文献类型： 外文期刊

作者： Hao, Hongjian ¹ ; Wang, Rong ¹ ; Li, Shicai ¹ ; Pian, Duo ¹ ; Peng, Ning ³ ; Sailike, Ahejiang ¹ ; Yu, Zhouchang ¹ ; Shi, Jiayi ¹ ; Wang, Xingbo ¹ ; Wang, Zihan ¹ ; Zhang, Wei ¹ ;

作者机构： 1.Northwest A&F Univ, Coll Grassland Agr, Yangling 712100, Shaanxi, Peoples R China

2.Tibet Acad Agr & Anim Husb Sci, Inst Pratacultural Sci, Lhasa 850000, Peoples R China

3.Northwest A&F Univ, Coll Life Sci, Yangling 712100, Shaanxi, Peoples R China

4.Shaanxi Engn Res Ctr Circular Agr, Yangling 712100, Shaanxi, Peoples R China

关键词： Soil organic carbon; Plant residue; Microbial residue; Ratio of bacteria residue to fungal residue; Vegetation restoration

期刊名称：PLANT AND SOIL （ 影响因子：4.9； 五年影响因子：5.2 ）

ISSN： 0032-079X

年卷期： 2024 年

页码：

收录情况： SCI

摘要： AimsPlant and microbial residues are the primary drivers mediating soil organic carbon (SOC) accumulation in terrestrial ecosystems. However, how plant residues and microbial residues affect SOC accumulation and the underlying mechanisms remain poorly understood, especially in the succession process of different vegetation types.MethodsIn this study, grasslands (GL) and Robinia pseudoacacia plantations (RP) restored for 10, 20, 30, and 40 years were used as research subjects on the Loess Plateau, and farmland was used as a control. Several indicators of soil physicochemical and plant characteristics, enzyme activity, amino sugar, lignin phenols were measured.ResultsThe results indicated that the contents of microbial and plant residue carbon in GL and RP increased with the increasing restoration years. However, the contribution of plant residue carbon to the SOC in GL and RP gradually decreased, while microbial residue carbon showed the opposite trend. In contrast, microbial residues were the main contributor to SOC in GL (62.8-75.1%), while plant residues were the main contributor to SOC in RP (47.2-58.3%). There was a difference in the bacterial and fungal residue carbon contribution to SOC between GL and RP. In GL, the dominant contributor to SOC changed from bacterial (47.7-37.2%) to fungal residues (15.1-37.9%). But in RP, it has always been dominated by fungal residue carbon (17.4-33.3%).ConclusionsMore SOC accumulated in GL and RP in the form of microbial and plant residue carbon, respectively. In GL and RP, the contribution of carbon from fungal residues increased with the increase of recovery years. Overall, our research not only contributes to understanding the complexity of the carbon cycle in ecosystems, but also provides a valuable scientific basis for the management of soil carbon pools in different vegetation types under climate change.