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Water Demand 
  
Fire Demand 
 Rate of fire demand is sometimes treated as a function of population and is 
worked out on the basis of empirical formulas: 
(i) As per GO Fire Demand 
 
(ii) Kuichling’s Formula 
 
 Where, Q = Amount of water required in litres/minute. 
 P = Population in thousand. 
(iii) Freeman Formula 
 
(iv) National Board of Fire Under Writers Formula 
      (a) For a central congested high valued city 
          (i) Where population < 200000 
 
          (ii) where population > 200000 
 Q = 54600 lit/minute for first fire 
 and Q=9100 to 36,400 lit/minute for a second fire. 
      (b) For a residential city. 
           (i) Small or low building, 
 Q=2,200 lit/minutes. 
           (ii) Larger or higher buildings, 
 Q=4500 lit/minute. 
 (v) Buston’s Formula 
 
  
Per Capita Demand (q) 
 
  
Page 2


  
Water Demand 
  
Fire Demand 
 Rate of fire demand is sometimes treated as a function of population and is 
worked out on the basis of empirical formulas: 
(i) As per GO Fire Demand 
 
(ii) Kuichling’s Formula 
 
 Where, Q = Amount of water required in litres/minute. 
 P = Population in thousand. 
(iii) Freeman Formula 
 
(iv) National Board of Fire Under Writers Formula 
      (a) For a central congested high valued city 
          (i) Where population < 200000 
 
          (ii) where population > 200000 
 Q = 54600 lit/minute for first fire 
 and Q=9100 to 36,400 lit/minute for a second fire. 
      (b) For a residential city. 
           (i) Small or low building, 
 Q=2,200 lit/minutes. 
           (ii) Larger or higher buildings, 
 Q=4500 lit/minute. 
 (v) Buston’s Formula 
 
  
Per Capita Demand (q) 
 
  
Assessment of Normal Variation 
(i)   
(ii)   
(iii)   
(iv)   
(v)  
(vi)  
  
Population forecasting Methods 
 
(i) Arithmetic increase method 
 
 Where, 
  Prospective or forecasted population after n decades from the present (i.e., 
last known census) 
  Population at present (i.e., last known census) 
  Number of decades between now & future. 
  Average (arithmetic mean) of population increases in the known decades. 
  
(ii) Geometric Increase Method 
 
 where, 
  Initial population. 
  Future population after ‘n’ decades. 
  Assumed growth rate (%). 
 
Page 3


  
Water Demand 
  
Fire Demand 
 Rate of fire demand is sometimes treated as a function of population and is 
worked out on the basis of empirical formulas: 
(i) As per GO Fire Demand 
 
(ii) Kuichling’s Formula 
 
 Where, Q = Amount of water required in litres/minute. 
 P = Population in thousand. 
(iii) Freeman Formula 
 
(iv) National Board of Fire Under Writers Formula 
      (a) For a central congested high valued city 
          (i) Where population < 200000 
 
          (ii) where population > 200000 
 Q = 54600 lit/minute for first fire 
 and Q=9100 to 36,400 lit/minute for a second fire. 
      (b) For a residential city. 
           (i) Small or low building, 
 Q=2,200 lit/minutes. 
           (ii) Larger or higher buildings, 
 Q=4500 lit/minute. 
 (v) Buston’s Formula 
 
  
Per Capita Demand (q) 
 
  
Assessment of Normal Variation 
(i)   
(ii)   
(iii)   
(iv)   
(v)  
(vi)  
  
Population forecasting Methods 
 
(i) Arithmetic increase method 
 
 Where, 
  Prospective or forecasted population after n decades from the present (i.e., 
last known census) 
  Population at present (i.e., last known census) 
  Number of decades between now & future. 
  Average (arithmetic mean) of population increases in the known decades. 
  
(ii) Geometric Increase Method 
 
 where, 
  Initial population. 
  Future population after ‘n’ decades. 
  Assumed growth rate (%). 
 
 where, 
  Final known population 
  Initial known population 
  Number of decades (period) between  and   
   
  
(iii) Incremental Increases Method 
 
 Where, 
  Average increase of population of known decades 
  Average of incremental increases of the known decades. 
  
(iv) Decreasing rate of growth method 
 Since the rate of increase in population goes on reducing, as the cities reach 
towards saturation, a method which makes use of the decrease in the percentage 
increase, in many a times used, and gives quite rational results. In this method, the 
average decrease in the percentage increase is worked out, and is then subtraced 
from the latest percentage increase for each successive decade. This method is 
however, applicable only in cases, where the rate of growth shows a downward 
trend. 
  
(v) Logistic Curve Method 
(a)  
 Where, 
  Population of the start point. 
  Saturation population 
  Population at any time t from the origin. 
  Constant. 
  
