1) flux exchange
通量交换
1.
Regional Atmospheric Model System is used in the study of water and energy flux exchange in Inner Mongolia.
ＲＡＭＳ模式被应用于内蒙半干旱草原地区地气系统水热通量交换及水循环过程研究。
2) exchange flux
交换通量
1.
Study on the exchange flux of the DIN through the sediment-water interface in the Yangtze Estuary;
长江口沉积物-水界面无机氮交换通量的模拟测定
2.
A Study on the Nutrients Exchange Flux between Bottom Sediment and Water Layer for Bohai Bay;
渤海湾沉积物和水界面间营养盐的交换通量研究
3.
The profile distribution of nutrients and exchange fluxes at the sediment-water interface were analyzed in the six sites of the inner Pearl River Estuary in April 2005.
2005年春季(4月)对珠江口内6个站位的营养盐剖面分布及沉积物-水界面的交换通量进行了全面研究。
3) exchange fluxes
交换通量
1.
The sediment-water interface nutrients exchange fluxes of BLG(Bailong-gang tideland) and LG(Laogang tideland) with sewage outfalls were studied compared with those of the CY(Chaoyang tideland) without sewage outfall.
通过对有排污口的老港(LG)、白龙港(BLG)潮滩和附近没有排污口的朝阳农场潮滩(CY)的沉积物-水界面营养盐通量的研究发现:污水排放造成潮滩上覆水体中营养盐含量增加,进而影响到潮滩沉积物-水界面营养盐氮磷的交换通量;各点中低潮滩的差异(特别是生物活动的影响),造成了中低潮滩对上覆水中N、P作用的差异;老港和白龙港潮滩由于污水的排放使影响沉积物-水界面营养盐交换通量的盐度因素的作用变得不太明显。
2.
According to the stagnant two film model, the direction and magnitude of exchange fluxes of PAHs across air water interface in Luhu Lake were calculated based on above data.
利用大流量采样器和半渗透膜装置对广州麓湖大气中气态多环芳烃和水体中溶解态多环芳烃进行了连续一年的观测,在此数据基础上,依据国内外通用的双膜理论计算了多环芳烃在广州麓湖水面上的交换通量。
4) exchanging flux
交换通量
1.
The exchanging fluxes of carbonyl sulfide(COS)were investigated by using static method for 6 tree species in Beijing city in fall.
树木与大气间COS的交换通量受树种、环境温度、光照、COS初始浓度等因素的影响 。
2.
The exchanging fluxes of carbonyl sulfide(COS)and dimethyl sulfide(DMS)were investigated by using static method between lawn and atmosphere.
COS和DMS的交换通量与环境温度、光照及初始浓度等因素有关 ,其中 ,周围大气COS的浓度对草坪吸收COS的影响最为明显 。
5) flux
[英][flʌks] [美][flʌks]
交换通量
1.
Monthly research of ammonia and phosphorus fluxes in water-sediment interface in East Lake Taihu(ELT,macrophyte dominated) and Meiliang Bay(MB,algae dominated) was processed with intact sediment cores' incubation and pore water diffusive model.
原柱样氮磷静态界面交换通量(Fi)在同一湖泊不同生态类型湖区有差异性,东太湖氨态氮和可溶性磷酸盐的年平均交换通量分别为(44。
2.
We studied IN fluxes and seasonal varieties at the sediment-water interface in northern Yangtze river.
对长江口北支地区沉积物 -水界面无机氮的交换通量及季节变化进行了研究。
3.
The exchange fluxes of dissolved inorganic phosphate are 6.
渤海莱州湾磷酸盐的交换通量为 6 7— 6 8μmol·m- 2 ·d- 1 。
6) exchange total fluxes
交换总通量
1.
A calculating system of dissolved inorganic nitrogen exchange total fluxes at the sediment-water interface in Yangtze estuary tidal wetlands was presented.
基于MapObjects组件式GIS技术和数学建模方法,以Visual Basic为开发平台,建立了长江口湿地沉积物-水界面无机氮交换通量空间插值模型、总通量量算模型和量算系统,该系统的主要功能包括对无机氮界面交换通量信息查询检索,空间插值分析,以及对长江口湿地不同岸段、不同季节无机氮交换总通量综合和动态量算。
补充资料：离子交换树脂交换量
分子式：
分子量：
CAS号：
性质：见离子交换当量。
分子量：
CAS号：
性质：见离子交换当量。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条