Difficulty: Easy
Correct Answer: All the above
Explanation:
Introduction / Context:Slope stability is a fundamental topic in highway alignment and geotechnical engineering. Failures such as landslides can be triggered by geometry, geology, and hydrology. A designer must understand how these factors combine before cutting, filling, or situating roads in hilly terrain.
Given Data / Assumptions:
Concept / Approach:Slope stability depends on resisting forces (shear strength) versus driving forces (self-weight, water pressure, surcharge). Material type and structure (nature of slope), inclination (angle), geologic defects (joints, bedding, faults), and groundwater regime (pore pressure) all alter the factor of safety.
Step-by-Step Solution:
Identify material factors: soil type, plasticity, rock discontinuities control cohesion and friction angle.Assess geometric factor: steeper angles raise driving shear stress along potential slip surfaces.Evaluate geologic setting: bedding planes dipping out of the slope, faults, and weathering zones reduce stability.Consider groundwater: elevated pore water pressure reduces effective stress and shear strength; seepage adds destabilizing forces.Verification / Alternative check:Engineers quantify stability via limit-equilibrium or numerical methods. Changing any listed factor (flattening a slope, draining groundwater, or buttressing weak layers) measurably increases the factor of safety, confirming their combined influence.
Why Other Options Are Wrong:Each single-factor option omits other equally critical influences; slope failures are multi-factor phenomena.
Common Pitfalls:Ignoring seasonal groundwater rise; assuming rock slopes are always stable; overlooking weak interlayers parallel to the slope face.
Final Answer:All the above
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