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Question 1
ప్రశ్న 1
A dam foundation lies in massive basalt with high intact compressive strength, but boreholes intersect continuous open cooling joints hydraulically connected to the proposed reservoir. Which finding should control the next engineering decision?
Explanation:
Sound intact basalt can still form a discontinuous rock mass. Cooling joints may provide connected pathways for water. Joint orientation and persistence can also affect the stability of foundation blocks. Pressure tests and geological mapping can help define the relevant hydraulic and structural conditions. Foundation suitability and any grouting or drainage should be based on those findings rather than rock name alone.
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Question 2
ప్రశ్న 2
A tunnel route crosses shale containing abundant smectite-group clay, and exploratory samples show swelling on wetting. The same reach has groundwater-bearing joints. Which construction response best integrates these findings?
Explanation:
Smectite-rich materials can expand as their moisture content increases. A groundwater-bearing joint system may expose freshly excavated shale to water. Swelling can generate deformation and pressure against tunnel support. Laboratory swelling tests and field hydrogeological data help estimate the hazard. Water control and appropriate support details must be selected for the actual ground response.
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Question 3
ప్రశ్న 3
A proposed reservoir extends across limestone outcrops that react strongly with dilute hydrochloric acid, and a nearby valley contains springs and mapped sinkholes. Which investigation should take priority before declaring the basin watertight?
Explanation:
An acid reaction is consistent with calcite-rich carbonate rock. Carbonate rocks may develop solution-enlarged fractures and cavities under suitable conditions. Sinkholes and nearby springs are evidence requiring investigation of possible hydraulic connections. Seepage may bypass the dam through the reservoir rim as well as through its foundation. Tracer tests and targeted subsurface investigations can help evaluate these potential leakage routes.
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Question 4
ప్రశ్న 4
A planned water-supply tunnel has two possible orientations in schist. In the first, persistent mica-rich foliation daylights into the sidewall for a long reach; in the second, the tunnel crosses foliation more obliquely but encounters a short fractured zone. Which choice is the most defensible?
Explanation:
Foliation gives schist a mechanically directional rock-mass structure. Persistent foliation surfaces can influence sidewall slabbing or the release of blocks. Crossing foliation may shorten exposure to a particular weakness but may introduce other unfavorable joint intersections. The short fractured zone on the alternative route must also be evaluated for stability and inflow. The proper decision compares complete geological risks and constructability for both orientations.
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Question 5
ప్రశ్న 5
A proposed road cut has a slope face dipping 58 degrees toward east. A persistent clay-coated bedding plane dips 36 degrees east, with an assumed effective friction angle of 29 degrees and negligible cohesion for screening. What is the most appropriate preliminary finding?
Explanation:
The discontinuity and cut slope face both dip toward east. A plane dipping less steeply than the face in the same direction can daylight in that face. The bedding dip of 36 degrees exceeds the stated friction angle of 29 degrees. These conditions identify a potentially unfavorable planar-sliding geometry. Persistence, groundwater pressure, block dimensions and shear parameters are still needed to evaluate actual stability.
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Question 6
ప్రశ్న 6
During pilot tunnelling, two intersecting joint sets define a detachable crown wedge, and water flows from one of the joints. Which response best addresses both structural and hydraulic risks?
Explanation:
Intersecting joints can isolate wedges that are able to move into the tunnel opening. Water pressure may reduce the shear resistance along their bounding planes. Block size and release geometry influence the necessary support arrangement. Appropriately anchored bolts and surface support can help restrain identified blocks. Groundwater treatment must be designed for actual connectivity and pressure rather than presumed watertightness.
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Question 7
ప్రశ్న 7
A dam-abutment borehole has a high RQD, while excavation mapping reveals one long clay-filled shear surface dipping toward the valley and crossing the intended foundation contact. What should the engineer infer?
Explanation:
RQD reflects the proportion of sufficiently long sound core pieces in a drilling run. It does not uniquely measure the condition of an individual persistent discontinuity. A clay-filled shear surface may have much lower resistance than intact rock. Its orientation and continuity may permit a kinematically unfavorable rock mass to move. Foundation evaluation should therefore include shear properties, water pressures and block geometry.
