Institute of Geosystems and Bioindication, Technische Universität Braunschweig, Langer Kamp 19c, D-38106 Braunschweig, Germany.
Faculty of Biology - Biotechnology, Vietnam National University, Ho Chi Minh University of Science, 227 Nguyen Van Cu, District 5, Ho Chi Minh City, Viet Nam..
Sci Total Environ. 2020 May 10;716:137035. doi: 10.1016/j.scitotenv.2020.137035. Epub 2020 Feb 3.
In order to assess the impact of recent industrialization and land-use changes in the Can Gio Mangrove Forest, a Biosphere Reserve in Southern Vietnam, we analyzed heavy metal (HM), total organic carbon (TOC) and total nitrogen (TN) concentrations in a Pb-dated sediment core, allowing for the environmental reconstruction of the last three decades. C/N ratios were very high (>20) until ~1990, reflecting highly refractory organic matter. Sediment Quality Guidelines (SQG's) violations were observed particularly after the establishment of industries in the area in the late-1990s. Chromium (Cr) and copper (Cu) exceeded the threshold effect levels (TEL); whereas nickel (Ni) was above the probable effects level (PEL), identifying the risk of potential adverse biological effects. Moderate contamination, mainly from cobalt (Co) and lead (Pb), was detected by the contamination factor (CF) index, with Pb levels likely originating from mainly anthropogenic sources, particularly after ~1992, as indicated by elevated enrichment factor (EF) values. A high positive correlation was found between Pb, Cr, Cu and Ni (r ≥ 0.8), while Co, cadmium (Cd) and TOC were highly positive correlated (r = 0.9). We identified evidence of point sources, atmospheric pollution and erosion as the main contributors to enhanced HM levels. However, negative values of the Geo-accumulation index (I-geo) indicated uncontaminated sediments. This discrepancy in pollution indices was likely due to the use of shale averages instead of regional levels as background values, as well as the influence of multiple stressors.
为了评估越南南部生物圈保护区——戈公红树林最近工业化和土地利用变化的影响,我们分析了 Pb 定年沉积物芯中的重金属 (HM)、总有机碳 (TOC) 和总氮 (TN) 浓度,从而对过去三十年的环境变化进行重建。C/N 比值非常高(>20),直到 1990 年左右,反映出高度难降解的有机物。上世纪 90 年代末,该地区建立了工业后,观察到沉积物质量准则 (SQG) 违规现象。铬 (Cr) 和铜 (Cu) 超过了阈值效应水平 (TEL);镍 (Ni) 高于可能的效应水平 (PEL),表明存在潜在生物不良效应的风险。污染因子 (CF) 指数显示出中度污染,主要来自钴 (Co) 和铅 (Pb),铅水平可能主要来自人为源,特别是在 1992 年左右之后,这表明富集因子 (EF) 值升高。Pb、Cr、Cu 和 Ni 之间存在高度正相关 (r≥0.8),而 Co、镉 (Cd) 和 TOC 之间存在高度正相关 (r=0.9)。我们发现有证据表明,点源、大气污染和侵蚀是造成重金属水平升高的主要原因。然而,地质累积指数 (I-geo) 的负值表明沉积物未受污染。污染指数的这种差异可能是由于使用了页岩平均值而不是区域水平作为背景值,以及受到多种胁迫因素的影响。