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基于可交换态和非交换态钾的福岛低放射性铯向糙米转移土壤筛选的先进方法。

Advanced approach for screening soil with a low radiocesium transfer to brown rice in Fukushima based on exchangeable and nonexchangeable potassium.

机构信息

Graduate School of Life and Environmental Sciences, Kyoto Prefectural University, 1-5, Shimogamo, Hangi-cho, Sakyo-ku, Kyoto 606-8522, Japan.

Tohoku Agricultural Research Center, NARO, 50, Harajukuminami, Arai, Fukushima 960-2156, Japan.

出版信息

Sci Total Environ. 2020 Nov 15;743:140458. doi: 10.1016/j.scitotenv.2020.140458. Epub 2020 Jun 25.

Abstract

Phytoavailable K in soil is a key to control the transfer factor of radiocesium from soil to brown rice. The transfer factors were determined for paddy fields cultivated in 2017 and 2018 under different K fertilization regimes in Fukushima Prefecture, Japan. Two phytoavailable forms of K, the exchangeable and nonexchangeable K contents were investigated for the surface soil sampled after the transplanting and fertilization as well as after harvest of rice in the same paddy fields. The exchangeable K content largely decreased from after transplanting and fertilization to after harvest, and the exchangeable K of the soil after harvest was negatively correlated with the transfer factor (r = -0.70, p < .001). Most soil samples after harvest showed that the transfer factors exponentially increased as the exchangeable K decreased; however, some of the samples indicated considerably low transfer factors (<0.005) despite being exchangeable K deficient, i.e., exchangeable K < 25 mg KO 100 g. Even though this value before usual fertilization has been effectively used as a threshold to determine whether supplemental K fertilization is required to reduce the radiocesium content in brown rice, additional screening was needed to estimate this radiocesium transfer more precisely. Thus, we found that not only the exchangeable K but also nonexchangeable K contents had a negative correlation with the transfer factor (r = -0.60, p < .001) of the soil samples after harvest but were not correlated with each other (r = -0.10). Furthermore, the results revealed that soil with nonexchangeable K > 50 mg KO 100 g indicated a considerably low transfer factor, even if exchangeable K deficient. Thus, via our field-scale experiments, we concluded that the criterion nonexchangeable K > 50 mg KO 100 g can be used as another threshold for use along with that of exchangeable K to differentiate soil with a low radiocesium transfer rate from exchangeable K deficient soil.

摘要

土壤中的有效钾是控制放射性铯从土壤向糙米转移的关键因素。本研究在日本福岛县开展,通过调查 2017 年和 2018 年不同钾肥施用量条件下稻田中放射性铯的转移系数,确定了可用于控制土壤向糙米中放射性铯转移的关键因素。研究人员调查了表层土壤中两种有效钾形态(可交换性钾和非交换性钾)的含量,这些土壤是在移栽和施肥后以及同一稻田收获后采集的。可交换性钾含量从移栽和施肥后到收获后大幅下降,收获后土壤的可交换性钾与转移系数呈负相关(r=-0.70,p<0.001)。大多数收获后土壤的转移系数随着可交换性钾的降低而呈指数增加;然而,一些土壤的可交换性钾含量低于 25mg KO 100g(即缺乏可交换性钾),但其转移系数却相当低(<0.005)。尽管在通常的施肥之前,这个值已被有效地用作确定是否需要补充钾肥来降低糙米中放射性铯含量的阈值,但仍需要进一步筛选以更准确地估计这种放射性铯的转移。因此,我们发现,不仅可交换性钾,而且非交换性钾含量与收获后土壤的转移系数(r=-0.60,p<0.001)呈负相关,但两者之间没有相关性(r=-0.10)。此外,研究结果表明,即使可交换性钾缺乏,如果土壤中非交换性钾含量>50mg KO 100g,则土壤的转移系数也会相当低。因此,通过我们的田间规模实验,我们得出结论,非交换性钾含量>50mg KO 100g可以作为另一个阈值,与可交换性钾阈值一起用于区分放射性铯转移率低的土壤和可交换性钾缺乏的土壤。

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