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We want the time required for a truncated cone-shaped tank or pond to drain through a circular orifice at the bottom. The tank is described only by the area at the top, the area at the orifice, and the initial height. We will use a volume balance together with the orifice flow law, then integrate from the full height down to zero.
Define the symbols as follows:
H1 = initial (starting) liquid height above the orifice centroid (a fixed parameter).A1 = initial area at height H1.A0 = area at the orifice centroid elevation.h = current liquid height above the orifice centroid (the variable of integration, running from 0 to H1).A(h) = cross-sectional area at height h.aor = orifice area.Cd = discharge coefficient.g = gravity.Because the pond sides are straight, the radius (conic section assumption) changes linearly with height. Since area is proportional to radius squared, the square root of the area also changes linearly with height. That is the geometric fact that makes the derivation tractable, and it gives the interpolation formula:
Squaring both sides of Eq. (1) gives the area at height h.
Eq. (3) will expand this into a polynomial form suitable for integration term by term.
Expanding the square in Eq. (2) separates A(h) into three terms, each a different power of h. This expanded form will simplify the integration later.
Next we use conservation of volume.
A thin slice of liquid of thickness dh at height h has volume equal to area times thickness.
This is the standard slice approximation behind calculus volume formulas.
The outflow through the orifice is given by the orifice equation.
Since the head driving the flow is the current height h, the flow rate is
The basic volume balance is that the rate of decrease of tank or pond volume equals the outflow rate. In differential form, we write the time element as volume change divided by flow rate.
Substitute Eq. (4) into Eq. (6). This simply replaces the thin-slice volume with area times thickness.
Now substitute the orifice law from Eq. (5) into Eq. (7).
Since Q depends on h, it must be part of the integral rather than being treated as a constant.
The total drain time is found by integrating the running variable h from the empty height h = 0 to the initial height h = H1.
In other words, we accumulate the tiny time pieces from the start of drainage to the end.
Substituting Eq. (8) into Eq. (9) yields the integral form for the drain time.
Now substitute the area formula from Eq. (3) into Eq. (10). This gives an explicit integrand written entirely in terms of the known endpoint areas and the variable height.
Dividing each of the three terms in the expanded numerator of Eq. (11) by √h and writing the square-root factors as fractional exponents makes the power-law structure explicit and prepares each term for direct application of the power rule:
Integrating term by term uses the standard power rules:
INT h^(-1/2) dh = 2 * h^(1/2)INT h^(1/2) dh = (2/3) * h^(3/2)INT h^(3/2) dh = (2/5) * h^(5/2)Applying these rules to each term and writing the antiderivative evaluated from h = 0 to h = H₁:
Since every term contains a positive power of h, evaluating at the lower limit h = 0 contributes nothing. Evaluating at h = H₁ directly substitutes H₁ for h in each term:
Simplifying: H₁1/2 = √H₁, H₁3/2/H₁ = √H₁, and H₁5/2/H₁2 = √H₁:
Factoring out √H₁ gives
Expanding the bracket term by term:
Collecting like terms:
Therefore the final spreadsheet formula is
=SQRT(H1)/(Cd*aor*SQRT(2*g))*((2/5)*A1 + (8/15)*SQRT(A0*A1) + (16/15)*A0)
In summary, the derivation works by combining three ideas: Eq. (1) gives the geometry of the truncated cone, Eq. (4) gives the small volume slice, and Eq. (5) gives the discharge through the orifice. Those are substituted into the volume balance, assembled into the integral in Eq. (9), and evaluated in Eq. (10) through Eq. (13). The result is the closed-form expression in Eq. (18).
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