秦朝中
作者: 佚名 发布时间: 2021年05月17日 09:17 浏览次数:

秦朝中

职称职务

研究员、博导




联系电话

13996265157

Email

chaozhong.qin@cqu.edu.cn

联系地址

重庆市沙坪坝区沙正街174

重庆大学A区资源与安全学院121

研究内容主要包括:数字岩心分析,多尺度渗流力学和基于微纳米芯片的多孔介质反应流动与传输,相关应用背景涉及非常规油气开发、燃料电池、二氧化碳地质封存和地下储能。目前与乌特列支大学,埃因霍温理工大学,苏黎世联邦理工学院,亚利桑那大学等海外研究机构保持紧密交流与合作,欢迎计算力学,渗流力学,油气工程等相关背景的研究生、博士和博士后加入我们。

个人简历

教育经历:

2009-032012-10,荷兰乌特列支大学/通用汽车欧洲研究院,地球科学,博士

2005-092008-07,中国科学技术大学,流体力学,硕士

2001-092005-06,西安交通大学,工程力学,学士

工作与研究经历:

2019-82019-9,同济大学,土木工程系,访问学者

2017-12019-11,荷兰埃因霍温理工大学,达西研究中心,执行主管

2016-112019-9,荷兰埃因霍温理工大学,机械工程系,研究员

2016-32016-5,美国普林斯顿大学,环境与土木工程学院,访问学者

2015-82015-9德国斯图加特大学,水力学系,访问学者

2014-12014-3德国弗劳恩霍夫应用研究促进协会,访问学者

2012-112016-10,荷兰乌特列支大学,地球科学,博士后

代表性研究项目

(1)自发渗吸微观动力学特性及其在两相达西模型中的量化,国家自然科学基金面上项目,127072053,主持,2021-2024

(2)煤岩多尺度渗流力学基础理论与物理模型研究,煤矿灾害动力学与控制国家重点实验室,主任基金,主持,2021-2022

(3)重庆市留创计划创新类项目,主持,2020

(4)Analysing spatial scaling effects in mineral reaction rates in porous media with a hybrid numerical model,瑞士国家自然科学基金,SNF-175673,参与,2018-012020-07

(5)A new paradigm in modeling flow and transport in porous media: revisiting foundations of porous media science,欧盟研究委员会,ERC-341225,,参与,2013-092019-08

代表性论文

[1]C. Qin, H. van Brummelen, M. Hefny, J. Zhao, Image-based modeling of spontaneous imbibition in porous media by a dynamic pore network model,Advances in Water Resources,152, 103932, 2021.

[2]S. Chen,C. Qin, B. Guo, Fully implicit dynamic pore-network modeling of two-phase flow and phase change in porous media,Water Resources Research, 56, e2020WR028510, 2020.

[3]M. Hefny,C. Qin, M.O. Saar, and A. Ebigbo, Synchrotron-based pro-network modeling of two-phase flow in Nubian Sandstone and implications for capillary trapping of carbon dioxide,International Journal of Greenhouse Gas Control, 103164, 2020.

[4]Y. Liu, J. Cai, M. Sahimi,C. Qin, A study of the role of microfractures in counter-current spontaneous imbibition by lattice Boltzmann simulation,Transport in Porous Media, 133, 313-332, 2020.

[5]C. Qin, and E.H. van Brummelen, A dynamic pore-network model for spontaneous imbibition in porous media,Advances in Water Resources, 133, 103402, 2019.

[6]C. Qin, B. Guo, M. Celia, and R. Wu, Dynamic pore-network modeling of air water flow through thin porous layers,Chemical Engineering Science, 202, 194-207, 2019.

[7]A.H. Tavangarrad, B. Mohebbi,C. Qin, S.M. Hassanizadeh, R. Rosati, J. Claussen, and B. Blümich, Continuum-scale modeling of water infiltration in a stack of two thin fibrous layers and their interface,Chemical Engineering Science, 207, 769-779, 2019.

[8]T. Hoang, C.V. Verhoosel,C. Qin, F. Auricchio, A. Reali, E.H. van Brummelen, Skeleton-stabilized immersogeometric analysis for incompressible viscous flow problems,Computer Methods in Applied Mechanics and Engineering. 344, 421–450, 2019.

[9]L. Zhuang, S.M. Hassanizadeh,C. Qin, and A. De Waal, Experimental Investigation of Hysteretic Dynamic Capillarity Effect in Unsaturated Flow,Water resources research, 53, doi.org/10.1002/2017WR020895, 2017.

[10]C. Qin, S.M. Hassanizadeh, and A. Ebigbo, Pore-scale network modeling of microbially-induced calcium carbonate precipitation (MICP): insights into scale dependence of biogeochemical reaction rates,Water Resources Research, 52, doi.org/10.1002/2016WR019128, 2016.

[11]C. Qin, Water transport in the gas diffusion layer of a polymer electrolyte fuel cell: dynamic pore-network modeling,Journal of the Electrochemical Society, 162, F1036-F1046, 2015.

[12]C. Qin, S.M. Hassanizadeh, Multiphase flow through multilayers of thin porous media: general balance equations and constitutive relationships for a solid-gas-liquid three-phase system,International Journal of Heat and Mass Transfer, 70, 693-708, 2014.


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