Begy Róbert-Csaba, Preoteasa Luminita, Timar-Gabor Alida, Mihăiescu Radu, Tănăselia Claudiu, Kelemen Szabolcs, Simon Hedvig
Babeş-Bolyai University, Faculty of Environmental Science and Engineering, 30 Fântânele Street, 400294, Cluj-Napoca, Romania; Interdisciplinary Research Institute on Bio-Nano-Science, Babes-Bolyai University, Treboniu Laurean 42, 400271 Cluj-Napoca, Romania.
University of Bucharest, Faculty of Geography, M. Kogălniceanu Blvd 36-46, Sector 5, 050107, Bucharest, Romania.
J Environ Radioact. 2016 Mar;153:167-175. doi: 10.1016/j.jenvrad.2015.12.020. Epub 2016 Jan 12.
This is the first study reporting recent sedimentation rates data (e.g. the past 120-150 years) for the Cruhlig Lake situated in the Danube Delta. The aim of this study is to analyse the recent sedimentation rates using the (210)Pb dating method and identifying the heavy metal pollutants and their variability in time. Five sediment cores were taken with a gravity corer and - after drying the sliced samples-physical parameters, organic material and inorganic carbon content were determined. The total (210)Pb content was measured via (210)Po by alpha spectrometry, while supported (210)Pb was measured by (226)Ra (trough short life (222)Rn daughters) with HPGe detectors. Heavy metals were determined by ICP-MS; from the 64 measured elements, only exceeding values of Al, As, Cd, Co, Cs, Cr, Cu, Fe, Hg, K, Li, Mg, Mn, Ni, Pb and Zn are discussed. After applying the CRS model, ages and sedimentation rates were calculated. The average sedimentation rate of the Cruhlig Lake is 0.21 ± 0.02 g/cm(2)y, Minimum values (0.05 ± 0.003 g/cm(2)y) are registered along the eastern shoreline of the lake before 1913, while maximum values are recorded due to the flooding in 2006 in the western side (1.34 ± 0.12 g/cm(2)y). Recent sedimentation rates divide the lake into three areas: the secluded eastern near shore part (0.63 ± 0.07 g/cm(2)y), the centre of the lake (0.92 ± 0.05 g/cm(2)y) and the dynamic western area, where most sediment transport takes place (1.13 ± 0.01 g/cm(2)y). The sedimentation pattern proves this lake to be very sensitive to fluvial discharge fluctuations. The building of the Iron Gate dams (1972 and 1985) had a negative impact on the sedimentation decreasing it with 58.74%, while after 1989 these values grew 2.25 times. The lake received a quantity of sediment rich in heavy metals in 1992 ± 3 y, which settled mostly on the eastern part. Values for Cd, Co, Cr, Hg, Pb and Zn are up to five times higher in 1980 ± 5 y in the eastern part of the lake, while Cd, Co, Cr and Ni are twice as high as the values measured for the marine substrate. Values of As show increasing of up to 150% in 2006 ± 2 y throughout the whole surface of the lake.
这是第一项报告多瑙河三角洲克鲁希格湖近期沉积速率数据(例如过去120 - 150年)的研究。本研究的目的是使用(210)Pb测年法分析近期沉积速率,并确定重金属污染物及其随时间的变化。用重力取芯器采集了五个沉积物岩芯,在将切片样品干燥后,测定了物理参数、有机物质和无机碳含量。通过α能谱法经由(210)Po测量总(210)Pb含量,而通过(226)Ra(通过短寿命(222)Rn子体)用HPGe探测器测量支持的(210)Pb。通过电感耦合等离子体质谱法测定重金属;在64种测量元素中,仅讨论了超过铝、砷、镉、钴、铯、铬、铜、铁、汞、钾、锂、镁、锰、镍、铅和锌的数值。应用CRS模型后,计算了年龄和沉积速率。克鲁希格湖的平均沉积速率为0.21±0.02 g/cm²·年,1913年之前在湖的东岸记录到最小值(0.05±0.003 g/cm²·年),而由于2006年西侧洪水记录到最大值(1.34±0.12 g/cm²·年)。近期沉积速率将湖泊分为三个区域:隐蔽的东部近岸部分(0.63±0.07 g/cm²·年)、湖中心(0.92±0.05 g/cm²·年)和动态的西部区域,这里发生了大部分泥沙输运(1.13±0.01 g/cm²·年)。沉积模式证明该湖对河流流量波动非常敏感。铁门大坝(1972年和1985年)的建造对沉积产生了负面影响,使其减少了58.74%,而1989年之后这些数值增长了2.25倍。1992±3年,该湖接收了大量富含重金属的沉积物,这些沉积物大多沉积在东部。1980±5年,湖东部的镉、钴、铬、汞、铅和锌的值高达五倍,而镉、钴、铬和镍是海洋基底测量值的两倍。2006±2年,整个湖面的砷值增长高达150%。