Japan Geoscience Union Meeting 2018

Presentation information

[JJ] Oral

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS14] Biogeochemistry

Wed. May 23, 2018 10:45 AM - 12:15 PM 101 (1F International Conference Hall, Makuhari Messe)

convener:Keisuke Koba(Center for Ecological Research, Kyoto University), Hideaki Shibata(Field Science Center fot Northern Biosphere, Hokkaido University), Naohiko Ohkouchi(海洋研究開発機構, 共同), Youhei Yamashita(Faculty of Environmental Earth Science, Hokkaido University), Chairperson:Nishina Kazuya, Shibata Hideaki(北海道大学北方生物圏フィールド科学センター)

11:30 AM - 11:45 AM

[MIS14-10] Kosa to volcanic-ash ratio in soil layers estimated by δ18O value and K-Ar dating

*Atsushi Nakao1, Mai Terashima1, Crawford Elliott2, Marion Wampler2, Ryoji Tanaka3, Junta Yanai1 (1.Graduate School of Life and Environmental Sciences, Kyoto Prefectural University, 2.The department of Geoscience, Georgia State University, 3.Institute of Planetary Materials, Okayama University)

Keywords:Kosa-dust, K-Ar dating, δ18O, volcanic-ash

The proportion of Kosa-dust and volcanic-ash as a parent material of soil was estimated by using stable isotopic analysis and radiometric dating method. This proportion is important to predict radiocesium mobility in the soil. Micaceous minerals, which can immobilize radiocesium by forming an inner-sphere complex, are abundant in Kosa-dust, while not in volcanic-ash.

Fifteen soils were collected from stacking layers of volcanic ash and Kosa-dust in an outcrop about 20 km north-east from Mt. Sanbe. These soils include four key tephra layers (Sanbe-Ikeda; 0.04 Ma, Sanbe-Sunahara; 0.05 Ma, Sanbe-Unnann; 0.07 Ma, Sanbe-Kisuki; 0.11 Ma) with rhyolitic or dacitic composition. The 2-20 μm particles were fractionated from these soils by using sieving and sedimentation methods after decomposing organic matters. SiO2 minerals (mainly quartz) were isolated from a portion of the 2-20 μm particles to determine their δ18O values. Potassium (K) content in the 2-20 μm particles was determined with atomic absorption spectrophotometry after they were digested with HF-HNO3 solution. Percentage of 40K in total K was calculated by the stable isotopic ratio. Amount of 40Ar remaining in K-bearing minerals was determined by mass spectrometry. Then K-Ar age was determined by using these values.

The δ18O values ranged from 8.64 to 15.14‰. The minimum value was similar to those of SiO2 in rhyolite or dacite, whereas the maximum value was in the range of those previously obtained from Kosa-dust. The K-Ar ages ranged from 33 to 400 Ma. Except for the oldest one, these ages were similar or younger than those of Kosa-dust previously investigated (180-200 Ma), whereas much older than those of the key tephra layers (i.e. from 0.04 to 0.11 Ma). Interestingly, the δ18O values and the K-Ar values showed a proportional relationship. Linear regression analysis obtained the following relationship; y = 0.034x + 7.93 (R2 = 0.88) by putting y = “δ18O” and x = “K-Ar age”. This linear relationship suggests that the soil layers in this study may be a mixture of volcanic-ash and Kosa-dust, both of which have a fixed or at least narrow range of δ18O and the K-Ar values. The proportion of Kosa-dust in the 2-20 μm particles may take a wide range of value from 15 to 95%.