Soil Salinity, Sodicity, Waterlogging and Reclamation MCQs 2026
50 questions with detailed answers · 0 from past papers · 5 quiz batches available
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- Q1 medium
A common reason reclamation of salt-affected land fails is applying leaching water without adequate
💡 Explanation:Without an outlet for saline water, leached salts cannot leave the field and may return to the root zone.
- Q2 medium
Biosaline agriculture focuses on productive use of saline land and water by growing
💡 Explanation:Biosaline agriculture uses salt-tolerant species, improved management and sometimes saline water where conventional crops fail.
- Q3 hard
Reuse of saline drainage water is safest when managed through blending, suitable irrigation scheduling and
💡 Explanation:Drainage water reuse requires matching water quality with crop tolerance, soil conditions, leaching and drainage.
- Q4 easy
The SI-compatible unit commonly used for soil electrical conductivity is
💡 Explanation:Soil and water salinity are commonly reported as decisiemens per meter, abbreviated dS/m.
- Q5 hard
The term black alkali is commonly associated with sodic soils because sodium disperses organic matter forming dark
💡 Explanation:Sodic conditions can disperse humus and produce dark surface staining, historically called black alkali.
- Q6 hard
Compared with sodic soils, saline soils often have better permeability because soluble salts promote
💡 Explanation:Electrolytes in saline soils compress the diffuse double layer and help clay particles remain flocculated.
- Q7 easy
Arid and semi-arid climates favor soil salinity because evaporation often exceeds
💡 Explanation:Low rainfall and high evaporation reduce natural leaching and concentrate salts near the soil surface.
- Q8 medium
In arid areas, a shallow water table within about one to two meters can promote salinization through
💡 Explanation:Shallow saline groundwater can move upward by capillarity; evaporation leaves salts in the upper soil.
- Q9 medium
Among the listed crops, the crop usually regarded as sensitive to salinity is
💡 Explanation:Beans are relatively salt-sensitive compared with barley, cotton and sugar beet.
- Q10 medium
Raised-bed planting can help in waterlogged or saline fields by improving root-zone aeration and
💡 Explanation:Beds elevate the crop root zone and allow excess water and salts to move away from the seed line.
- Q11 easy
During the early years after reclamation, a salt-affected field should preferably be planted with
💡 Explanation:Salt-tolerant crops help maintain production while reclamation gradually improves the root-zone environment.
- Q12 hard
Gypsum requirement estimates the amount of gypsum needed to replace a desired quantity of
💡 Explanation:Gypsum requirement is calculated to supply enough calcium to lower exchangeable sodium to a target level.
- Q13 medium
Hydraulic conductivity of a sodic soil usually decreases because clay particles become
💡 Explanation:Clay dispersion blocks pores and reduces the rate at which water can move through the soil.
- Q14 medium
Sodium adsorption ratio is mainly used as an index of the sodicity hazard of
💡 Explanation:SAR estimates the tendency of irrigation water to increase exchangeable sodium in soils.
- Q15 easy
Exchangeable sodium percentage is calculated as exchangeable sodium divided by cation exchange capacity, multiplied by
💡 Explanation:ESP expresses the proportion of the exchange complex occupied by sodium as a percentage.
- Q16 medium
Salt-affected soils are commonly classified using ECe, pH and
💡 Explanation:ECe measures salinity, pH indicates alkalinity and ESP or SAR indicates sodium hazard.
- Q17 medium
Specific ion toxicity in salt-affected soils is commonly caused by excessive sodium, chloride or
💡 Explanation:Besides osmotic stress, ions such as Na+, Cl- and boron can accumulate to toxic levels in sensitive crops.
- Q18 medium
The first physiological effect of salinity on many crops is reduced water uptake due to
💡 Explanation:Salts lower the soil water potential, making it harder for roots to extract water even when soil appears moist.
- Q19 easy
Brackish irrigation water is water containing appreciable amounts of
💡 Explanation:Brackish water has more dissolved salts than fresh water and must be managed according to crop tolerance, soil and drainage.
- Q20 medium
Flooding a saline field for leaching is effective only when the soil also has adequate
💡 Explanation:Leaching water must infiltrate and leave the profile; otherwise salts remain or return to the surface.
- Q21 hard
Pyrite and other acid-forming amendments aid sodic soil reclamation by generating acidity that releases
💡 Explanation:Acid dissolves calcium carbonate in calcareous soils, providing calcium for sodium replacement.
- Q22 hard
Elemental sulfur can help reclaim calcareous sodic soils because oxidation produces acid that dissolves
💡 Explanation:Acid generated from sulfur oxidation dissolves native CaCO3, releasing calcium to replace exchangeable sodium.
- Q23 medium
Adding organic matter to sodic soils helps reclamation by improving aggregation and
💡 Explanation:Organic amendments improve structure, microbial activity and permeability, supporting leaching of salts and sodium.
- Q24 medium
Interceptor drains along canals are designed mainly to reduce
💡 Explanation:Interceptor drains capture seepage water before it raises the water table in adjacent command areas.
- Q25 hard
Leaching requirement is the extra fraction of irrigation water needed to
💡 Explanation:Leaching requirement estimates how much additional water must pass through the root zone to maintain acceptable salinity.
