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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

机译:黄土高原坡地退耕还林对陆地生态系统碳动态的影响模拟-以陕西省安塞县为例

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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 Cm~(-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.
机译:倾斜土地转化计划(SLCP)于1999年在中国黄土高原启动,旨在减少水土流失和水土流失,是近几十年来世界上最大的生态修复项目。这项巨大的努力显着改善了植被状况,并有望具有增强陆地碳(C)固存的巨大潜力。但是,在区域范围内,SLCP的空间显式C后果仍是未知之数。我们以黄土高原的安塞县为例,基于通用整体生物地球化学模型系统(GEMS)评估了SLCP对生态系统C动力学的影响。结果表明,SLCP实施后的前五年(即1999-2003年),由于新林地产量低,生态系统碳储量(包括储存在生物质和土壤中的碳)略有减少,并且明显增加(主要是生物质)之后,这主要归功于年轻人工林的生长。总体而言,在过去的三十年中,研究区域一直是净碳汇,但SLCP极大地放大了该区域,2004-2010年的碳汇表明,该面积几乎是1978-1998年的十二倍(41.5对3.5 g Cm〜(-2)yr〜(-1))。这些结果凸显了SLCP在促进陆地碳固存中的重要性,这可能有助于缓解气候变化。然而,在生态恢复地区,特别是在土壤中,短链氯化石蜡的影响和相关的碳动态之间存在时滞,这要求未来为解决短链氯化石蜡的长期碳后果做出努力。

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