Bazin arrives at the following values of _m_:--

_Coefficients of Discharge of Standard Weir._

+----------------+--------------+--------+

| Head h metres. | Head h feet. | m |

+----------------+--------------+--------+

| 0.05 | .164 | 0.4485 |

| 0.10 | .328 | 0.4336 |

| 0.15 | .492 | 0.4284 |

| 0.20 | .656 | 0.4262 |

| 0.25 | .820 | 0.4259 |

| 0.30 | .984 | 0.4266 |

| 0.35 | 1.148 | 0.4275 |

| 0.40 | 1.312 | 0.4286 |

| 0.45 | 1.476 | 0.4299 |

| 0.50 | 1.640 | 0.4313 |

| 0.55 | 1.804 | 0.4327 |

| 0.60 | 1.968 | 0.4341 |

+----------------+--------------+--------+

Bazin compares his results with those of Fteley and Stearns in 1877

and 1879, correcting for a different velocity of approach, and finds a

close agreement.

_Influence of Velocity of Approach._--To take account of the velocity

of approach u it is usual to replace h in the formula by h + au²/2g

where [alpha] is a coefficient not very well ascertained. Then

Q = [mu]l (h + [alpha]u²/2g) [root]{2g(h + [alpha]u²/2g)}

= [mu]lh [root](2gh)(1 + [alpha]u²/2gh)^(3/2). (2)

Encyclopaedia Britannica, 11th Edition, "Husband" to "Hydrolysis" Volume 14, Slice 1 · 第 71 / 207 题