Effect of Vegetation Restoration on Forest Soil

A special issue of Forests (ISSN 1999-4907). This special issue belongs to the section "Forest Soil".

Deadline for manuscript submissions: 30 January 2026 | Viewed by 1370

Special Issue Editor


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Guest Editor
Institute of Loess Plateau, Shanxi University, Taiyuan, China
Interests: restoration ecology; biodiversity; ecological risk assessment; ecological modelling; landuse change

Special Issue Information

Dear Colleagues,

Ecosystem degradation is a critical global issue which is becoming increasingly concerning. It has serious negative impacts on the natural environment, human health, economic development, biodiversity, social stability, and cultural heritage, among many other aspects. As the United Nations Decade on Ecosystem Restoration moves forward, forest restoration on degraded and deforested land is expanding globally. Many field studies have assessed the ecological effects of restoration actions on plot and regional scales. However, the mechanisms of action of soil and vegetation remain unclear and need to be explored further. This Special Issue plans to explore the effects of vegetation restoration on soil health, as well as the mechanisms of action of soil and vegetation. This Special Issue is aimed at providing selected contributions on the sustainable development of ecosystems.

Potential topics include, but are not limited to, the following:

  • Effects of vegetation restoration;
  • Biodiversity and ecosystem function;
  • Action mechanisms of soil and vegetation;
  • Restoration outcome assessment;
  • Restoration strategies;
  • Role of soil microbes in vegetation restoration.

Prof. Dr. Yong Liu
Guest Editor

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Keywords

  • vegetation restoration
  • biodiversity
  • functions
  • soil health
  • ecosystem sustainability

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Published Papers (2 papers)

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Research

18 pages, 2560 KB  
Article
Vegetation Traits and Litter Properties Play a Vital Role in Enhancing Soil Quality in Revegetated Sandy Land Ecosystems
by Pengfei Zhang, Ming’an Shao, Xiao Bai and Chunlei Zhao
Forests 2025, 16(12), 1782; https://doi.org/10.3390/f16121782 - 27 Nov 2025
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Abstract
Desertification erodes arable land and human habitats. Vegetation restoration represents a critical process for improving the quality of sandy land by enhancing soil structure and nutrient cycling. This study aims to investigation how vegetation restoration affects soil physicochemical properties and soil quality. Five [...] Read more.
Desertification erodes arable land and human habitats. Vegetation restoration represents a critical process for improving the quality of sandy land by enhancing soil structure and nutrient cycling. This study aims to investigation how vegetation restoration affects soil physicochemical properties and soil quality. Five vegetated land types were selected (Pinus sylvestris var. mongholica Litv., PS; Amygdalus pedunculata Pall., AP; Salix psammophila, SP; Amorpha fruticosa L., AF; Artemisia desertorum Spreng., AD). Bare sandy land (BS) served as the control. The physicochemical properties of 270 soil samples from three vertical depth intervals (0–10, 10–20, and 20–30 cm) were analyzed. The findings demonstrated that vegetation restoration markedly improved the proportion of finer soil particles (clay and silt) and organic carbon, while the variations in total phosphorus, ammonia nitrogen, and nitrate nitrogen were not significant. To better understand the variations in soil quality in different vegetated lands, a soil quality index (SQI) was developed that considers multiple soil physical and chemical indicator selections and scoring methods. The SQI based on the minimum dataset and linear scoring method better differentiated the soil quality for sandy lands and showed higher values for SP among all five vegetated lands and BS. Improvements in soil quality were closely related to vegetation properties (density and coverage) and litter characteristics (thickness, water content, and total phosphorus content). Restoration strategies for sandy lands should focus more strongly on species selection, taking into account interspecific variations in litter production, physicochemical properties, canopy architecture, and planting density to more effectively improve soil quality. Full article
(This article belongs to the Special Issue Effect of Vegetation Restoration on Forest Soil)
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17 pages, 2675 KB  
Article
Unveiling the Carbon Secrets: How Forestry Projects Transform Biomass and Soil Carbon on the Tibet Plateau
by Man Cheng, Xia Xu, Zhixuan Chen, Yun Xiang, Yongli Wen and Xiao Wang
Forests 2025, 16(4), 631; https://doi.org/10.3390/f16040631 - 3 Apr 2025
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Abstract
Afforestation is regarded as a crucial approach to enhancing terrestrial carbon sinks. Nevertheless, in ecologically fragile regions, the impacts of afforestation on carbon in biomass and soil remain highly uncertain. This study employed field investigations to explore the effects of forestry ecological projects [...] Read more.
Afforestation is regarded as a crucial approach to enhancing terrestrial carbon sinks. Nevertheless, in ecologically fragile regions, the impacts of afforestation on carbon in biomass and soil remain highly uncertain. This study employed field investigations to explore the effects of forestry ecological projects on carbon stocks in biomass and soil within the Qinghai–Tibet Plateau, and to deeply analyze its key influencing factors. The key findings are summarized as follows: (1) The total vegetation carbon stocks of arbor forests and shrub forests (ranging from 7.7 to 24.0 Mg/ha) are 1.3–6.8 times that of grasslands (ranging from 3.5 to 6.1 Mg/ha). Afforestation-induced changes in biomass carbon are primarily attributed to the increase in carbon storage within the arbor-shrub layer, while exhibiting negligible effects on herbaceous layer carbon. (2) The soil organic carbon (SOC) stocks (0–100 cm depth) of forestland, shrubland, and grassland are 39.6–64.5 Mg/ha, 40.7–100.2 Mg/ha, and 43.1–121.9 Mg/ha, respectively. There are no significant differences in SOC stocks among shrubland, forestland, and grassland at either the 10- or 25-year development stage. The SOC stocks of 40-year-old shrubland and forestland are 1.5 and 2.3 times that of grassland, respectively. (3) For 10-year-old and 25-year-old arbor and shrub afforestation, biomass carbon increased while SOC decreased, showing a trade-off. In the case of 40- year-old afforestation, both biomass carbon and SOC increased synergistically. (4) Results from the random forest analysis indicate that the understory herbaceous diversity in this region has a significant impact on biomass carbon sequestration, and that soil total nitrogen, ammonium nitrogen, and nitrate nitrogen determine SOC sequestration. (5) Partial least squares analysis further demonstrates that afforestation promotes the retention of SOC stocks by increasing soil nutrients (especially nitrogen and nitrogen availability). Afforestation in alpine and arid regions, especially 40-year shrub afforestation, holds great carbon sequestration potential. The supplementation of soil nitrogen and phosphorus can enhance the carbon sequestration of this system. Full article
(This article belongs to the Special Issue Effect of Vegetation Restoration on Forest Soil)
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