JpGU-AGU Joint Meeting 2017

講演情報

[EE] ポスター発表

セッション記号 A (大気水圏科学) » A-GE 地質環境・土壌環境

[A-GE40] [EE] エネルギ・環境・水ネクサスと持続的発展

2017年5月22日(月) 10:45 〜 12:15 ポスター会場 (国際展示場 7ホール)

コンビーナ:張 銘(産業技術総合研究所地質調査総合センター地圏資源環境研究部門)、薛 強(中国科学院武漢岩土力学研究所)、温 志超(国立曇林科技大学)、川本 健(埼玉大学大学院理工学研究科)

[AGE40-P10] Preliminary environmental magnetic results of pedogenic processes in mine waste during plant growth.

*川崎 一雄1蒲池 浩之1酒井 英男1 (1.富山大学大学院理工学研究部(理学))

キーワード:Environmental magnetism, Pedogenesis, Athyrium yokoscense

The historic Kamegai Pb-Zn-Ag deposit at Mt. Hachibuse in Toyama, Japan, was mined between 1567 and 1926, leaving considerable mine waste in the region. This mine waste may generate acidic ground water containing high concentrations of sulphide and metals. Environmental magnetic results are reported here on the changes in magnetic properties of the Kamegai mine’s waste from the growth of the fern, Athyrium yokoscense. This fern is known to flourish at sites that are highly polluted with heavy metals such as cadmium, copper, lead and zinc. Six mixtures were prepared from two different soil types, mine waste and synthetic soils of mountain sand, vermiculite and artificial magnetite powder. One mixture of each soil type is a control soil sample without any fern and the other four were planted with Athyrium yokoscense. In-field magnetic susceptibility measurements of the soil surfaces were done about once a week for 20 weeks. Overall, the mean magnetic susceptibility of soils with ferns decreased more than the control soils without ferns. However, there is no obvious correlation between the decay rates of susceptibility and plant growth. After 20 weeks the soils were collected for further rock magnetic analyses. Higher mass susceptibilities were observed in soils with the fern, especially near the fern’s roots. More rapid stepwise isothermal remanent magnetization acquisition curves as well as alternating field demagnetization decay curves were observed in the soils with ferns, indicating that more low coercivity magnetic minerals, such as magnetite, were generated in these soils. Therefore, the mass susceptibilities appear to show magnetic enhancement by pedogenic processes. Conversely, the in-field magnetic susceptibility measurements for which the lower magnetic susceptibility were observed in the soils with ferns likely detect the spatial distribution of the fern’s roots.