The Contributions of Soil Fauna to the Accumulation of Humic Substances during Litter Humification in Cold Forests

被引:6
|
作者
Tan, Yu [1 ]
Yang, Kaijun [2 ,3 ]
Xu, Zhenfeng [1 ]
Zhang, Li [1 ]
Li, Han [1 ]
You, Chengming [1 ]
Tan, Bo [1 ]
机构
[1] Sichuan Agr Univ, Inst Ecol & Forestry, Coll Forestry, Forestry Ecol Engn Upper Reaches Yangtze River Ke, 211,Huimin Rd, Chengdu 611130, Peoples R China
[2] UAB, Global Ecol Unit, CSIC, CREAF, Catalonia 08913, Spain
[3] CREAF, Cerdanyola del Valles 08913, Catalonia, Spain
来源
FORESTS | 2022年 / 13卷 / 08期
基金
中国国家自然科学基金;
关键词
soil fauna; humic substances; humic acid; fulvic acid; humification degree; OPTICAL-PROPERTIES; CLIMATE-CHANGE; HUMUS FORMS; ACID-LIKE; DIVERSITY; MINERALIZATION; DECOMPOSITION; COMMUNITIES; TEMPERATURE; FEEDBACKS;
D O I
10.3390/f13081235
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
Litter humification is an essential process of soil carbon sequestration in forest ecosystems, but the relationship between soil fauna and humic substances has not been well understood. Therefore, a field litterbag experiment with manipulation of soil fauna was carried out in different soil frozen seasons over one year in cold forests. The foliar litter of four dominated tree species was selected as Birch (Betula albosinensis), Fir (Abies fargesii var. faxoniana), Willow (Salix paraplesia), and Cypress (Juniperus saltuaria). We studied the contribution of soil fauna to the accumulation of humic substances (including humic acid and fulvic acid) and humification degree as litter humification proceeding. The results showed that soil fauna with litter property and environmental factor jointly determined the accumulation of humic substances (humic acid and fulvic acid) and humification degree of four litters. After one year of incubation, the contribution rates of soil fauna to the accumulation of humic substances were 109.06%, 71.48%, 11.22%, and -44.43% for the litter of fir, cypress, birch, and willow, respectively. Compared with other stages, both growing season and leaf falling stage could be favorable to the contributions of soil fauna to the accumulation of humic substances in the litter of birch, fir, and cypress rather than in willow litter. In contrast, the contribution rates of soil fauna to humification degree were -49.20%, -7.63%, -13.27%, and 12.66% for the litter of fir, cypress, birch, and willow, respectively. Statistical analysis indicated that temperature changes at different sampling stages and litter quality exhibited dominant roles in the contributions of soil fauna on the accumulation of humus and litter humifiaction degree in the cold forests. Overall, the present results highlight that soil fauna could play vital roles in the process of litter humification and those strengths varied among species and seasons.
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收藏
页数:14
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