2/28/2015 Seepage Chapter 7 Laplace’s Equation 1
2/28/2015 Laplace’s Equation � � ���� A � ��� � � � ���� � ��� � Laplace’s Equation No storage No drainage Darcy’s Law Anisotropic Soil Isotropic Soil 2
2/28/2015 Solution of Laplace’s Equation Since water can Flow Line only flow due to a change in head, and equipotential lines are lines of constant head, the flow lines must be perpendicular to the equipotential Equipotential Line lines everywhere. h = constant Flow Nets h = H 1 h = H 2 Upstream and downstream surfaces are equipotential lines 3
2/28/2015 Flow Nets q = 0 q = 0 All impervious boundaries are flow lines Flow Nets Flow lines and equipotential lines are orthogonal 4
2/28/2015 Flow Nets “Square” Ideally, the “cells” in the flow net should be “square” Flow Net Example Flow lines are to upstream ground surface Flow lines are to face of toe filter faces Equipotential lines are to impervious boundaries Flow lines are to equipotential lines everywhere “Cells in the flow net are “square” everywhere 5
2/28/2015 Common Flow Net Mistakes Flow Lines Not Perpendicular Extraneous Equipotential Lines Not Square Common Flow Net Mistakes Not a right angle Disappearing Flow Lines Equipotential Lines Not Perpendicular 6
2/28/2015 Correctly Drawn Flow Net Seepage Calculations ∆� � � �� � � � � � � � � � � � � � 1 � � � � � � � � � 7
2/28/2015 Seepage Calculations Seepage Calculations ∆� � � � � � � � � � � � � � � � � � � � � � � ⋯ 8
2/28/2015 Seepage Calculations ∆� � � � Total head loss � � # of head drops Seepage Calculations � ∆� � �� � 3 flow channels � � � � � � 8 head drops H ⑧ ❶ ❷ ❸ ① ② ③ ④ ⑤ ⑥ ⑦ 9
2/28/2015 Flow Nets Flow Nets 10
2/28/2015 Example 1. What is the head at points a, b, c, d and e ? 2. What is the seepage rate beneath the dam? 16 m e a c � � 3 � 10 �� ��/��� b d Partial Flow Channels 11
2/28/2015 Partial Flow Channels ∆� � � � � � � � � � � � � � � � � � � � � � � � � � ⋯ Partial Flow Channels 12
2/28/2015 Partial Flow Channels 2.38 flow channels 6 head drops � � � 1 2.38 flow channels � � � 1 � � � 0.38 13
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