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Effects Of Snow Depth And Soil Substrate On Soil Microbial Biomass Content And Their Stoichiometry

Posted on:2017-09-18Degree:MasterType:Thesis
Country:ChinaCandidate:J ZhaoFull Text:PDF
GTID:2393330548476772Subject:Ecology
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Soil microbe is the most important decomposer in forest ecosystems and sensitive indicator to enviromental changes.It plays a crucial role inforest carbon(Cmic)?nitrogen(Nmic)and phosphorus(Pmic)cycles.We use a chloroform fumigation extration method to measure and compare the dynamics of Cmic?Nmic and Pmic under different depth of snow cover and soil substrates.The results were listed as following:(1)The Cmic and Nmic of SP3 treatment were higher than that of SP1 treatment and SP2 treatment in the early snow cover period(December)of 0-5 cm and 5-10 cm soil layers.The Cmic and Nmic of SP1 treatment and SP2 treatment were significantly higher than that of SP3 treatment in the late snow cover period(March)(P<0.05),and the Cmic and Nmic of SP1 treatment and SP2 treatment were significantly higher than that of 0-5 cm soil layers in SP3 treatment.Other stages had no responding changes.(2)The Cmic and Nmic dropped first and rised in different treatments of 0-5 cm soil layer from december to august next year(V shape);The range of SP1?SP2 ? SP3 changes(Cmic)was 43.34-171.99 mmol kg-1?51.98-166.81 mmol kg-1,the range of SP1?SP2 ? SP3 changes(Nmic)was 12.00-33.97 mmol kg-1?12.31-33.77 mmol kg-1?11.34-34.11 mmol kg-1.The Cmic and Nmic dropped after rising first and then continue rise and declined in SP1 treatment and SP2 treatment of 5-10 cm soil layer from december to august next year(M shape).The Cmic and Nmic had the trend of decline in SP3 treatment;The range of SP1?SP2 ? SP3 changes(Cmic)was 39.93-79.59 mmol kg-1?41.00-87.44 mmol kg-1?45.65-83.85 mmol kg-1,the range of SP1?SP2 ? SP3 changes(Nmic)was 6.40-17.16 mmol kg-1?6.41-15.05 mmol kg-1?8.77-14.23 mmol kg-1.(3)The Cmic:Nmic had no significant difference among three treatments of 0-5 cm and 5-10 cm soil layers(P>0.05).The C:Nmic of three treatments had same annual dynamics in 0-5 cm soil layer.Relative to 0-5 cm soil layer,The Cmic:Nmic of 5-10 cm soil layer changed stability.(4)Before the successsion:the Cmic Nmic and Pmic of A treatment were significantly higher than that of B or C treatment(P<0.05).The Cmic:Nmic of A treatment was lower than that of B or C treatment,but the Cmic:Pmie and N:Pmic of A treatment were higher than those of B or C treatment.The Cmic/soil carbon(Csoii),Nmic/soil nitrogen(Nsoil),and Pmic/phosphorus(Psoil)of A treatment were significantly higher than those of B or C treatment(P<0.05,except for the Nmic/Nsoil,of C treatment).(5)After the succession:the Cmic,Nmic,and Pmic of A treatment were significantly higher than that of B or C treatment(P<0.05).The Cmic:Nmic of A or B treatment was lower than that of C treatment,but the Cmic:Pmic and Nmic:Pmic of A treatment were higher than those of B or C treatment.The Cmic/Csoii,Nmic/Nsoii,and Pmic/Psoii of A treatment were higher than those of B or C treatment.(6)Through 10-year succession,the Cmic,Nmic,and Pmic of the three treatments increased(C treatment had the largest increase including 145.35%,243.29%and 58.39%).The Cmic:Nmic of the three treatments declined,but the Cmic:Pmic and Nmic:Pmic increased.Among the-three treatments,the Cmic:Nmic of B and C treatments decreased significantly(P<0.05),while the N:Pmic of A and C treatments increased significantly(P<0.05).The Cmic/Csoil,Nmic/Nsoil,and Pmic/Psoii of three treatments increased with the succession.
Keywords/Search Tags:Soil microbe, depth of snow cover, soil substrate, seasonal dynamics
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