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Deuterium in drinking water and its effects on cancer and longevity. 饮用水中的氘及其对癌症和寿命的影响。
IF 1.1 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2024-11-18 DOI: 10.1080/10256016.2024.2424454
Meiling Zhong, Jiaxue Wang, Ouyi Zhao, Qiuyi Li

This study investigates the spatial distribution of longevity levels, deuterium in drinking water, and cancer incidence rates, and further examines the impact of deuterium in drinking water on longevity and cancer incidence. Methods such as correlation coefficients and Kriging spatial interpolation were employed to uncover the characteristics of spatial distribution and identify correlations. Findings reveal that regions with higher longevity levels are mostly located on the eastern side of the Hu Huanyong Line (Heihe-Tengchong Line). Deuterium in drinking water decreases from low latitude, low elevation, and coastal areas to high latitude, high elevation, and inland regions. Notably, there is a positive correlation between deuterium content in drinking water and longevity levels, indicating that higher deuterium content is associated with increased longevity. Additionally, counties with lower deuterium content in drinking water show a reduced incidence of cancer cases.

本研究调查了长寿水平、饮用水中的氘和癌症发病率的空间分布,并进一步研究了饮用水中的氘对长寿和癌症发病率的影响。研究采用了相关系数和克里金空间插值法等方法来揭示空间分布特征并确定相关关系。研究结果表明,长寿地区主要分布在沪杭甬线(黑河-腾冲线)东侧。饮用水中的氘含量从低纬度、低海拔和沿海地区向高纬度、高海拔和内陆地区递减。值得注意的是,饮用水中的氘含量与长寿水平呈正相关,表明氘含量越高,寿命越长。此外,饮用水中氘含量较低的县癌症发病率也较低。
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引用次数: 0
Different continuous freshwater contributions to submarine groundwater discharge at a coastal peatland, southern Baltic Sea. 波罗的海南部沿海泥炭地海底地下水排放的不同连续淡水贡献。
IF 1.1 4区 环境科学与生态学 Q4 CHEMISTRY, INORGANIC & NUCLEAR Pub Date : 2024-11-11 DOI: 10.1080/10256016.2024.2422864
Anna-Kathrina Jenner, Rhodelyn Saban, Cátia M Ehlert von Ahn, Patricia Roeser, Iris Schmiedinger, Jürgen Sültenfuß, Anja Reckhardt, Michael Ernst Böttcher

The impact of freshwater sources like surface river runoff and submarine groundwater discharge (SGD) on coastal waters is currently in focus of intense debate and investigation. One of the ongoing challenges in SGD research is the characterization and quantification of the freshwater endmember contributions to the subsurface mixing zone and their influences on element balance and biogeochemical transformations. Long-term investigations of the sediment porewater composition provide characterization and understanding of the physical, hydrological and biogeochemical processes controlling the substance exchanges. In this study, we focus on the hydrochemical and stable isotope (δ2H, δ18O) compositions of sediment porewaters along the coastline of a southern Baltic Sea peatland. Coastal surface water and groundwater dynamics were monitored at two coastal sites using 5-m-long stationary lances over a 5-year period.The vertical compositional gradients were used to extrapolate to zero-salinity (ZS) components applying a binary mixing model on the salinity and water isotope composition. The results characterize a subterranean estuary (STE) with three potential mixing endmembers: two fresh groundwaters and the brackish Baltic Sea. Tritium-helium (3H-3He) porewater dating gave ages of more than about 20 years for the freshwater components. The ZS components were compared with other SGD sites along the southern Baltic Sea and North Sea and highlight the importance of local SGD studies for a proper groundwater endmember characterization as basis to understand hydrological and biogeochemical developments at the land-ocean continuum in times of current climate change.

地表径流和海底地下水排放(SGD)等淡水源对沿岸水域的影响,是目前激烈争论和调查的 焦点。目前,SGD 研究面临的挑战之一,是如何描述和量化淡水末端分子对次表层混合区的贡献, 以及它们对元素平衡和生物地球化学转化的影响。通过对沉积物孔隙水成分的长期研究,可以描述和了解控制物质交换的物理、水文和生物地球化学过程。在本研究中,我们重点研究了波罗的海南部泥炭地沿岸沉积物孔隙水的水化学和稳定同位素(δ2H、δ18O)组成。采用盐度和水同位素组成的二元混合模型,利用垂直成分梯度推断零盐度(ZS)成分。研究结果描述了一个地下河口(STE)的特征,该河口有三种潜在的混合内涵:两种淡水地下水和咸水波罗的海。氚-氦(3H-3He)孔隙水测年法给出了淡水成分超过 20 年的年龄。将 ZS 成分与波罗的海南部和北海沿岸的其他 SGD 地点进行了比较,并强调了当地 SGD 研究对于正确描述地下水终成体特征的重要性,这些终成体特征是了解当前气候变化时期陆地-海洋连续体的水文和生物地球化学发展的基础。
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Isotopes in Environmental and Health Studies
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