4.7 Article

Effects of afforestation and upslope distance on soil moisture and organic carbon, and trade-off between them, on the Loess Plateau hillslopes

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CATENA
卷 235, 期 -, 页码 -

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DOI: 10.1016/j.catena.2023.107687

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Vegetation restoration; Soil water; Organic carbon; Hillslope depth profile; Trade-off analysis

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Large-scale afforestation on the Loess Plateau of China may lead to increased soil moisture deficit and SOC loss, especially in downslope areas. Natural grassland, on the other hand, exhibits low water depletion and high SOC sequestration. Therefore, a vegetation restoration strategy involving afforestation of downslope patches within a contiguous grassland matrix may be an effective approach.
Large-scale afforestation is considered controversial as an ecosystem renewal strategy for the Loess Plateau of China, since it may increase soil organic carbon (SOC) but may also exacerbate water shortages. In our study, we aimed to clarify how afforestation and slope affect soil moisture content (SMC) and SOC and their interaction particularly for deep hillslope profiles on long hillslopes, in terms of the trade-off between soil moisture and organic carbon. This study investigated SMC and SOC density (SOCD) from 0 to 400 cm hillslope depth profiles at 20 m intervals uphill to 100 m in the May and October (the beginning and end of the growing period, respec-tively) from 2015 to 2017. The three sampling sites were located in Robinia pseudoacacia plantation, natural forest, and natural grassland as the control. Soil moisture deficit and SOC sequestration of plantation were compared to those of grassland, and the trade-off between SMC and SOCD was evaluated. The results showed that SMC and SOCD were the lowest in the Robinia pseudoacacia plantation, indicating that the plantation exhibited a greater soil moisture deficit and SOC loss than the grassland. In the plantation and natural forestland, the subsoil (100-400 cm) exhibited greater soil moisture deficit and SOC loss than the soil (0-100 cm). SOCD increased while SMC decreased with upslope distance for all hillslope layers in both plantation and natural forestland. The downslope sites exhibited more severe soil moisture deficit, and greater SOC loss than the upslope sites. Natural grassland exhibited low water depletion and high SOC sequestration. Further, the downslope plantation sites exhibited the lowest root mean square deviation for the relationship between SMC and SOCD. Based on these findings, a vegetation restoration strategy involving afforestation of downslope patches within a contiguous grassland matrix may achieve high-level maintenance of ecosystem services. These findings provide a theoretical basis for vegetation restoration on the Loess Plateau.

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