Difficulty: Medium
Correct Answer: 2.31
Explanation:
Introduction:
Irrigation flow sizing often reduces to converting a depth of water over an area and time into a steady discharge. This problem illustrates the straightforward volumetric approach for evapotranspiration (ET) demands when losses are neglected and application is uniform over the design period.
Given Data / Assumptions:
Concept / Approach:
Compute required daily (or total) volume and divide by time to obtain discharge. Since ET occurs uniformly over 20 days, the daily depth is 1 mm (0.001 m). Multiply by area to get daily volume; convert to L/s using 1 m^3 = 1000 L and 1 day = 86400 s.
Step-by-Step Solution:
Verification / Alternative check:
Alternatively, compute total volume (A * 0.020 m = 4000 m^3) and divide by 20 days to obtain the same daily rate; conversion yields 2.31 L/s again.
Why Other Options Are Wrong:
2.52 and 2.01 result from rounding or area mis-conversions; 1.52 assumes a smaller daily depth; 3.10 is too high for the given ET.
Common Pitfalls:
Forgetting that 1 ha = 10,000 m^2; confusing mm/day with cm/day; neglecting to convert days to seconds correctly when expressing L/s.
Final Answer:
2.31
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