基于土壤因素耦合的喀斯特流域水文干旱模拟——以贵州省为例
贺中华, 陈晓翔

The Hydrological Drought Simulating in Karst Basin Based on Coupled Soil Factors ——Taking Guizhou Province as A Case
Zhong-hua HE, Xiao-xiang CHEN
表5 土壤类型双因子耦合与径流深拟合模型
Table 5 The fitting models between the double-factors coupled of the soil types and runoff depths
因子 R R2 模型 F Sig. 因子 R R2 模型 F Sig.
12 0.464 0.215 WRD=0.021+0.726S12 10.425 0.003 37 0.174 0.030 WRD=0.063-2.234S37 1.183 0.284
13 0.464 0.215 WRD=0.021+2.336S13 10.424 0.003 38 0.174 0.030 WRD=0.063-1.189S38 1.183 0.284
14 0.464 0.215 WRD=0.021+13.843S14 10.425 0.003 39 0.174 0.030 WRD=0.063-0.522S39 1.183 0.284
15 0.464 0.215 WRD=0.021+2.764S15 10.425 0.003 45 0.047 0.002 WRD=0.046-0.368S45 0.085 0.772
16 0.464 0.215 WRD=0.021+1.057S16 10.425 0.003 46 0.047 0.002 WRD=0.046-0.141S46 0.085 0.772
17 0.464 0.215 WRD=0.021+6.931S17 10.425 0.003 47 0.047 0.002 WRD=0.046-0.924S47 0.085 0.772
18 0.464 0.215 WRD=0.021+3.688S18 10.425 0.003 48 0.047 0.002 WRD=0.046-0.491S48 0.085 0.772
19 0.464 0.215 WRD=0.021+1.619S19 10.424 0.003 49 0.047 0.002 WRD=0.046-0.216S49 0.085 0.772
23 0.547 0.299 WRD=-0.132+2.331S23 16.22 0.000 56 0.150 0.023 WRD=0.058-0.298S56 0.880 0.354
24 0.547 0.299 WRD=-0.132+13.815S24 10.425 0.000 57 0.150 0.023 WRD=0.058-1.956S57 0.880 0.354
25 0.547 0.299 WRD=-0.132+2.759S25 16.220 0.000 58 0.150 0.023 WRD=0.058-1.041S58 0.880 0.354
26 0.547 0.299 WRD=-0.132+1.055S26 16.219 0.000 59 0.150 0.023 WRD=0.058-0.457S59 0.880 0.354
27 0.547 0.299 WRD=-0.132+6.917S27 16.220 0.000 67 0.455 0.207 WRD=-0.052+5.504S67 9.942 0.003
28 0.547 0.299 WRD=-0.132+3.681S28 16.222 0.000 68 0.455 0.207 WRD=-0.052+2.929S68 9.942 0.003
29 0.547 0.299 WRD=-0.132+1.615S29 16.219 0.000 69 0.455 0.207 WRD=-0.052+1.285S69 9.942 0.003
34 0.174 0.030 WRD=0.063-4.463S34 1.183 0.284 78 0.001 0.000 WRD=0.045+0.008S78 0.000 0.996
35 0.174 0.030 WRD=0.063-0.891S35 1.183 0.284 79 0.001 0.000 WRD=0.045+0.003S79 0.000 0.996
36 0.174 0.030 WRD=0.063-0.341S36 1.183 0.284 89 0.087 0.008 WRD=0.051-0.27S89 0.293 0.592