Carol Eleonora, Sanci Romina, Tanjal Carolina, Acosta Rosario, Galliari Julieta
Centro de Investigaciones Geológicas, Consejo Nacional de Investigaciones Científicas y Técnicas, Universidad Nacional de La Plata, Argentina.
Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires, Consejo Nacional de Investigaciones Científicas y Técnicas, Universidad de Buenos Aires, Argentina.
Sci Total Environ. 2025 Sep 20;996:180193. doi: 10.1016/j.scitotenv.2025.180193. Epub 2025 Aug 4.
Marshes, which are intertidal ecosystems mainly distributed in mid- and high-latitudes, exhibit complex hydrological connectivity between tidal and continental waters. While this connectivity has been more widely studied on beaches, their understanding in marshes, especially in arid and semiarid regions, is limited. On the northern coast of Argentine Patagonia, in Bahía San Blas, there are semiarid marshes adjacent to beach ridges containing freshwater lenses that are being affected by population growth. Given this context, the study aims to identify, through hydrochemical and isotopic signatures, the hydrological connectivity of marshes in Bahía San Blas area in relation to the inputs received from tidal flows and from the discharge of fresh groundwater from adjacent beach ridges. The study, conducted using multiple geochemical tools such as analysis of major ions, soluble nutrients, stable (δH y δO) and radioactive (Rn) isotopes, allowed to identify the different water inputs that support the hydrology of the marshes. This research revealed that the hydrology of the marshes is determined by the interaction between tidal inflow and the discharge of fresh groundwater from adjacent beach ridges. Although the water mixing occurring in the marsh is difficult to detect using major ions due to processes such as salt concentration from evaporation, the use of stable and radioactive isotopes enabled the identification and quantification of fresh groundwater inputs reaching up to 65 %. Groundwater discharge also supplies nutrients from beach ridges into the marsh. The results highlight the usefulness of isotopic tracers and the importance of considering groundwater discharge in arid marshes, which is often underestimated. Furthermore, the study warns that the exploitation of freshwater lenses and urban expansion could affect both the hydrodynamics and hydrochemistry of marsh groundwater, underscoring the need for integrated management and conservation strategies in light of climate change and anthropogenic pressure.
沼泽是主要分布在中高纬度地区的潮间带生态系统,在潮汐水和陆地水之间表现出复杂的水文连通性。虽然这种连通性在海滩上得到了更广泛的研究,但在沼泽地,尤其是干旱和半干旱地区,人们对其了解有限。在阿根廷巴塔哥尼亚的北海岸,圣布拉斯湾有半干旱沼泽,毗邻含有淡水透镜体的海滩脊,这些沼泽正受到人口增长的影响。在此背景下,该研究旨在通过水化学和同位素特征,确定圣布拉斯湾地区沼泽与潮汐水流以及相邻海滩脊淡水地下水排放之间的水文连通性。该研究使用了多种地球化学工具,如主要离子分析、可溶性养分分析、稳定(δH和δO)和放射性(Rn)同位素分析,从而确定了支持沼泽水文的不同水源输入。这项研究表明,沼泽的水文状况是由潮汐流入与相邻海滩脊淡水地下水排放之间的相互作用决定的。尽管由于蒸发导致盐分浓缩等过程,使用主要离子难以检测沼泽中发生的水混合情况,但稳定和放射性同位素的使用能够识别和量化高达65%的淡水地下水输入。地下水排放还将海滩脊中的养分输送到沼泽中。研究结果突出了同位素示踪剂的实用性以及考虑干旱沼泽中地下水排放的重要性,而这一点常常被低估。此外,该研究警告说,对淡水透镜体的开采和城市扩张可能会影响沼泽地下水的水动力和水化学,强调了在气候变化和人为压力下制定综合管理和保护策略的必要性。