Hydraulic Conductivity

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Jul 24, 2020, 6:28:07 PM

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May 15, 2014, 9:00:37 AM

K = \frac{Q}{i \cdot A \cdot t_{E}}

$K = Q /( i * A * t_E )$

(Q) Total quantity of water

$(Q)"Total quantity of water"$

(i) Hydraulic gradient

$(i)"Hydraulic gradient"$

(A) Cross section are perpendicular to flow

$(A)"Cross section are perpendicular to flow"$

(t_{E}) Elapsed time during fall

$(t_E)"Elapsed time during fall"$

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61c7a538-dc0f-11e3-b7aa-bc764e2038f2

Hydraulic conductivity, symbolically represented as K, is a property of vascular plants, soils and rocks, that describes the ease with which a fluid (usually water) can move through pore spaces or fractures.

Where

$Q$ $Q$ is the total quantity of water for constant head
$i$ $i$ is the hydraulic gradient
$A$ $A$ is the cross section area (perpendicular to flow)
$t_{E}$ $t_E$ elapsed time during falling head

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