| 基于CT技术的巢湖沉积物孔隙结构三维重建的初步研究 |
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| 引用本文： | 肖洒,单保庆,张文强,温胜芳.基于CT技术的巢湖沉积物孔隙结构三维重建的初步研究[J].环境科学学报,2016,36(3):747-752. |
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| 作者姓名： | 肖洒 单保庆 张文强 温胜芳 |
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| 作者单位： | 1. 华中农业大学水产学院, 武汉 430070;2. 中国科学院生态环境研究中心环境水质学国家重点实验室, 北京 100085,中国科学院生态环境研究中心环境水质学国家重点实验室, 北京 100085,中国科学院生态环境研究中心环境水质学国家重点实验室, 北京 100085,清华大学公共管理学院, 北京 100085 |
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| 基金项目： | 国家水体污染控制与治理科技重大专项(No.2012ZX07101-002) |
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| 摘 要： | 为更好地了解分析沉积物孔隙结构特征,本文通过CT技术及相关软件,对巢湖沉积物孔隙结构进行了三维重建,展现了巢湖沉积物真实的三维孔隙结构,并以此为基础定量计算了孔隙度、孔隙连通性、曲率等沉积物孔隙结构参数.结果表明,巢湖表层沉积物孔隙度变化范围为0.28~0.75;曲率在2.83~9.31内变化,且在不同方向上表现出明显的差异性,Z方向上的较高曲率阻碍了孔隙水中的污染物扩散.沉积柱在垂直方向上,总体上随深度的增加,孔隙度减小,但在某些深度存在异常,可能是因为底栖动物活动或沉积条件变化.
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| 关 键 词： | 巢湖 沉积物 孔隙结构 孔隙度 曲率 |
| 收稿时间： | 2015/5/22 0:00:00 |
| 修稿时间： | 7/7/2015 12:00:00 AM |
Study on the three-dimensional pore structure of sediments in Chaohu Lake based on CT technique |
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| XIAO S,SHAN Baoqing,ZHANG Wenqiang and WEN Shengfang.Study on the three-dimensional pore structure of sediments in Chaohu Lake based on CT technique[J].Acta Scientiae Circumstantiae,2016,36(3):747-752. |
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| Authors: | XIAO S SHAN Baoqing ZHANG Wenqiang and WEN Shengfang |
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| Institution: | 1. College of Fisheries, Huazhong Agricultural University, Wuhan 430070;2. State Key Laboratory of Environmental Aquatic Chemistry, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085,State Key Laboratory of Environmental Aquatic Chemistry, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085,State Key Laboratory of Environmental Aquatic Chemistry, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085 and School of Public Policy & Management, Tsinghua University, Beijing 100085 |
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| Abstract: | The pore structure characteristics of sediments from Chaohu Lake were studied by using micro-CT three-dimension reconstruction technique, and the related parameters (porosity, pore connectivity, tortuosity, etc.) were all calculated quantificationally. The results showed that the surface sediments in Chaohu Lake had the porosity of 0.28~0.75, and the tortuosity of 2.83~9.31 which showed obvious difference in different directions. The higher tortuosity in the Z direction hindered the diffusion of the pollutants in the pore water. In the vertical direction, the porosity of the sediments generally decreased with the increase of depth, but in some depth, there are exceptions, which may be because of the change of the benthic animal activities or the deposition conditions. |
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| Keywords: | Chaohu Lake sediment pore structure porosity tortuosity |
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