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生态学杂志 ›› 2020, Vol. 39 ›› Issue (9): 2842-2850.doi: 10.13292/j.1000-4890.202009.016

• 研究报告 • 上一篇    下一篇

氮添加和升温对杉木林凋落物分解及碳氮磷化学计量特征的影响

王书丽1,黄立君1,袁希1,王建伟1,刘少敏1,方向民1,胡小飞2,郭晓敏1,张令1*   

  1. (1江西农业大学林学院, 江西省森林培育重点实验室, 南昌 330045;2南昌大学管理学院, 南昌 330031)
  • 出版日期:2020-09-10 发布日期:2021-03-10

Effects of nitrogen addition and warming on litter decomposition and C, N and P stoichiometric characteristics of Chinese fir.

WANG Shu-li1, HUANG Li-jun1, YUAN Xi1, WANG Jian-wei1, LIU Shao-min1, FANG Xiang-min1, HU Xiao-fei2, GUO Xiao-min1, ZHANG Ling1*   

  1.  (1College of Forestry, Jiangxi Agricultural University, Jiangxi Key Laboratory of Silviculture, Nanchang 330045, China; 2School of Management, Nanchang University, Nanchang 330031, China)
  • Online:2020-09-10 Published:2021-03-10

摘要: 通过研究氮(N)添加和升温对杉木林凋落物分解过程中碳(C)、N、磷(P)化学计量特征的影响,探索杉木林养分周转规律。利用江西千烟洲亚热带杉木(Cunninghamia lanceolata)人工林长期野外N添加(CK(0)、N1(50 kg N·hm-2·a-1)、N2(100 kg N·hm-2·a-1))控制试验平台,采集不同年龄杉木凋落物(一年生叶和二年生叶),在不同温度(20、30 ℃)条件下进行凋落物分解培养试验。结果表明:凋落物分解过程中,N添加对杉木凋落物C含量没有影响;N添加显著提高了分解过程中不同年龄凋落物的N含量,降低了凋落物P含量。相同N添加水平下,凋落物N、P含量表现为一年生叶>二年生叶。N添加对分解前期不同年龄凋落物的P含量表现为N2>N1>CK,分解后期凋落物P含量则与分解前期相反。N添加显著降低了凋落物C∶N,提高了凋落物C∶P、N∶P。在分解过程中,相同N水平下杉木凋落物C∶N、C∶P表现为二年生叶>一年生叶,N∶P趋势相反。分解过程中,温度升高显著提高C∶N、C∶P。相同温度下,不同年龄凋落物的C∶N表现为一年生叶>二年生叶。N∶P随温度升高而增大,不同年龄叶片的N∶P表现为一年生叶>二年生叶。在杉木林经营管理中,应考虑不同年龄凋落物分解、N添加和温度作用对土壤碳氮循环的影响。

关键词: 生态化学计量, 叶龄, 杉木, 养分周转

Abstract: Using an incubation experiment, we examined the effects of nitrogen (N) addition and warming on litter decomposition and carbon (C), nitrogen (N), and phosphorus (P) stoichiometric characteristics of Chinese fir (Cunninghamia lanceolata) leaves with different ages. We collected litter from a longterm N addition \[CK (0), N1 (50 kg N·hm-2·a-1), N2 (100 kg N·hm-2·a-1)\] experiment in subtropical Chinese fir plantation, Qianyanzhou, Jiangxi, China. Litters from one and two-year-old leaves of Chinese fir were used for incubation under two temperatures (20 and 30 ℃). The results showed that N addition did not affect C concentrations of decomposing Chinese fir litter, while significantly increased N concentrations and decreased P concentrations. Both N and P concentrations of decomposing litter were higher in one-year-old leaf than that in two-year-old leaf. In the early decomposition stage, litter P concentrations was higher with N2 than that with N1 or CK. Nitrogen addition significantly reduced litter C∶N ratio and increased litter C∶P and N∶P ratios. During decomposition, litter C∶N and C∶P ratios under the same N addition level were higher in two-year-old leaf than that in oneyearold leaf, while N∶P ratio showed the opposite trend. Litter C∶N and C∶P ratios were significantly increased with warming during litter decomposition. Under the same temperature, C∶N ratio was higher in one-year-old leaf than that in two-year-old leaf. Litter N∶P ratio increased with incubation temperature and was higher in one-year-old leaf than two-year-old leaf. Our results suggested that the effects of litter decomposition with different leaf ages, N input, and temperature on soil C and N cycling should be considered in the management of Chinese fir forests.

Key words: ecological stoichiometry, leaf age, Cunninghamia lanceolata, nutrient turnover.