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不同林龄杉木人工林土壤氮转化酶活性特征

Soil Enzyme Activity Related to Nitrogen Cycling in Chinese Fir (Cunninghamia lanceolata) Plantation with Different Stand Age

  • 摘要:
    目的 探讨土壤氮转化酶活性及根际效应随杉木生长发育的变化特征,为杉木人工林的施肥管理和可持续经营提供科学依据。
    方法 以不同发育阶段杉木人工林(7、15、24、34 a)为研究对象,测定根际与非根际土壤氮转化酶活性(β-葡萄糖苷酶(BG)、乙酰-β-D-氨基葡萄糖苷酶(NAG)、蛋白水解酶(PRO)、脲酶(URE)、亮氨酸氨基肽酶(LAP)、硝酸还原酶(NR)),探讨不同发育阶段杉木人工林土壤氮转化酶活性、根际效应及其与土壤理化性质的关系。
    结果 林龄和根际对6种土壤氮转化酶活性影响均存在显著差异(p<0.05);杉木林根际和非根际土壤氮转化酶活性均随林龄增加先下降后上升,不同林龄杉木根际土壤BG、NAG、PRO、URE和LAP活性均显著高于非根际土壤(p<0.05),根际与非根际土壤的NR活性差异因林龄而异,15 a和24 a杉木林根际土壤的NR活性极显著高于非根际土壤的(p<0.01),而7 a和34 a杉木林根际与非根际土壤的NR活性差异不显著(p>0.05)。15 a杉木林土壤NR活性的根际效应显著高于7 a和34 a杉木林(p<0.05)。杉木根际与非根际土壤酶活性的关键因素是碳氮比与铵态氮含量。
    结论 中亚热带杉木人工林在中龄林阶段土壤氮转化酶活性最低,说明在受氮沉降影响严重的中亚热带地区,氮仍可能是杉木速生期的主要限制因素之一,在今后的营林施肥措施上,应把重点放在中龄林阶段,以满足杉木对氮的需求,达到可持续经营管理的目的。

     

    Abstract:
    Objective To study the variation of soil nitrogen (N)-cycling enzyme activities and rhizosphere effect during the development of Chinese fir (Cunninghamia lanceolata) plantation and its driving factors.
    Method Rhizosphere and non-rhizosphere soils were collected from Chinese fir plantation with the ages of 7, 15, 24 and 34. The enzyme activities regulating soil nitrogen cycling (β-glucosidase (BG), acetyl-β-D-glucosaminidase (NAG), proteolytic enzyme (PRO), urease (URE), leucine aminopeptidase (LAP) and nitrate reductase (NR)) were measured. Redundancy analysis (RDA) and Pearson correlation were conducted to explore the relationship between soil nitrogen-cycling enzyme activities and the soil physico-chemical properties.
    Result Forest age and rhizosphere had significant effects on soil N-cycling enzyme activities (P<0.05). The enzyme activities regulating soil nitrogen cycling in the non-rhizosphere soil decreased at first and then increased with the increase of forest age. The activities of BG, NAG, PRO, URE and LAP in rhizosphere soil were significantly higher than those in non-rhizosphere soil (P<0.05). The difference of NR activity between rhizosphere and non-rhizosphere soil varied with forest age. The NR activity in rhizosphere soil was significantly higher than that of non-rhizosphere soil in 15- and 24-years-old Chinese fir plantations (P<0.01). The rhizosphere effects of soil NR activities in 15-years-old Chinese fir plantation were significantly higher than those in 7-years-old and 34-years-old Chinese fir plantations (P<0.05). The key factors regulating soil N-cycling enzyme activities in rhizosphere and non-rhizosphere soil were C/N and ammonium nitrogen content.
    Conclusion Soil N-cycling enzyme activities was the lowest in middle-age Chinese fir plantations in mid-subtropical China, indicating that nitrogen may still be one of the main limiting factors in the fast-growing stage of Chinese fir plantations. In the future, we should focus on the middle-age Chinese fir plantation, so as to meet the nitrogen demand of Chinese fir and achieve the purpose of sustainable management.

     

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