XIONG Yingnan, FENG Tianjiao, WANG Ping, et al. Effects of Long-term Artificial Forest Restoration on Soil Moisture and Nutrient Characteristics in the Loess Area of Western Shanxi Province, China[J]. 2022, 36(2): 228-237.
DOI:
XIONG Yingnan, FENG Tianjiao, WANG Ping, et al. Effects of Long-term Artificial Forest Restoration on Soil Moisture and Nutrient Characteristics in the Loess Area of Western Shanxi Province, China[J]. 2022, 36(2): 228-237. DOI: 10.13870/j.cnki.stbcxb.2022.02.029.
Effects of Long-term Artificial Forest Restoration on Soil Moisture and Nutrient Characteristics in the Loess Area of Western Shanxi Province, China
The Loess Plateau has always been one of the most serious soil erosion and environmental problems regions in China. Artificial vegetation restoration can effectively improve soil properties and soil quality
therefore clarifying the responses of soil moisture and nutrient properties to long-term artificial vegetation restoration is conducive to further effectively improving the eco-environment. This study selected three typical vegetation types
including natural restoration secondary forest land
artificial Robinia pseudoacacia forest land and artificial Pinus tabulaeformis forest land
during ecological restoration in the loess region of western Shanxi. By measuring soil physical properties
soil moisture contents and soil nutrients such as organic carbon
nitrogen
phosphorus and potassium contents
the differences under the long-term artificial vegetation restorations were comparatively analyzed. The results showed that:(1) The soil bulk density of secondary forest land
Robinia pseudoacacia forest land and Pinus tabulaeformis forest land in 0-20 cm shallow layer was 1.15
1.04 and 1.06 g/cm3
respectively. The soil bulk density increased with the increase of soil depth. (2) The soil moisture of secondary forest land in shallow layer was better than those of Robinia pseudoacacia forest land and Pinus tabulaeformis forest land. When soil moisture consumption period (before the start of growth season) transited to the accumulation period (at the beginning of the growth season)
the dynamic variations of soil moisture in secondary forest land were more dramatic. (3) The soil carbon storage in secondary forest land was higher
while the soil nitrogen and phosphorus storage in Pinus tabulaeformis forest land was higher. The vertical variations of soil nutrients of the three forest lands had significant differences with accumulation in surface layer. The contents of organic carbon
total nitrogen
total phosphorus
available nitrogen and available potassium all decreased with the increase of soil depth
while the contents of available phosphorus increased first and then decreased. Considering the soil moisture and nutrient condition
it was suggested that the secondary forest should be mainly conserved in the process of vegetation restoration to achieve the better water and carbon storage and other ecological benefits
which would be conducive to the optimization of stand management
and the promotion of vegetation restoration and ecological construction in the western Shanxi loess region.
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Soil Organic Carbon and Moisture Effects of Different Vegetation Restoration Types in the Mu Us Sandy Land
Variation of Stoichiometric Characteristics of Soil Nutrients in Collapse Mound of Eroded Red Soil Region
Change Characteristics of Soil Physical Properties at the Initial Natural Recovery Stage in Disaster Disturbed and Damaged Areas
Effects of Water Saving and Fertilizer Reducing on Water and Nutrients of Maize at Different Growth Stages in the Hetao Irrigated Area
The Correlation Between Soil Temperature and Water Content During the Natural Vegetation Restoration on the Loess Plateau
Related Author
WANG Defu
DONG Lingbo
LI Ao
YU Zhijing
DENG Lei
JIANG Chao1
2
CHEN Zhibiao1
Related Institution
College of Soil and Water Conservation Science and Engineering, Institute of Soil and Water Conservation, Northwest A&F University, State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Yangling
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling
Key Laboratory for Subtropical Mountain Ecology (Ministry of Science and Technology and Fujian Province Funded)
College of Geographical Sciences,Fujian Normal University
Institute of Geographical Sciences,Fujian Normal University