德国中部和东北部水基87Sr/86Sr等高线新图——以山区为重点

IF 1.7 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Aquatic Geochemistry Pub Date : 2023-03-16 DOI:10.1007/s10498-023-09412-5
A. Käßner, H. T. Kalapurakkal, B. Huber, M. Tichomirowa
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引用次数: 1

摘要

在这项研究中,我们提出了一个新的87Sr/86Sr德国中部和东北部等高线地图。这个地区的特点是沉积盆地和山区交替存在,岩性变化很大。由于岩性和岩石年龄对生物可利用锶的同位素组成有重大影响,德国中部和东北部应该显示高度变化的87Sr/86Sr比率。从岩性特征来看,Erzgebirge/Fichtelgebirge和Harz山脉的山区预计会有特别高的比率。与这些预测相反,已发表的德国中部和东北部87Sr/86Sr等高线图记录了相当均匀和低的87Sr/86Sr比率。从这一观察结果来看,我们怀疑现有的等高线地图可能是从一个不足的数据库中计算出来的,山区的代表性不足。我们的目标是收集德国中部和东北部各主要岩性的87Sr/86Sr基线,并绘制德国中部和东北部的精确等高线图。在第一步,我们评估了溪流和地下水作为生物可利用锶的代理的适用性。在选定的流域中,我们提出了混合关系和流网络模型。我们表明,地下水很容易受到非常局部的地质和人为影响,因此应该避免。相反,我们将进一步的采样集中在溪流上。总的来说,我们使用了119个地下水和溪流水的新测量值和一组23个辅助变量作为我们新的德国中部和东北部等高线地图的数据库。由于采样策略侧重于覆盖每个主要岩性,我们的测量结果和最终的等高线图显示了沉积盆地和山区之间的明显对比。对于已经充分采样的地区,将等值线图与已发表的和新的数据进行直接比较,结果显示出良好的一致性。虽然德国中部和东北部是已出版的等高线地图的一部分,但我们的新地图是第一个高精度预测山区87Sr/86Sr比率的地图。
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A New Water-Based 87Sr/86Sr Isoscape Map of Central and NE Germany, with Special Emphasis on Mountainous Regions

In this study, we present a new 87Sr/86Sr isoscape map of Central and NE Germany. This area is characterized by an alternation of sedimentary basins and mountainous regions with a very variable lithology. Since lithology and rock age have a major impact on the isotopic composition of biologically available strontium, Central and NE Germany should reveal highly variable 87Sr/86Sr ratios. From lithological characteristics, particularly high ratios are expected in the mountainous regions of the Erzgebirge/Fichtelgebirge and the Harz Mountains. In contrast to these predictions, published 87Sr/86Sr isoscape maps of Central and NE Germany record rather uniform and low 87Sr/86Sr ratios. From this observation, we suspected that existing isoscape maps might be computed from an insufficient database, with mountainous regions being underrepresented. Our goal was to gather 87Sr/86Sr baselines for each major lithology of Central and NE Germany and to produce an accurate isoscape map of Central and NE Germany. In the first step, we evaluated the suitability of stream water and groundwater as a proxy for biologically available strontium. In a selected watershed, we present mixing relationships and a stream network model. We show that groundwater is prone to very local geologic and anthropogenic influences and should thus be avoided. Instead, we focussed our further sampling on stream water. Altogether, we used 119 new measurements of groundwater and stream water and a set of 23 auxiliary variables as a database for our new isoscape map of Central and NE Germany. Due to a sampling strategy that focussed on covering each major lithology, our measurements and the final isoscape map show a clear contrast between sedimentary basins and mountainous regions. For regions that have been sufficiently sampled, a direct comparison of the isoscape map with published and new data shows good agreement. Although Central and NE Germany were part of published isoscape maps, our new map is the first that predicts 87Sr/86Sr ratios in mountainous regions with high accuracy.

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来源期刊
Aquatic Geochemistry
Aquatic Geochemistry 地学-地球化学与地球物理
CiteScore
4.30
自引率
0.00%
发文量
6
审稿时长
1 months
期刊介绍: We publish original studies relating to the geochemistry of natural waters and their interactions with rocks and minerals under near Earth-surface conditions. Coverage includes theoretical, experimental, and modeling papers dealing with this subject area, as well as papers presenting observations of natural systems that stress major processes. The journal also presents `letter''-type papers for rapid publication and a limited number of review-type papers on topics of particularly broad interest or current major controversy.
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