Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation Solution

STEP 0: Pre-Calculation Summary
Formula Used
Sorptivity = (Cumulative Infiltration Capacity-Hydraulic Conductivity*Time)/(Time^(1/2))
s = (Fp-k*t)/(t^(1/2))
This formula uses 4 Variables
Variables Used
Sorptivity - Sorptivity is a function of soil suction potential and measures the capacity of the medium to absorb or desorb liquid by capillarity.
Cumulative Infiltration Capacity - (Measured in Centimeter per Hour) - Cumulative Infiltration Capacity is calculated by subtracting the cumulative runoff from the cumulative rainfall.
Hydraulic Conductivity - (Measured in Centimeter per Hour) - Hydraulic Conductivity depends on the size and arrangement of the water-transmitting openings and on the dynamic characteristics of the fluid.
Time - (Measured in Hour) - Time is an ongoing and continuous sequence of events that occur in succession, from the past through the present, and to the future. Here it is for rainfall.
STEP 1: Convert Input(s) to Base Unit
Cumulative Infiltration Capacity: 20 Centimeter per Hour --> 20 Centimeter per Hour No Conversion Required
Hydraulic Conductivity: 2.93 Centimeter per Hour --> 2.93 Centimeter per Hour No Conversion Required
Time: 2 Hour --> 2 Hour No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
s = (Fp-k*t)/(t^(1/2)) --> (20-2.93*2)/(2^(1/2))
Evaluating ... ...
s = 9.99848988597778
STEP 3: Convert Result to Output's Unit
9.99848988597778 --> No Conversion Required
FINAL ANSWER
9.99848988597778 9.99849 <-- Sorptivity
(Calculation completed in 00.020 seconds)

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Infiltration Capacity Equation Calculators

Infiltration rate by Horton's equation
​ LaTeX ​ Go Infiltration Capacity at Any Time t = Final Steady State Infiltration Capacity+(Initial Infiltration Capacity-Final Steady State Infiltration Capacity)*exp(-(Decay Coefficient*Time))
Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation
​ LaTeX ​ Go Sorptivity = (Cumulative Infiltration Capacity-Hydraulic Conductivity*Time)/(Time^(1/2))
Philip's Equation
​ LaTeX ​ Go Cumulative Infiltration Capacity = Sorptivity*Time^(1/2)+Hydraulic Conductivity*Time
Kostiakov Equation
​ LaTeX ​ Go Cumulative Infiltration Capacity = Local Parameter a*Time^Local Parameter b

Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation Formula

​LaTeX ​Go
Sorptivity = (Cumulative Infiltration Capacity-Hydraulic Conductivity*Time)/(Time^(1/2))
s = (Fp-k*t)/(t^(1/2))

What is Infiltration Capacity?

The Infiltration Capacity is defined as the maximum rate of infiltration. It is most often measured in meters per day but can also be measured in other units of distance over time if necessary. The infiltration capacity decreases as the soil moisture content of soils surface layers increases

How to Calculate Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation?

Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation calculator uses Sorptivity = (Cumulative Infiltration Capacity-Hydraulic Conductivity*Time)/(Time^(1/2)) to calculate the Sorptivity, The Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation formula is defined as a measure of the capacity of the medium to absorb or desorb liquid by capillarity. Sorptivity is denoted by s symbol.

How to calculate Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation using this online calculator? To use this online calculator for Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation, enter Cumulative Infiltration Capacity (Fp), Hydraulic Conductivity (k) & Time (t) and hit the calculate button. Here is how the Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation calculation can be explained with given input values -> 9.99849 = (5.55555555555556E-05-8.13888888888889E-06*7200)/(7200^(1/2)).

FAQ

What is Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation?
The Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation formula is defined as a measure of the capacity of the medium to absorb or desorb liquid by capillarity and is represented as s = (Fp-k*t)/(t^(1/2)) or Sorptivity = (Cumulative Infiltration Capacity-Hydraulic Conductivity*Time)/(Time^(1/2)). Cumulative Infiltration Capacity is calculated by subtracting the cumulative runoff from the cumulative rainfall, Hydraulic Conductivity depends on the size and arrangement of the water-transmitting openings and on the dynamic characteristics of the fluid & Time is an ongoing and continuous sequence of events that occur in succession, from the past through the present, and to the future. Here it is for rainfall.
How to calculate Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation?
The Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation formula is defined as a measure of the capacity of the medium to absorb or desorb liquid by capillarity is calculated using Sorptivity = (Cumulative Infiltration Capacity-Hydraulic Conductivity*Time)/(Time^(1/2)). To calculate Sorptivity for Cumulative Infiltration Capacity is from Philip's Equation, you need Cumulative Infiltration Capacity (Fp), Hydraulic Conductivity (k) & Time (t). With our tool, you need to enter the respective value for Cumulative Infiltration Capacity, Hydraulic Conductivity & Time and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
How many ways are there to calculate Sorptivity?
In this formula, Sorptivity uses Cumulative Infiltration Capacity, Hydraulic Conductivity & Time. We can use 1 other way(s) to calculate the same, which is/are as follows -
  • Sorptivity = ((Infiltration Capacity at Any Time t-Hydraulic Conductivity)*2)/(Time^(-1/2))
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