首页> 美国卫生研究院文献>International Journal of Environmental Research and Public Health >Effects of Revegetation on Soil Organic Carbon Storage and Erosion-Induced Carbon Loss under Extreme Rainstorms in the Hill and Gully Region of the Loess Plateau
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Effects of Revegetation on Soil Organic Carbon Storage and Erosion-Induced Carbon Loss under Extreme Rainstorms in the Hill and Gully Region of the Loess Plateau

机译:黄土高原丘陵沟壑区极端暴雨条件下植被恢复对土壤有机碳存储和侵蚀诱导碳损失的影响

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摘要

Background: The Loess Plateau, an ecologically vulnerable region, has long been suffering from serious soil erosion. Revegetation has been implemented to control soil erosion and improve ecosystems in the Loess Plateau region through a series of ecological recovery programs. However, the increasing atmospheric CO2 as a result of human intervention is affecting the climate by global warming, resulting in the greater frequency and intensity of extreme weather events, such as storms that may weaken the effectiveness of revegetation and cause severe soil erosion. Most research to date has evaluated the effectiveness of revegetation on soil properties and soil erosion of different land use or vegetation types. Here, we study the effect of revegetation on soil organic carbon (SOC) storage and erosion-induced carbon loss related to different plant communities, particularly under extreme rainstorm events. Materials and methods: The erosion-pin method was used to quantify soil erosion, and soil samples were taken at soil depths of 0–5 cm, 5–10 cm and 10–20 cm to determine the SOC content for 13 typical hillside revegetation communities in the year of 2013, which had the highest rainfall with broad range, long duration and high intensity since 1945, in the Yanhe watershed. Results and discussion: The SOC concentrations of all plant communities increased with soil depth when compared with slope cropland, and significant increases (p < 0.05) were observed for most shrub and forest communities, particularly for natural ones. Taking the natural secondary forest community as reference (i.e., soil loss and SOC loss were both 1.0), the relative soil loss and SOC loss of the other 12 plant communities in 2013 ranged from 1.5 to 9.4 and 0.30 to 1.73, respectively. Natural shrub and forest communities showed greater resistance to rainstorm erosion than grassland communities. The natural grassland communities with lower SOC content produced lower SOC loss even with higher soil loss, natural secondary forest communities produced higher SOC loss, primarily because of their higher SOC content, and the artificial R. pseudoacacia community with greater soil loss produced higher SOC loss. Conclusions: These results indicate that natural revegetation is more effective in enhancing SOC storage and reducing soil erosion than artificial vegetative recovery on hillsides. However, natural secondary forest communities, with higher SOC content and storage capacity, may also contribute to larger SOC loss under extreme rainstorms.
机译:背景:黄土高原是生态脆弱的地区,长期以来一直遭受严重的土壤侵蚀。通过一系列生态恢复计划,在黄土高原地区进行了植被恢复,以控制土壤侵蚀和改善生态系统。但是,由于人为干预而导致的大气中二氧化碳的增加正在通过全球变暖影响气候,导致极端天气事件(例如风暴)的发生频率和强度增加,而风暴可能削弱植被恢复的效力并导致严重的土壤侵蚀。迄今为止,大多数研究已经评估了植被恢复对不同土地利用或植被类型的土壤特性和土壤侵蚀的有效性。在这里,我们研究植被恢复对土壤有机碳(SOC)存储和与侵蚀相关的碳损失的影响,这些碳损失与不同植物群落有关,尤其是在极端暴雨事件下。材料和方法:采用侵蚀针法定量土壤侵蚀,并在0–5 cm,5–10 cm和10–20 cm的土壤深度采集土壤样品,以确定13个典型的山坡植被群落的SOC含量。自1945年以来,延河流域的降水量最高,范围广,持续时间长,强度高,是2013年以来的最高水平。结果与讨论:与坡耕地相比,所有植物群落的SOC浓度均随土壤深度的增加而增加,大多数灌木和森林群落,特别是自然群落的SOC浓度均显着增加(p <0.05)。以天然次生林群落为参考(即土壤流失和SOC损失均为1.0),2013年其他12个植物群落的相对土壤流失和SOC损失分别为1.5至9.4和0.30至1.73。天然灌木和森林群落比草原群落对暴雨侵蚀的抵抗力更大。 SOC含量较低的天然草地群落即使土壤流失量较高也产生较低的SOC损失,天然次生林群落产生的SOC损失较高,这主要是因为它们的SOC含量较高,而土壤流失较大的人工刺槐群落产生的SOC损失较高。 。结论:这些结果表明,与在山坡上进行人工植被恢复相比,天然植被在提高SOC储量和减少土壤侵蚀方面更有效。但是,具有较高SOC含量和储存能力的天然次生林群落也可能在极端暴雨下导致更大的SOC损失。

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