scholarly journals Source Identification of Trace Elements in Peri-urban Soils in Eastern China

2018 ◽  
Vol 11 (3) ◽  
pp. 195-207 ◽  
Author(s):  
Long Sun ◽  
Manus Carey ◽  
Lei Yang ◽  
Li-Ding Chen ◽  
Shou-Juan Li ◽  
...  
2000 ◽  
Vol 64 (5) ◽  
pp. 867-877 ◽  
Author(s):  
R. C. Wang ◽  
G. T. Zhao ◽  
J. J. Lu ◽  
X. M. Chen ◽  
S. J. Xu ◽  
...  

AbstractZircon commonly occurs as one of important accessory HFSE-bearing minerals in A-type granite. A detailed electron microprobe study was carried out on zircon from the Laoshan complex, Eastern China, which is composed of I- and A-type granites. Zircon from the I-type rocks is relatively poor in trace elements (HfO2<2 wt.%, UO2, ThO2 and Y2O3 <1 wt.%), but that from the A-type rocks is richer in Hf, U, Th and Y. Hafnian zircon with a HfO2 content of up to 12.37 wt.% was found in the arfvedsonite granite, which is considered the most evolved facies in the A-type suite. Enrichment in Hf is generally observed at the rims of zircon crystals relative to the cores. The Hf enrichment in zircon, and the association of exotic REE- and HFSE-bearing minerals are linked to hydrothermal activity, suggesting that during the last stage of crystallization of the A-type magma, fluids enriched in REE, HFSE, F−, CO32− and PO43− were released.


2020 ◽  
Vol 42 (11) ◽  
pp. 3925-3947
Author(s):  
Edgar Hiller ◽  
Lenka Filová ◽  
Ľubomír Jurkovič ◽  
Martin Mihaljevič ◽  
Lucia Lachká ◽  
...  

2004 ◽  
Vol 260 (3) ◽  
pp. 509-518 ◽  
Author(s):  
G. D. Kanias ◽  
L. G. Viras ◽  
A. P. Grimanis

Author(s):  
Gang Wang ◽  
Hou-Qi Liu ◽  
Yu Gong ◽  
Yang Wei ◽  
Ai-Jun Miao ◽  
...  

2009 ◽  
Vol 9 (1) ◽  
pp. 1377-1405 ◽  
Author(s):  
V. Fiedler ◽  
R. Nau ◽  
S. Ludmann ◽  
F. Arnold ◽  
H. Schlager ◽  
...  

Abstract. A large SO2-rich pollution plume of Chinese origin was detected by aircraft based CIMS (Chemical Ionization Mass Spectrometry) measurements at 3–7.5 km altitude over the North Atlantic on 3 May 2006 during the INTEX (Intercontinental Chemical Transport Experiment) campaign. Additional trace gases (NO, NOy, CO, H2O) were measured and used for comparison and source identification. All measurements took place aboard the German research aircraft Falcon. The atmospheric SO2 mole fraction was markedly increased inside the plume and reached up to 900 pmol/mol. The measured ratio SO2/NOy of 1.4 suggests combustion of coal or fuel with a very high sulfur content as a source of the excess SO2. Accompanying FLEXPART particle dispersion model simulations indicate that the probed pollution plume originated at low altitudes over densely populated and industrialized areas in eastern China about 8–12 days prior to the measurements.


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