M. Tamaoki, T. Yabe, J. Furukawa, Mirai Watanabe, K. Ikeda, I. Yasutani, T. Nishizawa
{"title":"高等植物修复土壤放射性铯的潜力比较","authors":"M. Tamaoki, T. Yabe, J. Furukawa, Mirai Watanabe, K. Ikeda, I. Yasutani, T. Nishizawa","doi":"10.2525/ECB.54.65","DOIUrl":null,"url":null,"abstract":"In 2011, the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident occurred following the Great East Japan Earthquake at March 2011. As a result, a huge amount of radionuclides, such as I, cesium (Cs) and Cs, were discharged to the surrounding environment from the site of accident (Tokyo Electric Power Company, 2012). Agricultural lands and forests were heavily contaminated with these radionuclides, consequently, commercial distribution of many crops cultivated (and to be cultivated) in severely contaminated area, chiefly in Fukushima prefecture, have been restricted since agricultural products from these area often exceeded the regulatory level of radioactivity defined by laws in Japan (100 Bq kg ). Among the soil-contaminating radionuclides, C is the major radionuclide to be concerned since its half-life is relatively long (30.1 years; Chino et al., 2011) in comparison to other radionuclides released from the FDNPP. In addition, Cs can emit gamma ( )-ray, hence long-term biological effects by the -ray released from Cs in biota including wild animals might also be concerned. Indeed, following adverse effects in ecosystem in Fukushima have been reported; increased frequency of morphological abnormality in the pale grass blue butterfly (Hiyama et al., 2012), reduced abundance in common birds (Møller et al., 2012), and decrease in blood cell number in wild Japanese monkeys (Ochiai et al., 2014). Therefore, clean-up of radionuclides from the contaminated soil becomes a big issue in reconstruction and revitalization of Fukushima area. Previous studies relevant to Chernobyl accident showed that soil-penetrated Cs binds strongly to the clay and showed low mobility. For example, Kirk and Staunton (1989) showed that migration rate of Cs was less than 1 cm per year. Thus, the major portion of the Cs must be distributed in the upper 10 cm-thick surface layer of the soil column in most types of soils even seven years after of the accident (Arapis et al., 1997). In the FDNPP accident, contamination of Cs occurred in vast land area especially in Fukushima prefecture. Because of the high cost, decontamination of the large area polluted with Cs by conventional engineering methods remains an intractable problem. Furthermore, these methods often encompass negative effects for physical properties of the soil and also wreak ecosystem and landscape. Phytoremediation, the use of higher plants to clean-up the contaminants from soil through accumulation of contaminants in plants, is an alternative technology to conventional methods (Pilon-Smits and Freeman, 2006). The behavior of Cs in soil and plants is similar to that of potas-","PeriodicalId":11762,"journal":{"name":"Environmental Control in Biology","volume":"9 1","pages":"65-69"},"PeriodicalIF":0.0000,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"6","resultStr":"{\"title\":\"Comparison of Potentials of Higher Plants for Phytoremediation of Radioactive Cesium from Contaminated Soil\",\"authors\":\"M. Tamaoki, T. Yabe, J. Furukawa, Mirai Watanabe, K. Ikeda, I. Yasutani, T. Nishizawa\",\"doi\":\"10.2525/ECB.54.65\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In 2011, the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident occurred following the Great East Japan Earthquake at March 2011. As a result, a huge amount of radionuclides, such as I, cesium (Cs) and Cs, were discharged to the surrounding environment from the site of accident (Tokyo Electric Power Company, 2012). Agricultural lands and forests were heavily contaminated with these radionuclides, consequently, commercial distribution of many crops cultivated (and to be cultivated) in severely contaminated area, chiefly in Fukushima prefecture, have been restricted since agricultural products from these area often exceeded the regulatory level of radioactivity defined by laws in Japan (100 Bq kg ). Among the soil-contaminating radionuclides, C is the major radionuclide to be concerned since its half-life is relatively long (30.1 years; Chino et al., 2011) in comparison to other radionuclides released from the FDNPP. In addition, Cs can emit gamma ( )-ray, hence long-term biological effects by the -ray released from Cs in biota including wild animals might also be concerned. Indeed, following adverse effects in ecosystem in Fukushima