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阿拉伯湾西北部定年沉积物岩芯中磷积累的沉积时间趋势:磷能否用于支持沿海水生生境沉积物中的 Pb 年代序列?

Depositional time trends of phosphorous accumulation in a dated sediment core from the northwestern Arabian Gulf: Can phosphorous be used to support Pb chronologies in coastal aquatic sediments?

机构信息

Environment Protection Agency, Brookfields, Freetown, Sierra Leone; Environment and Life Sciences Research Center, Kuwait Institute for Scientific Research, Kuwait.

Environment and Life Sciences Research Center, Kuwait Institute for Scientific Research, Kuwait.

出版信息

Mar Pollut Bull. 2021 May;166:112213. doi: 10.1016/j.marpolbul.2021.112213. Epub 2021 Mar 11.

Abstract

The use of Pb dating for the reconstruction of contaminant profiles in undisturbed sediments is the most widely acceptable technique historically. Due to the uncertainties associated with the technique, dating of sediments have often been supported by ancillary evidence such as an alternative historical marker in the catchment that is preserved in the sedimentary records. The most widely used verification marker is Cs, which is attributed to global fallout from past nuclear weapons testing, and the Chernobyl accident. In the southern hemisphere, and the mid-latitudes, the Cs signal from Chernobyl fallout is often absent from the sedimentary records making it very difficult to verify the Pb chronologies in these natural archives. This study reports the spatial and temporal variability of total phosphorus (TP) and its forms in sediments from Kuwait Bay and provides evidence of the possibility of using Phosphorous as a potential marker to support dates derived from Pb dating. In the current study we report the spatial and temporal variations in the concentrations of Phosphorus from near-shore sediments from Kuwait. The mean (and range) of TP concentration in surficial sediments is 19.4 (12.2 to 24) μmol-P g dry weight. The highest concentrations were measured in the deepest portions of the Bay which is characterized by fine grained sediments. The vertical profile of TP in the sediments was characterized by a gradual increase in concentration from lower layers to a subsurface maximum (at approximately 4-5 cm) followed by an exponential decrease to the sediment-water interface. The sedimentary TP profile correlated remarkably well with changes in the population of Kuwait over the last three decades, suggesting that wastewater inputs into the Bay from treatment plants are an important source of phosphorus in the coastal waters. The decrease in concentration in sediment deposited over the last five years of the core is explained by the commissioning of an improved wastewater treatment plant with higher phosphorus removal efficiency. These fluctuations preserved in the sedimentary records linked to identifiable historical events provides powerful evidence that this nutrient associated with wastewater inputs in coastal aquatic environments can be used as ancillary information to support Pb dating.

摘要

利用 Pb 测年法重建未受干扰沉积物中的污染物分布,是迄今为止最广泛接受的技术。由于该技术存在不确定性,因此沉积物的测年通常需要得到辅助证据的支持,如流域中保存于沉积记录中的替代历史标记物。最广泛使用的验证标记物是 Cs,它归因于过去核武器试验的全球沉降物以及切尔诺贝利事故。在南半球和中纬度地区,来自切尔诺贝利沉降物的 Cs 信号通常不存在于沉积记录中,这使得很难验证这些自然档案中的 Pb 年代。本研究报告了科威特湾沉积物中总磷(TP)及其形态的时空变化,并提供了使用磷作为潜在标记物来支持 Pb 测年得出的日期的可能性的证据。在本研究中,我们报告了科威特近岸沉积物中磷浓度的时空变化。表层沉积物中 TP 的平均(和范围)浓度为 19.4(12.2 至 24)μmol-P g 干重。Bay 最深部分的浓度最高,该部分以细粒沉积物为特征。沉积物中 TP 的垂直分布特征是从下部分逐渐增加到次表面最大值(约在 4-5 cm 处),然后迅速减少到沉积物-水界面。沉积物中 TP 分布与过去三十年来科威特人口变化有很好的相关性,表明来自处理厂的废水输入是近岸水域磷的重要来源。由于新建了磷去除效率更高的污水处理厂,核心物中过去五年沉积的磷浓度有所下降。这些与可识别的历史事件相关的沉积记录中的波动为有力的证据,表明与废水输入相关的这种营养物质可作为辅助信息来支持 Pb 测年。

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