Takamatsu, Takejiro; Kawashima, Munetsugu; Matsushita, Rokuji; Koyama, Mutsuo (1985): Geochemistry on sediments in Lake Biwa [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.855096, Supplement to: Takamatsu, T et al. (1985): General Distribution Profiles of Thirty-six Elements in Sediments and Manganese Concretions of Lake Biwa. Japanese Journal of Limnology, 46(2), 115-127, https://doi.org/10.3739/rikusui.46.115
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Abstract:
Thirty sediment cores (30-40 cm in length), 47 Ekman dredge sediments, and Mn concretions were collected from Lake Biwa. The concentrations of 36 elements in the samples were determined by instrumental neutron activation, X-ray fluorescence, atomic absorption, and colorimetric analyses. The elements determined included Mn, P, As, Sb, Fe, Ni, Co, Zn, Cu, Pb, Hg, Cr, Ti, Na, K, Rb, Cs, Mg, Ca, Sr, Ba, Sc, Hf, La, Ce, Sm, Eu, Yb, Lu, U, Th, Au, Ta, Nd, Br and N. Based on statistical considerations and calculation of the concentration factors of the elements, the features of the elemental distribution in Lake Biwa sediment were determined. The main results are summarized as follows : (1) Concentrations of Mn and As were very high in the uppermost oxidized layer of the offshore sediment and Mn concretions. This resulted from the dissolution-deposition cycles of these elements within the sedimentary column and the bottom water. The fixation of As at the sediment surface is mainly attributed to the adsorption of arsenate onto Mn (II) -rich hydrous Mn (IV) oxide. (2) There were high concentrations of Zn, Cu, Pb and Hg in the recent sediments. Although the source of these elements is attributed to human activities, the individual distributions of Zn and Cu in the sediment may result from the deposition of metal-rich planktonic debris and subsequent degradation of the debris. (3) The orders of increasing concentrations of alkali metals and lanthanides in the sediment from the central region compared with the nearshore pediment were identical to the orders of increasing atomic numbers from Na to Cs and from La to Lu, respectively.
Source:
Grant, John Bruce; Moore, Carla J; Alameddin, George; Chen, Kuiying; Barton, Mark (1992): The NOAA and MMS Marine Minerals Geochemical Database. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V52Z13FT
Further details:
Warnken, Robin R; Virden, William T; Moore, Carla J (1992): The NOAA and MMS Marine Minerals Bibliography. National Geophysical Data Center, NOAA, https://doi.org/10.7289/V53X84KN
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Coverage:
Median Latitude: 35.328324 * Median Longitude: 136.103846 * South-bound Latitude: 35.263720 * West-bound Longitude: 136.065060 * North-bound Latitude: 35.392270 * East-bound Longitude: 136.144480
Comment:
From 1983 until 1989 NOAA-NCEI compiled the NOAA-MMS Marine Minerals Geochemical Database from journal articles, technical reports and unpublished sources from other institutions. At the time it was the most extended data compilation on ferromanganese deposits world wide. Initially published in a proprietary format incompatible with present day standards it was jointly decided by AWI and NOAA to transcribe this legacy data into PANGAEA. This transfer is augmented by a careful checking of the original sources when available and the encoding of ancillary information (sample description, method of analysis...) not present in the NOAA-MMS database.
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Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
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Datasets listed in this publication series
- Takamatsu, T; Kawashima, M; Matsushita, R et al. (1985): (page 140) Observation of manganese concretions in lake Biwa, Japan. https://doi.org/10.1594/PANGAEA.855094
- Takamatsu, T; Kawashima, M; Matsushita, R et al. (1985): (Table 2, pages 117), Elemental concentrations of Mn concretions from the sediment surface at site G (Lake Biwa, Japan). https://doi.org/10.1594/PANGAEA.855095