scholarly journals Quantifying Spatial Variability of Selected Soil Trace Elements and Their Scaling Relationships Using Multifractal Techniques

PLoS ONE ◽  
2013 ◽  
Vol 8 (7) ◽  
pp. e69326 ◽  
Author(s):  
Fasheng Zhang ◽  
Guanghua Yin ◽  
Zhenying Wang ◽  
Neil McLaughlin ◽  
Xiaoyuan Geng ◽  
...  
2020 ◽  
Vol 27 (11) ◽  
pp. 12428-12438 ◽  
Author(s):  
Micheline Ghosn ◽  
Céline Mahfouz ◽  
Rachida Chekri ◽  
Gaby Khalaf ◽  
Thierry Guérin ◽  
...  

2004 ◽  
Vol 49 (1-3) ◽  
pp. 39-52 ◽  
Author(s):  
G�raldine Amblard-Gross ◽  
Armand Maul ◽  
Jean-Fran�ois F�rard ◽  
Francine Carrot ◽  
Sophie Ayrault

1981 ◽  
Vol 4 ◽  
pp. 357-358
Author(s):  
J.J. Mortvedt

2013 ◽  
Vol 2013 (1) ◽  
pp. 4675
Author(s):  
Cambal Leah ◽  
Sara Gillooly ◽  
Brett Tunno ◽  
Drew Drew Michanowicz ◽  
Daniel Bain ◽  
...  

Geoderma ◽  
2022 ◽  
Vol 409 ◽  
pp. 115649
Author(s):  
G. Shrestha ◽  
R. Calvelo-Pereira ◽  
P. Roudier ◽  
A.P. Martin ◽  
R.E. Turnbull ◽  
...  

Author(s):  
Yu. Tyutyunnik ◽  
O. Shabatura ◽  
O. Blum ◽  
J. Daunis-i-Estadella

The bryogeochemical indication of atmospheric pollution in the central part of northern Ukraine is based on the use of moss P.schreberi species. The sampling system provided an empirical reference the moss sample data to a particular physical and geographical zone, taking into account the distance from the source of atmospheric pollution. This approach allowed developing a gradation of natural and man-caused conditions for the accumulation of chemical elements in moss samples. The data on the content of chemical elements in the moss-indicator were analysed and checked for comprehensive geostatistics (factor analysis methods, mapping of spatial correlations of significant factors, centered triangular charts and composite biplot). Results made possible to form a mutual hyperspace of geochemical factors and signs for its subsequent interpretation.The leading factor of the bryogeochemical indication is air pollution by a large dust of natural terrigenous and man-caused origin. Second factor connected with a finely dispersed man-caused-condensation aerosols impact; the third factor is identified by the behavior of titanium and vanadium as the effect of heat and power (TPP, boiler room) on atmospheric emissions; the fourth factor is аn impact of biogenesis, which is determined by active role of trace elements – sulfur and phosphorus; the fifth factor is connected with biogenic migration of trace elements – boron, copper and cobalt. The sixth factor is weak, and probably due to the behavior of manganese and chromium, associated with Eh-pH parameters of atmospheric precipitation and hydrometeors. The regional geostatistical analysis of the bryogeochemical data shows that the factor of the terrigenous dust uplift within the studied territory exhibits a spatial variability due to differences in the granulometric composition of the Quaternary deposits, the degree of soil retention and plowing, and differences in surface wind speeds. Spatial heterogeneity is obvious due to aman-caused factor showing a distribution of the dispersion of the Fe-S-Pb and V-Cd-Pb clusters on bipolar charts. Instead, such a geochemical factor as "biogenesis" shows a low spatial variability. The bryogeochemical indication is a good method for the assessment and monitoring of atmospheric pollution of large and varied natural and man-causedarea as well as the proposed geostatistical mapping of the atmogeochemic field showing that it is efficient todivide the territories by type of pollution.


2017 ◽  
Vol 14 (7) ◽  
pp. 1773-1792 ◽  
Author(s):  
Julie Tolu ◽  
Johan Rydberg ◽  
Carsten Meyer-Jacob ◽  
Lorenz Gerber ◽  
Richard Bindler

Abstract. The composition of sediment organic matter (OM) exerts a strong control on biogeochemical processes in lakes, such as those involved in the fate of carbon, nutrients and trace metals. While between-lake spatial variability of OM quality is increasingly investigated, we explored in this study how the molecular composition of sediment OM varies spatially within a single lake and related this variability to physical parameters and elemental geochemistry. Surface sediment samples (0–10 cm) from 42 locations in Härsvatten – a small boreal forest lake with a complex basin morphometry – were analyzed for OM molecular composition using pyrolysis gas chromatography mass spectrometry for the contents of 23 major and trace elements and biogenic silica. We identified 162 organic compounds belonging to different biochemical classes of OM (e.g., carbohydrates, lignin and lipids). Close relationships were found between the spatial patterns of sediment OM molecular composition and elemental geochemistry. Differences in the source types of OM (i.e., terrestrial, aquatic plant and algal) were linked to the individual basin morphometries and chemical status of the lake. The variability in OM molecular composition was further driven by the degradation status of these different source pools, which appeared to be related to sedimentary physicochemical parameters (e.g., redox conditions) and to the molecular structure of the organic compounds. Given the high spatial variation in OM molecular composition within Härsvatten and its close relationship with elemental geochemistry, the potential for large spatial variability across lakes should be considered when studying biogeochemical processes involved in the cycling of carbon, nutrients and trace elements or when assessing lake budgets.


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