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Question 8
ప్రశ్న 8
A low-resistivity anomaly under an alluvial valley is proposed as a productive freshwater aquifer. Nearby wells contain saline water, and boreholes in an adjacent area intercepted clay lenses. What is the strongest next step?
Explanation:
Low bulk resistivity may arise from saline pore water or clay minerals. It does not uniquely establish freshwater, porosity or sustainable discharge. Borehole records can distinguish clay lenses from sand and gravel where sampled. Hydraulic testing is needed to estimate the production response of a specific interval. Water sampling establishes whether the supply is chemically suitable for its intended use.
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Question 9
ప్రశ్న 9
In a granite upland, satellite imagery shows a lineament intersecting a valley. Resistivity data suggest a weathered zone, and one nearby borehole records a water-bearing fracture. Which decision follows logically?
Explanation:
Weathered and fractured crystalline rock can contain useful secondary groundwater openings. A lineament alone does not establish a productive fracture network. Electrical surveys can help locate changes in ground properties but do not measure well yield directly. A nearby water-bearing fracture is supporting evidence only if its spatial and hydraulic relationship is established. Targeted drilling and pumping tests provide essential confirmation before investment.
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Question 10
ప్రశ్న 10
A proposed tunnel passes beneath a buried valley. Seismic refraction indicates a fast upper unit, but boreholes show a softer, slower layer beneath it; resistivity data also vary laterally. What is the best interpretation strategy?
Explanation:
Conventional first-arrival seismic refraction can fail to resolve a slower layer beneath a faster layer. Electrical resistivity also has nonunique lithological interpretations. Borehole logs give direct information at sampled locations and can test the proposed geophysical sections. Agreement between different measurements may improve the predicted depth and extent of weak ground. Tunnel support design should use the reconciled rock and soil profile and acknowledge remaining uncertainty.
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Question 11
ప్రశ్న 11
A fractured rock tunnel passes below a piezometric surface at RL 164 m. Its exposed water-bearing joint is at RL 151 m, and the system is approximated as hydrostatic with water unit weight 10 kN/m3. Which pressure and engineering conclusion are consistent with these assumptions?
Explanation:
The relevant pressure head is the piezometric elevation minus the elevation of the joint. Thus the head difference is 164 - 151 = 13 m. Multiplying by the given water unit weight gives 13(10) = 130 kPa. This is the idealized gauge pressure before considering local hydraulic losses or construction-induced changes. Pressure and connectivity should inform tunnel stability and groundwater-treatment decisions.
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Question 12
ప్రశ్న 12
A water-conveyance tunnel approaches a mapped fault with gouge, open peripheral fractures and evidence of high groundwater head. The alternative route adds length but avoids the fault zone. What comparison is most appropriate?
Explanation:
Fault gouge can behave very differently from the intact host rock. Adjacent open fractures may provide significant inflow paths. Additional support and advance investigation may be needed to cross a damaged zone safely. A longer alternative may reduce geological uncertainty or treatment requirements. The preferred route should follow an integrated risk and cost assessment rather than length alone.
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Question 13
ప్రశ్న 13
A tunnel through alternating sandstone and weak shale can follow the bedding for 500 m or cross the shale horizon obliquely in a much shorter intersection. Both routes meet hydraulic grade requirements. Which initial geological judgment is sound?
Explanation:
Weak shale may deteriorate or deform after excavation and exposure to moisture. An alignment following the shale can create a prolonged section of difficult ground. A high-angle crossing can reduce the length of excavation within the weak unit. Nevertheless, discontinuity geometry and hydraulic conditions may make the crossing route hazardous in other ways. Both alternatives therefore require rock-mass and construction assessments before selection.
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Question 14
ప్రశ్న 14
After trial reservoir filling, a spring beyond a limestone ridge begins discharging water with a tracer previously introduced at a reservoir-side sinkhole. What should be inferred?
