The distribution of trace elements in some South Australian red-brown earths

1957 ◽  
Vol 8 (3) ◽  
pp. 246 ◽  
Author(s):  
RM McKenzie
Keyword(s):  
Trace Elements ◽  
South Australia ◽  
Mobile Elements ◽  
Soil Horizons ◽  
Surface Soils ◽  
Mean Values ◽  
Pattern Of Variation ◽  
Individual Profiles ◽  
Maximum Minimum ◽  
Distribution Of Trace Elements

The maximum, minimum, and mean values for six trace elements in four soil horizons are reported for 14 profiles of red-brown earths from South Australia, and the pattern of variation and distribution of these elements discussed. The elements studied could be arranged in a series of decreasing mobility in the soil, the order being cobalt > copper > gallium > vanadium > molybdenum > manganese. The most mobile elements had greater variations within profiles and, except for manganese, greater variations between profiles. Gallium, vanadium, and molybdenum contents were correlated with the amount of clay present in all surface soils, as well as in individual profiles, whereas cobalt and copper contents were correlated with clay only in individual profiles.

Total elements in forest soils affected by acid deposition in southern Quebec

1996 ◽  
Vol 76 (2) ◽  
pp. 165-171 ◽  
Author(s):  
Z. Q. Lin ◽  
W. H. Hendershot ◽  
P. H. Schuepp ◽  
G. G. Kennedy ◽  
P. Dutilleul
Keyword(s):  
Trace Elements ◽  
Acid Deposition ◽  
Forest Soils ◽  
Major And Trace Elements ◽  
Surface Soils ◽  
Mean Values ◽  
Podzolic Soils ◽  
Element Concentrations ◽  
The Mean ◽  
Element Enrichment

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

scholarly journals The potential of trace elements mapping in child’s natal tooth by laser ablation-ICPMS method

2021 ◽  
Author(s):  
Aneta Olszewska ◽  
Anetta Hanć
Keyword(s):  
Trace Elements ◽  
Spatial Distribution ◽  
Quantitative Assessment ◽  
Toxic Elements ◽  
Tooth Enamel ◽  
Perinatal Period ◽  
Potentially Toxic Elements ◽  
Metal Exposure ◽  
Icp Ms ◽  
Distribution Of Trace Elements

Abstract Purpose Tooth enamel might provide past chronological metabolic, nutritional status and trace metal exposure during development. Thus, the trace elements distribution embedded in tooth tissues represents an archive of the environmental conditions. The choice of biomarker is estimated as critical to the measurement of metal exposure. Natal teeth are defined as teeth being present at birth. Methods LA-ICP-MS provides a quantitative assessment of spatial distribution of trace elements in a natal tooth. The objective of the current study was to compare concentrations of building and other elements in a rare but reliable and valid biomarker - natal tooth. Results It have been reported presence of potentially toxic elements: Pb, Cu, Mn, Cd, Ni distributed in prenatally and perinatally formed enamel and dentine. Conclusions Analyses of deciduous enamel can provide answers into individuals’ earliest development, including critical pre- and perinatal period.

Distribution of trace elements between carbonate and non-carbonate phases of limestone

1977 ◽  
Vol 34 (1) ◽  
pp. 39-50 ◽  
Author(s):  
P.P. Parekh ◽  
P. Möller ◽  
P. Dulski ◽  
W.M. Bausch
Keyword(s):  
Trace Elements ◽  
Distribution Of Trace Elements

Mineralogical controls on the distribution of trace elements in metasomatized peridotite enclaves from Planany, Czech Republic

2007 ◽  
Vol 71 (1) ◽  
pp. 81-91 ◽  
Author(s):  
J. V. Owen ◽  
J. Dostal ◽  
M. Fisera
Keyword(s):  
Trace Elements ◽  
Czech Republic ◽  
Reference Frame ◽  
Outer Layer ◽  
Reaction Zones ◽  
Host Rocks ◽  
Distribution Of Trace Elements

AbstractSmall (m-scale) peridotite enclaves at Planany (central Czech Republic) are separated from their gneissic host rocks by a narrow (cm-scale) reaction rim comprising an inner, tremolite + phlogopite zone and an outer, essentially monomineralic phlogopite zone. Both retain an Mg# very similar to that of the peridotite (Mg# = 81), but relative to this reference frame, show large increases in LILE (K, Rb, Ba) and radionuclides (U, Th). On a smaller scale, however, there has been a mineralogically-controlled decoupling of various components, particularly among the HFSE and REE, the former favouring the phlogopite-rich outer layer of the reaction rim, the latter the amphibole-rich inner zone. Taken together, however, the reaction zones preserve key compositional features of their inferred protolith.

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