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水分管理对硫铁镉在水稻根区变化规律及其在水稻中积累的影响
引用本文:张雪霞,张晓霞,郑煜基,王荣萍,陈能场,卢普相.水分管理对硫铁镉在水稻根区变化规律及其在水稻中积累的影响[J].环境科学,2013,34(7):2837-2846.
作者姓名:张雪霞  张晓霞  郑煜基  王荣萍  陈能场  卢普相
作者单位:广东省生态环境与土壤研究所,广州,510650
基金项目:国家自然科学基金项目(41101212, 41071300); 广东省科学院野外科学实验站基金项目(sytz 2010 11); 广东省环保专项资金项目
摘    要:选取了酸性矿山废水污灌区重金属污染水稻土,通过盆栽试验研究了不同水分管理条件(60%最大田间持水量,80%最大田间持水量,最大田间持水量,前期淹水+抽穗扬花期烤田,全生育期淹水)下水稻根际土壤及其不同器官(稻根、茎叶和籽粒)中硫、Fe和Cd的含量变化.结果表明,随着土壤水分含量的增加,在分蘖期根际土壤中Cd的含量略有升高,在成熟期对水稻根际土壤中Fe和Cd含量的影响不大;水稻不同器官对铁的吸收逐渐增加,对Cd的吸收则逐渐减少,两者呈明显的负相关关系;但抽穗扬花期烤田对水稻各器官对Fe的吸收影响不大,却明显增加了各器官中Cd的含量.除旱作处理外,不同水分管理方式下,土壤中全硫和有效硫含量随着土壤水分含量增加逐渐减少,抽穗扬花期烤田能明显增加根际土壤中总硫和有效硫含量,水稻对Cd的吸收与根际硫含量增加存在协同关系.上述结果证实,水稻对Cd的吸收不仅与Fe吸收有关,土壤中硫的充分供给能显著增加Cd在水稻中的积累.

关 键 词:酸性矿山废水      水稻  水分管理
收稿时间:2012/10/22 0:00:00
修稿时间:1/6/2013 12:00:00 AM

Accumulation of S, Fe and Cd in Rhizosphere of Rice and Their Uptake in Rice with Different Water Managements
ZHANG Xue-xi,ZHANG Xiao-xi,ZHENG Yu-ji,WANG Rong-ping,CHEN Neng-chang and LU Pu-xiang.Accumulation of S, Fe and Cd in Rhizosphere of Rice and Their Uptake in Rice with Different Water Managements[J].Chinese Journal of Environmental Science,2013,34(7):2837-2846.
Authors:ZHANG Xue-xi  ZHANG Xiao-xi  ZHENG Yu-ji  WANG Rong-ping  CHEN Neng-chang and LU Pu-xiang
Institution:Guangdong Institute of Eco-environmental and Soil Sciences, Guangzhou 510650, China;Guangdong Institute of Eco-environmental and Soil Sciences, Guangzhou 510650, China;Guangdong Institute of Eco-environmental and Soil Sciences, Guangzhou 510650, China;Guangdong Institute of Eco-environmental and Soil Sciences, Guangzhou 510650, China;Guangdong Institute of Eco-environmental and Soil Sciences, Guangzhou 510650, China;Guangdong Institute of Eco-environmental and Soil Sciences, Guangzhou 510650, China
Abstract:The interactions between the concentrations of sulfur, iron and cadmium in the rhizosphere and their uptakes in rice (Oryza sativa L.) were studied using paddy soil which was contaminated by acid mine drainage under five water-management treatments of 60%, 80%, 100% field moisture capacity (FMC), flooded throughout the entire rice growth period and flooded followed by keeping 80% FMC after heading-flowering period. The water managements had no significant influence on the Fe and Cd concentrations in rhizosphere soil in maturity stage, although the concentration of Cd slightly increased with the increase of soil moisture in the tillering stage. However, the uptake of Fe and Cd in rice was obviously related to water managements. The increase of soil moisture enhanced the uptake of Fe, but decreased the uptake of Cd in different organs of rice (roots, stems and leaves, grains) except for Cd uptake of the root in the 60% FMC treatment. However, aerobic treatment after heading-flowering period enhanced Cd uptake in rice in all treatments, but did not influence the uptake of Fe in rice. On the other hand, the increase of soil moisture reduced the concentrations of total sulfur and available sulfur in the rhizosphere soil except for the 60% FMC treatment, which corresponded with the reduction of Cd uptake in rice. And the aerobic treatment promoted Cd uptake in rice, which was also positively related to the increase of total sulfur and available sulfur in rhizosphere soil. Therefore, it was concluded that the uptake and speciation of sulfur in rhizosphere soil other than the change of Fe concentration induced by water management could play an important role in Cd uptake of rice.
Keywords:acid mine drainage  sulfur  cadmium  rice  water management
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