Enrichment of trace elements from long-range aerosol transport in sandy podzolic soils of southwest France

1994 ◽  
Vol 73 (1) ◽  
pp. 235-246 ◽  
Author(s):  
E. Saur ◽  
C. Juste
2018 ◽  
Vol 176 ◽  
pp. 08011 ◽  
Author(s):  
Fábio J. S. Lopes ◽  
Juan Luis Guerrero-Rascado ◽  
Jose A. Benavent-Oltra ◽  
Roberto Román ◽  
Gregori A. Moreira ◽  
...  

During the period of August-September 2016 an intensive campaign was carried out to assess aerosol properties in São Paulo-Brazil aiming to detect long-range aerosol transport events and to characterize the instrument regarding data quality. Aerosol optical properties retrieved by the GALION - LALINET SPU lidar station and collocated AERONET sunphotometer system are presented as extinction/ backscatter vertical profiles with microphysical products retrieved with GRASP inversion algorithm.


Tellus B ◽  
1984 ◽  
Vol 36 (3) ◽  
pp. 163-178 ◽  
Author(s):  
Josef M. Pacyna ◽  
Arne Semb ◽  
Jan E. Hanssen

Soil Research ◽  
1963 ◽  
Vol 1 (1) ◽  
pp. 74 ◽  
Author(s):  
KG Tiller

The mineralogy and chemistry of weathering and soil formation have been studied at 17 widely separated sites with contrasting climatic conditions on comparatively uniform dolerite in Tasmania. The clay and fine sand mineralogy of the soils has been related to their degree of weathering. These studies have shown large chemical and mineralogical changes accompanying the initial stages of weathering in some krasnozem soils. The reorganization of cobalt, zirconium, nickel, copper, molybdenum, manganese, and zinc during genesis of four soil groups has been considered in terms of the factors involved. Some of these results indicate that the clay horizon of the podzolic soils has probably been formed by weathering in situ. Seasonal waterlogging in certain horizons has strongly mfluenced the chemistry and mineralogy of weathering in many of these soils. This study has shown that the composition of the parent material has only influenced the geochemistry of trace elements in less weathered soils and that pedogenic factors assumed greater significance as the soils became more strongly weathered. Geomorphic processes had a marked influence on the geochemistry of some soils by the truncation of mature soil profiles.


2018 ◽  
Vol 176 ◽  
pp. 05053
Author(s):  
Talianu Camelia

The aims of the study is to identify the paths of the long-range transported aerosols over Austria and their potential origin, and to estimate their properties, using lidar measurements from EARLINET stations closest to Austria from Germany and Romania and aerosol transport models. As of now, there is no lidar station in Austria. The study is part of a project to estimate the usefulness of a lidar station located in Vienna, Austria.


2006 ◽  
Vol 40 (19) ◽  
pp. 3536-3547 ◽  
Author(s):  
T. Kindap ◽  
A. Unal ◽  
S.-H. Chen ◽  
Y. Hu ◽  
M.T. Odman ◽  
...  
Keyword(s):  

1996 ◽  
Vol 76 (2) ◽  
pp. 165-171 ◽  
Author(s):  
Z. Q. Lin ◽  
W. H. Hendershot ◽  
P. H. Schuepp ◽  
G. G. Kennedy ◽  
P. Dutilleul

Major and trace elements (Al, As, Ba, Ca, Cd Co, Cr Cs, Cu Eu Fe, Hf, K, La, Lu, Mg, Mn, Na, Ni, Pb, Rb, Sb, Sc, Si, Sm, Sr, Ta, Tb, Th, Ti, U, V, Yb and Zn) in forest soils from three acid-deposition-affected locations in southern Quebec were investigated. Total element concentrations in the surface layer (0–20 cm) of the Podzolic soils were mostly well within the range of element concentrations in Podzols reported worldwide but showed higher mean values for most elements. The mean concentrations of elements (except Zn, at 124 μg g−1) were also generally comparable to the respective elemental baseline data established for Canadian soils. Element concentrations (μg g−1) of Cs (6.2) Sc (19 8) V (106) Rb (194) K (26 500) and Al (76 900) in the surface soils were significantly higher at the 940-m elevation than the concentrations from the sites at 650 and 770 m along the Roundtop Mountain slope, but Ca (1120) and Ni (4.4) were lowest at the 940-m elevation A similar trend with elevation was not observed at the other mountain location (White Peak). Enrichment-factor (EF) analysis showed significant element enrichment (EF ≥ 10) for Cd, Rb and Sb but impoverishment (EF ≤ 0.1) for Ca, Cu and Ni in topsoils. Key words: Major and trace elements, surface soils, acid deposition


2012 ◽  
Vol 77 ◽  
pp. 144-151 ◽  
Author(s):  
S.S. Prijith ◽  
Marina Aloysius ◽  
Mannil Mohan ◽  
Naseema Beegum ◽  
K. Krishna Moorthy

1992 ◽  
Vol 26 (7) ◽  
pp. 1309-1324 ◽  
Author(s):  
C.E. Amunsen ◽  
J.E. Hanssen ◽  
A. Semb ◽  
E. Steinnes

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