- Q26 easy
Open surface drains in irrigated fields are used primarily to remove
💡 Explanation:Open drains help remove runoff and shallow seepage water, reducing waterlogging and salinity risk.
- Q27 medium
Subsurface tile drainage is installed mainly to
💡 Explanation:Subsurface drains collect and remove excess groundwater, improving aeration and reducing salt accumulation.
- Q28 medium
Rice tolerates flooded conditions better than many upland crops because its plants develop
💡 Explanation:Aerenchyma tissue allows oxygen transport from shoots to roots under submerged conditions.
- Q29 medium
The high pH of sodic soils is largely associated with hydrolysis of
💡 Explanation:Sodium carbonate and exchangeable sodium generate alkaline conditions, often pushing pH above 8.5.
- Q30 hard
Irrigation water with high residual sodium carbonate tends to increase soil sodicity because it precipitates calcium and magnesium as
💡 Explanation:Carbonate and bicarbonate ions remove Ca and Mg from solution, increasing the relative sodium hazard.
- Q31 hard
Residual sodium carbonate in irrigation water evaluates the hazard caused by carbonate and bicarbonate reducing soluble
💡 Explanation:High RSC water can precipitate Ca and Mg, leaving sodium dominant and increasing sodicity risk.
- Q32 medium
After applying gypsum to a sodic soil, the displaced sodium must be removed mainly by
💡 Explanation:Chemical replacement alone is incomplete; leaching and drainage are needed to remove sodium salts from the root zone.
- Q33 easy
The primary reclamation practice for saline but non-sodic soils is
💡 Explanation:Since saline soils mainly contain soluble salts, they are reclaimed by dissolving and removing salts from the root zone.
- Q34 medium
Capillary rise from a shallow saline water table causes salinization by carrying salts toward the surface where water
💡 Explanation:In arid climates, upward movement and evaporation leave salts concentrated in the upper soil profile.
- Q35 medium
A common cause of waterlogging in canal-irrigated areas is seepage combined with
💡 Explanation:Canal seepage, over-irrigation and poor drainage raise the water table and saturate the root zone.
- Q36 easy
Waterlogging in agriculture means the crop root zone is saturated long enough to cause
💡 Explanation:When pores are filled with water, gas exchange slows and roots suffer from oxygen deficiency.
- Q37 medium
Effective drainage is essential in salinity reclamation because it removes
💡 Explanation:Without drainage, leached salts remain in the profile or return upward with a rising water table.
- Q38 easy
Leaching of saline soils means applying good quality water to move salts
💡 Explanation:Leaching dissolves and carries soluble salts downward beyond the main rooting depth when drainage is adequate.
- Q39 medium
Gypsum improves a sodic soil because calcium from gypsum replaces exchangeable sodium and the sodium is then
💡 Explanation:Calcium displaces sodium from exchange sites; adequate water and drainage are then needed to remove sodium salts.
- Q40 easy
The amendment most commonly used for reclaiming sodic soils is
💡 Explanation:Gypsum provides soluble calcium that replaces exchangeable sodium on the soil exchange complex.
- Q41 medium
Poor infiltration and surface sealing in sodic soils are mainly caused by
💡 Explanation:Exchangeable sodium weakens aggregation and disperses clay, clogging pores and reducing hydraulic conductivity.
- Q42 easy
A white crust on the soil surface in arid irrigated fields usually indicates accumulation of
💡 Explanation:Evaporation draws saline water upward and leaves salts behind as a whitish surface crust.
- Q43 hard
Sodium adsorption ratio of irrigation water is calculated from sodium relative to
💡 Explanation:SAR = Na / sqrt((Ca + Mg) / 2), with ionic concentrations expressed in milliequivalents or millimoles of charge per liter.
- Q44 medium
A saline-sodic soil generally has both ECe greater than 4 dS/m and
💡 Explanation:Saline-sodic soils contain enough soluble salts and exchangeable sodium to meet both saline and sodic criteria.
- Q45 medium
A sodic soil is commonly characterized by ESP above 15 and soil pH usually
💡 Explanation:High exchangeable sodium hydrolyzes and disperses soil colloids, giving sodic soils a high pH and poor physical condition.
- Q46 medium
A typical saline soil has ECe greater than 4 dS/m, ESP less than 15 and pH usually
💡 Explanation:Saline soils have high soluble salts but not enough exchangeable sodium to disperse clay; pH is commonly below 8.5.
- Q47 easy
Soil sodicity is mainly a problem of excessive
💡 Explanation:Sodicity is diagnosed by high exchangeable sodium percentage or related sodium hazard indices that affect structure and infiltration.
- Q48 easy
The most common laboratory measure used to assess soil salinity is
💡 Explanation:ECe, measured in dS/m, estimates the concentration of soluble salts in the soil saturation extract.
- Q49 medium
Among common field crops, the crop generally considered relatively salt tolerant is
💡 Explanation:Barley is one of the more salt-tolerant cereals and is often used as an initial crop on moderately saline land.
- Q50 easy
Soil salinity refers to the presence in the root zone of excessive
💡 Explanation:Salinity is caused by soluble salts accumulating to levels that restrict water uptake and crop growth.