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SSC 200 Exam 3 Questions with Correct Answers Latest Update 2026/2027

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SSC 200 Exam 3 Questions with Correct Answers Latest Update 2026/2027 Cohesion - Answers Attraction between water molecules due to hydrogen bonding; explains surface tension. Adhesion - Answers Attraction between water molecules and solid surfaces (soil particles); causes water to stick to soil. Surface tension - Answers Result of cohesive forces at the air-water interface that allow water to resist external force. Capillarity - Answers Movement of water in small pores or wicks caused by cohesion + adhesion; stronger in smaller pores. Gravitational potential - Answers Positive energy from gravity pulling water downward; drains macropores. Matric potential - Answers Negative potential from adhesion/cohesion in pores; strongest in small pores; controls plant water uptake. Osmotic potential - Answers Negative potential from dissolved salts; water moves from low to high salt concentration. Total water potential - Answers Sum of gravitational + matric + osmotic; determines water-flow direction. Macropores - Answers Large pores that drain quickly; between saturation and field capacity; water unavailable to plants. Mesopores - Answers Medium pores holding capillary water between field capacity and wilting point; plant-available. Micropores - Answers Very small pores; water held too tightly (between wilting point and oven dry); unavailable. Saturation - Answers All pores filled with water; no air. Field capacity - Answers Water held against gravity after drainage stops; best for plant growth. Wilting point - Answers Water held too tightly for plants to extract. Air dry / Hygroscopic - Answers Only thin film of adhesive water remains; not usable. Oven dry - Answers No water remaining in soil. Gravitational water - Answers Between saturation and field capacity; drains freely; not available. Plant-available water - Answers Between field capacity and wilting point; stored in mesopores. Unavailable water - Answers Between wilting point and oven dry; held in micropores. Clayey soil water holding - Answers High total water; many micropores; less available water. Sandy soil water holding - Answers Low total water; more macropores; drains rapidly. Gypsum block - Answers Measures soil water by electrical resistance. Tensiometer - Answers Measures tension of water due to adhesion with soil. TDR (Time Domain Reflectometry) - Answers Uses radar pulses to estimate volumetric water content. Bulk density formula - Answers BD = Weight of oven-dry soil ÷ Volume of soil. Gravimetric water content - Answers (Wet weight − Dry weight) ÷ Dry weight. Volumetric water content - Answers (Wet weight − Dry weight) ÷ Total volume or Gravimetric × BD. Porosity formula - Answers 1 − (Bulk density ÷ 2.65 g/cm³). Condensation - Answers Water vapor changes to liquid. Infiltration - Answers Water enters the soil surface. Runoff - Answers Precipitation that flows across land surface. Evaporation - Answers Liquid water becomes vapor. Transpiration - Answers Plants release water vapor through leaves. Evapotranspiration (ET) - Answers Evaporation + transpiration = total water loss to atmosphere. Sandy soils infiltration - Answers Fast infiltration; low water storage. Clayey soils infiltration - Answers Slow infiltration; higher storage; more lateral flow.

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Institution
SSC 200
Course
SSC 200

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SSC 200 Exam 3 Questions with Correct Answers Latest Update 2026/2027

Cohesion - Answers Attraction between water molecules due to hydrogen bonding; explains
surface tension.

Adhesion - Answers Attraction between water molecules and solid surfaces (soil particles);
causes water to stick to soil.

Surface tension - Answers Result of cohesive forces at the air-water interface that allow water
to resist external force.

Capillarity - Answers Movement of water in small pores or wicks caused by cohesion + adhesion;
stronger in smaller pores.

Gravitational potential - Answers Positive energy from gravity pulling water downward; drains
macropores.

Matric potential - Answers Negative potential from adhesion/cohesion in pores; strongest in
small pores; controls plant water uptake.

Osmotic potential - Answers Negative potential from dissolved salts; water moves from low to
high salt concentration.

Total water potential - Answers Sum of gravitational + matric + osmotic; determines water-flow
direction.

Macropores - Answers Large pores that drain quickly; between saturation and field capacity;
water unavailable to plants.

Mesopores - Answers Medium pores holding capillary water between field capacity and wilting
point; plant-available.

Micropores - Answers Very small pores; water held too tightly (between wilting point and oven
dry); unavailable.

Saturation - Answers All pores filled with water; no air.

Field capacity - Answers Water held against gravity after drainage stops; best for plant growth.

Wilting point - Answers Water held too tightly for plants to extract.

Air dry / Hygroscopic - Answers Only thin film of adhesive water remains; not usable.

Oven dry - Answers No water remaining in soil.

Gravitational water - Answers Between saturation and field capacity; drains freely; not available.

Plant-available water - Answers Between field capacity and wilting point; stored in mesopores.

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