Explanation:
Recovery of a properly introduced tracer can provide direct evidence of hydraulic connectivity. The route may pass through solution passages within karstified carbonate rock. Such a leakage path can bypass a cutoff limited to the dam axis. Discharge monitoring and further geological investigation are needed to assess the extent and significance of leakage. Feasible treatment, water-management and safety measures must then be evaluated against the reservoir requirements.
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Question 15
ప్రశ్న 15
Two alternative dam axes are identified. Axis X crosses a fault with documented geologically recent displacement; Axis Y lies on less fractured rock but needs a larger excavation. Which investigation priority best reflects engineering geology?
Explanation:
A fault with evidence of recent displacement may present a surface-rupture hazard. Direct ground offset cannot be assumed to be prevented by ordinary structural strengthening or grouting. The alternative axis may involve increased excavation but lower geological hazard. The comparison should include fault activity, foundation stability, seepage and whole-project feasibility. A geologically defensible decision cannot rest solely on initial excavation quantities.
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Question 16
ప్రశ్న 16
A dam abutment shows sound rock at the surface but a deep, connected fracture network from packer tests. A shallow clay-rich seam is also present near the founding level. Which treatment concept best matches the evidence?
Explanation:
The shallow seam and deeper fracture network present different engineering problems. Weak material may reduce foundation shear strength or cause nonuniform deformation. Connected deep fractures may provide seepage pathways beneath or around the dam. Local foundation preparation, grouting and drainage serve different purposes and are not automatically interchangeable. The design should address each mapped condition and verify the effectiveness of the proposed treatment.
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Question 17
ప్రశ్న 17
Petrographic study of aggregate from a proposed quarry identifies abundant weathered particles and reactive sulfide minerals such as pyrite, while nearby foundation excavations show iron-stained acidic drainage. What should the project geologist recommend?
Explanation:
Pyrite can oxidize when exposed to oxygen and water under favorable conditions. Oxidation products may lead to acidic drainage and related durability concerns. Weathered rock particles can also have properties different from fresh intact material. Petrographic examination and appropriate performance testing help evaluate aggregate suitability. The project should assess both material durability and potential environmental effects of excavation and quarry runoff.
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Question 18
ప్రశ్న 18
A reservoir access road and a nearby well platform are planned on granite that has weathered extensively to clay-rich material. A fresh granite core taken below the weathered zone is very strong. What is the most appropriate foundation decision?
Explanation:
Weathering can transform feldspar-bearing granite into weak, clay-rich residual material. Its shear strength, compressibility and permeability may differ greatly from fresh granite. A strong deep core does not establish the engineering properties at a shallow foundation level. Groundwater changes can further influence the behaviour of the weathered zone. Foundations should be selected using the encountered material profile and relevant geotechnical measurements.
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Question 19
ప్రశ్న 19
A tunnel portal is proposed below an old landslide in smectite-bearing shale. Rainfall increases pore pressure along clay-rich bedding, and the planned road cut would remove support at the toe. Which approach is most appropriate?
Explanation:
An old landslide indicates that the slope has experienced movement in the past. Clay-rich bedding can act as a weak surface, particularly when pore pressure rises. Excavating the toe may reduce support and reactivate movement. Portal location and construction sequence must be informed by slope geometry, groundwater and material properties. Stabilization may require a combination of avoidance, drainage and appropriately designed structural measures.
వివరణ:
Question 20
ప్రశ్న 20
A tunnel intersects a mapped fractured aquifer supplying hillside springs. The proposed excavation could act as a drain, while a resistivity survey shows several low-resistivity zones of uncertain lithology. What is the most suitable investigation plan?
Explanation:
A tunnel can drain water from connected fractures when its hydraulic head is lower than the surrounding aquifer. This may change spring discharge and local groundwater levels. Low electrical resistivity can reflect several properties and does not establish the required hydraulic connection. Baseline measurements and hydraulic tests help distinguish meaningful effects from natural seasonal variation. Mitigation may involve route changes, pregrouting or controlled drainage, depending on the verified conditions.
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Question 21
ప్రశ్న 21
A pumping-station site occupies saturated, loose sand beside a river. A mapped active fault is nearby, and a seismic study indicates possible strong ground shaking. Which integrated hazard assessment is most appropriate?
