Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.chemgeo.2021.120458 |
The triple argon isotope composition of groundwater on ten-thousand-year timescales | |
Seltzer, Alan M.; Krantz, John A.; Ng, Jessica; Danskin, Wesley R.; Bekaert, David V.; Barry, Peter H.; Kimbrough, David L.; Kulongoski, Justin T.; Severinghaus, Jeffrey P. | |
通讯作者 | Seltzer, AM (corresponding author), Woods Hole Oceanog Inst, Marine Chem & Geochem Dept, Woods Hole, MA 02543 USA. |
来源期刊 | CHEMICAL GEOLOGY
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ISSN | 0009-2541 |
EISSN | 1872-6836 |
出版年 | 2021 |
卷号 | 583 |
英文摘要 | Understanding the age and movement of groundwater is important for predicting the vulnerability of wells to contamination, constraining flow models that inform sustainable groundwater management, and interpreting geochemical signals that reflect past climate. Due to both the ubiquity of groundwater with order ten-thousand-year residence times and its importance for climate reconstruction of the last glacial period, there is a strong need for improving geochemical dating tools on this timescale. Whereas C-14 of dissolved inorganic carbon and dissolved He-4 are common age tracers for Late Pleistocene groundwater, each is limited by systematic uncertainties related to aquifer composition and lithology, and the extent of water-rock interaction. In principle, radiogenic Ar-40 in groundwater acquired from decay of 40K in aquifer minerals should be insensitive to some processes that impact C-14 and He-4 and thus represent a useful, complementary age tracer. In practice, however, detection of significant radiogenic Ar-40 signals in groundwater has been limited to a small number of studies of extremely old groundwater (>100 ka). Here we present the first high-precision (<1 parts per thousand) measurements of triple Ar isotopes (Ar-40, Ar-38, Ar-36) in groundwater. We introduce a model that distinguishes radiogenic Ar-40 from atmospheric Ar-40 by using the non-radiogenic Ar isotopes (Ar-36, Ar-38) to correct for mass-dependent fractionation. Using this model, we investigate variability in radiogenic Ar-40 excess (Delta Ar-40) across 58 groundwater samples collected from 36 wells throughout California (USA). We find that Delta Ar-40 ranges from similar to 0 parts per thousand (the expected minimum value) to +4.2 parts per thousand across three study areas near Fresno, San Diego, and the western Mojave Desert. Based on measurements from a network of 23 scientific monitoring wells in San Diego, we find evidence for a strong dependence of Delta Ar-40 on aquifer lithology. We suggest that Delta Ar-40 is fundamentally controlled by the weathering of old K-bearing minerals and thus reflects both the degree of groundwater-rock interaction, which is related to groundwater age, and the integrated flow through different geological formations. Future studies of Late Pleistocene groundwater may benefit from high-precision triple Ar isotope measurements as a new tool to better interpret C-14- and He-4-based constraints on groundwater age and flow. |
英文关键词 | Noble gas Groundwater Isotope geochemistry Groundwater dating |
类型 | Article |
语种 | 英语 |
开放获取类型 | Green Published |
收录类别 | SCI-E |
WOS记录号 | WOS:000702309700010 |
WOS关键词 | GREAT ARTESIAN BASIN ; NOBLE-GASES ; MOLECULAR-DIFFUSION ; MOJAVE DESERT ; CALIFORNIA ; FRACTIONATION ; WATER ; CRUSTAL ; HELIUM ; EOCENE |
WOS类目 | Geochemistry & Geophysics |
WOS研究方向 | Geochemistry & Geophysics |
来源机构 | United States Geological Survey |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/362844 |
作者单位 | [Seltzer, Alan M.; Krantz, John A.; Bekaert, David V.; Barry, Peter H.] Woods Hole Oceanog Inst, Marine Chem & Geochem Dept, Woods Hole, MA 02543 USA; [Ng, Jessica; Kulongoski, Justin T.; Severinghaus, Jeffrey P.] Scripps Inst Oceanog, Geosci Res Div, La Jolla, CA USA; [Danskin, Wesley R.; Kulongoski, Justin T.] US Geol Survey, Calif Water Sci Ctr, San Diego, CA USA; [Kimbrough, David L.] San Diego State Univ, Geol Sci, San Diego, CA 92182 USA |
推荐引用方式 GB/T 7714 | Seltzer, Alan M.,Krantz, John A.,Ng, Jessica,et al. The triple argon isotope composition of groundwater on ten-thousand-year timescales[J]. United States Geological Survey,2021,583. |
APA | Seltzer, Alan M..,Krantz, John A..,Ng, Jessica.,Danskin, Wesley R..,Bekaert, David V..,...&Severinghaus, Jeffrey P..(2021).The triple argon isotope composition of groundwater on ten-thousand-year timescales.CHEMICAL GEOLOGY,583. |
MLA | Seltzer, Alan M.,et al."The triple argon isotope composition of groundwater on ten-thousand-year timescales".CHEMICAL GEOLOGY 583(2021). |
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