Modeling the effects of the Sloping Land Conversion Program on terrestrial ecosystem carbon dynamics in the Loess Plateau: A case study with Ansai County, Shaanxi province, China

被引:17
作者
Zhou, Decheng [1 ,2 ]
Zhao, Shuqing [1 ,2 ]
Liu, Shuguang [3 ,4 ]
Zhang, Liangxia [5 ]
机构
[1] Peking Univ, Coll Urban & Environm Sci, Beijing 100871, Peoples R China
[2] Peking Univ, Minist Educ, Key Lab Earth Surface Proc, Beijing 100871, Peoples R China
[3] Natl Engn Lab Forest Ecol & Appl Technol Southern, Changsha 410004, Hunan, Peoples R China
[4] Cent South Univ Forest & Technol, Changsha 410004, Hunan, Peoples R China
[5] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
基金
中国国家自然科学基金; 湖南省自然科学基金;
关键词
Ecological restoration; Land use/cover change (LUCC); Carbon stocks; Carbon sequestration; General Ensemble Biogeochemical Modeling System (GEMS); SOIL ORGANIC-CARBON; NET PRIMARY PRODUCTIVITY; CLIMATE-CHANGE; GREEN PROJECT; CYCLE; MANAGEMENT; STORAGE; SEQUESTRATION; AFFORESTATION; CONSEQUENCES;
D O I
10.1016/j.ecolmodel.2014.05.016
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The Sloping Land Conversion Program (SLCP), preferentially initiated to reduce water loss and soil erosion in the Loess Plateau of China in 1999, is the largest eco-restoration project in the world in recent decades. This massive effort improved the vegetation conditions markedly and was expected to have a great potential to enhance terrestrial carbon (C) sequestration. However, the spatially-explicit C consequences of the SLCP remain largely unknown at the regional scale. Using Ansai County in the Loess Plateau as a case study, we assessed the impacts of the SLCP on ecosystem C dynamics based on the General Ensemble Biogeochemical Modeling System (GEMS). The results showed that ecosystem C stock (including C stored in biomass and soil) decreased slightly in the first five years after the implementation of the SLCP (i.e., 1999-2003) due to the low production of the newly forested land, and increased evidently (mostly in biomass) thereafter thanks primarily to the growth of young plantations. Overall, the study area functioned as a net C sink in the past three decades, yet the magnitude was greatly amplified by the SLCP, indicated by a C sink in 2004-2010 nearly twelve times that in 1978-1998(41.5 vs. 3.5 g C m(-2) yr(-1)). These results highlight the importance of the SLCP in promoting terrestrial C sequestration which may help mitigate climate change. Nevertheless, there were time-lags between the impact of the SLCP and the associated C dynamics in the eco-restored areas, particularly in the soil, calling for future efforts toward addressing long-term C consequences of the SLCP. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:47 / 54
页数:8
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