验证适用于受人类活动影响的大型河流流域的外210Pb沉积物测年方法

IF 1.7 2区 地球科学 Q3 GEOGRAPHY, PHYSICAL
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引用次数: 0

摘要

对阿拉巴马州莫比尔河流域内受以下因素影响的五个地点的沉积物动态进行了评估:(i) 水坝和水闸的使用;(ii) 城市化;(iii) 工业/采矿作业;(iv) 洪水;以及 (v) 风暴潮事件。对三种广泛使用的基于过量 210Pb(ex210Pb)的沉积物定年模型(即恒定供给率模型 CRS、恒定初始浓度模型 CIC 和平流扩散方程 ADE)和两种最新开发的模型(即孔隙度变化模型 PV 和无扩散孔隙度变化模型 PVWD)进行了测试,以确定它们是否适用于这些人为改变的湖泊和沿岸地区。为了验证外 210Pb 模型的结果,我们使用了传统的时间标记,包括区域水文记录和历史航空 图像。我们发现,由于目前 137Cs 在沉积物中的存量较低,传统使用的时间标记已不再有用。我们利用排水与湖泊面积之比来确定径流和大气中放射性核素的相对贡献。利用对物理特性(如孔隙度、体积密度和干密度、含水量以及沉积物地球化学成分)的统计分析来支持沉积物迁移和遗址开发假设。在利用这些代用指标构建每个地点的沉积物历史时,我们发现 CIC 和 ADE 模型产生的年龄不可靠,因为它们违反了孔隙度和 ex210Pb 活性随深度呈指数递减的要求。我们发现 PV 和 PVWD 这两个考虑了异质孔隙度的新模型产生了更可靠的沉积沉积年龄。与 CRS 模型相比,这两个模型产生的年龄的不确定性更低,优于所测试的其他传统模型。我们的结论是,PV 和 PVWD 模型更适用于经历侵蚀和突然沉积事件的环境,在我们的研究中,这些事件是由大坝建设和风暴潮事件造成的。模型敏感性分析表明,PV 和 PVWD 模型的平均颗粒密度越小,沉积物年龄越小。前 210Pb 活性分析不确定性越高,沉积速率越低,所有五个模型的估计年龄也越高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Validating ex210Pb sediment dating methods applied to a large anthropogenically-impacted river basin

Sediment dynamics in five sites within the Mobile River Basin, Alabama, impacted by (i) dam-and-lock use, (ii) urbanization, (iii) industrial/mining practices, (iv) flooding, and (v) storm surge events were evaluated to understand better anthropogenic impacts on regional sediment budgets. Three widely used sediment dating models based on excess 210Pb (ex210Pb) (i.e., Constant Rate of Supply, CRS, Constant Initial Concentration, CIC, and Advective Dispersion Equation, ADE) and two recently developed ones (i.e., Porosity Variation, PV and Porosity Variation Without Diffusion, PVWD) were tested to determine their applicability to these anthropogenically altered lacustrine and coastal areas. To verify results from ex210Pb models, we used conventional time markers, including regional hydrograph records and historical aerial images. We found that the traditionally used time-marker 137Cs is no longer useful due to its current low inventories in the sediments. Drainage-to-lake area ratios were used to determine relative runoff and atmospheric radionuclide contributions. Statistical analysis of physical properties such as porosity, bulk and dry density, water content, and sediment geochemical compositions were utilized to support sediment transport and site development hypotheses. When constructing the sediment history at each site using these proxies, we found that the CIC and ADE models produced unreliable ages because of violation of requirements for exponentially decreasing porosity and ex210Pb activity with depth. We found that two new models, PV and PVWD, that account for heterogeneous porosity, produced more reliable sediment depositional ages. These two models produced ages with lower uncertainties than the CRS model, outperforming the other conventional models tested. We conclude that the PV and PVWD models are more applicable for environments experiencing erosional and abrupt depositional events, which in our study resulted from dam construction and storm-surge events. Model sensitivity analysis showed that decreasing average particle density produces younger sediment ages by the PV and PVWD models. Higher ex210Pb activity analytical uncertainty resulted in lower sedimentation rates and higher estimated ages by all five models.

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来源期刊
Quaternary Geochronology
Quaternary Geochronology 地学-地球化学与地球物理
CiteScore
4.40
自引率
22.20%
发文量
130
审稿时长
20 weeks
期刊介绍: Quaternary Geochronology is an international journal devoted to the publication of the highest-quality, peer-reviewed articles on all aspects of dating methods applicable to the Quaternary Period - the last 2.6 million years of Earth history. Reliable ages are fundamental to place changes in climates, landscapes, flora and fauna - including the evolution and ecological impact of humans - in their correct temporal sequence, and to understand the tempo and mode of geological and biological processes.
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