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植被恢复类型和年龄对中国北方东居延海荒漠区地表粗糙度的影响。

Effects of the types and ages of vegetation restoration on land surface roughness in the Eastern Hobq Desert, Northern China.

机构信息

College of Geographical Science, Inner Mongolia Normal University, Hohhot 010022, China.

College of Geographical Science, Inner Mongolia Normal University, Hohhot 010022, China.

出版信息

Sci Total Environ. 2024 Dec 10;955:176837. doi: 10.1016/j.scitotenv.2024.176837. Epub 2024 Oct 11.

Abstract

Vegetation restoration has an important remodelling effect on near-surface characteristics, and consequent changes in land surface roughness (LSR) are key influences on soil wind erosion processes. However, the effects of vegetation restoration types and ages on LSR and the underlying mechanisms are not fully understood. In this study, the sand-fixing vegetation restoration area of the Hobq Desert was examined in comparison to a bare sand control area. The LSR of four artificial vegetation types (Salix psammophila, Caragana korshinskii, Artemisia ordosica, and Populus simonii) with restoration age of 36 years, and Salix psammophila and Caragana korshinskii after different periods of restoration (20, 28, 36 and 45 years) were measured using Structure-from-Motion (SfM) photogrammetry. Near-surface characteristics that may affect LSR were also measured. The results showed that vegetation restoration was associated with a 230-409 % higher LSR compared to the control site (1.74 mm). LSR in the different vegetation restoration areas were ranked, from high to low, as follows: AO (8.85 mm) > CK (7.89 mm) > SP (6.70 mm) > PS (6.61 mm). LSR also increased with time since restoration, with the greatest rate of increase during the first 20 years. The change of LSR is mainly affected by the change of near-surface characteristics, with the direct effects of biological crust thickness (0.331), litter thickness (0.289), soil bulk density (-0.239), and clay content (0.171) being significant. Stem diameter, litter density, biological crust coverage, and soil organic matter affected LSR indirectly, mainly through acting on the above factors. Finally, LSR was effectively estimated based on biological crust thickness, litter thickness, and soil bulk density (R = 0.904). The research results will help to further deepen the understanding of the influence mechanism of vegetation restoration on LSR, and provide scientific basis and practical reference for vegetation ecological restoration in similar areas.

摘要

植被恢复对近地表特征具有重要的改造作用,而地表粗糙度(LSR)的变化则是土壤风蚀过程的关键影响因素。然而,植被恢复类型和年龄对 LSR 的影响及其内在机制尚不完全清楚。本研究以库布齐沙漠风沙固定植被恢复区为研究对象,与裸沙对照区进行对比。采用基于结构光的摄影测量技术(SfM),对 4 种人工植被类型(沙柳、柠条、油蒿和新疆杨)的恢复年龄分别为 36 年、沙柳和柠条不同恢复年限(20、28、36 和 45 年)的 LSR 进行了测量,同时还测量了可能影响 LSR 的近地表特征。结果表明,与对照区相比,植被恢复区的 LSR 增加了 230%至 409%(1.74mm)。不同植被恢复区的 LSR 排序为:AO(8.85mm)>CK(7.89mm)>SP(6.70mm)>PS(6.61mm)。LSR 也随恢复时间的增加而增加,在前 20 年增加最快。LSR 的变化主要受近地表特征变化的影响,生物结皮厚度(0.331)、凋落物厚度(0.289)、土壤容重(-0.239)和粘粒含量(0.171)的直接影响显著。茎直径、凋落物密度、生物结皮盖度和土壤有机质通过作用于上述因素间接影响 LSR。最后,基于生物结皮厚度、凋落物厚度和土壤容重,可以有效地估算 LSR(R2=0.904)。研究结果有助于进一步深化对植被恢复对 LSR 影响机制的认识,为类似地区的植被生态恢复提供科学依据和实践参考。

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