Congratulations to Yi Niu who defended his dissertation on December 7, 2017

Advisor: M. Clara Castro

 

Abstract:

Due to their temperature dependency, stable noble gases (He, Ne, Ar, Kr, and Xe) have been routinely used as indicators of past climate in sedimentary systems for over four decades. However, noble gas studies in fractured systems, where infiltration is rapid, remain scarce. In this dissertation, noble gas studies in fractured systems are presented, including two studies in ice-covered regions, one in the Greenland Ice Sheet (GrIS) and the other in the Athabasca Glacier (AG) of the Columbia Icefield in the Canadian Rockies, as well as two studies in a tropical basaltic island, the Island of Maui, Hawaii. Noble gases in the GrIS (Chapter 2) and the AG (Chapter 3) studies are used to constrain glacial meltwater sources, water source altitude and water residence times. In Maui, noble gases are first used to characterize the different water sources contributing to groundwater recharge (e.g., fog, orographic and synoptic-scale rain), and to assess whether the timing and location of recharge can be estimated based on atmospheric noble gas signatures (Chapter 4). In Chapter 5, the potential for noble gases to record temporal variations is assessed. Noble gases are used together with oxygen and hydrogen isotopic composition data to further constrain water source altitudes in Maui. 

Noble gases in the meltwater samples from both the GrIS and the AG are dominated by a partially equilibrated air-saturated water (ASW) component rather than trapped air in the glacial ice. Water source altitudes based on Xe range between 0.8 and 2.4 km for most samples from the GrIS and between 2.5 and 3.5 km for the AG. A crustal He component, observed in almost all samples in both studies, is used to estimate water residence times. Most meltwater samples from the GrIS yield water residence times between ~100 and ~400 years while two samples yield older ages of ~2000 and ~4000 years. In contrast, samples from the AG yield a younger average of ~160 years. Water samples were collected in Maui from rain events, springs from perched aquifers, and wells tapping the basal aquifer in June 2014 and February 2016. All samples are in disequilibrium with the atmosphere at the collection point and do not represent the mean annual air temperature. Distinct noble gas signatures in spring and basal aquifer samples suggest that the two types of aquifers are separate entities. In June 2014, noble gases in rainwater and basal aquifer display an ice-like signature possibly related to synoptic-scale rain. The basal aquifer yields similar noble gas signatures in both sampling seasons, while temporal variations are observed in rainwater and spring samples. A few springs and wells yield samples with a significant mantle He component in both years. A combined dataset of noble gas and water stable isotopic composition yield source altitudes for rainwater samples between 0.1 and 3 km above sea level (asl). Water source altitudes for most groundwater samples range between 1.5 and 5.5 km asl, indicating that the water source contributing to groundwater recharge that originates at higher altitudes in the atmosphere was not sampled.