Explanation:
Earthquake shaking may generate excess pore-water pressure in susceptible saturated granular soil. The resulting strength loss can lead to settlement or lateral spreading near a riverbank. A nearby fault may also present a direct rupture hazard depending on its location and activity. Site-specific investigations are needed to establish groundwater conditions, stratigraphy and seismic demands. Foundation and mitigation options should respond to the combined hazards rather than a single factor.
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Question 22
ప్రశ్న 22
A reservoir basin is underlain by gypsum-bearing beds with sinkholes, while a second candidate basin is underlain by comparatively intact granite with local joints. Which conclusion is most defensible for preliminary site selection?
Explanation:
Gypsum dissolves readily under suitable water-chemistry and flow conditions. Existing sinkholes suggest that solution-related ground changes may already be present. Reservoir impoundment can alter hydraulic gradients and increase leakage through connected openings. Granite is less prone to dissolution of this kind but may still contain permeable fractures. Both sites need investigations, with the gypsum site requiring particular attention to karst hazards.
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Question 23
ప్రశ్న 23
During rapid reservoir drawdown, a hillside containing an old translational slide shows high piezometric pressures that have not yet dissipated. A new access road would add fill near its crest. Which engineering action is most appropriate?
Explanation:
Rapid drawdown can remove external water support faster than pore pressures dissipate within a slope. A persistent slide surface may then have reduced effective-stress shear resistance. Placing fill near the crest may increase driving forces on the unstable mass. Site selection should account for both reservoir operations and planned construction loading. A stability analysis and suitable mitigation are needed before committing to the road alignment.
వివరణ:
Question 24
ప్రశ్న 24
Two piezometers in the SAME hydraulically connected unit are 400 m apart along a straight line. At A, ground RL is 142 m and depth to water is 6 m; at B, ground RL is 139 m and depth to water is 11 m. What is the average hydraulic-head gradient magnitude ALONG their connecting line, and where does head decrease?
Explanation:
Hydraulic head elevation at A is 142 - 6 = 136 m. At B it is 139 - 11 = 128 m. The head difference is 8 m over a 400 m separation. The average gradient magnitude along that line is 8/400 = 0.020, with head decreasing from A toward B. Two wells establish this component of the hydraulic gradient, not the complete two-dimensional groundwater-flow direction.
వివరణ:
Question 25
ప్రశ్న 25
A city must choose among three water-conveyance tunnel and reservoir layouts. Layout I is shortest but crosses an active fault and gypsum karst; Layout II is longer through mapped competent rock with some treatable joints; Layout III crosses expansive shale and a water-bearing landslide zone. Which selection process is most defensible?
Explanation:
No single geological index can rank the safety and feasibility of all three layouts. Active faults and karst can create hazards that are difficult to mitigate. Expansive shale and landslide zones introduce distinct deformation and groundwater risks. Even competent rock requires assessment of joints, seepage and excavation conditions. A defensible decision weighs verified hazards, feasible treatments, project performance and uncertainty across the alternatives.
వివరణ:
Answer Key సమాధానాల పట్టిక
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Question 1 ప్రశ్న 1Answer: C. Map joint persistence and hydraulic connection, perform appropriate water-pressure tests, and assess seepage control and rock-mass stability before acceptance. సమాధానం: C.
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Question 2 ప్రశ్న 2Answer: A. Test swelling behaviour and groundwater conditions, then plan moisture control and support or lining capable of accommodating the assessed deformation. సమాధానం: A.
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Question 3 ప్రశ్న 3Answer: D. Investigate karst passages and hydraulic links toward the springs using geological mapping, suitable drilling and tracer or other hydrogeological tests. సమాధానం: D.
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Question 4 ప్రశ్న 4Answer: B. Compare discontinuity-controlled block stability, excavation conditions and groundwater for both routes rather than relying on intact-rock strength or tunnel length alone. సమాధానం: B.
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Question 5 ప్రశ్న 5Answer: A. Planar sliding is kinematically possible because the plane daylights and its dip exceeds friction angle; a full stability assessment is still needed. సమాధానం: A.
