Li Yi-Chun, Chen Yong, Tang Ming-Deng, Li Lin-Feng, Lin Xiao-Yang, Wang Yan-Hong, Xu Di-Hao, Ai Shao-Ying
Institute of Agricultural Resources and Environment, Guangdong Academy of Agricultural Sciences, Guangzhou 510640, China.
Key Laboratory of Plant Nutrition and Fertilizer in South Region, Ministry of Agriculture, Guangzhou 510640, China.
Huan Jing Ke Xue. 2020 Nov 8;41(11):5143-5150. doi: 10.13227/j.hjkx.202004166.
Cadmium (Cd) contamination in the agricultural soils of China is a serious and growing environmental problem that urgently needs to be controlled and completely remediated. The biogeochemical cycles of nitrogen (N), sulfur (S), and iron (Fe), and the coupled cycles of Fe-N and Fe-S have been reported to control Cd transportation in the soil-rice system. Exploring practical remediation strategies for Cd from the perspective of the application of nutrients such as N, S, and Fe for rice growth is expected to obtain farm-specific and state-of-the-art technologies and products to reduce the accumulation of Cd in rice grains. Using our earlier study as a basis, the rhizosphere bag-pot experiment with ferrous sulfate (FeSO) and ferric nitrate[Fe(NO)] treatments was conducted to investigate Cd bioavailability in rhizosphere soil and Cd translocation in rice plants, and to highlight some possible factors and mechanisms controlling Cd accumulation in rice grains. The results showed that both FeSO and Fe(NO) treatments reduced the bioavailable Cd (NHAc-Cd) content in rhizosphere soil, with the decreasing extent being significantly lower in the former (55.6%) than in the latter (76.0%). Both FeSO and Fe(NO) treatments changed the distribution characteristics of Cd in rice tissues, and the FeSO treatment increased the Cd content in brown rice (0.6 mg·kg), but the Fe(NO) treatment decreased the Cd content in brown rice (0.1 mg·kg). Adsorption or co-precipitation of Cd by iron plaque, increased accumulations of Cd in root, stem, and leaf, and enhanced translocations of Cd from root, stem, and nodule to brown rice occurred with the increased Cd content in brown rice of the FeSO treatment. However, the decreased Cd content in brown rice with the Fe(NO) treatment was ascribed to adsorption or co-precipitation of Cd by poorly crystalline Fe oxides and solid Fe sulfides, decreased accumulations of Cd in stem and nodule, and weakened translocations of Cd from root, leaf, and nodule to brown rice. These findings provide a scientific basis for the exploration and application of nutritive soil amendment, and will have significance in regards to the remediation of Cd-contaminated agricultural soils in China.
中国农业土壤中的镉(Cd)污染是一个严重且日益严峻的环境问题,亟待加以控制和彻底修复。据报道,氮(N)、硫(S)和铁(Fe)的生物地球化学循环以及铁 - 氮和铁 - 硫的耦合循环控制着土壤 - 水稻系统中镉的迁移。从施用氮、硫、铁等养分促进水稻生长的角度探索镉的实际修复策略,有望获得针对农场具体情况的先进技术和产品,以减少镉在稻米中的积累。以我们早期的研究为基础,进行了硫酸亚铁(FeSO)和硝酸铁[Fe(NO)]处理的根际袋盆栽试验,以研究根际土壤中镉的生物有效性以及镉在水稻植株中的转运,并突出一些控制镉在稻米中积累的可能因素和机制。结果表明,FeSO和Fe(NO)处理均降低了根际土壤中生物可利用镉(NHAc - Cd)的含量,前者(55.6%)的降低幅度明显低于后者(76.0%)。FeSO和Fe(NO)处理均改变了镉在水稻组织中的分布特征,FeSO处理使糙米中镉含量增加(0.6 mg·kg),而Fe(NO)处理使糙米中镉含量降低(0.1 mg·kg)。FeSO处理使糙米中镉含量增加,是由于铁膜对镉的吸附或共沉淀、根、茎和叶中镉积累增加以及镉从根、茎和节向糙米的转运增强。然而,Fe(NO)处理使糙米中镉含量降低,归因于无定形铁氧化物和固态硫化铁对镉的吸附或共沉淀、茎和节中镉积累减少以及镉从根、叶和节向糙米的转运减弱。这些研究结果为营养性土壤改良剂的探索和应用提供了科学依据,对于中国镉污染农田土壤的修复具有重要意义。