Analysis of Water Volume Required to Reach Steady Flow in the Constant Head Well Permeameter Method

Author:

Amoozegar Aziz1ORCID,Heitman Joshua L.1

Affiliation:

1. Crop and Soil Sciences Department, North Carolina State University, Campus Box 7620, Raleigh, NC 27695-7620, USA

Abstract

The most common method for in situ measurement of saturated hydraulic conductivity (Ksat) of the vadose zone is the constant head well permeameter method. Our general objective is to provide an empirical method for determining volume of water required for measuring Ksat using this procedure. For one-dimensional infiltration, steady state reaches as time (t) → ∞. For three-dimensional water flow from a cylindrical hole under a constant depth of water, however, steady state reaches rather quickly when a saturated bulb forms around the hole. To reach a quasi-steady state for measuring Ksat, we assume an adequate volume of water is needed to form the saturated bulb around the hole and increase the water content outside of the saturated bulb within a bulb-shaped volume of soil, hereafter, referred to as wetted soil volume. We determined the dimensions of the saturated bulb using the Glover model that is used for calculating Ksat. We then used the values to determine the volume of the saturated and wetted bulbs around the hole. The volume of water needed to reach a quasi-steady state depends on the difference between the soil saturated and antecedent water content (Δθ). Based on our analysis, between 2 and 5 L of water is needed to measure Ksat when Δθ varies between 0.1 and 0.4 m3 m−3, respectively.

Funder

USDA-NIFA Multi-State Project 4188

North Carolina Agricultural Research Service (NCARS), NC State University

Publisher

MDPI AG

Subject

Earth-Surface Processes,Waste Management and Disposal,Water Science and Technology,Oceanography

Reference48 articles.

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3. SSSA (2023). Glossary of Soil Science Terms, Soil Science Society of America. Available online: https://www.soils.org/publications/soils-glossary/.

4. Hillel, D. (2004). Introduction to Environmental Soil Physics, Elsevier Academic Press.

5. Skaggs, R.W., and van Schilfgaarde, J. (1999). Agricultural Drainage, Soil Science Society of America, Inc.. Monograph No. 38.

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