NOMOGRAPH FOR HYDRAULIC CONDUCTIVITY AND INTRINSIC PERMEABILITY OF WATER-SOIL SYSTEM

Soil Science ◽  
1972 ◽  
Vol 113 (5) ◽  
pp. 375-377 ◽  
Author(s):  
ADAM ZANKER
1998 ◽  
Vol 3 (1) ◽  
pp. 9
Author(s):  
N.M. Somaratne ◽  
K.R.J. Smettem

A physically based model of soil surface scaling is proposed. The governing equations are formulated on the principle of conservation of mass assuming Darcy's law applies to suspension flowing through the soil surface. The model incorporates the physics of surface sealing by mechanisms that capture suspended particles moving with infiltrating water. As a result of particle retention in the soil system, the intrinsic porosity is reduced and hulk density is increased, resulting in changes to soil hydraulic properties such as moisture retention and hydraulic conductivity. Empirical functions are developed to describe the changes of these properties as the seal develops. With this approach, the seal can be mathematically described by well defined initial and boundary conditions and transient seal properties can be simulated in a physically realistic manner.


2006 ◽  
Vol 43 (1) ◽  
pp. 59-69 ◽  
Author(s):  
Zheng-yi Feng ◽  
Jonathan TH Wu

An approximate solution method, referred to as the epsilon method, allows flow characteristics such as flow rate and exit gradient to be determined for seepage through a two-layer soil system. The finite element program SEEP was employed to analyze flow characteristics of an impervious dam with sheet pile on a layered soil. Extensive analyses were performed for different conditions, including soil layer thickness, soil hydraulic conductivity, dam width, and sheet pile depth. The flow rate and exit gradient were determined for each condition analyzed. The results were reduced to simple charts, called the epsilon curves. The epsilon curves allow a designer to obtain solutions to the seepage problem without a computer code and to verify solutions obtained from a computer code. They are especially useful when searching for an optimum design of a masonry dam. The epsilon curves can be extended to a soil system comprising more than two layers. An example of a single-row sheet pile structure in a three-layer system is given to illustrate how to use the method for multiple-layer systems. The method was verified by comparing the results with those obtained from the SEEP program, and excellent agreement was noted.Key words: seepage, dam, sheet pile, layered soil, hydraulic conductivity.


1990 ◽  
Vol 41 (2) ◽  
pp. 215-228 ◽  
Author(s):  
P. S. BLACKWELL ◽  
A. J. RINGROSE-VOASE ◽  
N. S. JAYAWARDANE ◽  
K. A. OLSSON ◽  
D. C. MCKENZIE ◽  
...  

2020 ◽  
Vol 53 (2) ◽  
Author(s):  
Guanglong Zhu ◽  
Lifeng Gu ◽  
Yu Shi ◽  
Huize Chen ◽  
Yuqian Liu ◽  
...  

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