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Question 1
ప్రశ్న 1
In irrigation engineering, what is meant by the effective root zone of a crop?
Explanation:
The effective root zone is the portion of the soil profile occupied by roots that actively contribute substantially to crop water uptake. Its depth depends on the crop, growth stage, soil conditions and any restrictive layers. Root-zone depth is important because soil-water storage available to the crop is calculated over this depth. Water stored far below the effective root zone may not be readily accessible to the crop. Therefore Option B is correct.
వివరణ:
Question 2
ప్రశ్న 2
Which condition best describes a saturated soil?
Explanation:
At saturation, the soil pore space is essentially filled with water. Volumetric water content at saturation is therefore approximately equal to porosity when entrapped air is negligible. Saturation is wetter than field capacity because gravitational water has not yet drained from the large pores. Most upland crops do not require permanent saturation and may suffer from poor aeration under prolonged saturated conditions. Therefore Option C is correct.
వివరణ:
Question 3
ప్రశ్న 3
Which description most accurately defines field capacity of a well-drained agricultural soil?
Explanation:
Field capacity is the moisture condition reached after a thoroughly wetted soil has drained most of its readily drainable gravitational water. At that stage, downward drainage continues only relatively slowly compared with the initial drainage following saturation. Field capacity is commonly treated as the practical upper limit of plant-available soil-water storage. It is below saturation and above permanent wilting point. Therefore Option A is correct.
వివరణ:
Question 4
ప్రశ్న 4
What is the permanent wilting point in the soil-water-plant system?
Explanation:
Permanent wilting point represents the lower practical limit of soil-water availability for ordinary crop use. At this condition, the remaining water is held strongly enough that roots cannot extract water at the rate needed to sustain the plant. The soil still contains water, so permanent wilting point is not the same as an oven-dry condition. Water below this limit is generally considered unavailable for conventional irrigation calculations. Therefore Option D is correct.
వివరణ:
Question 5
ప్రశ్న 5
Which statement best describes hygroscopic water in soil?
Explanation:
Hygroscopic water is strongly adsorbed on soil-particle surfaces. The forces holding this water are much stronger than those acting on readily plant-available soil moisture. It therefore does not contribute appreciably to crop water supply under normal conditions. Hygroscopic water can remain in soil even when the soil feels air-dry. Therefore Option B is correct.
వివరణ:
Question 6
ప్రశ్న 6
For irrigation calculations, what is total available water in the crop root zone?
Explanation:
Plant-available soil water is conventionally bounded above by field capacity and below by permanent wilting point. Water above field capacity is prone to gravitational drainage and is not counted as stable root-zone storage. Water below permanent wilting point is held too strongly for normal plant extraction. Therefore total available water is based on the difference between field-capacity and wilting-point water contents integrated over the effective root depth. Hence Option C is correct.
వివరణ:
Question 7
ప్రశ్న 7
Which expression correctly represents readily available water, RAW, when p is the allowable fraction of total available water that can be depleted before significant crop water stress begins?
Explanation:
Total available water extends from field capacity to permanent wilting point, but crops are generally irrigated before that entire reserve is exhausted. The depletion fraction p specifies the portion of total available water that can be used before significant water stress is expected. Accordingly, RAW = p × TAW. The appropriate p depends on crop sensitivity, rooting characteristics, evaporative demand and management criteria. Therefore Option A is correct.
వివరణ:
Question 8
ప్రశ్న 8
A soil has volumetric water content at field capacity of 0.32 and at permanent wilting point of 0.14. If the effective root depth is 0.80 m, what is the total available water in the root zone?
Explanation:
For volumetric moisture contents, total available water is TAW = 1000(θFC - θPWP)Zr in millimetres. The moisture-content difference is 0.32 - 0.14 = 0.18. Multiplying by 0.80 m gives an equivalent water depth of 0.144 m. This is 144 mm of total available water in the root zone. Therefore Option D is correct.
వివరణ:
Question 9
ప్రశ్న 9
A crop has an effective root depth of 1.20 m in a uniform soil with θFC = 0.30 and θPWP = 0.18. What is the total available soil water?
Explanation:
The volumetric available-water fraction is 0.30 - 0.18 = 0.12. Over a root depth of 1.20 m, the available-water depth is 0.12 × 1.20 = 0.144 m. Converting metres of water to millimetres gives 144 mm. This represents the theoretical root-zone water storage between field capacity and permanent wilting point. Therefore Option B is correct.
