油松人工林火烧迹地早期土壤入渗动态
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秦倩倩, 邱聪, 郑大柽, 刘艳红
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Soil infiltration dynamics in early period of a post-fire Pinus tabulaeformis plantation
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QIN Qian-Qian, QIU Cong, ZHENG Da-Cheng, LIU Yan-Hong
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表2 油松人工林土壤入渗特征的三因素方差分析
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Table 2 Three-way ANOVA analysis of soil infiltration characteristics in a Pinus tabulaeformis plantation
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指标 Index | 火烧干扰 Fire disturbance (df = 1) | 土壤深度 Soil depth (df = 3) | 时间 Time (df = 7) | 火烧 × 深度 Fire × Depth (df = 3) | 火烧 × 时间 Fire × Time (df = 7) | 深度 × 时间 Depth × Time (df = 21) | 火烧 × 深度 × 时间 Fire × Depth × Time (df = 21) | 初渗速率 Initial infiltration rate (mm·min-1) | 2.10 | 0.22 | 8.93*** | 0.75 | 1.05 | 0.49 | 0.38 | 稳渗速率 Steady infiltration rate (mm·min-1) | 0.06 | 0.69 | 8.37*** | 0.25 | 2.70* | 0.43 | 0.60 | 入渗总量 Cumulative-infiltration volume (mm) | 0.28 | 0.62 | 8.93*** | 0.36 | 2.06 | 0.48 | 0.55 | 饱和导水率 Saturated hydraulic conductivity (mm·min-1) | 0.51 | 0.38 | 9.31*** | 0.49 | 1.67 | 0.43 | 0.47 |
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