1. 中央民族大学 生命与环境科学学院,北京,100081
2. 西藏农牧学院 高原生态研究所,西藏,林芝,860000
3. 西藏自治区生态安全联合实验室,西藏,林芝,860000
4. 西藏农牧学院 西藏高原森林生态教育部重点实验室,西藏,林芝,860000
纸质出版:2020
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代松家, 段斐, 方江平, 等. 不同生境条件下西藏原始冷杉林凋落物分解特征与土壤养分的关系[J]. 水土保持通报, 2020,40(3):56-63.
Dai Songjia, Duan Fei, Fang Jiangping, et al. Relationship Between Decomposition Characteristics of Litters and Soil Nutrients in Tibetan Fir Forest Under Different Habitat Conditions[J]. Bulletin of Soiland Water Conservation, 2020, 40(3): 56-63.
代松家, 段斐, 方江平, 等. 不同生境条件下西藏原始冷杉林凋落物分解特征与土壤养分的关系[J]. 水土保持通报, 2020,40(3):56-63. DOI: 10.13961/j.cnki.stbctb.2020.03.009.
Dai Songjia, Duan Fei, Fang Jiangping, et al. Relationship Between Decomposition Characteristics of Litters and Soil Nutrients in Tibetan Fir Forest Under Different Habitat Conditions[J]. Bulletin of Soiland Water Conservation, 2020, 40(3): 56-63. DOI: 10.13961/j.cnki.stbctb.2020.03.009.
[目的
]
研究不同生境条件下(林内、林外、林缘)藏东南急尖长苞冷杉林(Abies georgei var.smithii)凋落物分解特征与土壤养分特征之间的关系,为深入了解高寒高山森林生态系统物质循环过程提供依据。[方法
]
采用野外分解袋法和室内分析相结合,在林内、林外、林缘3种不同生境条件下对藏东南急尖长苞冷杉林凋落物进行了原位分解试验。[结果
]
分解速率总体上呈现出:林内 > 林缘 > 林外的特点,逐月分解率的变异系数表现为:林内(34.83%)
<
林缘(57.35%)
<
林外(72.09%);Olson指数衰减模型的模拟结果显示不同生境条件下(林内、林缘、林外)凋落物分解50%需要的时间为2.11,2.52,2.34 a,分解95%需要的时间为8.96,10.01,10.84 a;3种不同生境土壤养分在空间上差异显著,林内生境中与凋落物分解速率呈现极显著相关的土壤养分因子有土壤总有机碳(TOC)含量、N含量、土壤微生物量碳(SMBC)含量、土壤微生物量氮(SMBN)含量以及W
C
:W
N
值;林外、林缘生境中与凋落物分解速率相关性最大的为土壤TOC含量,其次为W
C
:W
N
值。[结论
]
生境条件的差异对凋落物分解速率有显著影响,在不同的生境条件下对凋落物分解影响起主导作用的土壤养分因素不同,凋落物—土壤生物地化循环紧密联系,相互作用关系复杂,生境作用效应突出。
[Objective] The relationship between litter decomposition characteristics and soil nutrient characteristics of Abies georgei var. smithii forest in Southeastern Tibet under different habitat conditions
i.e.
in forest (IF)
outside forest (OF)
and beside forest (BF) was studied to provide basic data for further understanding the material circulation process of the alpine forest ecosystem.[Methods] Based on field decomposition bag method and indoor analysis
in situ decomposition experiments were conducted on A. georgei forest litters in Southeast Tibet under three different habitats.[Results] The decomposition rate showed the characteristics of IF > BF > OF
and the variation coefficient of the monthly decomposition rate represented the characteristics of IF (34.83%) < BF(57.35%) < OF (72.09%). According to the simulation results of the Olson exponential decay model
the decomposition times of litters in different habitat conditions (IF
BF
and OF) were 2.11
2.52
and 2.34 years
respectively
and 95% of decomposition times were 8.96
10.01
and 10.84 years
respectively. Soil nutrients in the three different habitats were significantly different in space. The soil nutrient factors in the forest habitats with significant correlation with the litter decomposition rate were soil total organic carbon (TOC) content
N content
soil microbial biomass carbon content
soil microbial biomass nitrogen content
and WC:WN value. The soil TOC content was maximum correlated with the decomposition rate of litter in the habitats outside and at forest margins
followed by WC:WN value.[Conclusion] The difference of habitat conditions had a significant impact on the decomposition rate and nutrient release rate of litters
and different soil nutrient factors played a leading role in the decomposition of litters under different habitat conditions. The litter-soil biogeochemical cycle was closely related to complex interaction and a prominent habitat effect.
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