  
Development of Ground Water 
Page 4


  
Water Demand 
  
Fire Demand 
 Rate of fire demand is sometimes treated as a function of population and is 
worked out on the basis of empirical formulas: 
(i) As per GO Fire Demand 
 
(ii) Kuichling’s Formula 
 
 Where, Q = Amount of water required in litres/minute. 
 P = Population in thousand. 
(iii) Freeman Formula 
 
(iv) National Board of Fire Under Writers Formula 
      (a) For a central congested high valued city 
          (i) Where population < 200000 
 
          (ii) where population > 200000 
 Q = 54600 lit/minute for first fire 
 and Q=9100 to 36,400 lit/minute for a second fire. 
      (b) For a residential city. 
           (i) Small or low building, 
 Q=2,200 lit/minutes. 
           (ii) Larger or higher buildings, 
 Q=4500 lit/minute. 
 (v) Buston’s Formula 
 
  
Per Capita Demand (q) 
 
  
Assessment of Normal Variation 
(i)   
(ii)   
(iii)   
(iv)   
(v)  
(vi)  
  
Population forecasting Methods 
 
(i) Arithmetic increase method 
 
 Where, 
  Prospective or forecasted population after n decades from the present (i.e., 
last known census) 
  Population at present (i.e., last known census) 
  Number of decades between now & future. 
  Average (arithmetic mean) of population increases in the known decades. 
  
(ii) Geometric Increase Method 
 
 where, 
  Initial population. 
  Future population after ‘n’ decades. 
  Assumed growth rate (%). 
 
 where, 
  Final known population 
  Initial known population 
  Number of decades (period) between  and   
   
  
(iii) Incremental Increases Method 
 
 Where, 
  Average increase of population of known decades 
  Average of incremental increases of the known decades. 
  
(iv) Decreasing rate of growth method 
 Since the rate of increase in population goes on reducing, as the cities reach 
towards saturation, a method which makes use of the decrease in the percentage 
increase, in many a times used, and gives quite rational results. In this method, the 
average decrease in the percentage increase is worked out, and is then subtraced 
from the latest percentage increase for each successive decade. This method is 
however, applicable only in cases, where the rate of growth shows a downward 
trend. 
  
(v) Logistic Curve Method 
(a)  
 Where, 
  Population of the start point. 
  Saturation population 
  Population at any time t from the origin. 
  Constant. 
  
  
Development of Ground Water 
 
Darcy Law’s 
 (i)  (For Laminar flow) 
 Where, 
 Q = Discharge 
 k = Coefficient of permeability 
 i = Hydraulic gradient   
 A = Area of flow. 
 (ii)   
 Where, V = Discharge velocity 
 (iii)   
 Where,  Seepage velocity 
  Porosity. 
 (iv)   
 Where, 
  Constant having value 400. 
  Hydraulic gradient 
  Effective size of soil particle 
  Dynamic viscosity. 
 (v)   
 Where, 
  Shape factor (which is a function of porosity), packing and grain size 
distribution). 
  Average size of particle. 
  Kinematic viscosity. 
 
 
Specific yield 
   
Page 5


  
Water Demand 
  
Fire Demand 
 Rate of fire demand is sometimes treated as a function of population and is 
worked out on the basis of empirical formulas: 
(i) As per GO Fire Demand 
 
(ii) Kuichling’s Formula 
 
 Where, Q = Amount of water required in litres/minute. 
 P = Population in thousand. 
(iii) Freeman Formula 
 
(iv) National Board of Fire Under Writers Formula 
      (a) For a central congested high valued city 
          (i) Where population < 200000 
 
          (ii) where population > 200000 
 Q = 54600 lit/minute for first fire 
 and Q=9100 to 36,400 lit/minute for a second fire. 
      (b) For a residential city. 
           (i) Small or low building, 
 Q=2,200 lit/minutes. 
           (ii) Larger or higher buildings, 
 Q=4500 lit/minute. 
 (v) Buston’s Formula 
 
  
Per Capita Demand (q) 
 
  
Assessment of Normal Variation 
(i)   
(ii)   
(iii)   
(iv)   
(v)  
(vi)  
  
Population forecasting Methods 
 
(i) Arithmetic increase method 
 
 Where, 
  Prospective or forecasted population after n decades from the present (i.e., 
last known census) 
  Population at present (i.e., last known census) 
  Number of decades between now & future. 
  Average (arithmetic mean) of population increases in the known decades. 
  
(ii) Geometric Increase Method 
 
 where, 
  Initial population. 
  Future population after ‘n’ decades. 
  Assumed growth rate (%). 
 
 where, 
  Final known population 
  Initial known population 
  Number of decades (period) between  and   
   
  
(iii) Incremental Increases Method 
 
 Where, 
  Average increase of population of known decades 
  Average of incremental increases of the known decades. 
  
(iv) Decreasing rate of growth method 
 Since the rate of increase in population goes on reducing, as the cities reach 
towards saturation, a method which makes use of the decrease in the percentage 
increase, in many a times used, and gives quite rational results. In this method, the 
average decrease in the percentage increase is worked out, and is then subtraced 
from the latest percentage increase for each successive decade. This method is 
however, applicable only in cases, where the rate of growth shows a downward 
trend. 
  
