Spatial uncertainty analysis of the saturated soil hydraulic conductivity in a subtropical watershed

2021 ◽  
Vol 80 (21) ◽  
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Rodrigo César Vasconcelos dos Santos ◽  
Mauricio Fornalski Soares ◽  
Luís Carlos Timm ◽  
Tirzah Moreira Siqueira ◽  
Carlos Rogério Mello ◽  
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Mauricio Fornalski Soares ◽  
Luana Nunes Centeno ◽  
Luís Carlos Timm ◽  
Carlos Rogério Mello ◽  
Douglas Rodrigo Kaiser ◽  
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Vol 191 ◽  
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Author(s):  
Luana Nunes Centeno ◽  
Luís Carlos Timm ◽  
Klaus Reichardt ◽  
Samuel Beskow ◽  
Tamara Leitzke Caldeira ◽  
...  

2017 ◽  
Vol 48 (8) ◽  
pp. 908-919 ◽  
Author(s):  
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Vahedberdi Sheikh ◽  
Mohsen Hossein-Alizadeh ◽  
Hasan Rezaii-Moghadam

Soil Research ◽  
2001 ◽  
Vol 39 (4) ◽  
pp. 851 ◽  
Author(s):  
P. L. Libardi ◽  
P. L. Libardi ◽  
K. Reichardt ◽  
K. Reichardt

The method of Libardi to estimate soil hydraulic conductivity in the field, during the redistribution of soil water, is discussed and improved. It is shown that if the saturated soil water content is measured at the soil surface, values at any other depth can be calculated from the database used to compute hydraulic conductivity. Since the saturated soil water content is difficult to measure and critical to the establishment of the hydraulic conductivity functions, this is an important refinement of the method. It is also shown that the unit hydraulic gradient assumption, which is part of the methodology, does not introduce significant errors in the estimation of soil hydraulic conductivity.


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