两种不同土壤对水稻镉吸收及其动态积累特征的影响

Effects of Two Different Paddy Soils on Cd Uptake and Dynamic Accumulation Characteristics of Rice

  • 摘要:
      目的  探究水稻在不同土壤上的镉吸收转运动态特征。
      方法  选择我国轻中度镉超标水稻土红砂泥(普通铁聚水耕人为土)和油泥土(普通铁渗水耕人为土),采用盆栽试验种植水稻,分别在水稻幼苗期、分蘖中期、孕穗中期和成熟期分析不同器官镉累积的动态特征。
      结果  水稻种植前油泥土CaCl2提取态镉浓度(0.02 mg kg−1)比红砂泥(0.15 mg kg−1)低86.7%,导致苗期至分蘖中期油泥土水稻植株体内镉的平均累积速率(0.09 μg plant−1 d−1)比红砂泥(0.32 μg plant−1 d−1)低71.9% ,但分蘖中期至孕穗中期油泥土水稻植株体内镉平均累积速率(0.038 μg plant−1 d−1)比红砂泥(0.073 μg plant−1 d−1)低47.9%,表明分蘖中期之前是土壤类型影响水稻植株体内镉积累的关键期。到了成熟期,由于红砂泥上水稻植株体内镉向糙米的分配比率(11.0%)低于油泥土(16.6%),加之两种土壤上成熟期水稻植株体内镉累积量均下降,且红砂泥上水稻植株体内镉累积量下降率(28.9%)高于油泥土(18.2%)。油泥土水稻糙米镉累积量比红砂泥低44.4%。
      结论  土壤差异除了通过影响土壤有效态镉浓度而影响水稻对镉的吸收外,也通过影响水稻植株体内镉的转运过程,进一步影响糙米镉含量。

     

    Abstract:
      Objective  The aims were to study the dynamic uptake and transport characteristics of cadmium (Cd) within rice in different soils.
      Method  Slightly to moderately Cd-contaminated paddy soils including reddish sandy soil (Typic Fe-accumulic-Stagnic Anthrosols) and slurry soil (Typic Fe-leachi-Stagnic Anthrosols) in China were selected to plant rice through a pot experiment. Rice plants were sampled respectively at the seedling, mid-tillering, mid-booting, and mature stages for the determination of Cd accumulation in different tissues.
      Result  The results showed that the CaCl2-extractable Cd concentration (0.02 mg kg−1) in the slurry soil was 86.7% lower than that in the reddish sandy soil (0.15 mg kg−1). Thus, the average accumulation rate of Cd in the slurry soil (0.09 μg plant−1 d−1) during the seedling to mid-tillering period was 71.9% lower than that in the reddish sandy soil (0.32 μg plant−1 d−1), while the average accumulation rate of Cd in the slurry soil (0.038 μg plant−1 d−1) was 47.9% lower than that in the reddish sandy soil (0.073 μg plant−1 d−1) during the mid-tillering to booting period, indicating the seedling to mid-tillering stage was the key period for soil types to affect Cd accumulation in rice. At the mature stage, the distribution rate of Cd in brown rice in the reddish sandy soil (11.0%) was lower than that in the slurry soil (16.6%). Furthermore, the Cd amounts in mature rice were reduced in both two soils, and the reduction rate in the red sandy soil (28.9%) was higher than that in the slurry soil (18.2%). As a result, Cd amount of brown rice in the slurry soil was 44.4% lower than that in the reddish sandy soil.
      Conclusion  This study indicates that soil differences influence not only the Cd availability in soil and uptake by rice but also the transport of Cd within rice plant, and further regulate Cd concentration in brown rice.

     

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