Mining areas characterized by high underground water levels are one of
the most important types of coal mining areas in China. In regions with
high groundwater levels, the soil ecological environment is destroyed
due to surface subsidence induced by coal mining and soil disturbances.
There are a variety of soil factors each with different degrees of
spatial variation, and the impact on soil microbial communities is
particularly severe. In order to explore the change and driving
mechanism of soil microbial community structure in coal mining
subsidence areas with high underground water levels, we sought to
elucidate these mechanisms by studying soil samples collected at
different depths (SL: 0-20 cm, ML: 20-40 cm, DL: 40-60 cm) of a deep
coal seam subsidence area (T1) and shallow coal seam subsidence area
(T2) and their control non-subsidence areas (W1 and W2) within a typical
coal mine area with high underground water levels in southwest Shandong
Province. These soil samples were used for determination and analysis of
their physicochemical properties and microbial diversity. The results
show that coal mining subsidence has significant effects on the soil
physicochemical properties and soil microbial community. With the
increase in sampling depth, the soil water content (SWC), bulk density
(BD), and soil pH increased, whereas the contents of soil
alkali-hydrolyzable nitrogen (AN), available phosphorus (AP), available
potassium (AK), and soil organic matter (SOM) decreased. Compared with
the non-subsidence area, the soil alkalinity in the subsidence area was
lower and the soil moisture content, affected by the underground water
level, was higher; the richness and diversity of the microbial community
was lower in the subsidence area despite its higher relative abundance
of Actinobacteria, Chloroflexi, and Myxomycota species. In addition,
species of Thelebolales and Pleosporales were dominant in T1 and T2,
respectively. Soil pH was observed to be the most important
physicochemical factor affecting microbial communities, followed by AN
and AP. The results of our study provide a theoretical basis for soil
ecological restoration and land reclamation in mining areas with high
underground water levels.