Arid
DOI10.5194/hess-25-1211-2021
Triple oxygen isotope systematics of evaporation and mixing processes in a dynamic desert lake system
Voigt, Claudia; Herwartz, Daniel; Dorador, Cristina; Staubwasser, Michael
通讯作者Voigt, C (corresponding author), Univ Cologne, Inst Geol & Mineral, Zulpicher Str 49b, D-50674 Cologne, Germany. ; Voigt, C (corresponding author), Aix Marseille Univ, Ctr Natl Rech Sci CNRS, CEREGE, Aix En Provence, France.
来源期刊HYDROLOGY AND EARTH SYSTEM SCIENCES
ISSN1027-5606
EISSN1607-7938
出版年2021
卷号25期号:3页码:1211-1228
英文摘要This study investigates the combined hydrogen deuterium and triple oxygen isotope hydrology of the Salar del Huasco, an endorheic salt flat with shallow lakes at its centre that is located on the Altiplano Plateau, N Chile. This lacustrine system is hydrologically dynamic and complex because it receives inflow from multiple surface and groundwater sources. It undergoes seasonal flooding, followed by rapid shrinking of the water body at the prevailing arid climate with very high evaporation rates. At any given point in time, ponds, lakes, and recharge sources capture a large range of evaporation degrees. Samples taken between 2017 and 2019 show a range of delta O-18 between 13.3 parts per thousand and 14.5 parts per thousand, dexcess between 7 parts per thousand and 100 parts per thousand, and O-17-excess between 19 and -108 per meg. A pan evaporation experiment conducted on-site was used to derive the turbulence coefficient of the Craig-Gordon isotope evaporation model for the local wind regime. This, along with sampling of atmospheric vapour at the salar ( -21.0 +/- 3.3 parts per thousand for delta O-18, 34 +/- 6 parts per thousand for d-excess and 23 +/- 9 per meg for O-17-excess), enabled the accurate reproduction of measured ponds and lake isotope data by the Craig-Gordon model. In contrast to classic delta H-2- delta O-18 studies, the O-17-excess data not only allow one to distinguish two different types of evaporation - evaporation with and without recharge - but also to identify mixing processes between evaporated lake water and fresh flood water. Multiple generations of infiltration events can also be inferred from the triple oxygen isotope composition of inflow water, indicating mixing of sources with different evaporation histories. These processes cannot be resolved using classic delta H-2- delta O-18 data alone. Adding triple oxygen isotope measurements to isotope hydrology studies may therefore significantly im- prove the accuracy of a lake's hydrological balance - i.e. the evaporation-to-inflow ratio (E / I) - estimated by water isotope data and application of the Craig-Gordon isotope evaporation model.
类型Article
语种英语
开放获取类型Green Submitted, gold
收录类别SCI-E
WOS记录号WOS:000627626700001
WOS关键词AQUEOUS SALT-SOLUTIONS ; PAMPA DEL TAMARUGAL ; HYDROGEN ISOTOPES ; STABLE HYDROGEN ; ATACAMA DESERT ; WATER ; PRECIPITATION ; FRACTIONATION ; VARIABILITY ; PHYTOLITHS
WOS类目Geosciences, Multidisciplinary ; Water Resources
WOS研究方向Geology ; Water Resources
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/350515
作者单位[Voigt, Claudia; Herwartz, Daniel; Staubwasser, Michael] Univ Cologne, Inst Geol & Mineral, Zulpicher Str 49b, D-50674 Cologne, Germany; [Voigt, Claudia] Aix Marseille Univ, Ctr Natl Rech Sci CNRS, CEREGE, Aix En Provence, France; [Dorador, Cristina] Univ Antofagasta, Ctr Biotecnol, Angamos 601, Antofagasta 1270300, Chile
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GB/T 7714
Voigt, Claudia,Herwartz, Daniel,Dorador, Cristina,et al. Triple oxygen isotope systematics of evaporation and mixing processes in a dynamic desert lake system[J],2021,25(3):1211-1228.
APA Voigt, Claudia,Herwartz, Daniel,Dorador, Cristina,&Staubwasser, Michael.(2021).Triple oxygen isotope systematics of evaporation and mixing processes in a dynamic desert lake system.HYDROLOGY AND EARTH SYSTEM SCIENCES,25(3),1211-1228.
MLA Voigt, Claudia,et al."Triple oxygen isotope systematics of evaporation and mixing processes in a dynamic desert lake system".HYDROLOGY AND EARTH SYSTEM SCIENCES 25.3(2021):1211-1228.
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