Identifying recharge processes into a vast fossil aquifer based on dynamic groundwater 81Kr age evolution

JOURNAL OF HYDROLOGY

卷:587

Article

Ram, Roi^1,2  Burg, Avihu²  Zappala, Jake C.^3,4  Yokochi, Reika⁵  Yechieli, Yoseph^1,2  Purtschert, Roland⁶  Jiang, Wei⁷  Lu, Zheng-Tian⁷  Mueller, Peter³  Bernier, Ryan⁵  Adar, Eilon M.¹ 

[1] Ben Gurion Univ Negev, Zuckerberg Inst Water Res, Blaustein Inst Desert Res, Sede Boker Campus 8499000, Sede Boqer, Israel

[2] Geol Survey Israel, 32 Yeshayahu Leibowitz St, IL-9692100 Jerusalem, Israel

[3] Argonne Natl Lab, Phys Div, 9700 S Cass Ave, Lemont, IL 60439 USA

[4] Univ Chicago, Dept Phys, 5720 S Ellis Ave, Chicago, IL 60637 USA

[5] Univ Chicago, Dept Geophys Sci, 5734 S Ellis Ave, Chicago, IL 60637 USA

[6] Univ Bern, Phys Inst, Climate & Environm Phys, Hsch Str 6, CH-3012 Bern, Switzerland

[7] Univ Sci & Technol China, CAS Ctr Excellence Quantum Informat & Quantum Phy, Hefei Natl Lab Phys Sci Microscale, 96 JinZhai Rd, Hefei 230026, Anhui, Peoples R China

关键词: Kr-81;    C-14;    Old groundwater dating;    Nubian Sandstone Aquifer;    Sinai-Negev Basin;    Mixing;   

DOI  :  10.1016/j.jhydrol.2020.124946

来源: Elsevier

【 摘 要 】

Water in deep aquifers in arid regions is often considered to be fossil when modern recharge rates are negligible relative to the reservoir capacity. Over the past five decades, the Nubian Sandstone Aquifer (NSA) in the arid region of the Sinai Peninsula (Egypt) and the Negev Desert (Israel) has been considered to contain fossil water based on C-14 dating, which revealed C-14 ages of about 30 kyr over most of the aquifer. However, this relatively homogeneous age distribution contradicts the expected increase in groundwater age in the direction of decreasing piezometric head along the flow trajectories. Here, dating results with the longer-lived Kr-81 radioisotope (t(1/2) = 229 +/- 11 kyr) are presented, highlighting a wide age range of 40 kyr to 630 kyr in the confined sections of the aquifer, all with very low C-14 activity ( < 1 pmC). Elevated Kr-81 and C-14 activities were only observed within or close to the system's recharge areas. These findings support a new perception of groundwater replenishment during different epochs from the early mid-Pleistocene to the Holocene. By tracking the downstream age evolution, rejuvenation was identified in places where the confinement had been breached. At other locations, the existence of an older groundwater body contributing to the aquifer was detected by means of strongly depleted Kr-81 activity. High spatial heterogeneity in groundwater ages close to the discharge zone of the system is attributed to pronounced age stratification with depth. Calculated ages in the more isolated sections of the system were used to assess regional flow velocity, hydraulic conductivity, and their agreement with present recharge rates. We conclude that groundwater ages should be reevaluated with Kr-81 in regional aquifers where low C-14 activities prevail. With an effective age range beyond one million years, this may enable the reconstruction of recharge history well into the Pleistocene and provide crucial information for the management of groundwater resources.

【 授权许可】

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