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不同Hg浓度下水稻中Hg的分布累积特征

周俊1,刘鸿雁1**,吴龙华2,骆永明2,杜布云3,于萍萍1   

  1. (1贵州大学资源与环境工程学院, 贵阳 550025; 2中国科学院南京土壤研究所土壤环境与污染修复重点实验室, 南京 210008; 3中国科学院地球化学研究所环境地球化学国家重点实验室, 贵阳 550002)
  • 出版日期:2013-06-10 发布日期:2013-06-10

Distribution and accumulation characteristics of Hg in rice (Oryza sativa L.) under different concentrations of soil Hg. 

ZHOU Jun1, LIU Hong-yan1**, WU Long-hua2, LUO yong-ming2, DU Bu-yun3, YU Ping-ping1   

  1. (1College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China; 2Key Laboratory of Soil Environment and Pollution Remediation, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China; 3State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China)
  • Online:2013-06-10 Published:2013-06-10

摘要: 利用土壤盆栽实验方法,研究了土壤中Hg的形态分布,以及不同Hg浓度下,水稻不同生长时期各组织中Hg的分布规律和累积特征。土壤Hg存在的形态为:有机结合态>残渣态>>氧化态>>溶解与可交换态≈特殊吸附态,在水稻的生长过程中,土壤中的Hg呈现从残渣态向有机结合态转化的趋势,有机结合态Hg平均占比为61.7%,是土壤Hg最重要的存在形态。Hg在水稻不同部位的浓度分布呈现W>W>W>W>W籽粒,分析表明,水稻根、茎和籽粒中的Hg与土壤各形态Hg浓度呈显著或极显著正相关,但在水稻生长后期叶片中Hg与土壤Hg浓度的相关性不显著,叶片Hg与大气Hg进行交换起主要作用,改变了累积状况。随着土壤Hg浓度的增加和生长期的延长,根对Hg的束缚能力逐渐增加,根部Hg累积量增大,所占比例上升,而茎和叶的累积量相对稳定。

关键词: 状态转换, 非光化学猝灭, LHCⅡ磷酸化, 光系统

Abstract: A pot experiment was conducted to study the distribution of Hg forms in soil and the distribution and accumulation characteristics of Hg in rice (Oryza sativa L.) plant during its various growth stages under different concentrations of soil Hg. The main Hg forms in the soil were in the order of organic bound > residual >> oxidizable >> dissoluble and exchangeable ≈ specifically adsorbed. During rice growth season, the Hg in soil presented a transformation trend from residual to organic bound, and the organic bound Hg occupied 61.7% of the total Hg, being the most important existing form of Hg in soil. The Hg concentration in different organs of rice was in the order of root > leaf > stem > ear > grain. The Hg concentrations in rice root, stem, and grain were significantly positively correlated with the concentrations of all the Hg forms in soil. However, at the late growth stages of rice, the leaf Hg concentration had less correlation with soil Hg concentration, indicating that the exchange between leaf Hg and atmospheric Hg played a major role, and changed the Hg accumulated status. With the increase of soil Hg concentration and the extension of rice growth phase, the Hg binding capacity of rice root increased gradually, and the cumulative amount and the proportion of root Hg increased, while the accumulation amount of stem and leaf Hg was relatively stable.

Key words: state transition, LHCⅡ phosphorylation, photosystem, NPQ.