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河流稀土元素地球化学研究进展 被引量:48
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作者 王中良 刘丛强 +3 位作者 徐志方 韩贵琳 朱建明 张劲 《地球科学进展》 CAS CSCD 2000年第5期553-558,共6页
河流系统中 ,稀土元素 ( REE)受区域地质背景、风化作用、溶液化学以及水与颗粒物相互作用等因素的影响发生分异。河流悬浮物显示轻稀土 ( LREE)适度富集 ;河水显示重稀土 ( HREE)富集 ,或在 HREE富集的基础上又有适度的中稀土 ( MREE)... 河流系统中 ,稀土元素 ( REE)受区域地质背景、风化作用、溶液化学以及水与颗粒物相互作用等因素的影响发生分异。河流悬浮物显示轻稀土 ( LREE)适度富集 ;河水显示重稀土 ( HREE)富集 ,或在 HREE富集的基础上又有适度的中稀土 ( MREE)富集 ;与其它微量元素相比 ,REE在河水与颗粒物之间有较小的分配系数 ( K≈ 1 0 -6) ;河流沉积物多显示平坦的 REE配分模式。 展开更多
关键词 河流 稀土元素 风化 溶液化学 地球化学
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贵州阿哈湖物质循环过程的微量元素地球化学初步研究 被引量:7
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作者 宋柳霆 王中良 +2 位作者 滕彦国 王金生 梁莉莉 《地球与环境》 CAS CSCD 北大核心 2012年第1期9-17,共9页
对贵州阿哈湖夏季和冬季分层湖水的水化学参数、溶解态微量元素和悬浮颗粒物微量元素进行了对比研究。结果显示:阿哈湖湖水夏季热分层和化学分层均较明显,而冬季湖水处于混合状态。夏季湖泊物质循环过程对生源要素Si、DOC以及Mn、Fe、Cr... 对贵州阿哈湖夏季和冬季分层湖水的水化学参数、溶解态微量元素和悬浮颗粒物微量元素进行了对比研究。结果显示:阿哈湖湖水夏季热分层和化学分层均较明显,而冬季湖水处于混合状态。夏季湖泊物质循环过程对生源要素Si、DOC以及Mn、Fe、Cr、Co、Ni、Zn和Mo等微量元素的分布和迁移转化均产生了重要影响。夏季湖泊底层水体中溶解态Mn、Fe、Co和Ni的含量较高,主要受有机质降解和Fe、Mn氧化还原循环的影响,而且Mn的循环强度高于Fe循环,溶解态Cr在底层水体中仅有小幅升高;另外,沉积物孔隙水向上覆水体的释放作用对底层水体中溶解态重金属浓度的升高可能也有一定的影响。溶解态Zn和Mo在夏季底层水体中的含量呈现逐渐降低的趋势,主要受到金属硫化物形成以及钼酸盐沉淀的影响。夏季悬浮颗粒物的Mn、Fe、Cr、Co、Ni、Zn和Mo均在氧化还原界面附近呈明显富集趋势,主要受铁锰氧化物/氢氧化物吸附/解吸、氧化还原作用等水-粒相互作用过程的控制和影响;此外,金属硫化物的形成可能也对底层水体中悬浮颗粒物Zn、Mo和Ni含量的升高有一定贡献。 展开更多
关键词 阿哈湖 物质循环过程 微量元素 水-粒相互作用
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基于弱作用力的固液相微界面作用模拟方法 被引量:1
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作者 陈志和 方群生 郑键鹏 《应用基础与工程科学学报》 EI CSCD 北大核心 2022年第5期1152-1160,共9页
为了探究固液相微界面作用的物质输移机制,丰富水-沙-污染物微界面作用的数值模拟方法,本文基于光滑粒子流体动力学方法(SPH)耦合电场力、布朗运动力、曳力等弱作用力,构建复杂微界面作用模型,模拟了细颗粒泥沙吸附Pb^(2+)的微界面作用... 为了探究固液相微界面作用的物质输移机制,丰富水-沙-污染物微界面作用的数值模拟方法,本文基于光滑粒子流体动力学方法(SPH)耦合电场力、布朗运动力、曳力等弱作用力,构建复杂微界面作用模型,模拟了细颗粒泥沙吸附Pb^(2+)的微界面作用过程.模拟结果演示了细颗粒泥沙与Pb^(2+)的微界面作用全过程,Pb^(2+)进入液膜,由液膜迁移至颗粒内,逐渐填满液膜和孔道,最终填充空腔.微界面作用动力学分析结果表明模拟结果符合准二级动力学模式;微界面作用模式识别结果表明0~10min为膜扩散阶段,10~60min为膜扩散和颗粒内扩散并存阶段,60~210min为颗粒内扩散阶段.模拟结果具有较好的微界面作用动力学相似性和微界面作用模式一致性.该方法适用于微米尺度下的微界面作用过程模拟,为水-沙-污染物交互作用的微观尺度建模提供新思路. 展开更多
关键词 微米尺度 水-沙-污染物 细颗粒泥沙 PB2+ 微界面作用 SPH方法 弱作用力
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SPH模拟研究细长体入水问题 被引量:1
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作者 裴志博 杨秀峰 王晓亮 《无人系统技术》 2022年第3期40-49,共10页
传统的数值方法难以模拟跨域无人航行器跨水—空交界面过程中的复杂交界面及流固耦合问题。针对跨域无人航行器入水问题,应用光滑粒子法(SPH)模拟研究了细长体入水过程。首先,对SPH方法进行了改进:为了提高数值稳定性,同时使用了传统的... 传统的数值方法难以模拟跨域无人航行器跨水—空交界面过程中的复杂交界面及流固耦合问题。针对跨域无人航行器入水问题,应用光滑粒子法(SPH)模拟研究了细长体入水过程。首先,对SPH方法进行了改进:为了提高数值稳定性,同时使用了传统的钟形函数和双曲型核函数;为了提高计算精度,在SPH方法中加入了粒子迁移技术并进行了简化处理。然后,应用SPH方法模拟了水平圆柱入水过程,液面形态演变和入水深度变化的模拟结果均与试验相符。最后,应用SPH方法模拟研究了细长体入水问题。结果表明,文中方法能够有效模拟细长体入水过程中细长体的运动和自由液面的演化问题,细长体的密度和入水速度会影响入水过程中的自身运动和液面形态。 展开更多
关键词 跨域无人航行器 物体入水 光滑粒子法 流固耦合 数值模拟
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A 3-D SPH model for simulating water flooding of a damaged floating structure 被引量:3
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作者 郭凯 孙鹏楠 +1 位作者 曹雪雁 黄潇 《Journal of Hydrodynamics》 SCIE EI CSCD 2017年第5期831-844,共14页
With the quasi-static analysis method, the terminal floating state of a damaged ship is usually evaluated for the risk assessment. But this is not enough since the ship has the possibility to lose its stability during... With the quasi-static analysis method, the terminal floating state of a damaged ship is usually evaluated for the risk assessment. But this is not enough since the ship has the possibility to lose its stability during the transient flooding process. Therefore, an enhanced smoothed particle hydrodynamics(SPH) model is applied in this paper to investigate the response of a simplified cabin model under the condition of the transient water flooding. The enhanced SPH model is presented firstly including the governing equations, the diffusive terms, the boundary implementations and then an algorithm regarding the coupling motions of six degrees of freedom(6-DOF) between the structure and the fluid is described. In the numerical results, a non-damaged cabin floating under the rest condition is simulated. It is shown that a stable floating state can be reached and maintained by using the present SPH scheme. After that, three-dimensional(3-D) test cases of the damaged cabin with a hole at different locations are simulated. A series of model tests are also carried out for the validation. Fairly good agreements are achieved between the numerical results and the experimental data. Relevant conclusions are drawn with respect to the mechanism of the responses of the damaged cabin model under water flooding conditions. 展开更多
