CHARACTERIZATION OF PORE SIZE DISTRIBUTIONS WITHIN SOILS BY MERCURY INTRUSION AND WATER-RELEASE METHODS
- 1 May 1985
- journal article
- research article
- Published by Wolters Kluwer Health in Soil Science
- Vol. 139 (5) , 400-404
- https://doi.org/10.1097/00010694-198505000-00004
Abstract
I measured and interpreted soil pore size distributions for undisturbed, oven-dried peds using mercury intrusion porosimetry. The pore size distributions were compared with those calculated from moisture release data. A correlation between water retention difference by water-release methods and water storage pore volumes (50 to 0.5 μ) by mercury intrusion was established with an R2 = 0.58 over a variety of soil texture and bulk density ranges. Most of the variation occurred for soil samples high in either sand or clay. In addition, root-restricting class limits were developed based on volume of root size pores (200 to 10 μ) within oven-dried peds that were large enough to permit root tip and root hair penetration. © Williams & Wilkins 1985. All Rights Reserved.This publication has 3 references indexed in Scilit:
- STABILITY OF SOIL PORES DURING MERCURY INTRUSION POROSIMETRYEuropean Journal of Soil Science, 1978
- MEASUREMENT OF PORE SIZES IN FINE‐TEXTURED SOILS: A REVIEW OF EXISTING TECHNIQUESEuropean Journal of Soil Science, 1977
- Soil damage by intensive arable cultivation: temporary or permanent?Philosophical Transactions of the Royal Society of London. B, Biological Sciences, 1977