Chapter 4: Problem 180
An article in Journal of Hydrology ["Use of a Lognormal Distribution Model for Estimating Soil Water Retention Curves from Particle-Size Distribution Data" \((2006,\) Vol. \(323(1),\) pp. \(325-334)]\) considered a lognormal distribution model to estimate water retention curves for a range of soil textures. The particle-size distribution (in centimeters) was modeled as a lognormal random variable \(X\) with \(\theta=-3.8\) and \(\omega=0.7 .\) Determine the following: (a) \(P(X<0.02)\) (b) Value for \(x\) such that \(P(X \leq x)=0.95\) (c) Mean and variance of \(X\)
Short Answer
Step by step solution
Understanding Lognormal Distribution
Calculating P(X < 0.02)
Calculating Value of x for P(X ≤ x) = 0.95
Finding Mean and Variance of X
Unlock Step-by-Step Solutions & Ace Your Exams!
-
Full Textbook Solutions
Get detailed explanations and key concepts
-
Unlimited Al creation
Al flashcards, explanations, exams and more...
-
Ads-free access
To over 500 millions flashcards
-
Money-back guarantee
We refund you if you fail your exam.
Over 30 million students worldwide already upgrade their learning with 91Ó°ÊÓ!
Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Soil Water Retention
- Soil water retention curves depict the relationship between soil water content and soil water potential.
- The particle-size distribution in soil is a significant factor affecting water retention.
- Estimating soil water retention involves modeling soil as a composition of different particle sizes, influencing overall porosity and capacity to retain water.
Step-by-Step Solution
- Firstly, understanding the type of distribution: A Lognormal Distribution, where the natural logarithm of the variable is normally distributed, allows handling skewed data like soil particles efficiently.
- Computing probabilities for given conditions: This involves transforming the lognormal variable into a standard normal form to use familiar statistical methods.
- Finding specific data points: By utilizing percentile information and rearranging equations, we find specific values that meet certain probability criteria.
- Calculating Mean and Variance: This provides a summary statistic that describes the expected value and variability of soil particle size, crucial for interpreting various soil behaviors and engineering practices.
Probability Estimation
Here’s a simple overview:
- Transform the soil particle size value to a logarithmic scale, utilizing the parameters provided, such as mean \(\theta\) and standard deviation \(\omega\).
- Use statistical tables or calculators to find the cumulative probability corresponding to this transformed value.
- This process helps in estimating the likelihood of soil particles being below a certain size, which directly impacts water retention capacity.
Mean and Variance
- The mean of the lognormal distribution (\( \mu_X \)) provides an average particle size when measured over many samples, helping in understanding general trends.
- Variance (\( \sigma_X^2 \)) indicates the level of spread or dispersion around the mean, giving an idea about the diversity of particle sizes.
- These statistics are calculated using specific formulas: \( \mu_X = e^{\theta + \frac{\omega^2}{2}} \) and\( \sigma_X^2 = (e^{\omega^2} - 1) \cdot e^{2\theta + \omega^2} \).
Journal of Hydrology
- The journal publishes high-quality studies, often employing statistics and models to address significant hydrological questions.
- Articles often serve as references for educational purposes, providing methodologies that can be applied or adapted in various contexts.
- By contributing to global knowledge, journals like this foster innovation and progress in tackling water-related challenges.