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Land use types control solid wash-off rate and entrainment coefficient of Fukushima-derived $$^{137}$$Cs, and their time dependence

セシウム137の流出率, 濃度, 濃度減少速度に対する土地利用の影響

脇山 義史*; 恩田 裕一*; 吉村 和也; 五十嵐 康記*; 加藤 弘亮*

Wakiyama, Yoshifumi*; Onda, Yuichi*; Yoshimura, Kazuya; Igarashi, Yasunori*; Kato, Hiroaki*

This study provides the results of observations of plot-scale $$^{137}$$Cs wash-off from various land uses (two uncultivated farmlands, two cultivated farmlands, three grasslands and one forest) from 2011 to 2014. Annual $$^{137}$$Cs wash-off rate ranged from 0.0026 to 7.5% per year, and more vegetation cover resulted in lower sediment discharge. $$^{137}$$Cs concentration observed in uncultivated farmland plot decreased with time and the rate was lower than those of riverine, suggesting that contributions of $$^{137}$$Cs from the upslope area may be insignificant to that in riverine. A negative relationship between $$^{137}$$Cs concentration normalized by initial deposition amount and sediment concentration in runoff water was found. Cultivation appeared to cause enhanced soil erosion and resulted in constant relatively low $$^{137}$$Cs concentration. A contribution of coarse organic matter to $$^{137}$$Cs wash-off was suggested in the forest, which had relatively high $$^{137}$$Cs concentration and low sediment discharge.

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