100 Percent Passing 10 100 90 74 20 60 80 32 70- 15 Clay 40 60 - 50 he soil using the Triangular 50 Silty clay Sàndy clay 60 40 Silty clay loam Clay loàm Soil 30 Sandy clay loam 20 Loàm Silty loam 10 Percenta Percentage of clay

Q: Which of the following most nearly gives the internal degree of indeterminacy? 102 34 28 84 Next ▸ ◄…

A: Is question is from structural analysis in this question a frame given and we are asked to find out…

Q: 21

A: The no of member are m =  17 The no of reaction r = 4 The no of joint = 9

Q: 2. What is the N, V and M values, draw the diagrams. 4m 3 m G1 4 t/m ↓↓↓↓ 2 m 4t

A: The frame is given asTo find:-Axial force, shear force and bending moment diagramsConcept:-Axial…

Q: 1 2 T - 3 CONCACA NIDO Force diagrams - Inclined plane 5 Performs various tests by modifying the…

A:

Q: 3. Find the following: I 2 -1 [B] -5 4 [4]- 7 3 3 3 4 5 a. [A] + [B] b. [А]-[8] C. 3[A] d. (A][B]

A:

Q: 2. Find the equation for the four linear sections of the moment diagram below. 25 kips |25 kips 25…

A:

Q: Q2. Fit a polynomial and find C @T-0 T -50 -20 10 70 100 C 0.125 0.128 0.134 0.144 0.15

A: The above answer has good explanation

Q: Did you mean influence for member JI when you wrote JK. If you did mean JK the member why use JK.

A: Given: A truss  Required: To clarify regarding the typing of JI and JK

Q: find l for the impact of hardness on humans and the environment along with the bibliography

A: Impact of hardness on humans One of the most obvious effects of hard water is skin irritation and…

Field applications of hydraulic conductivity

Hydraulic conductivity is one of the hydraulic properties of soil defined as a measurement of the ability of a porous medium to permit water movement or fluid flow through it. It is denoted by the letter K. It is influenced by the density and viscosity of the fluid. It is also called permeability. Hydraulic conductivity is defined as the ratio of velocity to the hydraulic gradient. The different methods used to determine the hydraulic conductivity are laboratory methods (constant head permeability tests and falling head tests), in-situ field methods (pumping in and pumping out tests), small scale field tests (infiltration tests and slug tests), and indirect methods such as estimation from grain size, consolidation test data, and horizontal capillary test. The pedotransfer function (PTF) method is a specific empirical estimating approach employed in the soil sciences is also used to determine the hydraulic conductivity of the soil.