have been reported; increased frequency of morphological abnormality in the pale grass blue butterfly (Hiyama et al., 2012), reduced abundance in common birds (Møller et al., 2012), and decrease in blood cell number in wild Japanese monkeys (Ochiai et al., 2014). Therefore, clean-up of radionuclides from the contaminated soil becomes a big issue in reconstruction and revitalization of Fukushima area. Previous studies relevant to Chernobyl accident showed that soil-penetrated Cs binds strongly to the clay and showed low mobility. For example, Kirk and Staunton (1989) showed that migration rate of Cs was less than 1 cm per year. Thus, the major portion of the Cs must be distributed in the upper 10 cm-thick surface layer of the soil column in most types of soils even seven years after of the accident (Arapis et al., 1997). In the FDNPP accident, contamination of Cs occurred in vast land area especially in Fukushima prefecture. 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引用次数: 6
摘要
2011年,福岛第一核电站(FDNPP)事故发生在2011年3月东日本大地震之后。因此,大量的放射性核素,如I、铯(Cs)和铯从事故现场排放到周围环境(东京电力公司,2012)。农田和森林受到这些放射性核素的严重污染,因此,在严重污染地区(主要是福岛县)种植(和将要种植)的许多作物的商业分销受到限制,因为这些地区的农产品往往超过日本法律规定的放射性管制水平(100 Bq kg)。在污染土壤的放射性核素中,碳是最值得关注的放射性核素,因为它的半衰期较长(30.1年;Chino et al., 2011),与FDNPP释放的其他放射性核素相比。此外,Cs可释放γ射线,因此,Cs释放的γ射线对包括野生动物在内的生物群也可能产生长期的生物效应。事实上,福岛生态系统的负面影响已经被报道;浅草蓝蝴蝶形态异常频率增加(Hiyama et al., 2012),普通鸟类丰度减少(Møller et al., 2012),野生日本猴子血细胞数量减少(Ochiai et al., 2014)。因此,从受污染土壤中清除放射性核素成为福岛地区重建与振兴的一大课题。以往与切尔诺贝利事故相关的研究表明,土壤渗透的铯与粘土结合强烈,流动性低。例如Kirk和Staunton(1989)表明,Cs的迁移速率小于1 cm /年。因此,即使在事故发生7年后,大多数类型的土壤中,Cs的主要部分仍然分布在土柱表层10 cm厚的上部(Arapis et al., 1997)。在福岛核电站事故中,碳污染发生在大片土地上,特别是福岛县。由于成本高,用常规的工程方法对大面积的铯污染进行净化仍然是一个棘手的问题。此外,这些方法往往会对土壤的物理性质产生负面影响,也会破坏生态系统和景观。植物修复,即利用高等植物通过污染物在植物中的积累来清除土壤中的污染物,是一种替代传统方法的技术(Pilon-Smits和Freeman, 2006)。土壤和植物中碳元素的行为与钾元素相似
Comparison of Potentials of Higher Plants for Phytoremediation of Radioactive Cesium from Contaminated Soil
In 2011, the Fukushima Daiichi Nuclear Power Plant (FDNPP) accident occurred following the Great East Japan Earthquake at March 2011. As a result, a huge amount of radionuclides, such as I, cesium (Cs) and Cs, were discharged to the surrounding environment from the site of accident (Tokyo Electric Power Company, 2012). Agricultural lands and forests were heavily contaminated with these radionuclides, consequently, commercial distribution of many crops cultivated (and to be cultivated) in severely contaminated area, chiefly in Fukushima prefecture, have been restricted since agricultural products from these area often exceeded the regulatory level of radioactivity defined by laws in Japan (100 Bq kg ). Among the soil-contaminating radionuclides, C is the major radionuclide to be concerned since its half-life is relatively long (30.1 years; Chino et al., 2011) in comparison to other radionuclides released from the FDNPP. In addition, Cs can emit gamma ( )-ray, hence long-term biological effects by the -ray released from Cs in biota including wild animals might also be concerned. Indeed, following adverse effects in ecosystem in Fukushima have been reported; increased frequency of morphological abnormality in the pale grass blue butterfly (Hiyama et al., 2012), reduced abundance in common birds (Møller et al., 2012), and decrease in blood cell number in wild Japanese monkeys (Ochiai et al., 2014). Therefore, clean-up of radionuclides from the contaminated soil becomes a big issue in reconstruction and revitalization of Fukushima area. Previous studies relevant to Chernobyl accident showed that soil-penetrated Cs binds strongly to the clay and showed low mobility. For example, Kirk and Staunton (1989) showed that migration rate of Cs was less than 1 cm per year. Thus, the major portion of the Cs must be distributed in the upper 10 cm-thick surface layer of the soil column in most types of soils even seven years after of the accident (Arapis et al., 1997). In the FDNPP accident, contamination of Cs occurred in vast land area especially in Fukushima prefecture. Because of the high cost, decontamination of the large area polluted with Cs by conventional engineering methods remains an intractable problem. Furthermore, these methods often encompass negative effects for physical properties of the soil and also wreak ecosystem and landscape. Phytoremediation, the use of higher plants to clean-up the contaminants from soil through accumulation of contaminants in plants, is an alternative technology to conventional methods (Pilon-Smits and Freeman, 2006). The behavior of Cs in soil and plants is similar to that of potas-