22-Agric-B7 Principles of Hydrology · May 2014
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
National Exams — May 2014 — 04-Agric-B7, Principles of Hydrology (Soil Hydrology). Three-hour, open-book exam; any non-communicating calculator is permitted. Format: five questions constitute a complete paper, each of equal value; most questions require an answer involving calculations.
Reference texts: Chow, Maidment & Mays, Applied Hydrology — IDF curves, unit-hydrograph/critical-duration behaviour, Horton infiltration, flood-frequency analysis; Viessman & Lewis, Introduction to Hydrology — hydrologic cycle terminology, detention-pond routing; Todd & Mays, Groundwater Hydrology — Thiem equation for confined and unconfined aquifers, well-test assumptions.
Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.
Given.
| Year | Peak discharge, $Q$ (m$^3$/s) |
|---|---|
| 2013 | 10 |
| 2012 | 22 |
| 2011 | 28 |
| 2010 | 15 |
| 2009 | 8 |
Find. (a) The 2-year and 10-year return-period discharges, $Q_2$ and $Q_{10}$, assuming a log-normal population. (b) A check on the log-normality assumption itself.
Approach. Transform each discharge to $y=\log_{10}Q$, compute the sample mean $\bar y$ and standard deviation $s_y$ of the transformed data, then back-transform using $Q_T=10^{\bar y + z_T s_y}$, where $z_T$ is the standard-normal variate for return period $T$ ($z_T=0$ at $T=2$ yr, since 50% non-exceedance corresponds to the median; $z_T=1.282$ at $T=10$ yr, the standard-normal deviate for 90% non-exceedance).
(b) Checking the log-normality assumption. The standard graphical check is to rank the five discharges, assign each an empirical exceedance probability with a plotting-position formula (Weibull, $p=m/(n+1)$, $m=1$ for the largest), convert each probability to its standard-normal variate $z$, and plot $\log_{10}Q$ against $z$ on ordinary (or, equivalently, $Q$ directly on log-normal probability paper). If the population is genuinely log-normal, these points should scatter closely about a straight line, since a log-normal variable is by definition one whose logarithm plots as a straight line against a normal probability scale. A quantitative companion check is the sample skewness coefficient of the log-transformed data: a true normal (hence log-normal, in logs) population has zero skew, so a computed skewness for $y=\log_{10}Q$ close to zero supports the assumption, while a strongly non-zero value would argue against it.
| Quantity | Result |
|---|---|
| $\bar y=\overline{\log_{10}Q}$ | 1.174 |
| $s_y$ | 0.227 |
| $Q_2$ (2-yr return period) | 14.9 m$^3$/s |
| $Q_{10}$ (10-yr return period) | 29.2 m$^3$/s |