Using Capacitance Sensors for the Continuous Measurement of the Water Content in the Litter Layer of Forest Soil
Figure 4
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 () and the gravimetric water content (WCweight; Square) in the layer in a temperate broad-leaved secondary forest at Yamashiro Experimental Forest (YMS) from May to September 2013. Error bars are standard deviations.