Choi Yong-Ho, Kang Hee-Suk, Jun In, Keum Dong-Kwon, Park Hyo-Kook, Choi Geun-Sik, Lee Hansoo, Lee Chang-Woo
Nuclear Environment Research Division, Korea Atomic Energy Research Institute, P.O. Box 105, Yuseong, Daejeon 305-600, Republic of Korea.
J Environ Radioact. 2007;93(3):157-69. doi: 10.1016/j.jenvrad.2006.12.008. Epub 2007 Feb 8.
The transfer of 90Sr to rice plants following its acute ground deposition was examined experimentally in a greenhouse. Lysimeters were flooded after being filled with the soil monoliths from 12 paddy fields. A solution of 90Sr was applied to the standing water in the flooded lysimeters at the pre-transplanting stage or booting stage. Applied 90Sr was mixed with the topsoil only after the pre-transplanting application (PTA). The transfer was quantified with the areal transfer factor (TF(a), m2 kg(-1)-dry) defined as the ratio of the plant concentration to the initial ground deposition. In the PTA, the first-year TF(a) values in the 12 soils were in the range of 8.2 x 10(-3) -2.1 x 10(-2) and 1.7 x 10(-4) -3.6 x 10(-4) for the straws and hulled seeds, respectively. The TF(a) values from the booting-stage application (BSA) were higher than those from the PTA by a factor of up to four. The ratios of the seed TF(a) to the straw TF(a) were, on the whole, higher in the BSA. The 90Sr TF(a) in the PTA was negatively correlated with the soil pH and, to a lesser degree, the exchangeable Ca content. In the second year, the TF(a) in the PTA reduced to 53-90% of that in the first year. A more significant reduction, in general, occurred in a sandier soil. Based on the four consecutive years' transfer data, an overall half-time of the 90Sr TF(a) was estimated to be 2.2 years.
在温室中通过实验研究了急性地面沉降后90锶向水稻植株的转移情况。在装满来自12个稻田的土壤单块后,将渗漏计淹水。在移栽前阶段或孕穗期,将90锶溶液施用于淹水渗漏计中的积水。仅在移栽前施用(PTA)后,施用的90锶才与表土混合。转移量用面积转移因子(TF(a),m2 kg(-1)-干)进行量化,该因子定义为植物浓度与初始地面沉降的比值。在PTA中,12种土壤中第一年秸秆和糙米的TF(a)值分别在8.2×10(-3)-2.1×10(-2)和1.7×10(-4)-3.6×10(-4)范围内。孕穗期施用(BSA)的TF(a)值比PTA的TF(a)值高出四倍。总体而言,BSA中种子TF(a)与秸秆TF(a)的比值更高。PTA中90锶的TF(a)与土壤pH呈负相关,与可交换钙含量的相关性较小。在第二年,PTA中的TF(a)降至第一年的53-90%。一般来说,在砂质土壤中减少更为显著。根据连续四年的转移数据,估计90锶TF(a)的总体半衰期为2.2年。