Major to ultra trace elements in rainfall collected in suburban Tokyo

• Published in: Atmospheric environment (1994) Vol. 41; no. 33; pp. 6999 - 7010
• Main Authors: Shimamura, Tadashi, Iwashita, Masato, Iijima, Satoe, Shintani, Megumi, Takaku, Yuichi
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01.10.2007; Elsevier Science
• Subjects: Applied sciences; Atmospheric pollution; Enrichment factor; Exact sciences and technology; Platinum group element; Pollutants physicochemistry study: properties, effects, reactions, transport and distribution; Pollution; Rainwater; Rare earth element; Trace element; Asia; Honshu; Japan; INW, Japan, Honshu, Tokyo Prefect., Tokyo; Rainwater; Trace element; Enrichment factor; Rare earth element; Platinum group element; Elementary analysis; Lanthanide; Chemical analysis; Atmospheric fallout; Ultratrace compound; Trace compound; Urban area; Wet deposition; Ion chromatography; ICP mass spectroscopy; Rain water; Geogenic factor; Pollution source inventory; Chemical composition; Atmospheric precipitation; Platinoid; Anthropogenic factor
• ISSN: 1352-2310; 1873-2844
• DOI: 10.1016/j.atmosenv.2007.05.010

Major to ultra trace elements such as rare earth elements (REEs), platinum group elements (PGEs) in 20 rainfall events from suburban Tokyo were determined by inductively coupled plasma mass spectrometry (ICP-MS). Anion species were also determined by an ion chromatography (IC). The concentrations of PGEs were so low that only Pt was detected in some rainfall events. Enrichment factors (EFs), refer to soil and sea salt components, were calculated for the measured elements (with Al and Na as references). Be, (Na), Mg, (Al), Si, Cl, K, Fe, Rb, Sr, REEs (except La, Gd), Ta, and U were mostly originated from natural materials (soil and sea salt). For Li, B, Ca, Mn, Sr, Ba, and Cs, the contribution of natural materials was significant. EFs for Cu, Zn, As, Se, Sb, Cd, Pb, Bi, Ag, Te, Au, Pt, SO 4-S and NO 3-N exceeded 100 indicating non-crustal, non-sea salt origin, presumably anthropogenic; however, contribution of volcanic gases could not be excluded for As, Se, Te and Bi. Pt seemed to be uniformly distributed worldwide and a catalyst for automobile emission control may be the main source. Au also showed uniform distribution. On the other hand, EFs for Zr, Nb, Hf and Th were less than unity. Probably these elements resided in acid resistant refractory fine minerals that did not decompose with acid treatment, and did not evaporate and ionize in the ICP. An alternative explanation is that the concentration of these elements was lower in the soil of the sampling area than the average crust. In the crust normalized REE pattern plot, La, Eu and Gd showed clear positive anomalies. La and Gd could have anthropogenic components. A possible source of La and Gd is cracking catalyst for petrol refining, but this source does not fully explain the anomaly. The source of Gd may also be Gd-DTPA (Gadolinium (III) diethyltriaminepentaacetic acid) used for Magnetic Resonance Imaging (MRI) contrast agents. The Eu origin may be soil with higher concentration than the crust average.