Natsuki Yoshikawa

137Cs in irrigation water and its effect on paddy fields in Japan after the Fukushima nuclear accident

There is concern that radiocesium deposited in the environment after the accident at the Fukushima Daiichi Nuclear Power Plant (FDNPP) in March 2011 will migrate to paddy fields through hydrological pathways and cause serious and long-lasting damage to the agricultural activities. This study was conducted in the Towa region of Nihonmatsu in the northern part of Fukushima Prefecture, Japan, (1) to quantify (137)Cs in stream water used to irrigate paddy fields by separating the dissolved and particulate components in water samples and then fractionating the particulate components bonded in different ways using a sequential extraction procedure, and (2) to determine the amounts of radiocesium newly added to paddy fields in irrigation water relative to the amounts of radiocesium already present in the fields from the deposition of atmospheric fallout immediately after the FDNPP accident. Three catchments were studied, and the (137)Cs activity concentrations in stream water samples were 79-198 mBq L(-1) under stable runoff conditions and 702-13,400 Bq L(-1) under storm runoff conditions. The residual fraction (F4, considered to be non-bioavailable) was dominant, accounting for 59.5-82.6% of the total (137)Cs activity under stable runoff conditions and 69.4-95.1% under storm runoff conditions. The (137)Cs newly added to paddy fields in irrigation water only contributed 0.03-0.05% of the amount already present in the soil (201-348 kBq m(-2)). This indicates that the (137)Cs inflow load in irrigation water is negligible compared with that already in the soil. However, the contribution from the potentially bioavailable fractions (F1+F2+F3) was one order of magnitude larger, accounting for 0.20-0.59%. The increase in the dissolved and soluble radiocesium fraction (F1) was especially large (3.0% to infinity), suggesting that radiocesium migration in irrigation water is increasing the accumulation of radiocesium in rice.

Can Paddy Fields Mitigate Flood Disaster? Possible Use and Technical Aspects of the Paddy Field Dam

To address the recent increase of flood risk, an unconventional measure for flood disaster mitigation using existing paddy fields with enhancement of their function has been recently introduced as an inexpensive and environmentally sustainable means of flood control. This measure is called the paddy field dam (PFD), in which rainwater is intentionally and temporarily stored in paddy fields during intense rainfall, by installing runoff control devices at the drainage outlet of paddy field plots. Although the PFD has been proven to have a large flood control function by our in situ investigation and simulation, there are various obstacles to overcome toward wide propagation of this measure. The fact that farmers have no economic incentive to undertake PFD practices is a most serious obstacle to increasing their implementation. In this article, we describe the effects of PFD and review issues that must be resolved before this type of work can be undertaken more widely.

Measurement and estimation of radiocesium discharge rate from paddy field during land preparation and mid-summer drainage

In this research, we evaluated the range of (137)Cs discharge rates from paddy fields during land preparation and mid-summer drainage. First, we investigated (137)Cs discharge loads during land preparation and mid-summer drainage and their ratio to the (137)Cs inventory of paddy field soil. We found that total discharge rates were 0.003-0.028% during land preparation and 0.001-0.011% during mid-summer drainage. Next, we validated the range of obtained total discharge of (137)Cs from the paddy fields using a simplified equation and literature review. As a result, we conclude that the range of total outflow loads of suspended solids for the investigated paddy field was generally representative of paddy fields in Japan. Moreover, the (137)Cs discharge ratio had a wide range, but was extremely small relative to (137)Cs present in paddy field soil before irrigation.