(v) Logistic Curve Method 
(a)  
 Where, 
  Population of the start point. 
  Saturation population 
  Population at any time t from the origin. 
  Constant. 
  
  
Development of Ground Water 
 
Darcy Law’s 
 (i)  (For Laminar flow) 
 Where, 
 Q = Discharge 
 k = Coefficient of permeability 
 i = Hydraulic gradient   
 A = Area of flow. 
 (ii)   
 Where, V = Discharge velocity 
 (iii)   
 Where,  Seepage velocity 
  Porosity. 
 (iv)   
 Where, 
  Constant having value 400. 
  Hydraulic gradient 
  Effective size of soil particle 
  Dynamic viscosity. 
 (v)   
 Where, 
  Shape factor (which is a function of porosity), packing and grain size 
distribution). 
  Average size of particle. 
  Kinematic viscosity. 
 
 
Specific yield 
   
 Where,  Specific yield. 
 Volume of water yielded under gravity effect. 
 Total volume of water drained. 
Specific retention 
   
 Where,  Specific retention. 
 Volume of water retain under gravity effect. 
 Total volume of water. 
  
Where,  Porosity. 
Slot Opening 
Slot size  of D10 of gravel pack material. 
Slot size  of aquifer design on the basis of finest aquifer.  
Well Losses 
Jacob-equilibrium formula for confined aquifer, 
 
Where, 
 Drawdown in observation well after time t. 
 Radial distance of observation well from main pump well. 
 Coefficient of transmissibility = k.d 
 Coefficient of storage. 
 
 Drawdown of observation well at time   
 Drawdown of observation well at time   
    Where,  and  is the distance of drawdown in 
time  and  respectively. 
  
Quality control of Water Supplies 
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FAQs on Environmental Engineering Formulas for Civil Engineering Exam - Environmental Engineering - Civil Engineering (CE)

1. What are some commonly used formulas in environmental engineering for civil engineering exams?
Ans. Some commonly used formulas in environmental engineering for civil engineering exams include: 1. Mass balance equation: Q = C * V, where Q is the flow rate, C is the concentration, and V is the volume of the substance. 2. Hazen-Williams formula: Q = 0.849 * C * D^2.63 * S^0.54, where Q is the flow rate, C is the Hazen-Williams coefficient, D is the pipe diameter, and S is the pipe slope. 3. Manning's equation: Q = (1.486/n) * A * R^(2/3) * S^(1/2), where Q is the flow rate, n is the Manning's roughness coefficient, A is the cross-sectional area, R is the hydraulic radius, and S is the slope of the channel. 4. Darcy's law: Q = K * A * (h1 - h2)/L, where Q is the flow rate, K is the hydraulic conductivity, A is the cross-sectional area, h1 and h2 are the hydraulic head at two points, and L is the length of the flow path. 5. Ideal gas law: PV = nRT, where P is the pressure, V is the volume, n is the number of moles, R is the ideal gas constant, and T is the temperature.
2. How do you calculate the flow rate using the Hazen-Williams formula?
Ans. The flow rate (Q) using the Hazen-Williams formula can be calculated using the equation: Q = 0.849 * C * D^2.63 * S^0.54. Here, C is the Hazen-Williams coefficient, D is the pipe diameter, and S is the pipe slope. To calculate the flow rate, substitute the respective values of C, D, and S into the formula and solve for Q.
3. What is the significance of Manning's equation in environmental engineering?
Ans. Manning's equation is widely used in environmental engineering for the design and analysis of open channel flow systems. It relates the flow rate (Q) to various parameters such as the Manning's roughness coefficient (n), cross-sectional area (A), hydraulic radius (R), and slope of the channel (S). By using Manning's equation, engineers can determine the flow characteristics, such as velocity and discharge, in open channels and design efficient and sustainable drainage systems, irrigation canals, and stormwater management systems.
4. How is the mass balance equation applied in environmental engineering?
Ans. The mass balance equation is a fundamental tool in environmental engineering that is used to quantify the movement and distribution of substances in a system. It states that the rate of change of mass within a system is equal to the difference between the rate of mass entering and leaving the system, plus the rate of mass generation or consumption within the system. In environmental engineering, the mass balance equation is used to analyze and design processes such as water treatment, air pollution control, and waste management systems, ensuring that the concentrations and quantities of various substances are properly managed and controlled.
5. What is the role of Darcy's law in environmental engineering?
Ans. Darcy's law is a fundamental principle in environmental engineering that describes the flow of fluids through porous media, such as soil and rock. It states that the flow rate (Q) is proportional to the hydraulic conductivity (K), cross-sectional area (A), and the difference in hydraulic head (h1 - h2) divided by the length of the flow path (L). In environmental engineering, Darcy's law is used to analyze groundwater flow, design groundwater extraction and remediation systems, and assess the movement of contaminants in the subsurface. It helps engineers understand and predict the behavior of fluids in porous media, ensuring the effective management and protection of groundwater resources.
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