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研究副教授

梁修雨

  • 简历
  • 科研
  • 教学
  • 发表论著

梁修雨,2012年毕业于南京大学,获水文学及水资源专业博士学位。曾任南京大学水科学研究中心助理研究员、副研究员。主要从事地下水资源与环境方向的研究工作,具体包括流域尺度浅层地下水流及溶质的时间尺度性、饱和-非饱和水流耦合模拟、以及地表-地下水交互。发表科技论文20余篇,其中以第一/通讯作者身份在水资源领域顶级期刊Water Resources Research等上发表SCI论文16篇。主持包括国家自然科学基金、国家水专项子任务和江苏省自然科学基金3项。长期担任水资源领域多个学术期刊的审稿人,包括Advance in Water Resources,Journal of Hydrology,Hydrological Processes,Groundwater,Hydrogeology Journal,Stoch Environ Res Risk Assess等。

 

目前任职
南方科技大学,环境科学与工程学院,研究副教授

 

工作经历
2018.02 – 今,    南方科技大学,    环境科学与工程学院, 研究副教授
2015.07 – 2018.01,南京大学,   水科学研究中心,  副研究员
2012.07 – 2015.07,南京大学,   水科学研究中心,  助理研究员
2016.11 – 2017.11,美国德州农工大学,地质与地球物理系, 访问学者
2013.08 – 2014.08,美国爱荷华大学, 地球科学系,   博士后

 

教育背景
2009.09 – 2012.06,南京大学,  地球科学与工程学院,水文学及水资源,博士
2005.09 – 2008.06,安徽理工大学, 地球与环境学院,地质工程(水文地质),硕士
2001.09 – 2005.06,安徽理工大学, 地球与环境学院,资源环境与城乡规划,学士

 

科研项目
[1]. 国家自然科学基金青年项目,基于随机方法的饱和-非饱和带水流时间尺度性研究,2014年1月-2016年12月,主持
[2]. 江苏省自然科学基金青年项目,土壤含水率和地下位的时间尺度性研究,2013年7月-2016年7月,主持
[3]. 国家重大水专项“十二五”淮河项目子任务,八里河流域水质目标管理方案研究,2015年6月-2018年12月,60万,共同主持
[4]. 国家自然科学基金重点项目,我国西南地区基岩裂隙水的形成与分布规律及探测理论研究,2014年1月-2018年12月,核心参与
[5]. 江苏省科技示范工程,江苏省耕地污染防治科技示范工程,2015年7月-2018年6月,参与

 

奖励与荣誉
[1]. 2011, 南京大学光华奖学金一等奖
[2]. 2011, 南京大学优秀研究生

主要研究方向:

