首页> 外文期刊>Journal of limnology >Differences between groundwater fauna in shallow and in deep intergranular aquifers as an indication of different characteristics of habitats and hydraulic connections
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Differences between groundwater fauna in shallow and in deep intergranular aquifers as an indication of different characteristics of habitats and hydraulic connections

机译:浅层和深层粒间含水层中地下水动物区系的差异表明生境和水力联系的不同特征

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The fauna in the hyporheic zones of rivers has been relatively well studied but that from the phreatic zone remains comparatively unknown and there are few investigations into deeper intergranular aquifers (over 30 m in depth) due to technical difficulties. Two shallow boreholes of 29 m depth and two deep boreholes of 100 m depth, both near Ljubljana (Slovenia), were sampled more than 30 times between 14 January 2008 and 3 March 2009. On each occasion 14.4 to 18.0 m(3) of water were abstracted using a high-capacity pump, then filtered by means of a plankton net with a mesh size of 60 mu m. Organisms larger than 2 mm were damaged by the pump rotors, but their identification was still possible, while smaller representatives of the Copepoda (Crustacea) passed the rotors without damage. A near-by artesian borehole was sampled on 6 occasions. Water chemistry, physical properties and faunal composition analyses were carried out for each borehole. A total of 32 taxa, 24 of which were stygobites, were identified. Copepoda alone were represented by 16 species, 15 of which were stygobites. The shallow boreholes differ from the deep boreholes in their higher temperatures and higher concentrations of K+, Na+, Ca2+, Mg2+ and SO42- ions. The copepod communities in samples from the shallow boreholes differ sharply from those from the deep boreholes. There were also clear differences between shallow boreholes in two aquifers located a few kilometres apart, in physical and chemical characteristics as well as in fauna composition. Taxa with different ecological affinities, collected from groundwater, are indicators of hydraulic connections between different parts of an aquifer as well as of communication between surface and subsurface water bodies. The present study suggests that subterranean fauna, as well as epigean fauna, can provide effective support for classical dye/salt tracing experiments.
机译:对河流水流带的动物区系进行了比较充分的研究,但潜水区的动物区系仍然相对未知,由于技术上的困难,对深层粒间含水层(深度超过30 m)的研究很少。在2008年1月14日至2009年3月3日期间,对卢布尔雅那(斯洛文尼亚)附近的两个深度为29 m的浅井眼和两个深度为100 m的深井眼进行了采样,采样次数超过30次。每次取水14.4至18.0 m(3)。用大容量泵抽提水,然后用网眼大小为60微米的浮游生物过滤。大于2毫米的生物体被泵的转子损坏,但仍然可以识别它们,而(足类(甲壳纲)的较小代表通过转子却没有受到损坏。 6次对附近的自流井进行了采样。对每个钻孔进行水化学,物理性质和动物组成分析。总共确定了32个分类单元,其中有24个为后sty类。 pe足目仅由16个物种代表,其中15个是后go。浅孔与深孔的区别在于它们的较高温度和较高的K +,Na +,Ca2 +,Mg2 +和SO42-离子浓度。浅孔样品中的pe足类群落与深孔样品中的po足类群落明显不同。在相距数公里的两个含水层中的浅孔之间,在物理和化学特征以及动物群组成方面也存在明显差异。从地下水中收集的具有不同生态亲和力的分类单元是含水层不同部分之间的水力连接以及地表水与地下水体之间的连通的指标。本研究表明,地下动物群以及表生动物群可以为经典的染料/盐示踪实验提供有效的支持。

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