వివరణ:
Question 10
ప్రశ్న 10
For the soil in the previous type of calculation, TAW is 144 mm. If the allowable depletion fraction p is 0.50, what is the readily available water?
Explanation:
Readily available water is RAW = p × TAW. Here p = 0.50 and TAW = 144 mm. Therefore RAW = 0.50 × 144 = 72 mm. In a simple scheduling interpretation, irrigation would be considered before depletion substantially exceeds this amount if crop stress is to be avoided. Therefore Option C is correct.
వివరణ:
Question 11
ప్రశ్న 11
A root zone is 0.90 m deep. Its volumetric water content at field capacity is 0.30 and its current volumetric water content is 0.22. Neglecting losses, what net irrigation depth is required to restore the root zone to field capacity?
Explanation:
The soil-water deficit relative to field capacity is θFC - θcurrent = 0.30 - 0.22 = 0.08. Multiplying by the 0.90 m root depth gives 0.072 m of water. This equals a net irrigation depth of 72 mm. The calculation assumes the water is stored uniformly within the specified root zone and ignores application losses. Therefore Option A is correct.
వివరణ:
Question 12
ప్రశ్న 12
A uniform root zone has θFC = 0.30, θPWP = 0.15 and current volumetric water content θ = 0.21 over a depth of 0.80 m. How much plant-available water remains above permanent wilting point?
Explanation:
Remaining plant-available water is measured above the permanent wilting point rather than above field capacity. The available moisture fraction remaining is 0.21 - 0.15 = 0.06. Over 0.80 m, this is 0.06 × 0.80 = 0.048 m. Converting to millimetres gives 48 mm. Therefore Option D is correct.
వివరణ:
Question 13
ప్రశ్న 13
A soil has gravimetric moisture contents of 25% at field capacity and 12% at permanent wilting point. Its dry bulk density is 1.40 Mg/m³, water density may be taken as 1.00 Mg/m³, and effective root depth is 0.80 m. What is the total available water depth?
Explanation:
Gravimetric water content must first be converted to volumetric water content using θv = wρb/ρw. The gravimetric available-water difference is 0.25 - 0.12 = 0.13, giving a volumetric difference of 0.13 × 1.40 = 0.182. Multiplying by the 0.80 m root depth gives 0.1456 m of water. This is 145.6 mm of total available water. Therefore Option B is correct.
వివరణ:
Question 14
ప్రశ్న 14
A soil has gravimetric water content of 24% at field capacity and 16% at the time irrigation is to be applied. Dry bulk density is 1.50 Mg/m³ and the effective root depth is 0.60 m. Taking water density as 1.00 Mg/m³, what net depth is required to refill the root zone to field capacity?
Explanation:
The gravimetric moisture deficit is 0.24 - 0.16 = 0.08. Converting to a volumetric deficit gives 0.08 × 1.50/1.00 = 0.12. Over a root depth of 0.60 m, the required storage is 0.12 × 0.60 = 0.072 m. This is a net irrigation depth of 72 mm. Therefore Option C is correct.
వివరణ:
Question 15
ప్రశ్న 15
A two-layer root zone consists of 0.40 m of soil with θFC = 0.30 and θPWP = 0.15, underlain by 0.60 m with θFC = 0.28 and θPWP = 0.16. What is the total available water in the full root zone?
Explanation:
Available water must be calculated for each soil layer separately because the moisture limits differ. In the upper layer, storage is (0.30 - 0.15) × 0.40 × 1000 = 60 mm. In the lower layer, storage is (0.28 - 0.16) × 0.60 × 1000 = 72 mm. Adding the two contributions gives 132 mm. Therefore Option A is correct.
వివరణ:
Question 16
ప్రశ్న 16
For the same two-layer root zone, current volumetric water contents are 0.22 in the upper 0.40 m and 0.20 in the lower 0.60 m. What net depth is required to restore both layers to field capacity?
Explanation:
The upper-layer deficit is (0.30 - 0.22) × 0.40 × 1000 = 32 mm. The lower-layer deficit is (0.28 - 0.20) × 0.60 × 1000 = 48 mm. The total root-zone deficit is therefore 32 + 48 = 80 mm. This is the net depth that must be stored if both layers are to return to field capacity. Therefore Option D is correct.
