CHENG Hanting, LI Qinfen, WANG Xiaomin, et al. Effects of Different Vegetation Restoration Strategies on Soil Penetrability of Karst Ecosystem in Guizhou Province[J]. 2020, 34(6): 110-116.
DOI:
CHENG Hanting, LI Qinfen, WANG Xiaomin, et al. Effects of Different Vegetation Restoration Strategies on Soil Penetrability of Karst Ecosystem in Guizhou Province[J]. 2020, 34(6): 110-116. DOI: 10.13870/j.cnki.stbcxb.2020.06.017.
Effects of Different Vegetation Restoration Strategies on Soil Penetrability of Karst Ecosystem in Guizhou Province
the influence of vegetation restoration on soil infiltration process in different ecosystems has been a hot topic. The purpose of this study was to explore the influence of different vegetation restoration strategies on the spatial change of soil infiltration characteristics. Through the analysis of soil bulk density
soil porosity
soil organic matter
and soil penetrability characteristics of natural grass shrub mixed forest
secondary forest land
natural grassland
mango land
nut land
and corn land in the experimental area of rocky desertification control in Guizhou
the results showed that: For different vegetation restoration strategies
there are significant differences in soil bulk density
porosity
and organic matter content
which are manifested in natural vegetation restoration (grass shrub mixed forest and secondary forest land) and straw returning planting mode can effectively reduce soil bulk density and increase soil porosity. With the increase of soil depth
soil bulk density increased
soil porosity and organic matter content changed in the opposite direction. Different vegetation restoration methods and soil depth significantly changed the soil water permeability characteristics
among which
the soil permeability of natural vegetation restoration (grass shrub mixed forest and secondary forest land) was higher than that of artificial vegetation restoration (mango land and nut land)
mainly because under the condition of nature vegetation restoration
soil disturbance was small
plant roots and litter increased
which changes the physical properties of soil
reduces soil bulk density
and improves the comprehensive benefits of soil porosity. With the increase of soil depth
steady infiltration rate and cumulative infiltration amount decreased. By measuring the soil hydrological characteristics of different vegetation restoration methods
we can provide a scientific basis for the evaluation of vegetation restoration methods and soil infiltration performance in karst areas.
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references
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