1) sedimentation flux
沉积通量
1.
Investigation of sedimentation fluxes, TEQ and sources of PCDD/Fs in Qingdao coastal sea.;
青岛近海PCDD/Fs的沉积通量、毒性当量及来源
2.
Based on the 210Pb method, sedimentation rates and sedimentation flux were measured in the Jiaozhou Bay of the Shandong Peninsula.
胶州湾西北部大沽河口外海域近百年来沉积速率为0 768cm/a,沉积通量为0 7716g/(cm2·a)。
2) Sedimentary flux
沉积通量
1.
Sedimentary flux of Lake Taibai,Hubei Province and correlations with precipitation and human activities in its catchment during the last century;
近百年来湖北太白湖沉积通量变化与流域降水量和人类活动的关系
2.
Firstly, the remnant sedimentary flux has been calculated basing on Later Cenozoic isopach map of Chengdu basin which has been made from the borehole data in the basin by Sufer software.
根据成都盆地已有的钻孔资料和原始数据,用Sufer软件制作成都盆地晚新生代等厚图,利用等厚线计算了成都盆地残留的沉积通量,并通过成都盆地的地质演化再造恢复了成都盆地潜在的沉积通量,结果表明,成都盆地潜在的沉积通量为1665km3。
3.
Based on drilling, seismic and outcrop data, a sedimentary flux study is conducted on Tertiary deposits in south-west depression of Tarim Basin, plane isograms of sedimentary flux at different periods are plotted.
根据钻井资料、地震资料及露头剖面资料,对塔里木盆地西南坳陷第三纪沉积物进行了沉积通量研究,编制了不同时期沉积通量的平面等值线图;结合沉积演化特征探讨了青藏高原隆升与研究区西南缘沉积物的响应,提出了青藏高原西北缘在中新世以前隆升缓慢,之后隆升幅度增大,上新世是快速隆升期,高原的形成过程不是以整体抬升为主,而是分块体阶段性抬升的结果。
4) phosphorous fluxes in sedimentary cores
磷沉积通量
5) sediment flux
沉积物通量
1.
The denuded sediment flux in the upper reaches of the Yangtze River is the most important factor which exerts the influence on the evolution and equilibrium of the fluvial lacustrine systems in the Yangtze River drainage area.
长江上游剥蚀沉积物通量是影响长江流域河湖体系平衡的最重要因素。
2.
Based on the thickness of the strata,the Late Permian-Eogene sediment flux of theJunggar inland Basin is calculated in this paper.
本文根据地层厚度资料，对准噶尔内陆盆地晚二叠世－早第三世的沉积物通量进行了计算。
6) nutrient accumulation rate
营养盐沉积通量
补充资料：传质通量
分子式：
CAS号：
性质：又称传质通量。单位时间、单位面积所传过去的物质质量，用符号N表示，其单位为kg/(m2·s)。
CAS号：
性质：又称传质通量。单位时间、单位面积所传过去的物质质量，用符号N表示，其单位为kg/(m2·s)。
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