爱沙尼亚北部一个小的二辉石湖泊的沉积动力学

J. Terasmaa, J. Punning
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引用次数: 11

摘要

在长达一年的观测中,维纳湖表层和表层沉积物的沉降通量在230 ~ 1400 mg m -2 d -1之间变化。大部分群落由颗粒物有机质(POM)组成。全湖底表层沉积物干物质中POM含量平均在50%以上。湖泊叶绿素a分布和POM含量的季节变化揭示了新鲜浮游颗粒在沉积中的重要作用。分层过程中沉降物中POM与颗粒无机物之间的强相关性表明矿物颗粒呈絮状沉降。沿海地区的再悬浮导致沉积物集中到湖盆深处。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sedimentation dynamics in a small dimictic lake in northern Estonia
During a yearlong observation, settling fluxes of seston in the epilimnion and hypo- limnion of Lake Viitna Linajarv varied from 230 to 1400 mg m -2 d -1 . Most of the seston consisted of particulate organic matter (POM). The POM content in the dry matter of surface sediments sampled from the entire lake floor was on average over 50%. Seasonal changes in the distribution of chlorophyll a in the lake and the content of POM reveal the important role of fresh planktonic particles in the deposition. A strong correlation between POM and particulate inorganic matter in the settling matter during stratification indicates flocculent settling of the mineral particles. Resuspension from the littoral zone results in the focusing of sediment into the deep basin of the lake.
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