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Elemental and Mineralogical Analysis of Beachrocks in Southern Coastal Region Sri Lanka

机译:斯里兰卡南部沿海地区滩涂的元素和矿物学分析

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Beachrock is coastal sediment that has been cemented primarily by calcium carbonate within the intertidal zone in tropical and subtropical regions. Considering that beachrock has the potential to inhibit coastal erosion, we performed laboratory tests to understand the formation mechanism of beachrocks in southern coastal regions of Sri Lanka. The mineralogical composition of beachrock samples were identified by FT-IR spectroscopic technique. The constituents of minerals present in the beachrocks were further confirmed by XRD analysis. Elemental concentrations of beachrock samples have been examined using WD-XRF spectrometry. The formative environment (sea water) was analyzed using EDTA titration, AAS, UV/Vis spectroscopy and Iron Chromatography. The results reveal the presence of minerals aragonite, calcite, orthoclase, quartz, albite, kaolinite and lime in the beachrocks. According to the results, there is a high probability to precipitate CaCO3 from the sea water in southern coastal regions indicating a positive formative environment for beachrocks. Hence, by appropriate regulation of the conditions could foster the development of manmade beachrocks to control the coastal erosion.
机译:滩石是沿海沉积物,主要在热带和亚热带地区的潮间带内由碳酸钙固结。考虑到滩涂有抑制海岸侵蚀的潜力,我们进行了实验室测试,以了解斯里兰卡南部沿海地区滩涂的形成机理。通过FT-IR光谱技术鉴定了滩涂样品的矿物学组成。 XRD分析进一步证实了滩涂中存在的矿物成分。使用WD-XRF光谱仪检查了滩石样品的元素浓度。使用EDTA滴定,AAS,UV / Vis光谱和铁色谱法分析了形成环境(海水)。结果揭示了在海滩岩中存在矿物文石,方解石,正长石,石英,钠长石,高岭石和石灰。根据结果​​,很可能会沉淀出CaCO 3 来自南部沿海地区的海水表明沙滩岩形成了积极的形成环境。因此,通过适当地调节条件,可以促进人造滩涂的发展,以控制海岸侵蚀。

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