Decision support for the selection of reference sites using 137Cs as a soil erosion tracer

被引:6
|
作者
Arata, Laura [1 ]
Meusburger, Katrin [1 ]
Burge, Alexandra [1 ]
Zehringer, Markus [2 ]
Ketterer, Michael E. [3 ]
Mabit, Lionel [4 ]
Alewell, Christine [1 ]
机构
[1] Univ Basel, Dept Environm Sci, Environm Geosci, Basel, Switzerland
[2] State Lab Basel City, Basel, Switzerland
[3] Metropolitan State Univ Denver, Dept Chem, Denver, CO USA
[4] FAO IAEA Agr & Biotechnol Lab, Soi1 & Water Management & Crop Nutr Lab, Vienna, Austria
基金
瑞士国家科学基金会;
关键词
D O I
10.5194/soil-3-113-2017
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The classical approach of using Cs-137 as a soil erosion tracer is based on the comparison between stable reference sites and sites affected by soil redistribution processes; it enables the derivation of soil erosion and deposition rates. The method is associated with potentially large sources of uncertainty with major parts of this uncertainty being associated with the selection of the reference sites. We propose a decision support tool to Check the Suitability of reference Sites (CheSS). Commonly, the variation among Cs-137 inventories of spatial replicate reference samples is taken as the sole criterion to decide on the suitability of a reference inventory. Here we propose an extension of this procedure using a repeated sampling approach, in which the reference sites are resampled after a certain time period. Suitable reference sites are expected to present no significant temporal variation in their decay-corrected Cs-137 depth profiles. Possible causes of variation are assessed by a decision tree. More specifically, the decision tree tests for (i) uncertainty connected to small-scale variability in Cs-137 due to its heterogeneous initial fallout (such as in areas affected by the Chernobyl fallout), (ii) signs of erosion or deposition processes and (iii) artefacts due to the collection, preparation and measurement of the samples; (iv) finally, if none of the above can be assigned, this variation might be attributed to "turbation" processes (e.g. bioturbation, cryoturbation and mechanical turbation, such as avalanches or rockfalls). CheSS was exemplarily applied in one Swiss alpine valley where the apparent temporal variability called into question the suitability of the selected reference sites. In general we suggest the application of CheSS as a first step towards a comprehensible approach to test for the suitability of reference sites.
引用
收藏
页码:113 / 122
页数:10
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