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    张恒, 王晶君, 孟琳, 夏海乾, 石俊雄. 贵州省典型植烟土壤氮素矿化研究[J]. 中国烟草科学, 2013, 34(3): 1-5. DOI: 10.3969/j.issn.1007-5119.2013.03.001
    引用本文: 张恒, 王晶君, 孟琳, 夏海乾, 石俊雄. 贵州省典型植烟土壤氮素矿化研究[J]. 中国烟草科学, 2013, 34(3): 1-5. DOI: 10.3969/j.issn.1007-5119.2013.03.001
    ZHANG Heng, WANG Jingjun, MENG Lin, XIA Haiqian, SHI Junxiong. Nitrogen Mineralization of Typical Tobacco-growing Soils in Guizhou Province[J]. CHINESE TOBACCO SCIENCE, 2013, 34(3): 1-5. DOI: 10.3969/j.issn.1007-5119.2013.03.001
    Citation: ZHANG Heng, WANG Jingjun, MENG Lin, XIA Haiqian, SHI Junxiong. Nitrogen Mineralization of Typical Tobacco-growing Soils in Guizhou Province[J]. CHINESE TOBACCO SCIENCE, 2013, 34(3): 1-5. DOI: 10.3969/j.issn.1007-5119.2013.03.001

    贵州省典型植烟土壤氮素矿化研究

    Nitrogen Mineralization of Typical Tobacco-growing Soils in Guizhou Province

    • 摘要: 为明确贵州省典型植烟土壤的氮素矿化规律,以贵州省典型植烟土壤黄壤、石灰土、紫色土为研究对象,采用Stanford长期好气间歇淋洗培养法,研究了其土壤氮素矿化过程。结果表明,在好气性培养过程中,贵州省典型植烟土壤氮素矿化速率出现快速下降—缓慢下降—趋于稳定的变化过程,矿化速率表现为石灰土>黄壤>紫色土。土壤矿化氮累积量随着培养时间的推进而增加,矿化氮累积量表现为石灰土>黄壤>紫色土。矿化氮累积主要集中在培养的0~63 d,占总矿化氮累积量的78.42%~83.36%。土壤矿化氮量与土壤有机质含量存在显著或极显著的正相关关系,并能与培养时间通过多元回归的方法建立不同类型典型植烟土壤的矿化氮累积量预测模型。

       

      Abstract: In order to investigate the organic nitrogen mineralization of tobacco-growing soils, three typical tobacco-growing soils: Yellow soil, Calcareous soil and Purple soil were chosen to measure the nitrogen mineralization by using the Stanford aerobic incubation method. The results indicated that the soil mineralization rate showed a tendency to decrease significantly, decrease gently and tend to be stable under aerobic condition. The average mineralization rate was Calcareous soil > Yellow soil > Purple soil. The accumulation of the soil mineralizable N increased slowly with the incubation time under aerobic condition. The tendency of the accumulation of the mineralizable N was similar with that of the soil mineralization rate. The accumulation of the mineralizable N increased rapidly from 0 to 63 days, accounting for about 78.42%~83.36% of the total accumulation of the mineralizable N. The accumulation of the mineralizable N was positively correlated with soil organic matter content. Prediction models of the accumulation of the mineralizable N in different typical tobacco-growing soils were also constructed by using soil mineralizable N content, organic matter content, and incubation time.

       

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