TY - JOUR
T1 - Structural factors of biogenic birnessite produced by fungus Paraconiothyrium sp. WL-2 strain affecting sorption of Co 2+
AU - Yu, Qianqian
AU - Sasaki, Keiko
AU - Tanaka, Kazuya
AU - Ohnuki, Toshihiko
AU - Hirajima, Tsuyoshi
N1 - Funding Information:
Financial support was provided to KS by the Japan Society for the Promotion of Science (JSPS Grant-in-Aid for Scientific Research No. 22246117 ) and the funding program for the Next Generation of World-Leading Researchers ( GR078 ). A student scholarship was provided to QY by the Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT). The XAFS measurement was performed with the approval of the Photon Factory, KEK (Proposal no. 2009G145, 2009G676 and 2012G179). The collection of XRD patterns was performed at the Center of Advanced Instrumental Analysis at Kyushu University.
PY - 2012/6/5
Y1 - 2012/6/5
N2 - The surface reactivity of biogenic birnessite is attributed to its structure. However, structural control of heavy metal adsorption on biogenic birnessite is not well understood. Here a poorly-crystalline birnessite was produced by the fungus Paraconiothyrium sp. WL-2 strain under ambient pH and temperature conditions. The structure was characterized by X-ray absorption spectroscopy and X-ray diffraction. Sorption behaviors of Co 2+ were compared with Zn 2+. The primary product of the Mn bio-oxidation is hexagonal birnessite with a turbostratic structure. XAFS analysis demonstrated that the biogenic birnessite consists of octahedral sheets with Mn(IV) as the central metal and some vacant sites. Mn(III) atoms are coordinated to some of the vacant sites in the interlayer. The adsorption of Co 2+ by the biogenic birnessite is higher than Zn 2+. The excess adsorption of Co 2+ than Zn 2+ is nearly the same as the excess release of Mn from the biogenic birnessite. These results strongly suggested that the interlayer Mn(III) can oxidize the adsorbed Co 2+ to Co 3+, resulting in excess adsorption of Co 2+ compared to Zn 2+ by biogenic birnessite.
AB - The surface reactivity of biogenic birnessite is attributed to its structure. However, structural control of heavy metal adsorption on biogenic birnessite is not well understood. Here a poorly-crystalline birnessite was produced by the fungus Paraconiothyrium sp. WL-2 strain under ambient pH and temperature conditions. The structure was characterized by X-ray absorption spectroscopy and X-ray diffraction. Sorption behaviors of Co 2+ were compared with Zn 2+. The primary product of the Mn bio-oxidation is hexagonal birnessite with a turbostratic structure. XAFS analysis demonstrated that the biogenic birnessite consists of octahedral sheets with Mn(IV) as the central metal and some vacant sites. Mn(III) atoms are coordinated to some of the vacant sites in the interlayer. The adsorption of Co 2+ by the biogenic birnessite is higher than Zn 2+. The excess adsorption of Co 2+ than Zn 2+ is nearly the same as the excess release of Mn from the biogenic birnessite. These results strongly suggested that the interlayer Mn(III) can oxidize the adsorbed Co 2+ to Co 3+, resulting in excess adsorption of Co 2+ compared to Zn 2+ by biogenic birnessite.
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U2 - 10.1016/j.chemgeo.2012.03.029
DO - 10.1016/j.chemgeo.2012.03.029
M3 - Article
AN - SCOPUS:84860172248
SN - 0009-2541
VL - 310-311
SP - 106
EP - 113
JO - Chemical Geology
JF - Chemical Geology
ER -