报告人：Ciaran Harman, Johns Hopkins University

报告摘要：The transit time of water through hydrologic systems is a fundamental control on the biological and chemical transformations that occur within them. New approaches to characterizing these transit times are changing the way we interpret hydrologic tracer dynamics, and are generating more detailed insights into transit times through complex, time-variable hydrologic systems. However these analyzes have typically been separated from analyzes of the hydraulics that drive flow responses. In this talk I will introduce the current methods, and show how it is possible to extend them to generalize relationships between total storage and discharge (which underlie many hydrologic models) into a more nuanced relationship between the age distribution of storage and the age distribution of discharge. This unifies spatially-lumped representations of flow and transport into a single representation that captures the emergent result of interactions between celerity and velocity in hydrologic systems.

Results from a range of systems including small experimental watersheds, stream reaches and their associated hyporheic zones, and an experimental lysimeter, suggest ways that the structure of the transit time distributions, and their variability in time, can be related to the structure of the hydrologic system. This suggests, first, the proposed approach might form the basis of future lumped models of flow and solute transport at subwatershed scales, and second, future research in this area might focus on relating the emergent, unified, flow and transport properties revealed by this type of analysis to the structure of the critical zone.

报告时间：2016年8月31日（周三）下午14: 30－16: 00

报告地点：地理科学馆411会议室

主持人：  汤秋鸿 研究员

陆地水循环及地表过程院重点实验室

2016-08-29