knitr::opts_chunk$set( echo = TRUE, warning = FALSE, message = FALSE, comment = "# >" )
Dissolve 40 g of SHMP in 1 L of deionized water. Use an ultrasonic bath to ensure complete dissolution. The solution is stable for approximately one month.
Hydrometers are graduated to be read at the bottom of the meniscus. However, readings must be taken at the top of the meniscus in opaque soil suspensions.
Lower the hydrometer into a 1 L cylinder filled with 125 mL of SHMP solution and 875 mL of deionized water. When stabilized (after 20 s), record both the reading at the bottom (zero or composite correction factor) and at the top of the meniscus (meniscus correction factor).
If the soil sample contains primarily clay or silt, weigh out 50 g of soil (accuracy ±0.01 g) in a 500 mL screw bottle (in 3-fold replication). If the sample is sandy, take 100 g each. Add 125 mL SHMP to the soil. Agitate the mixture for 16 h in a horizontal shaker.
Completely transfer the soil solution into the sedimentation cylinder using the squirt bottle. Fill up to the 1 L mark with deionized water. Cap the cylinder with parafilm. Agitate the solution by turning the cylinder upside down and back 30 times during 1 min.
Place the sedimentation cylinder at a bench where it can stand undisturbed for the next 4 to 6 h.
Insert the hydrometer into the soil solution as soon as possible and take the first reading the latest after 40 s at top of the meniscus. Measure the temperature of the slurry. Repeat this measurement at 2, 5, 15, 30, 60, 120, 240, and 360 min. In any case, record the exact reading time. The measurements may be reduced to an initial reading after 40 s and a second one after 240 or 360 min (Ashworth et al., 2001). Rinse the hydrometer after each measurement. If the ambient temperature changes, recalibrate the hydrometer.
The following table may serve as a sample template to record the data
| Sample data | Time [min] | Hydrometer reading | Correction | Temperature [°C] | | ----------- | ---------- | ------------------ | ---------- | ---------------- | | S1 | 0.66 | 39 | 2 | 23 | | S1 | 2.00 | 33 | 2 | 23 | | S1 | 5.00 | 29 | 2 | 23 | | S1 | 15.00 | 23 | 2 | 23 | | S1 | 30.00 | 22 | 2 | 23 | | S1 | 60.00 | 20 | 2 | 23 | | S1 | ... | ... | ... | ... | | S2 | ... | ... | ... | ... |
A complete description of how to calculate the particle size
distribution from the recorded hydrometer readings is available in the
respective ASTM guideline (ASTM D422-63, 2007). The
algorithm has also been implemented into this package using the
# Load envalysis library(envalysis) # Load and look at sample data data(clayloam) clayloam # Calculate the particle size distribution tex <- texture(reading ~ blank + time + temperature, clayloam, plot = T) tex
Further soil classification and plotting may be done with the soiltexture package.
# Load soiltexture library(soiltexture) # Prepare data germansoil <- data.frame(t(tex$din["Estimate",] * 100)) names(germansoil) <- toupper(names(germansoil)) ussoil <- data.frame(t(tex$usda["Estimate",] * 100)) names(ussoil) <- toupper(names(ussoil)) # Get texture class, for example, in accordance with the German # "Bodenartendiagramm" (DE.BK94.TT) TT.points.in.classes(germansoil, class.sys = "DE.BK94.TT") # Get USDA texture class (USDA.TT) TT.points.in.classes(ussoil, class.sys = "USDA.TT")
The analyzed soil is a clay loam (German: "Toniger Lehm", Lt2).
Ashworth, J., Keyes, D., Kirk, R., & Lessard, R. (2001). Standard Procedure in the Hydrometer Method for Particle Size Analysis. Communications in Soil Science and Plant Analysis 32, 633-642. DOI: 10.1081/CSS-100103897.
ASTM D422-63 (2007). Standard Test Method for Particle-Size Analysis of Soils. Technical standard. ASTM International, West Conshohocken, PA.
Bouyoucos, G.J., (1927). The hydrometer as a new method for the mechanical analysis of soils. Soil Science 23, 343–354.
Moeys, J., Shangguan, W., Petzold, R., Minasny, B., Rosca, B., Jelinski, N., Zelazny, W., Souza, R.M.S., Safanelli, J.L., & ten Caten, A. (2018). soiltexture: Functions for Soil Texture Plot, Classification and Transformation. URL: https://CRAN.R-project.org/package=soiltexture.
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