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生态学杂志 ›› 2021, Vol. 40 ›› Issue (7): 2076-2084.doi: 10.13292/j.1000-4890.202107.021

• 研究报告 • 上一篇    下一篇

模拟氮沉降与外源养分和碳源耦合对杉木林土壤碳氮转化的后期影响

郑琪1,2,王小东1,2,3,卜文圣1,2,刘斌1,2,袁平成2,幸娇萍1,2*,陈伏生1,2   

  1. (1鄱阳湖流域森林生态系统保护与修复国家林业和草原局重点实验室, 江西农业大学, 南昌 330045;2江西农业大学林学院, 南昌 330045; 3江西省林业科学院, 南昌 330032)
  • 出版日期:2021-07-10 发布日期:2021-07-12

Effects of nitrogen deposition and its coupling with exogenous nutrients and carbon sources on soil carbon and nitrogen transformation in Cunninghamia lanceolata plantations at the later stage of treatments.

ZHENG Qi1,2, WANG Xiao-dong1,2,3, BU Wen-sheng1,2, LIU Bin1,2, YUAN Ping-cheng2, XING Jiao-ping1,2*, CHEN Fu-sheng1,2   

  1. (1Key Laboratory of State Forestry and Grassland Administration on Forest Ecosystem Protection and Restoration of Poyang Lake Watershed, Nanchang 330045, China; 2College of Forestry, Jiangxi Agricultural University, Nanchang 330045, China; 3Jiangxi Academy of Forestry, Nanchang 330032, China).
  • Online:2021-07-10 Published:2021-07-12

摘要: 氮沉降、磷等养分供应和碳输入影响森林土壤有机碳的稳定性。本研究以丘陵山区杉木人工林表层土壤为对象,研究氮沉降与外源养分和碳源耦合对其有机碳矿化和矿质氮释放的后期影响,分别对土壤做以下条件处理:未做处理(CK)、单独添加外源氮\[N\]、添加外源氮和碳源\[N+C\]、外源氮和非氮养分添加\[N+nutrient\]、外源氮、非氮养分和碳源等混合添加\[N+both\]。结果表明:在土壤培养720 d期间,不同处理土壤有机碳矿化积累量随着培养时间的增加呈上升趋势,而矿化速率则逐渐下降;施加360 d后,各组土壤中NH4+-N、NO3--N和矿质氮含量均高于CK,且彼此之间无差异;施加720 d后,各组土壤中NH4+-N含量均高于CK,但无明显差异;土壤中NO3--N和矿质氮含量均高于CK,且\[N\]处理最高,\[N+nutrient\]、\[N+both\]处理次之,最低是\[N+C\]处理;720 d时土壤中β葡萄糖苷酶活性依次为\[N+both\]、\[N+C\]、CK和\[N\]处理;土壤中N-乙酰-葡萄胺糖苷酶活性为\[N+both\]处理显著高于其他处理;土壤中酸性磷酸酶活性为\[N+both\]、\[N+C\]处理显著高于\[N\]处理和CK。在氮沉降背景下,碳和非氮养分的长时间输入将影响土壤有机碳分解,从而减弱森林土壤碳汇功能。

关键词: 杉木, 氮沉降, 有机碳稳定性, 酶活性

Abstract: Nutrients supply and carbon input affect the stability of soil organic carbon in forests. In this study, we examined the effects of nitrogen deposition, coupling exogenous nutrients and carbon sources on soil organic carbon mineralization and mineral nitrogen release in a Chinese fir (Cunninghamia lanceolata) plantation in hilly mountainous area at the later stage of the treatments. Soils were treated with following conditions: no addition (CK); N addition alone \[N\]; N and carbon additions \[N+C\]; N and non-N nutrient additions \[N+nutrient\]; N, non-N nutrients and carbon additions \[N+both\]. The results showed that the total mineralization of soil organic carbon under different treatments increased with time extension during 720 days incubation, while the mineralization rate gradually decreased. After 360 days incubation, the contents of soil NH4+-N, NO3--N, and mineral nitrogen under all the treatments were higher than those under CK. After 720 days incubation, the contents of NO3--N and mineral nitrogen were the highest under the \[N\] treatment, followed by the treatments \[N+nutrient\], \[N+both\], and \[N+C\]. The activity of β-glucosidase was the highest under the \[N+both\] treatment, followed by \[N+C\], CK, and \[N\]. The activity of β-N-acetyl-glucosaminidase was the highest under the \[N+both\] treatment. The activity of acid phosphatase was higher under the treatment of \[N+both\] and \[N+C\] than that under the \[N\] treatment and CK. Under the background of nitrogen deposition, long-term input of non-nitrogen nutrient and carbon into soils will promote soil organic carbon decomposition and thus weaken soil carbon sequestration in forests.

Key words: Cunninghamia lanceolata, nitrogen deposition, organic carbon stability, enzyme activity.