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 |   |  10.425 |  0.003 |  37 |  0.174 |  0.030 |   |  1.183 |  0.284 |     | 13 |  0.464 |  0.215 |   |  10.424 |  0.003 |  38 |  0.174 |  0.030 |   |  1.183 |  0.284 |     | 14 |  0.464 |  0.215 |   |  10.425 |  0.003 |  39 |  0.174 |  0.030 |   |  1.183 |  0.284 |     | 15 |  0.464 |  0.215 |   |  10.425 |  0.003 |  45 |  0.047 |  0.002 |   |  0.085 |  0.772 |     | 16 |  0.464 |  0.215 |   |  10.425 |  0.003 |  46 |  0.047 |  0.002 |   |  0.085 |  0.772 |     | 17 |  0.464 |  0.215 |   |  10.425 |  0.003 |  47 |  0.047 |  0.002 |   |  0.085 |  0.772 |     | 18 |  0.464 |  0.215 |   |  10.425 |  0.003 |  48 |  0.047 |  0.002 |   |  0.085 |  0.772 |     | 19 |  0.464 |  0.215 |   |  10.424 |  0.003 |  49 |  0.047 |  0.002 |   |  0.085 |  0.772 |     | 23 |  0.547 |  0.299 |   |  16.22 |  0.000 |  56 |  0.150 |  0.023 |   |  0.880 |  0.354 |     | 24 |  0.547 |  0.299 |   |  10.425 |  0.000 |  57 |  0.150 |  0.023 |   |  0.880 |  0.354 |     | 25 |  0.547 |  0.299 |   |  16.220 |  0.000 |  58 |  0.150 |  0.023 |   |  0.880 |  0.354 |     | 26 |  0.547 |  0.299 |   |  16.219 |  0.000 |  59 |  0.150 |  0.023 |   |  0.880 |  0.354 |     | 27 |  0.547 |  0.299 |   |  16.220 |  0.000 |  67 |  0.455 |  0.207 |   |  9.942 |  0.003 |     | 28 |  0.547 |  0.299 |   |  16.222 |  0.000 |  68 |  0.455 |  0.207 |   |  9.942 |  0.003 |     | 29 |  0.547 |  0.299 |   |  16.219 |  0.000 |  69 |  0.455 |  0.207 |   |  9.942 |  0.003 |     | 34 |  0.174 |  0.030 |   |  1.183 |  0.284 |  78 |  0.001 |  0.000 |   |  0.000 |  0.996 |     | 35 |  0.174 |  0.030 |   |  1.183 |  0.284 |  79 |  0.001 |  0.000 |   |  0.000 |  0.996 |     | 36 |  0.174 |  0.030 |   |  1.183 |  0.284 |  89 |  0.087 |  0.008 |   |  0.293 |  0.592 |      
		 | 
	
	
		 | 
	
	
		 |