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CivilWater Resources Management
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Dicken's formula for finding discharge is

A

Q=CтЛЕA3/5Q = C \cdot A^{3/5}Q=CтЛЕA3/5

B

Q=CтЛЕA3/4Q = C \cdot A^{3/4}Q=CтЛЕA3/4

C

Q=CтЛЕA4/5Q = C \cdot A^{4/5}Q=CтЛЕA4/5

D

none of the above

Correct Answer

тЪЩя╕П TE тАв Technical Concept & PrincipleCivilWater Resources Management
Option B

Q=CтЛЕA3/4Q = C \cdot A^{3/4}Q=CтЛЕA3/4

Quick Summary:

Dicken's formula is an empirical formula used to estimate the maximum flood discharge from a catchment area. It relates the peak flood discharge (QQQ) to the catchment area (AAA) using a constant (CDC_DCDтАЛ) that varies based on the geographical and climatic characteristics of the region.

тЪЩя╕ПTETechnical SolutionConcept & Principle
ЁЯТб Explanation

Dicken's formula is an empirical formula used to estimate the maximum flood discharge from a catchment area. It relates the peak flood discharge (QQQ) to the catchment area (AAA) using a constant (CDC_DCDтАЛ) that varies based on the geographical and climatic characteristics of the region.

ЁЯФв Key Formulas

Q=CDтЛЕA3/4Q = C_D \cdot A^{3/4}Q=CDтАЛтЛЕA3/4 тАФ Dicken's formula for peak discharge estimation

тЪЩя╕П Working Principle

The formula assumes that the peak discharge is proportional to a power of the catchment area. This relationship accounts for the fact that as the catchment size increases, the intensity and duration of rainfall causing peak discharge do not increase linearly, leading to the exponent being less than 1.

ЁЯУМ Key Points
  • тЦ╕

    Dicken's formula is primarily used for basins in North and Central India.

  • тЦ╕

    The constant CDC_DCDтАЛ (Dicken's constant) depends on the rainfall intensity, soil type, and catchment characteristics.

  • тЦ╕

    It is an empirical method, meaning it is based on historical data rather than derived from physical fluid dynamics laws.

  • тЦ╕

    Other similar empirical formulas include Ryves formula (Q=CтЛЕA2/3Q = C \cdot A^{2/3}Q=CтЛЕA2/3) and Inglis formula.

тЬЕ Advantages
  • тЦ╕

    Simple to apply

  • тЦ╕

    Requires minimal meteorological data

тЭМ Disadvantages / Limitations
  • тЦ╕

    Regional specificity (limited accuracy outside North India)

  • тЦ╕

    Does not account for complex watershed parameters

ЁЯЫая╕П Applications / Uses
  • тЦ╕

    Estimation of peak flood for small to medium drainage basins

  • тЦ╕

    Design of highway culverts and small bridges

ЁЯУД Additional Information
  • тЦ╕

    Dicken's formula: Q=CDтЛЕA3/4Q = C_D \cdot A^{3/4}Q=CDтАЛтЛЕA3/4

  • тЦ╕

    Ryves formula: Q=CRтЛЕA2/3Q = C_R \cdot A^{2/3}Q=CRтАЛтЛЕA2/3

  • тЦ╕

    Inglis formula: Q=124тЛЕAA+10.4Q = \frac{124 \cdot A}{\sqrt{A + 10.4}}Q=A+10.4тАЛ124тЛЕAтАЛ

  • тЦ╕

    Option A (A3/5A^{3/5}A3/5) and C (A4/5A^{4/5}A4/5) are incorrect exponents for this specific empirical relation.

ЁЯУК Diagram / Illustration
Dicken's FormulaQ = C ┬╖ A^{3/4}Q: Peak Discharge (m┬│/s)A: Catchment Area (km┬▓)
тЬЕ

B is correct тАФ Dicken's formula for finding flood discharge is represented as Q=CтЛЕA3/4Q = C \cdot A^{3/4}Q=CтЛЕA3/4.

Core Concepts Used
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Empirical Hydrology Flood Estimation Catchment Area Characteristics
ЁЯТб EXAM TIP

Always remember the exponents: Dicken uses 3/4, Ryves uses 2/3. Examiners frequently test the variation in these empirical coefficients.

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