Study on the Relationship Between the Release Characteristics of Organic Carbon from Litters and Soil Organic Carbon Pool in Tibetan Primitive Dark Coniferous Forest
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Study on the Relationship Between the Release Characteristics of Organic Carbon from Litters and Soil Organic Carbon Pool in Tibetan Primitive Dark Coniferous Forest
DUAN Fei, FANG Jiangping, ZHOU Chenni. Study on the Relationship Between the Release Characteristics of Organic Carbon from Litters and Soil Organic Carbon Pool in Tibetan Primitive Dark Coniferous Forest[J]. 2020, 34(3): 349-355.
DOI:
DUAN Fei, FANG Jiangping, ZHOU Chenni. Study on the Relationship Between the Release Characteristics of Organic Carbon from Litters and Soil Organic Carbon Pool in Tibetan Primitive Dark Coniferous Forest[J]. 2020, 34(3): 349-355. DOI: 10.13870/j.cnki.stbcxb.2020.03.050.
Study on the Relationship Between the Release Characteristics of Organic Carbon from Litters and Soil Organic Carbon Pool in Tibetan Primitive Dark Coniferous Forest
结合野外凋落物分解袋法和室内分析试验,对藏东南2种典型暗针叶林—急尖长苞冷杉(Abies georgei var. Smithii)和林芝云杉(Picea likiangensis var. linzhiensis)凋落物的分解和有机碳释放特征进行研究,分析了2种亚高山暗针叶林凋落物有机碳释放速率与土壤有机碳及其组分之间的关系。结果表明:藏东南2种原始暗针叶林凋落物分解均呈现出雨季分解快(4—9月)、旱季分解慢(10—翌年3月),前期分解快(3—9月)、后期分解慢(10—翌年2月)的特征,且冷杉(PLLF)分解速率大于云杉(AGSF),Olson指数衰减模型能够较好地模拟2种暗针叶林凋落物的分解,冷杉(PLLF)和云杉(AGSF)凋落物半分解时间为2.11,2.52年;分解95%时间为8.96,10.84年;2种暗针叶林凋落物中有机碳含量表现出先上升后下降,再平稳降低的趋势,而2种暗针叶林凋落物中有机碳释放速率表现出先短暂富集再释放的模式;2种暗针叶林土壤总有机碳(TOC)及其活性组分(MBC、POC、LOC)含量都具有明显的表聚性(p<0.01),且同一土壤层次内TOC、MBC、POC、LOC互相之间均呈极显著正相关关系(p<0.01);2种暗针叶林凋落物分解进程中有机碳的释放速率与表层土(0—10 cm)中TOC、MBC、POC、LOC含量、10—20 cm土层中的TOC、MBC含量以及20—40 cm土层中MBC含量之间呈现显著的正相关(p<0.05)。
Abstract
The decomposition and organic carbon release characteristics of litters of Abies georgei var. smithii and Picea likiangensis var. linzhiensis in two typical dark coniferous forests in southeastern Tibet were studied by combining the method of litter decomposition bag and laboratory analysis
the relationship between organic carbon release rate and soil organic carbon and its components in two subalpine dark coniferous forests was analyzed
the results showed that the decomposition of litters in the two original dark coniferous forests in southeastern Tibet showed the characteristics of fast decomposition in rainy season (April to September)
slow decomposition in dry season (October to march)
fast decomposition in early stage (march to September) and slow decomposition in late stage (October to February). The decomposition rate of fir (PLLF) was higher than that of spruce (AGSF). Olson exponential decay model could well model the decomposition of litter in two dark coniferous forests. The half-decomposition time of litter in fir (PLLF) and spruce (AGSF) were 2.11 and 2.52 years. The 95% of decomposition time were 8.96 and 10.84 years. The organic carbon content in the litters of the two dark coniferous forests showed a trend of first rising
then falling
and then steadily declining
while the release rate of organic carbon in the litters showed a pattern of first brief enrichment and then release. The contents of total organic carbon (TOC) and its active components (MBC
POC and LOC) in the soil of the two dark coniferous forests were obviously surficial (p<0.01)
and the contents of TOC
MBC
POC and LOC in the same soil layer were significantly positively correlated with each other (p<0.01). There was a significant positive correlation between the release rate of organic carbon in the decomposition process of litters of the two dark coniferous forests and the contents of TOC
MBC
POC and LOC in the topsoil (0-10 cm)
TOC and MBC in the soil layer of 10—20 cm and MBC in the soil layer of 20—40 cm (p<0.05).
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