LI Hongyun, XIN Ying, ZHAO Yusen. Characteristics of Microbial Biomass Carbon in Soil Aggregates of Burned Area Under Different Restorations[J]. 2016, 30(5): 342-347.
DOI:
LI Hongyun, XIN Ying, ZHAO Yusen. Characteristics of Microbial Biomass Carbon in Soil Aggregates of Burned Area Under Different Restorations[J]. 2016, 30(5): 342-347. DOI: 10.13870/j.cnki.stbcxb.2016.05.057.
Characteristics of Microbial Biomass Carbon in Soil Aggregates of Burned Area Under Different Restorations
In order to explore the effects of different restoration approaches on soil aggregates’ formation and it’s cycle carbon of severely burned area in Greater Xing’an Mountains
the artificial restoration (Larix gmelini and Pinus sylvestris var. mongolica) and the natural regeneration of forest in Greater Xing’an Mountains after the severely burned in 1987 respectively were chosen as the research object and analyzed the distribution features of organic carbon
microbial biomass carbon and K2SO4-extractable carbon in soil aggregates under different restoration approaches. The results showed that: (1) There were significant difference (P<0.05) for the contents of organic carbon
microbial biomass carbon and K2SO4-extractable carbon in soil aggregates among different forest types
which the characteristics were Larix gmelini plantation>natural secondary forest>Pinus sylvestris var. mongolica plantation. (2) Under different vegetation restorations
soil organic carbon and microbial biomass carbon presented an increasing trend along with increasing of particle size of aggregate
and the large aggregates were significant higher amounts of both the soil organic carbon and microbial biomass carbon than the micro aggregates(P<0.05)
the K2SO4-extractable carbon mainly distributed in the 1~0.5 mm particle size and larger size aggregate. (3) The organic carbon and microbial biomass carbon in soil aggregates mainly distributed in soil surface layer (0—5 cm)
which the contents decreased with the increase of soil depth. Except >2 mm and 2~1 mm aggregates
the contents of K2SO4-extractable carbon in soil aggregates presented a decreasing trend along with the increase of soil depth. (4) Microbial biomass carbon had significant positive correlations (P<0.01) with soil organic carbon and K2SO4-extractable carbon
revealing that microbial biomass carbon had close relationship with soil organic carbon and K2SO4-extractable carbon.
Soil Aggregates and Organic Carbon Distribution Characteristics Based on Long-Term Organic Substitution
Response of Soil Total Nitrogen Distribution to Erosion under Ecological Restoration in Qinling Water Source Area
Spatial Variation Characteristics of Soil Aggregate Stability and Erodibility in Typical Small Watershed of Loess Alpine Region
Effects of Biological Soil Crusts on Soil Aggregate Distribution and Stability in Vegetation Concrete Slopes
Response of Phosphorus Components and Organic Carbon Molecular Structures in Soil Aggregates to Nitrogen and Phosphorus Additions in Evergreen Broad-leaved Forests
Related Author
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Related Institution
Institute of Environment Resource and Soil Fertilizer, Zhejiang Academy of Agricultural Sciences
Zhejiang Key Laboratory of Soil Remediation and Quality Improvement
State Key Laboratory of Water Engineering Ecology and Environment in Arid Area, Xi'an University of Technology
State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University
College of Ecological Environment Engineering, Qinghai University