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垂向环流作用下湖泊沉积物磷迁移行为 被引量:5
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作者 刘园园 褚克坚 +5 位作者 陆滢 华祖林 KY Sereyvatanak 顾莉 刘晓东 徐龙龙 《中国环境科学》 EI CAS CSCD 北大核心 2021年第6期2843-2852,共10页
以巢湖十五里河入湖河口原位底泥为研究对象,通过室内模型实验,模拟了垂向环流的动水条件下,溶解态无机磷(DIP)在泥水界面的释放-吸附过程,探讨了不同强度环流对河口底泥DIP迁移的影响行为.结果表明:垂向环流扰动会引起上覆水中溶解氧(... 以巢湖十五里河入湖河口原位底泥为研究对象,通过室内模型实验,模拟了垂向环流的动水条件下,溶解态无机磷(DIP)在泥水界面的释放-吸附过程,探讨了不同强度环流对河口底泥DIP迁移的影响行为.结果表明:垂向环流扰动会引起上覆水中溶解氧(DO)和悬浮颗粒物(SPM)含量明显上升,且其平衡浓度与扰动强度均呈正相关,但悬浮物中值粒径(D_(50))则随扰动强度的增大而降低;垂向环流作用下沉积物DIP的释放量随时间呈“Λ”型分布,显著区别于其他动水扰动情形,释放峰值与环流强度成显著正相关(P=0.047<0.05),但平衡值则与之呈显著负相关(P=0.034<0.05);环流扰动的增强促进了DIP在沉积物上的吸附,并构建了耦合天然水动力效应的沉积物DIP Freundlich等温吸附经验公式:lgQe=2.7074e^(1.3487τ)+0.9463e^(-1.4830τ)lgCe. 展开更多
关键词 垂向环流 浅水湖泊 沉积物 DIP 释放 吸附
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EXPERIMENTS OF THREE-DIMENSIONAL FLOW STRUCTURE IN BRAIDED RIVERS 被引量:13
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作者 HUA Zu-lin GU Li chu ke-jian 《Journal of Hydrodynamics》 SCIE EI CSCD 2009年第2期228-237,共10页
The braided river is a typical river pattern in nature, but there is a paucity of comprehensive data set describing the three-dimensional flow field in the braided river. A physical model experiment was used to study ... The braided river is a typical river pattern in nature, but there is a paucity of comprehensive data set describing the three-dimensional flow field in the braided river. A physical model experiment was used to study the flow characteristics in the typical braided river with a mid-bar between two anabranches. In the experiment, two kinds of mid-bar with the ratios of its length to maximal width of 3 and 5 were considered. Moreover, the mid-bar could be moved to adjust the width of two anabranches. The detailed measurements of velocity were conducted using an acoustic Doppler velocimeter over a grid defined throughout the whole braided river region, including the bifurcation, two anabranches and the confluence. In two kinds of mid-bar braided models, a separation zone was observed in the anabranch of the model in which the ratio of length to maximal width of mid-bar is 3, however the separation zone was not found in another model in which the ratio is 5. In addition, the opposite secondary cells were observed at the bend apex of anabranch in two models, and different longitudinal velocity distributions in the entrance region of anabranch account for this opposite flow structure. Finally, turbulent kinetic energy were shown and compared in different situations. The high turbulence occurs at the place with strong shear, especially at the boundary of the separation zone and the high velocity passing flow. 展开更多
关键词 braided river three-dimensional flow structure secondary flow turbulent kinetic energy
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