Using Capacitance Sensors for the Continuous Measurement of the Water Content in the Litter Layer of Forest Soil

<table>Temporal variation in (a) hourly precipitation, (b) volumetric soil water content at a depth of 0–5 cm in mineral soil depth, and (c) water content obtained using the LWC method (<svg height="17" id="M64" style="vertical-align:-4.47035pt" version="1.1" viewbox="0 0 105.2625 17" width="105.2625" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
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</svg>) and the gravimetric water content (WC<sub>weight</sub>; Square) in the <svg height="11.175" id="M65" style="vertical-align:-0.0pt" version="1.1" viewbox="0 0 9.2749996 11.175" width="9.2749996" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
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</svg> layer in a temperate broad-leaved secondary forest at Yamashiro Experimental Forest (YMS) from May to September 2013. Error bars are standard deviations.</table>

Applied and Environmental Soil Science

fig4

Figure 4

Figure 4: Using Capacitance Sensors for the Continuous Measurement of the Water Content in the Litter Layer of Forest Soil 