中国农业科学 ›› 2015, Vol. 48 ›› Issue (2): 241-250.doi: 10.3864/j.issn.0578-1752.2015.02.04

• 耕作栽培·生理生化 • 上一篇    下一篇

外源四价硒条件下硫对小麦硒吸收的影响机制

刘新伟,段碧辉,赵小虎,郭再华,胡承孝,赵竹青   

  1. 华中农业大学微量元素研究中心/农业部长江中下游耕地保育重点实验室,武汉430070
  • 收稿日期:2014-03-10 出版日期:2015-01-16 发布日期:2015-01-16
  • 通讯作者: 赵竹青,Tel:027-87288578
  • 作者简介:刘新伟,E-mail:jiangcunzhen@163.com
  • 基金资助:
    国家自然科学基金项目(31201501)、湖北省产业规划支持项目

Effects of Sulfur on Selenium Uptake in Wheat and Its Mechanism when Amended with Selenite

LIU Xin-wei, DUAN Bi-hui, ZHAO Xiao-hu, GUO Zai-hua, HU Cheng-xiao, ZHAO Zhu-qing   

  1. Microelement Research Center, Huazhong Agricultural University/Key Laboratory of Arable Land Conservation (Middle and Lower Reaches of Yangtze River), Ministry of Agriculture, Wuhan 430070
  • Received:2014-03-10 Online:2015-01-16 Published:2015-01-16

摘要: 【目的】研究硫肥对外源四价硒条件下土壤硒赋存形态和价态变化的影响,旨在揭示硫调控小麦硒吸收的作用机制。【方法】以郑麦9023为试验材料,通过苗期土培和水培进行,土培试验设3个硫水平,分别为0、150和300 mg·kg-1,硫源为硫磺,2个硒水平,分别为0和5 mg·kg-1,硒源为亚硒酸钠,生长至70 d收获并取土样;水培试验先将幼苗在1/5 Hogland-Arnon营养液中培养2周,然后开始进行处理,设3个硫水平,分别为0、1和2 mmol·L-1,硫源为硫酸镁,硒水平为10 µmol·L-1,2种硒源,分别为亚硒酸钠和硒酸钠,培养24 h后收获,土培和水培试验均为完全交互设计,重复4次,采用HG-AFS-8220型双道原子荧光光度计对小麦地上部和根以及土壤中硒含量进行测定,根据与植物硒吸收的相关性,将土壤总硒分成不同赋存形态和价态。【结果】施用适量硒和硫对小麦生长均有一定的促进作用;150 mg·kg-1硫可以显著降低小麦地上部和根中硒含量和硒累积量,降幅分别可达61.7 %、34.4%和55.7%、24.7%,但是这种降低不会随施硫量的增加而显著变化;施硫可以显著降低土壤pH值,最高可降低0.50个单位,并增加了土壤有机质含量,最高可增加0.78 g·kg-1。施硫可以显著降低土壤中水溶态硒含量,并显著增加铁锰氧化物结合态硒含量,也增加了有机结合态和残渣态硒含量,而对交换态硒含量无显著影响,表明施硫促使了硒在土壤中的钝化。施硫可以显著降低水溶态中各种价态硒含量,其降幅基本一致,施硫可以增加交换态中四价硒含量而显著减少六价硒含量,表明施硫抑制了硒在土壤中向高效价态的转化。小麦对四价硒和六价硒的吸收差异与是否施硫密切相关,无硫时,六价硒处理下小麦地上部和根中硒含量分别为四价硒处理的44.7和22.4倍,而硫浓度为1 mmol·L-1时,其硒含量迅速降为四价硒处理的2.8倍和51.8%,表明硫可以显著缩小小麦对四价和六价硒的吸收能力差异。【结论】施用适量硫肥在改善小麦生长的同时,可以通过降低土壤pH和提高有机质含量,促使水溶态硒在土壤中向铁锰氧化物结合态、有机结合态及残渣态的钝化,并抑制交换态中四价硒向六价态的转化,从而降低小麦对硒的吸收。因此,可以通过在高硒缺硫地区增施硫肥以及缺硒高硫地区减施硫肥来有效调控作物体内的硒含量