关键词 Smoothed particle hydrodynamics(SPH) fluid-structure interaction water flooding wave-body interaction damaged vessel
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An experimental study on the influences of wind erosion on water erosion 被引量:2
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作者 YANG Huimin GAO Yuan +3 位作者 LIN Degen ZOU Xueyong WANG Jing'ai SHI Peijun 《Journal of Arid Land》 SCIE CSCD 2017年第4期580-590,共11页
In semi-arid regions, complex erosion resulted from a combination of wind and water actions has led to a massive soil loss and a comprehensive understanding of its mechanism is the first step toward prevention of the ... In semi-arid regions, complex erosion resulted from a combination of wind and water actions has led to a massive soil loss and a comprehensive understanding of its mechanism is the first step toward prevention of the erosion. However, the mutual influences between wind erosion and water erosion have not been fully understood. This research used a wind tunnel and two rainfall simulators and simulated two rounds of alternations between wind erosion and water erosion(i.e., 1^(st) wind erosion–1^(st) water erosion and 2^(nd) wind erosion–2^(nd) water erosion) on three slopes(5°, 10°, and 15°) with six wind speeds(0, 9, 11, 13, 15, and 20 m/s) and five rainfall intensities(0, 30, 45, 60, and 75 mm/h). The objective was to analyze the influences of wind erosion on succeeding water erosion. Results showed that the effects of wind erosion on water erosion were not the same in the two rounds of tests. In the 1^(st) round of tests, wind erosion first restrained and then intensified water erosion mostly because the blocking effect of wind-sculpted micro-topography on surface flow was weakened with the increase in slope. In the 2^(nd) round of tests, wind erosion intensified water erosion on beds with no rills at gentle slopes and low rainfall intensities or with large-size rills at steep slopes and high rainfall intensities. Wind erosion restrained water erosion on beds with small rills at moderate slopes and moderate rainfall intensities. The effects were mainly related to the fine grain layer, rills and slope of the original bed in the 2^(nd) round of tests. The findings can deepen our understanding of complex erosion resulted from a combination of wind and water actions and provide scientific references to regional soil and water conservation. 展开更多
关键词 wind-water interaction sandy soil particle size surface roughness wind and water erosion
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Modelling large deformation and soil–water–structure interaction with material point method:Briefing on MPM2017 conference 被引量:1
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作者 Alexander Rohe Dongfang Liang 《Journal of Hydrodynamics》 SCIE EI CSCD 2017年第3期393-396,共4页
The 1st International Conference on the Material Point Method for "Modelling Large Deformation and Soil–Water–Structure Interaction"(MPM2017)was held in Delft,The Netherlands on 10-13 January 2017.This is the fi... The 1st International Conference on the Material Point Method for "Modelling Large Deformation and Soil–Water–Structure Interaction"(MPM2017)was held in Delft,The Netherlands on 10-13 January 2017.This is the first conference organised by the Anura3D MPM Research Community,following a series of international workshops and symposia previously held in The Netherlands,UK,Spain and Italy,as part of the European Commission FP7 Marie-Curie project MPM-DREDGE.We are delighted to present seven contributions in this Special Column of the Journal of Hydrodynamics,and take this opportunity to announce that the 2nd conference,MPM2019,will be held in Cambridge,UK in January 2019. 展开更多
关键词 Material point method soil–water–structure interaction meshfree methods particle methods
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