వివరణ:
Question 17
ప్రశ్న 17
A field requires a net irrigation depth of 60 mm to refill the crop root zone. If field application efficiency is 75%, what gross depth must be applied at the field inlet, neglecting other conveyance losses?
Explanation:
Application efficiency is the ratio of water beneficially stored in the root zone to water delivered for field application. Therefore the required gross field depth is net depth divided by efficiency. The calculation is 60/0.75 = 80 mm. The additional 20 mm represents the allowance for application losses under the stated efficiency. Therefore Option B is correct.
వివరణ:
Question 18
ప్రశ్న 18
For the same uniform soil with unchanged θFC and θPWP, what happens to total available water in the root zone if the effective rooting depth increases from 0.60 m to 0.90 m?
Explanation:
For uniform soil, TAW is proportional to the effective root depth when field-capacity and wilting-point moisture contents remain unchanged. Increasing root depth from 0.60 to 0.90 m multiplies the storage by 0.90/0.60 = 1.5. Thus total available water increases by 50 percent. This assumes roots can effectively extract water throughout the additional soil depth. Therefore Option C is correct.
వివరణ:
Question 19
ప్రశ్న 19
What normally happens when a freely drained soil is wetted to saturation and then allowed to drain without further inflow?
Explanation:
At saturation, essentially all pore spaces are water-filled. Once external water supply stops, gravity causes water in the larger and better-connected pores to drain downward. The drainage rate becomes much smaller after this readily drainable water has left the root zone. The remaining condition is described approximately as field capacity in irrigation practice. Therefore Option A is correct.
వివరణ:
Question 20
ప్రశ్న 20
Why is routine irrigation designed to refill the active root zone approximately to field capacity rather than deliberately maintaining an ordinary upland crop soil at saturation?
Explanation:
Water added beyond the storage needed to reach field capacity is increasingly subject to gravitational drainage below the root zone. Maintaining ordinary upland soils in a saturated condition also displaces air from pore spaces. Many crop roots require oxygen for respiration and can be harmed by prolonged poor aeration. Irrigation management therefore generally aims to replenish the useful soil-water reservoir without unnecessary saturation and deep percolation. Therefore Option D is correct.
వివరణ:
Question 21
ప్రశ్న 21
Two soils have the same field-capacity water content, but Soil X has a much higher permanent wilting-point water content than Soil Y. Which soil has the larger available-water capacity, assuming equal root depth?
Explanation:
Available-water capacity depends on the difference between field-capacity and permanent-wilting-point water contents. If field capacity is the same for both soils, the soil with the lower wilting-point water content has the larger difference. Therefore Soil Y stores more water within the conventional plant-available range. A high total water content does not necessarily mean that more of the water can be extracted by plants. Hence Option B is correct.
వివరణ:
Question 22
ప్రశ్న 22
A crop root zone has TAW = 120 mm and the allowable depletion fraction p = 0.40. If root-zone depletion has reached 55 mm, which interpretation is most appropriate under this scheduling criterion?
Explanation:
The readily available water is RAW = p × TAW = 0.40 × 120 = 48 mm. A depletion of 55 mm is larger than this threshold. The root zone still contains some plant-available water because the full TAW of 120 mm has not been depleted. However, under the stated management criterion, crop water stress may begin once depletion exceeds the 48 mm readily available amount. Therefore Option C is correct.
వివరణ:
Question 23
ప్రశ్న 23
A net root-zone deficit of 72 mm is to be replenished over an irrigated area of 2.0 hectares. Neglecting application losses, what volume of water must be stored in the soil?
Explanation:
A depth of 72 mm is 0.072 m. Two hectares correspond to 20,000 m². The required stored volume is depth multiplied by area, or 0.072 × 20,000. This gives 1440 m³ of net root-zone storage. Therefore Option A is correct.
వివరణ:
Question 24
ప్రశ్న 24
Consider the following statements about soil-water-plant relationships: I. Field capacity is below saturation in a freely drained soil. II. Permanent wilting point is the lower conventional limit of plant-available water. III. Total available water in a uniform root zone is proportional to θFC - θPWP and effective root depth. IV. Readily available water is generally only a fraction of total available water. Which option is correct?
