Responses of soil labile organic carbon and water-stable aggregates to reforestation in southern subtropical China

被引:10
作者
Chen, Yuanqi [1 ,2 ]
Zhang, Yu [3 ]
Yu, Shiqin [2 ]
Li, Feng [2 ]
Liu, Suping [2 ]
Zhou, Lixia [2 ]
Fu, Shenglei [4 ]
机构
[1] Hunan Univ Sci & Technol, Hunan Prov Key Lab Coal Resources Clean Utilizat, Xiangtan 411201, Hunan, Peoples R China
[2] Chinese Acad Sci, Key Lab Vegetat Restorat & Management Degraded Ec, South China Bot Garden, Guangzhou 510650, Guangdong, Peoples R China
[3] Hunan Univ Sci & Technol, Sch Life Sci, Hunan Prov Key Lab Econ Crops Genet Improvement &, Xiangtan 411201, Hunan, Peoples R China
[4] Henan Univ, Coll Environm & Planning, Key Lab Geospatial Technol Middle & Lower Yellow, Minist Educ, Kaifeng 475004, Henan, Peoples R China
基金
中国国家自然科学基金;
关键词
reforestation; carbon stability; forest type; soil aggregate; carbon fraction; VEGETATION RESTORATION; CLIMATE-CHANGE; STAND AGE; FRACTIONS; FOREST; PLANTATION; STABILITY; DYNAMICS; MATTER; BIOMASS;
D O I
10.1093/jpe/rtaa087
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Aims Reforestation can enhance soil carbon (C) stability and promote soil C accumulation. Experimental results are, however, highly variable, and the efficacy of reforestation in enhancing soil C stability is still in debate. Consequently, it remains unclear how the different soil C pools respond to reforestation in forest ecosystems. Methods The response of different soil C fractions to reforestation was examined in five subtropical forests, including the plantations of Eucalyptus urophylla (EU), Acacia crassicarpa (AC), Castanopsis hystrix (CH) and 10 species mixed (MX), and a naturally recovered shrubland (NS). Soil labile C fractions (readily oxidized organic C by KMnO4: ROC; dissolved organic C: DOC), distribution of aggregate-size classes and aggregate-associated C from different soil layers (0-10, 10-20, 20-40 and 40-60 cm) were evaluated. Important Findings We found that reforestation and forest type did not affect ROC concentration, yet the highest DOC concentration was detected in NS at four soil layers. Aggregate C concentration was the highest in all aggregate-size classes of CH at 0-10 cm depth. In addition, forest type did not alter the proportion of soil water-stable aggregates at four soil layers. However, soil depths significantly affected the distribution of soil aggregates with >0.25 mm aggregates dominating in the topsoils (0-20 cm), but 0.053-2 mm aggregates being dominant in the deep soils (20-60 cm). These results indicate that reforestation and forest type affected soil DOC (0-60 cm) and aggregate C (0-10 cm). Furthermore, soil DOC and aggregate C were more susceptive to reforestation than ROC. The findings suggest that plantations reduce soil DOC concentration, highlighting that C leaching loss may decrease compared with natural recovery. Moreover, C. hystrix plantation may enhance soil C stability by physical protection in topsoil. This study provides valuable information on tree species selection for reforestation concerning soil C sequestration in southern subtropical China.
引用
收藏
页码:191 / 201
页数:11
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