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Question 6 ప్రశ్న 6Answer: C. Determine wedge geometry and water head, then assess appropriately anchored bolts and surface support with suitable drainage or sealing. సమాధానం: C.
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Question 7 ప్రశ్న 7Answer: B. The persistent weak surface may control rock-block stability despite high RQD, so orientation, shear strength and groundwater pressure require specific assessment. సమాధానం: B.
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Question 8 ప్రశ్న 8Answer: D. Correlate the anomaly with borehole lithology, screened-interval hydraulic tests and groundwater chemistry before estimating usable yield. సమాధానం: D.
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Question 9 ప్రశ్న 9Answer: A. Treat the intersection as a promising but unconfirmed target, verify structural connectivity with mapping and targeted drilling, and evaluate yield by a pumping test. సమాధానం: A.
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Question 10 ప్రశ్న 10Answer: C. Recognize the seismic low-velocity-layer limitation, reconcile both surveys with boreholes and revise the geological model before choosing tunnel support. సమాధానం: C.
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Question 11 ప్రశ్న 11Answer: B. 130 kPa; water pressure on the discontinuity warrants assessment of inflow, block stability and groundwater control. సమాధానం: B.
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Question 12 ప్రశ్న 12Answer: D. Compare the extra length with fault-zone instability, inflow control, support demand, construction risk and the feasibility of treatment. సమాధానం: D.
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Question 13 ప్రశ్న 13Answer: A. Shorter exposure to weak shale may favor the crossing route, but the bedding and joint orientations, groundwater and construction impacts still need evaluation. సమాధానం: A.
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Question 14 ప్రశ్న 14Answer: C. A hydraulic connection through the reservoir rim is supported, requiring quantification of leakage and evaluation of practicable cutoff or site-management options. సమాధానం: C.
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Question 15 ప్రశ్న 15Answer: B. Assess potential surface-rupture hazard and foundation conditions before selecting an axis, including whether avoiding the fault outweighs the additional excavation. సమాధానం: B.
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Question 16 ప్రశ్న 16Answer: D. Evaluate local weak-seam treatment separately from seepage-reduction grouting and pressure-relief drainage, with field verification of each objective. సమాధానం: D.
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Question 17 ప్రశ్న 17Answer: A. Investigate sulfide oxidation and durability, test the aggregate for applicable concrete-use requirements, and assess water-quality or drainage controls rather than approving the rock solely for apparent hardness. సమాధానం: A.
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Question 18 ప్రశ్న 18Answer: C. Map the weathering profile and groundwater, obtain strength and compressibility information for the actual founding materials, and adjust foundation depth or treatment accordingly. సమాధానం: C.
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Question 19 ప్రశ్న 19Answer: D. Reassess slope stability under excavation and wet-season conditions; consider portal relocation, drainage, staged excavation and engineered reinforcement where justified. సమాధానం: D.
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Question 20 ప్రశ్న 20Answer: B. Establish groundwater heads and spring baselines, investigate fault and joint connectivity, and use drilling and hydraulic tests to assess inflow and drawdown before designing sealing or drainage. సమాధానం: B.
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Question 21 ప్రశ్న 21Answer: C. Assess shaking demand, liquefaction and lateral-spreading potential, and any surface-rupture exposure before selecting the foundation and ground-improvement strategy. సమాధానం: C.
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Question 22 ప్రశ్న 22Answer: D. Give special weight to potential dissolution, leakage and collapse in the gypsum basin while investigating the granite site's discontinuities before comparing overall feasibility. సమాధానం: D.
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Question 23 ప్రశ్న 23Answer: A. Reevaluate stability under drawdown and added loading, and consider alignment adjustment, drainage and stabilization before adding the crest fill. సమాధానం: A.
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Question 24 ప్రశ్న 24Answer: D. 0.020, from A toward B. సమాధానం: D.
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Question 25 ప్రశ్న 25Answer: C. Compare site-specific fault rupture, dissolution and leakage, swelling, instability, treatment feasibility, hydraulic requirements, environmental effects and whole-life cost, using further investigation where uncertainty matters. సమాధానం: C.
