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Water

Water can be present at four locations and contribute as either a destabilising or a stabilising action.

Parameters

Parameter Symbol Units Notes
Water unit weight γw kN/m³ default 9.81
Ponded water at toe Hw m external water (lake, valley aquifer) leaning against the slope face
Water in the discontinuity Zw m water depth in the joint, generates uplift U on the plane
Water in the tension crack Zt m only with TC; generates force V perpendicular to the crack
Pressure distribution none / triangular max-mid / triangular max-toe / triangular max-at-crack-base
Permeable slope bool connects ponded and joint water hydrostatically

Force decomposition

Action Formula Direction
Uplift on the failure plane U = ½·γw·Zw·swet perpendicular to the plane, pushing the wedge outward
Water in the crack V = ½·γw·Zt² perpendicular to the crack, pushing the wedge toward the valley
Ponded at toe Up = ½·γw·Hw² perpendicular to the slope face, pushing back into the wedge (stabilising)

Pressure distribution

The four options control how the pore water pressure varies along the failure plane:

  • None — no uplift on the plane (default when Zw = 0)
  • Triangular max at mid-height — pressure peaks at L/2, zero at toe and at crest
  • Triangular max at toe — pressure peaks at the toe (typical of valley aquifer)
  • Triangular max at crack base — pressure peaks at the bottom of the tension crack (typical of perched aquifer)

Permeable slope toggle

When enabled, the external ponded water and the joint water are hydraulically connected. Zw is overridden to match Hw, and U/Up are computed consistently to avoid double counting.

On the section

  • U vector: perpendicular to the failure plane, halfway along O→C
  • V vector: perpendicular to the TC, halfway along C→D
  • Up vector: perpendicular to the slope face, halfway along O→B

The blue dashed line shows the water level at the toe (Hw) and the water depth in the crack (Zt) is shown by a dashed level on the tension crack.