Explanation:
Statement I is correct because gravitational drainage removes water after saturation before field capacity is reached. Statement II correctly identifies permanent wilting point as the lower conventional limit of water available to crops. Statement III follows directly from the root-zone storage relation for volumetric water contents. Statement IV is correct because irrigation is normally scheduled before the entire available reserve is exhausted. Therefore all four statements are correct and Option D is the valid answer.
వివరణ:
Question 25
ప్రశ్న 25
A crop is grown in a soil with TAW = 160 mm. The selected readily available fraction is p = 0.50, and current root-zone depletion is 70 mm. No rainfall is expected. What is the most appropriate interpretation?
Explanation:
With TAW = 160 mm and p = 0.50, the readily available water is 80 mm. The current depletion of 70 mm remains below that threshold. Thus the crop has not yet reached the selected management limit under the stated criterion. Irrigation should nevertheless be scheduled in time to prevent depletion from materially exceeding about 80 mm if water stress is to be avoided. Therefore Option B is correct.
వివరణ:
Answer Key సమాధానాల పట్టిక
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Question 1 ప్రశ్న 1Answer: B. The soil depth from which the crop extracts a major part of the water required for growth సమాధానం: B.
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Question 2 ప్రశ్న 2Answer: C. Essentially all pore spaces are filled with water, apart from possible small amounts of entrapped air సమాధానం: C.
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Question 3 ప్రశ్న 3Answer: A. The soil-water content remaining after excess gravitational water has drained and downward drainage has become relatively slow సమాధానం: A.
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Question 4 ప్రశ్న 4Answer: D. The soil-water content at which a plant can no longer extract sufficient water and remains wilted unless water is added సమాధానం: D.
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Question 5 ప్రశ్న 5Answer: B. It is water held very tightly as thin adsorbed films on soil particles and is generally unavailable to plants సమాధానం: B.
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Question 6 ప్రశ్న 6Answer: C. The water stored between field capacity and permanent wilting point over the effective root depth సమాధానం: C.
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Question 7 ప్రశ్న 7Answer: A. RAW = p × TAW సమాధానం: A.
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Question 8 ప్రశ్న 8Answer: D. 144 mm సమాధానం: D.
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Question 9 ప్రశ్న 9Answer: B. 144 mm సమాధానం: B.
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Question 10 ప్రశ్న 10Answer: C. 72 mm సమాధానం: C.
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Question 11 ప్రశ్న 11Answer: A. 72 mm సమాధానం: A.
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Question 12 ప్రశ్న 12Answer: D. 48 mm సమాధానం: D.
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Question 13 ప్రశ్న 13Answer: B. 145.6 mm సమాధానం: B.
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Question 14 ప్రశ్న 14Answer: C. 72 mm సమాధానం: C.
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Question 15 ప్రశ్న 15Answer: A. 132 mm సమాధానం: A.
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Question 16 ప్రశ్న 16Answer: D. 80 mm సమాధానం: D.
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Question 17 ప్రశ్న 17Answer: B. 80 mm సమాధానం: B.
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Question 18 ప్రశ్న 18Answer: C. It increases by 50%, assuming the additional depth has the same soil properties సమాధానం: C.
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Question 19 ప్రశ్న 19Answer: A. Gravitational water drains from the larger pores and the soil water content approaches field capacity సమాధానం: A.
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Question 20 ప్రశ్న 20Answer: D. Because water substantially above field capacity tends to drain and prolonged saturation can reduce root-zone aeration సమాధానం: D.
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Question 21 ప్రశ్న 21Answer: B. Soil Y, because available water is the difference between field capacity and permanent wilting point సమాధానం: B.
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Question 22 ప్రశ్న 22Answer: C. The depletion has exceeded RAW = 48 mm, so irrigation is due if the aim is to avoid significant water stress సమాధానం: C.
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Question 23 ప్రశ్న 23Answer: A. 1440 m³ సమాధానం: A.
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Question 24 ప్రశ్న 24Answer: D. I, II, III and IV సమాధానం: D.
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Question 25 ప్రశ్న 25Answer: B. The depletion is still below RAW = 80 mm, but irrigation should be planned before depletion materially exceeds about 80 mm if the chosen no-stress criterion is to be maintained సమాధానం: B.
