A digital pH meter was used to measure the soil pH in 1:5 soil/1 M KCl solutions (Mettler Toledo
FE20/El20, Shanghai, China). The soil water content (SWC) was calculated by using the oven-drying method. Soil samples were oven dried for 48 h at 105°C. The SWC (%) was calculated by using the following formula:
where W1 is the weight of wet soil plus box, W2 represents the weight of dry soil plus box, and W3 represents box weight.
HOBO®
Micro Station Data Loggers (H21-002) were installed to check the soil temperature (°C) and volumetric soil moisture content (m
3/m
3) during the study period. Soil moisture conditions were monitored using an automatic soil moisture smart sensor (HOBO Micro Station #H21-002 Data Logger; Onset Computer Corp., Bourne, MA, United States; #S-SMx-M005;
Supplementary Figure 5). To measure the soil temperature, HOBO 12-bit temperature smart sensors (S-TMB-M0xx) were connected to HOBO
Micro Station Data Loggers. Automatic measurements were obtained every 10 s (
Supplementary Figures 6, 7). All measurements were recorded using the HOBO®
Micro Station Data Logger.
Umair M., Sun N., Du H., Hui N., Altaf M., Du B., Yin S, & Liu C. (2020). Bacterial Communities Are More Sensitive to Water Addition Than Fungal Communities Due to Higher Soil K and Na in a Degraded Karst Ecosystem of Southwestern China. Frontiers in Microbiology, 11, 562546.