Euphotic layer of the sea refers to the layer where phytoplankton can photosynthesize; therefore, the retrieval of the euphotic depth is in favor of estimating ocean primary production.

海水真光层是指海洋浮游植物进行光合作用的水层,海水真光层深度的反演有利于对海洋初级生产力的估算。

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4、

Retrieval of euphotic layer depth of South China Sea by remote sensing

南海真光层深度的遥感反演

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5、

Ocean primary productivity is based on chla, which mainly denotes itself as the integral of the velocity of photosynthesis of chlorophyll and the density of chlorophyll in euphotic layer.

海洋初级生产力是基于海洋叶绿素a进行计算的,主要为叶绿素光合作用速率与遥感得到的叶绿素浓度在真光层的积分。

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6、

○ 2 The influence of variation in optical properties of various waters on the accuracy of OPP retrieval was studied through radiative transfer model in the euphotic layer, which may be more sufficient to determine the level of uncertainty of OPP product.

○2应用真光层中的辐射传输模式分析不同水体光学特性的变化对OPP反演精度的影响,这对于分析OPP产品的不确定性可能更加有效。

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7、

New production and nitrogen sources in the euphotic zone of open ocean

大洋真光层中的新生产力和N的来源

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8、

So new productivity in euphotic zone is assimilating capacity with carbon imported from outside and supporting capacity to product of high trophic level.

所以,新生产力表现为真光层对外部输入碳的同化能力和供次级或更高营养级生产所需营养的能力。

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9、

Particulate organic carban fluxes from euphotic zone estimated with~ ( 234) Th deficiency in winters in the northwestern North Pacific Ocean

~(234)Th示踪法测定北太平洋西北海域冬季真光层中颗粒态有机碳输出通量

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10、

Particle dynamics in the euphotic zone ⅵ. the utility of tracer~ ( 234) th for studying particle dynamics in the upper water column of the northeastern South China Sea

真光层的颗粒动力学&Ⅵ.南海东北部海域上层水体颗粒动力学的示踪研究

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11、

Biological production and consumption of DMS, primarily taking place within the marine euphotic zone, are considered to be the predominate source and sink of DMS in seawater.

DMS的生物生产与消耗主要发生在海洋真光层。生物的生产与消耗被认为是海洋中DMS的主要来源和去除途径。

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