Abstract

The impact of machines on forest soils is regularly assessed and quantified using absolute bulk density, which is most frequently obtained by soil cores. However, to allow for repeated measurements at the exact same locations, non-destructive devices are increasingly being used to determine soil bulk density and moisture content in field studies. An example of such a device is a nuclear moisture and density gauge (NMDG), originally designed as a control measurement for soil bulk density and moisture content in geotechnical applications. Unlike road construction or foundation projects that use mineral soil or gravel, forest soils have complex structures and the presence of organic matter, which can skew moisture and density readings from a NMDG. To gain further knowledge in this respect, we performed controlled tests in a sandbox to quantify the influence of varying amounts of saturated organic matter (3, 5, 10, and 15%) mixed with mineral soil in different layers (0–5, 0–10, 0–20 and 0–40 cm) on the accuracy of soil moisture content obtained by a NMDG and soil theta probe at varying depths. Main results illustrated that the presence of saturated organic matter per se was not problematic but moisture content overestimations and related underestimation of dry bulk density occurred when the tested measurement depth was below the created organic layer. Since forest soils often exhibit higher organic matter contents in the upper horizon, correction factors are suggested to minimize the moisture content variations between NMDG and reference method. With the use of correction factors, NMDG can present a non-destructive, fast, and accurate method of measuring soil moisture and bulk density in forestry applications.

Highlights

  • DescriptionThe ML3 measures soil moisture content and temperature[1].Its sealed plastic body is attached to four sensing rods which insert directly into the soil for taking readings.A waterproof plug connects to a choice of signal cables.Both extension cables and extension tubes can be used.The soil moisture output signal is a differential analogue DC voltage

  • This is converted to soil moisture by a data logger or meter using the supplied general soil calibrations

  • Take care when attaching cables to ensure that the connectors are clean, undamaged and properly aligned before pushing the parts together

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Summary

Introduction

The ML3 measures soil moisture content and temperature[1]. The soil moisture output signal is a differential analogue DC voltage. Take care when attaching cables to ensure that the connectors are clean, undamaged and properly aligned before pushing the parts together. For soil temperature near the surface dig a trench and install horizontally as shown below. 12 ML3s can be connected if you do not use the temperature sensor. For this you will need a 5 gland expansion lid GP2-G5-LID. Up to 60 ML3s can be connected to a DL2e logger (if not using the temperature sensor channel). Up to 30 ML3s can be connected if reading the temperature sensor. These details illustrate connection to Channels 57 and 58 using a LAC1 input card configured in 15-channel mode, and warm-up channel

63: DL2e terminal
Soil moisture reading
Result
Full Text
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