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In This Article

  • Summary
  • Abstract
  • Introduction
  • Protocol
  • Representative Results
  • Discussion
  • Acknowledgements
  • Materials
  • References
  • Reprints and Permissions

Summary

This article features a simple evaporation experiment using a hydraulic property instrument for a soil sample. Through efficient means, measurements can be taken over a series of days to generate high-quality data.

Abstract

The measurement of soil hydraulic properties is critical in understanding the physical components of soil health as well as integrated knowledge of soil systems under various management practices. Collecting reliable data is imperative for informing decisions that affect agriculture and the environment. The simple evaporation experiment described here uses instrumentation in a laboratory setting to analyze soil samples collected in the field. The soil water tension of the sample is measured by the instrument, and tension data is modeled by software to return soil hydraulic properties. This method can be utilized to measure soil water retention and hydraulic conductivity and give insight into differences in treatments or environmental dynamics over time. Initial establishment requires a user, but data acquisition is automated with the instrument. Soil hydraulic properties are not easily measured with traditional experiments, and this protocol offers a simple and optimal alternative. Interpretation of results and options for extending the data range are discussed.

Introduction

Soil water retention and hydraulic conductivity within natural and human-altered environments help us understand and observe changes in soil health and functionality. Quantifying hydraulic properties through the soil water retention curve (SWRC) and soil water conductivity curve offers insight into key drivers of soil physical behavior and water movement characterization1. The relationship between volumetric water content (θ) and matric head (h) is represented within an SWRC, and the ranges within the curve describe the saturation point, field capacity, and permanent wilting point2. Soil management practices, amendm....

Protocol

1. Soil sampling and sample preparation

NOTE: A schematic diagram of the workflow of this method can be found in Figure 1.

  1. Sample collection
    1. Excavate the top few centimeters above the desired sampling depth to remove unwanted debris, particularly loose organic litter and soil surface crusting.
    2. Place the metal sampling core level on the surface of the exposed soil, with the sharp edge side facing the soil surface;.......

Representative Results

Upon completing a proper measurement campaign following the protocol above, it will be possible to view the data output of the experiment in the analysis software. Output curves originate from tensiometer readings that measure water tension (hPa) over time (t), and the initial curve of this data is generated immediately after termination of the campaign. Selected examples of tension curves of two soil samples can be examined to illustrate optimal and suboptimal results (Figure 2). Optimal re.......

Discussion

The simple evaporation experiment approach using the method that is described here is an efficient means to develop the SWRC and hydraulic conductivity curves. Simplicity and accuracy of data measurement make it a viable alternative to more traditional methods14. The method described here goes beyond the user manual and current literature to synthesize and expand on finer points of this intricate instrument. Particular attention needs to be paid to the soil sample collection, transport, and analys.......

Acknowledgements

The authors gratefully acknowledge the financial support provided by the Canadian Foundation for Innovation (John Evans Leadership Fund) in the acquisition of the hydraulic property analyser instrument.

....

Materials

NameCompanyCatalog NumberComments
4 L Buchner Flasks (two)Variousn/aContainers for water degassing
20 mL Syringe, fine tipBDBD-302830
Coffee filterVariousn/aPrevents soil travel out of core while soaking
HYPROP Complete SetHoskin110813/E240-M020210tensiometer shaft auger, tube for vacuum syringe and refilling adapter, auger guide, HYPROP USB adapter, HYPROP sensor unit, tensiometer shafts (50 mm and 25 mm), saturation plate, refilling adapter, silicone gasket, set of o-rings, LABROS balance, software, cables
HYPROP Refill UnitHoskin108899/ E240-M020258vacuum pump, vacuum mount, beaker mount, refilling adapters
Large Plastic TubsVariousn/aHolds water and soil cores during saturation
METER hammering holderHoskin100255/E240-100201
Rubber MalletHome Depot18CT1031Sample collection tool used with hammering holder
ShovelHome Depot83200
Soil Sampling Ring incl. 2 capsHoskin100254/E240-100101
Stir plate/ Stirring BarVariousn/a
TrowelHome Depot91365

References

  1. Malaya, C., Sreedeep, S. Critical review on the parameters influencing soil-water characteristic curve. J Irrig Drain Eng. 138 (1), 55-62 (2011).
  2. Schelle, H., Heise, L., Jänicke, K., Durner, W.

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Soil Water PotentialSoil ConductivityHydraulic PropertiesEvaporation ExperimentSoil HealthData AcquisitionSoil Water RetentionHydraulic ConductivityInstrumentationLaboratory AnalysisAgricultural ManagementEnvironmental DynamicsTreatment DifferencesAutomated Data Collection

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