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8 土壤相对湿度双因子耦合与径流深拟合模型
Table 8 The fitting models between the double-factors coupled of the soil relative humidity and runoff depths
因子 R R2 模型 F Sig. 因子 R R2 模型 F Sig.
12 0.558 0.312 WRD=-0.024+2.777S12 17.195 0.000 34 0.126 0.016 WRD=0.054-0.222S34 0.612 0.439
13 0.558 0.312 WRD=-0.024+2.644S13 17.197 0.000 35 0.126 0.016 WRD=0.054-0.205S35 0.612 0.439
14 0.558 0.312 WRD=-0.024+0.786S14 17.197 0.000 36 0.292 0.085 WRD=0.015-0.144S36 3.269 0.079
15 0.558 0.312 WRD=-0.024+0.726S15 17.197 0.000 37 0.496 0.246 WRD=0.012-0.168S37 11.092 0.072
16 0.558 0.312 WRD=-0.024+2.024S16 17.196 0.000 45 0.148 0.022 WRD=0.021+0.16S45 0.851 0.362
17 0.558 0.312 WRD=-0.024+3.116S17 17.197 0.000 46 0.148 0.022 WRD=0.021+0.446S46 0.851 0.362
23 0.128 0.016 WRD=0.05-0.967S23 0.562 0.458 47 0.148 0.022 WRD=0.021+0.687S47 0.851 0.362
24 0.151 0.023 WRD=0.059-0.342S24 0.890 0.351 56 0.146 0.021 WRD=0.072-0.433S56 0.802 0.376
25 0.151 0.023 WRD=0.059-0.315S25 0.890 0.351 57 0.155 0.024 WRD=0.076-0.723S57 0.891 0.352
26 0.126 0.016 WRD=0.049-0.728S26 0.565 0.457 67 0.647 0.419 WRD=-0.008+3.8S67 24.496 0.00
27 0.128 0.016 WRD=0.05-1.139S27 0.562 0.458