1. 饱和-非饱和水流耦合模拟
2. 地表-地下水交互
3. 地下水年龄分布
4. 流域尺度地下水流及溶质的时间尺度性
 

(1)期刊论文
[1]. Liang, X.Y., H.B. Zhan, K. Schilling, 2018. Spatiotemporal Responses of Groundwater Flow and Aquifer-River Exchanges to Flood Events, Water Resources Research. DOI:10.1002/2017WR022046
[2]. Liang, X.Y*., H.B. Zhan*, Y.K. Zhang, J. Liu, 2018. Underdamped Slug Tests with Unsaturated-Saturated Flows by Considering Effects of Wellbore Skins. Hydrological Processes. (In press)
[3]. Liang, X.Y*., H.B. Zhan*, Y.K. Zhang, K. Schilling, 2017. Base flow recession from Unsaturated-Saturated porous media considering lateral unsaturated discharge and aquifer compressibility, Water Resources Research, 53(9), 7832-7852. DOI: 10.1002/2017WR020938.
[4]. Liang, X.Y*., H.B. Zhan, Y.K. Zhang, J. Liu, 2017. On the coupled unsaturated-saturated flow process induced by vertical, horizontal, and slant wells in unconfined aquifers. Hydrology and Earth System Sciences, 21(2): 1251-1262. DOI:10.5194/hess-21-1251-2017.
[5]. Zhao, Y., Y.-K. Zhang*, and X. Liang*(通讯作者), 2017. Three-Dimensional Hydromechanical Modeling during Shearing by Nonuniform Crust Movement, Geofluids, Article ID 9605313, 14 pages, 2017. doi:10.1155/2017/9605313
[6]. Yang, C., Y.-K. Zhang, X.Y. Liang*(通讯作者), 2017. Analysis of temporal variation and scaling of hydrological variables based on a numerical model of the Sagehen Creek watershed. Stoch Environ Res Risk Assess, 1-12. DOI:10.1007/s00477-017-1421-0.
[7]. Liang, X.Y., Keith. Schilling, Y.-K. Zhang, J. Christopher, 2016. Co-Kriging Estimation of Nitrate-Nitrogen Loads in an Agricultural River, Water Resources Management, 30(5):1771-1784.
[8]. Zhao, Y.Q., Y.-K. Zhang, X.Y. Liang*(通讯作者), 2016. Analytical Solutions of Three-Dimensional Groundwater Flow to a Well in a Leaky Sloping Fault-Zone Aquifer, Journal of Hydrology, 539:204–213.
[9]. Yang, C., Y.-K. Zhang, X.Y. Liang*(通讯作者), 2016. Effects of temporally correlated infiltration on water flow in an unsaturated-saturated system. Stoch Environ Res Risk Assess, 30(7): 2009-2017. DOI:10.1007/s00477-015-1119-0
[10]. Liang, X.Y., Y.-K. Zhang, Keith. Schilling, 2016. Effect of heterogeneity on spatiotemporal variations of groundwater level in a bounded unconfined aquifer. Stoch Environ Res Risk Assess, 30(1): 1-8. DOI: 10.1007/s00477-014-0990-4.
[11]. Liang, X.Y., Y.-K. Zhang, 2015. Analyses of uncertainties and scaling of groundwater level fluctuations. Hydrology and Earth System Sciences, 01/2015; 12(1):1-23.
[12]. Liang, X.Y., Y.-K. Zhang, Keith. Schilling, 2015. Analytical solutions for two-dimensional groundwater flow with subsurface drainage tiles. Journal of Hydrology, 521(0): 556-564.
[13]. Liang, X.Y., Y.-K. Zhang, 2013. Temporal and spatial variation and scaling of groundwater levels in a bounded unconfined aquifer. Journal of Hydrology, 479: 139-145.
[14]. Liang, X.Y., Y.-K. Zhang, 2013. Groundwater flow with a variable source in a heterogeneous aquifer bounded by fluctuating river stages. Advance in Water Resources, 58:1-9.
[15]. Liang, X.Y., Y.-K. Zhang, 2012. A new analytical method for groundwater recharge and discharge estimation. Journal of Hydrology, 450: 17-24.
[16]. Liang, X.Y., Y.-K. Zhang, 2012. Analytical Solution for Drainage and Recession from an Unconfined Aquifer. Groundwater, 50(5): 793-798.
[17]. Schilling, K. E., C. S. Jones, C. F. Wolter, X. Liang, Y. K. Zhang, A. Seeman, T. Isenhart, D. Schnoebelen, and M. Skopec, 2017. Variability of nitrate-nitrogen load estimation results will make quantifying load reduction strategies difficult in Iowa, Journal of Soil and Water Conservation, 72(4), 317-325.
[18]. 王莹, 张幼宽, 梁修雨*(通讯作者), 谢显传,2018. 沙颍河流域安徽段水环境容量计算及动态分析, 人民黄河(出版中)
[19]. 杨晨, 张幼宽, 梁修雨*(通讯作者), 2015. 分形入渗下非饱和-饱和系统中水流的时空变化, 南京大学学报(自然科学), 51(06): 1279-1290.
[20]. 杨晨, 张幼宽, 梁修雨*(通讯作者), 2015. 非均质性对非饱和—饱和系统水流时空变化的作用, 高校地质学报,21(3): 559-568
[21]. 吴海燕, 傅世锋, 蔡晓琼, 汤坤贤, 曹超, 陈庆辉, 2015. 梁修雨. 东山岛地下水“三氮”空间分布特征, 环境科学, 36(09): 3203-3211.
[22]. 郑玉虎, 张幼宽, 梁修雨, 2015. 贾鲁河中牟段河岸带地下水流及水质特征研究, 高校地质学报,21(2): 234-242
[23]. 鲁海峰, 姚多喜, 梁修雨, 郭立全, 沈丹, 2013. 采动底板横观各向同性岩体应力解析解, 地下空间与工程学报, 9(5): 1050-1056.
[24]. 陈荦, 张幼宽, 梁修雨, 袁文波, 潘田, 2013. 土壤-含水层侧渗系统在净化河水中的应用以郑州市索须河工程为例, 水文地质与工程地质,40(4): 93-98.

 

(2)学术会议论文与报告
[1] Liang, X.Y., H.B. Zhan, Y.-K. Zhang, 2017. Effects of Unsaturated Zones on Baseflow Recession: Analytical Solution and Application, AGU Fall meeting, New Orleans, December 11-15.
[2] Zhan, H.B., X.Y., Liang, 2017. Baseflow Recession from Unsaturated-Saturated Flow, GSA Annual Meeting in Seattle, Washington, October 25.
[3] Liang, X.Y., Keith. Schilling, Y.-K. Zhang, J. Christopher, 2016. Estimation of nitrate-nitrogen loads in an Iowa river using kriging and rating curve methodologies, AGU Fall meeting, San Francisco, December 12-16.
[4] Yang, C., Y.-K. Zhang, X.Y. Liang, J.D. Liu, 2016. Temporal variation and scaling of hydrological variables in a typical watershed, AGU Fall meeting, San Francisco, December 12-16.
[5] Liang, X.Y. and Y.-K. Zhang, 2015. The uncertainties and temporal scaling of groundwater level fluctuations in a bounded aquifer, AGU Fall meeting, San Francisco, December 14-18.
[6] Zhao, Y.Q., X.Y. Liang, Y.-K. Zhang, 2015. Hydromechanical modeling of tectonically driven groundwater flow, AGU Fall meeting, San Francisco, December 14-18.
[7] Yang, C., Y.-K. Zhang, X.Y. Liang, 2014. Damping effect of an unsaturated-saturated system on tempospatial variations of pressure head and specific flux, AGU Fall meeting, San Francisco, December 15-19.
[8] Liang, X.Y. and Y.-K. Zhang, 2013. Temporal and spatial variation and scaling of groundwater levels in a bounded unconfined aquifer, AGU Fall meeting, San Francisco, December 9-13.
[9] Zhang, Y.-K., C. Yang, X.Y. Liang, 2015. Temporal variation and scaling of hydrological variables in a typical watershed, International Groundwater Forum, Xi’an, July 6-7.
[10] Liang, X.Y. and Y.-K. Zhang, 2012. Temporal variation of hydrogeological variables and its implication, International Groundwater Forum, Baoding, July 6-7.
[11] Zhang, Y.-K., and X.Y. Liang, 2011. A new analytic method for recharge and discharge estimation using observed groundwater levels, International Groundwater Forum, Wuhan, July 14-15, 2011.