Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.5194/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
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ISSN | 1027-5606 |
EISSN | 1607-7938 |
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 |
推荐引用方式 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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