个人简介 Personal Profile 国家杰出青年基金获得者，教育部“长江学者”特聘教授。1999年成都理工学院沉积学博士毕业，2001年同济大学海洋科学博士后出站、并留校任教至今；2001年评为副教授，2004年晋升教授；现任海洋地质国家重点实验室主任。主要从事南海深海沉积过程和南海陆源碎屑沉积物从源到汇的海陆结合研究，通过现代过程现场观测和大洋钻探长期记录分析，研究深海沉积动力过程的机理及其不同时间尺度的全球变化响应。主持国家自然科学基金重大研究计划项目、重点项目等10余项，代表性研究成果在Science、Earth-Science Reviews、Geology等期刊上发表。曾获法国国家棕榈学术骑士勋章。 研究方向Research Directions 海洋沉积学,深海沉积动力学,环境演变与全球变化,沉积物源汇过程,粘土矿物与碳循环,海洋观测系统 2. 机电结构优化与控制 研究内容：在对机电结构进行分析和优化的基础上，运用控制理论进行结构参数的调整，使结构性能满足设计要求。1. 仿生结构材料拓扑优化设计, 仿生机械设计 研究内容：以仿生结构为研究对象，运用连续体结构拓扑优化设计理论和方法，对多相仿生结构(机构)材料进行2. 机电结构优化与控制 研究内容：在对机电结构进行分析和优化的基础上，运用控制理论进行结构参数的调整，使结构性能满足设计要求。1. 仿生结构材料拓扑优化设计, 仿生机械设计 研究内容：以仿生结构为研究对象，运用连续体结构拓扑优化设计理论和方法，对多相仿生结构(机构)材料进行整体布局设计。 整体布局设计。 项目情况 在研科研项目1. “南海南部深海沉积搬运过程及其对海洋碳循环影响的锚系观测研究”（编号42130407），2022.1-2026.12，国家自然科学基金重点项目。项目简介：陆源和海源颗粒有机碳向深海的搬运过程，是海洋碳循环的关键组成部分，对全球气候的多尺度变化产生重要影响。但是，前人研究多忽视了陆源颗粒有机碳向深海的侧向搬运过程，而这种过程在发育大量陆源物质输入的边缘海尤其重要。本项目选择南海南部湄公河岸外和巽他陆架以北的深海区域，通过布设深海锚系，原位观测深层海流和沉积搬运动力过程的连续时间变化序列；通过沉积物捕集器样品的陆源/海源颗粒通量、稳定/放射性有机碳同位素、粘土矿物、锶/钕同位素、微区层析成像等测试分析，研究南海南部深海陆源和海源颗粒有机碳的侧向搬运和垂向沉降作用、陆源粘土矿物的源汇搬运过程、以及粘土矿物与陆源/海源颗粒有机碳的相互作用，定量评估世界级大型河流（湄公河）和宽广陆架（巽他陆架）输入南海深海颗粒有机碳效率，揭示深海沉积搬运过程对颗粒有机碳保存或降解的影响机制。本项研究对于探索深海过程影响海洋碳循环和全球气候变化机理具有重要的科学意义。2. “国际大洋钻探计划合作研究”（编号20590780200），2020.10-2023.9，上海市“科技创新行动计划”国际科技合作项目。项目简介：国际大洋钻探计划（IODP）是地球科学领域迄今规模最大、影响最深、历时最久的国际大科学计划，五十多年来取得的科学成就，为地球系统科学的发展做出巨大贡献。目前，美国、日本和欧洲作为平台提供者共同领导IODP。中国是IODP大家庭的积极成员，近期提出成为与美、日、欧并驾齐驱的IODP平台提供者并进入IODP领导层的发展目标。本项目围绕中国IODP的这一战略目标，利用我国在东南亚和“一带一路”国家合作的优势，与美国、印度尼西亚、马来西亚和泰国建立国际科技合作伙伴关系，提出在南海南部巽他陆架实施大洋钻探航次，回答热带低纬地区的海平面变化、流域演化和全球碳循环等国际前沿科学问题。该航次的组织和实施将是中国作为第四个钻探平台自主执行的第一个IODP航次，将有力地促成中国成为IODP国际大科学计划的领导成员，推动我国实施创新驱动发展战略，对解决全球变化等人类命运共同体面对的可持续发展问题具有重要意义。3. “青藏高原典型河流沉积物源汇过程及其对极端气候变化的响应研究”（编号2019QZKK020403），2019.11-2024.10，第二次青藏高原综合科学考察研究任务二子专题。项目简介：河流沉积物从源头到边缘海盆地输送过程中所组成的“源-汇”系统，对于全球物质循环、碳循环及水循环都具有重要的意义。而“亚洲水塔”青藏高原是全球主要大河的发源地，每年向周边海洋输送大量的物质。要理解这一巨大的“源-汇”系统的动力机制及其对全球气候和环境的影响，不仅需要对河流上游的青藏高原开展工作，也要同时在河流下游及边缘海盆地开展样品采集分析和动力观测工作。本子专题将全流域河流沉积物的矿物学和地球化学分析与流域关键地区、河口和临近深海沉积动力观测有机结合，旨在获取雅鲁藏布江—布拉马普特拉河和澜沧江—湄公河等流域河流沉积物从源到汇输送过程中沉积物的组成成分及动力条件等的空间变化，从而研究青藏高原河流沉积物从源到汇输入过程和动力机制，特别是河口及河流下游等沉积物汇区的沉积动力过程和机制，评估其对边缘海盆地的沉积贡献。利用河口和临近深海实时观测系统所获数据和悬浮沉积物样品，捕捉台风、强降雨等极端天气事件的信号，对比其与背景天气条件下的异同，从而评估河流沉积物源汇过程对极端天气事件的响应，并评估极端天气事件对观测地区水土保持、农业活动等的影响。 报考意向 招生信息 海洋与地球科学学院 硕士研究生 序号 专业 招生人数 年份 1 海洋科学 2 2024 博士研究生 序号 专业 招生人数 年份 1 海洋科学 2 2024 博士1： 海洋地质学(古海洋学；微体古生物学；海洋沉积学；大陆边缘盆地与石油地质；岩石矿物与宝石学) 报考意向 姓名: 手机号码： 邮箱： 毕业院校： 所学专业： 报考类型： 博士 硕士 个人简历*： 上传附件 支持扩展名：.rar .zip .doc .docx .pdf .jpg .png .jpeg 成绩单*： 上传附件 支持扩展名：.rar .zip .doc .docx .pdf .jpg .png .jpeg 其他材料： 上传附件 支持扩展名：.rar .zip .doc .docx .pdf .jpg .png .jpeg 备注： 提交 科研项目 在研科研项目1. “南海南部深海沉积搬运过程及其对海洋碳循环影响的锚系观测研究”（编号42130407），2022.1-2026.12，国家自然科学基金重点项目，负责人；2. “国际大洋钻探计划合作研究”（编号20590780200），2020.10-2023.9，上海市“科技创新行动计划”国际科技合作项目，负责人；3. “青藏高原典型河流沉积物源汇过程及其对极端气候变化的响应研究”（编号2019QZKK020403），2019.11-2024.10，第二次青藏高原综合科学考察研究任务二子专题，负责人； 研究成果 主要刊物论文20231. 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