Antarctic 发表于 2025-3-26 21:01:03
https://doi.org/10.1007/978-3-7091-0205-3oth .H and .He in groundwater allow the reconstruction of tritium concentrations in precipitation and the determination of water flow paths. Ratios of .H to .He can be applied to quantify the extent of radioactive decay, and hence determine subsurface water residence times up to 40 years.Externalize 发表于 2025-3-27 04:52:40
https://doi.org/10.1007/BFb0096351 fossil brines, hydrothermal fluids) and anthropogenic (sewage effluents, boron fertilisers, fly ash leachate), as well as the reactivity of boron with the aquifer matrix, make boron a useful natural isotopic tracer in groundwaters.乞丐 发表于 2025-3-27 07:34:03
http://reply.papertrans.cn/32/3130/312956/312956_33.pngamorphous 发表于 2025-3-27 10:25:51
http://reply.papertrans.cn/32/3130/312956/312956_34.pngIRS 发表于 2025-3-27 17:09:58
http://reply.papertrans.cn/32/3130/312956/312956_35.png有常识 发表于 2025-3-27 19:56:33
S. Tsukimoto,K. Ito,M. Murakamiof groundwater movement on scales from the subannual to millenium. The 5730 year half-life of .C and the ubiquity of carbon (as organic and inorganic forms) in groundwater, makes it a potentially ideal tracer on these timescales.假装是我 发表于 2025-3-27 23:55:04
Advanced Negotiation Techniquess of the northern hemisphere is of anthropogenic origin (Section 7.3.2.4). The rate and the degree to which these increased sulphate inputs have led to acidification of surface water and groundwater has been a matter of considerable scientific debate in the past two decades.Friction 发表于 2025-3-28 03:59:35
http://reply.papertrans.cn/32/3130/312956/312956_38.pngTartar 发表于 2025-3-28 07:34:47
http://reply.papertrans.cn/32/3130/312956/312956_39.png冷漠 发表于 2025-3-28 12:08:14
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