1. 福建农林大学林学院,福州,350002
2. 国家林业和草原局杉木工程技术研究中心,福州,350002
3. 福建省闽侯白沙国有林场, 福建 闽侯,350102
纸质出版:2023
移动端阅览
沈健, 何宗明, 董强, 等. 滨海防护林土壤CO2排放和土壤因子对计划火烧的响应[J]. 水土保持学报, 2023,37(1):254-261.
Responses of Soil CO2 Emission and Soil Factors to Prescribed Fire in Coastal Shelterbelt[J]. 2023, 37(1): 254-261.
沈健, 何宗明, 董强, 等. 滨海防护林土壤CO2排放和土壤因子对计划火烧的响应[J]. 水土保持学报, 2023,37(1):254-261. DOI: 10.13870/j.cnki.stbcxb.2023.01.033.
Responses of Soil CO2 Emission and Soil Factors to Prescribed Fire in Coastal Shelterbelt[J]. 2023, 37(1): 254-261. DOI: 10.13870/j.cnki.stbcxb.2023.01.033.
为研究林火对滨海沙地森林生态系统碳循环的干扰作用
以尾巨桉防护林(Eucalyptus urophylla × Eucalyptus grandis)和木麻黄防护林(Casuarina equisetifolia)为研究对象
利用LI-8100土壤CO
2
通量全自动测量系统测定不同防护林火烧迹地和对照样地的土壤CO
2
通量
同时测定样地内土壤温湿度和土壤pH、全量碳氮和矿质氮含量
并分析不同林地土壤CO
2
通量与水热因子关系以及土壤理化特性的变化。结果表明:2种防护林火烧迹地土壤CO
2
通量均显著低于对照样地
尾巨桉林火烧迹地和对照样地土壤CO
2
通量月平均值分别为2.47
3.32 μmol/(m
2
·s)
木麻黄林分别为2.48
3.28 μmol/(m
2
·s)。林火干扰后2种防护林土壤温度和湿度均高于对照样地
在指数函数模型中尾巨桉林和木麻黄林10 cm处土壤温度解释土壤总呼吸的10.4%~21.4%
在二项式函数模型中尾巨桉林和木麻黄林10 cm处土壤湿度解释土壤总呼吸的15.8%~29.4%
在双变量回归模型中土壤温湿度以及其交互作用共同解释土壤总呼吸的33.1%~66.8%。轻度火干扰对尾巨桉和木麻黄林地土壤pH、全量碳氮和矿质氮含量的影响较小
2种防护林火烧迹地土壤pH均有所升高
NH
4
+
-N、NO
3
-
-N含量均有所下降。综上所述
林火干扰导致研究区内2种防护林土壤碳排放显著降低
不同样地土壤温度、湿度的双变量模型拟合效果均优于单因素模型
土壤碳排放受到两者的共同影响
为气候变暖背景下林火干扰对滨海沙地防护林土壤碳平衡影响的研究提供参考数据和理论支持。
To study the disturbance effect of forest fire on the carbon cycle of coastal sandy forest ecosystem
taking Eucalyptus urophylla × Eucalyptus grandis plantation and Casuarina equisetifolia plantation as research objects
the LI-8100 soil CO
2
flux automatic measurement system was used to measure the soil CO
2
flux of burned and control plots in different plantations. A
t the same time
soil temperature and moisture
soil pH
total carbon
total nitrogen and mineral nitrogen contents in the sample plots were measured. The relationship between soil CO
2
flux and water and heat factors as well as the changes of soil physical and chemical properties were analyzed. The results showed that the soil CO
2
fluxes in the burnt plots were significantly lower than those in control plots
the monthly average of soil CO
2
fluxes in the E. urophylla × E. grandis forest burned plots and the control plots was 2.47 and 3.32 μmol/(m
2
·s)
respectively
and that in C. equisetifolia forest was 2.48 and 3.28 μmol/(m
2
·s)
respectively. After the forest fire disturbance
the soil temperature and moisture of the two shelterbelt forests were higher than those of the control plots
in the exponential function model
soil temperature at 10 cm of E. urophylla × E. grandis and C. equisetifolia forest explained 10.4%~21.4% of the total soil respiration. In the binomial function model
soil moisture at 10 cm in E. urophylla × E. grandis forest and C. equisetifolia forest explained 15.8%~29.4% of the total soil respiration. In the bivariate regression model
soil temperature and humidity and their interaction together explained 33.1%~66.8% of the total soil respiration. Mild fire disturbance had little effect on soil pH
total carbon
total nitrogen and mineral nitrogen content in E. urophylla × E. grandis and C. equisetifolia forest
the soil pH of the burned area in the two types of forest both increased
and the contents of NH
4
+
-N and NO
3
-
-N decreased. In summary
forest fire disturbance would significantly reduce soil carbon emission of two shelterbelt forests in the study area. The fitting effects of the bivariate model of soil temperature and humidity in different plots were all better than those of the single factor-model
indicating that soil carbon emission was affected by both
which could provide reference
data and theoretical support for the research on the impact of forest fire disturbance on the soil carbon balance of coastal sandy shelter forests under the background of climate warming.
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