关键词: 普通小麦, 亚硒酸盐, 硫磺, 硒形态, 硒价态

Abstract: 【Objective】This study was conducted to investigate the effects of sulfur (S) on the fractions and species of amended selenite in soil by applying S fertilizer, and explore the mechanism through which S controls the selenium (se) uptake of wheat. 【Method】Wheat (Triticum aestivum L. cv. Zhengmai 9023) was chosen as the test material, and underwent seedling stage soil cultivation and solution cultivation. A potted soil experiment was performed on wheat and the application amounts of S were 0, 150, and 300 mg?kg-1, respectively, Sulfur was used as S source, Se source was selenite (Na2SeO3) and it was designated at 0 and 5 mg?kg-1. The wheat seedlings were harvested on the 70th day after sowing and soil samples were taken. The treatments started two weeks after the seedlings were planted in hydroponic experiment which the nutrient solution was made with 1/5 Hogland-Arnon formula. Different amounts of S were added in the experiment: 0, 0.1, and 2 mmol?L-1; Se was designed at 10 µmol?L-1. Se and S was supplied to plants in the form of sodium selenite (Na2SeO3), sodium selenate (Na2SeO4?10H2O) and magnesium sulfate (MgSO4?7H2O), respectively. Wheat was harvested after 24 h. A fully interactional design was performed and each treatment was repeated four times in potted soil experiment and hydroponic experiment. The hydride generation atomic fluorescence spectrometer model HG-AFS-8220 was used to measure the Se content in shoot and root of wheat and soil. Based on the Se absorption of plant and the correlation of selenium content in soil, Se content in the soil was divided into different fractions and species. 【Result】Applications of both Se and S resulted in stimulation to wheat growth with appropriate amount. S was applied at 150 mg?kg-1 significantly reduced the content and accumulation of Se in shoots and roots of wheat by 61.7% and 35.5% , 55.7% and 24.7%, respectively, but such reduction won’t change significantly with the increasing S application to soil. Application of S significantly decreased the pH value and obviously increased the organic matter content as much as 0.5 units and 0.78 g?kg-1, respectively. Application of S significantly decreased soluble Se and increased Fe/Mn oxide-bound Se, also increased organic matter-bound Se and residual Se obviously, with no significant effect on exchangeable Se, showing that S application can prompted the passivation of Se in soil. Application of S also significantly decreased the content of various Se species in the soluble Se, and obviously increased the content of Se(IV) and significantly decreased the content of Se(VI) in the exchangeable Se, showing that application of S retarded the conversion of Se to the efficient species in soil. S had a profound effect on the intake of Se by wheat seedlings when Se(IV) and Se(VI) was applied. The Se content in shoot and root of wheat in the Se(VI)-treatment was 44.7 and 22.4 times, respectively, the content in Se(IV)-treatment, while with a S rate of 1 mmol?L-1, their Se contents were less than 2.8 times and 51.8% of the Se(IV)-treatment, showing that S application significantly reduced the differences of absorption capacity in wheat between the treatments of Se(IV) and Se(VI). 【Conclusion】In addition to improving wheat growth, an appropriate amount of S fertilizer can reduce soil pH and increase organic content, causing soluble Se in soil to be Fe/Mn oxide-bound, organic matter-bound and residual Se, and retarding the conversion of Se(IV) to Se(VI) in the exchangeable Se, thus reducing Se uptake by wheat. Therefore, the content of Se in crops can be effectively controlled by increasing S in the high Se and deficient S area and reducing S in the deficient Se and high S area.

Key words: common wheat, selenite, sulfur, selenium fraction, selenium species