ORIGINAL RESEARCH
Soil Cations Explain the Variation of Soil
Extracellular Activities and Microbial Elemental
Limitations on Subtropical Grassland, China
More details
Hide details
1
Guizhou Institution of Prataculture, Guizhou Academy of Agricultural Sciences, Guiyang 550006, Guizhou, China
2
Guizhou Province Songbaishan Reservoir Management Office, Guiyang 550025, Guizhou, China
3
College of Animal Sciences, Guizhou University, Guiyang 550025, Guizhou, China
4
School of Life Sciences, Guizhou Normal University, Guiyang 550025, Guizhou, China
Submission date: 2023-05-04
Final revision date: 2023-12-01
Acceptance date: 2023-12-07
Online publication date: 2024-04-24
Publication date: 2024-05-23
Corresponding author
Leilei Ding
Guizhou Institution of Prataculture, Guizhou Academy of Agricultural Sciences, Guiyang 550006, Guizhou, China
Puchang Wang
School of Life Sciences, Guizhou Normal University, Guiyang 550025, Guizhou, China
Pol. J. Environ. Stud. 2024;33(4):4061-4070
KEYWORDS
TOPICS
ABSTRACT
The objective of this study was to compare the effects of grazing and non-grazing on the
physicochemical properties, stoichiometry, ecto-enzyme activities, and microbial element limitations
of soils at five depths in subtropical grassland, China, and to identify the influencing factors of enzyme
activities and element limitations. Results showed that grazing, soil depth, and the interaction between
grazing and depth remarkably changed soil available phosphorus (AP), available potassium (AK),
available calcium (ACa) and available magnesium contents (AMg), bulk density (BD), water content
(WC), and β-glucosidase activity (βGC) (p = 6.702e-9 - 0.04739). Compared with no g razing, g razing
remarkably declined the 0-5 cm soil AP by 73.10% (p = 0.0250), the 0-5, 5-10, 10-20 cm soil WC by
47.19% (p = 0 .0042), 3 7.19% ( p = 0 .0090), a nd 3 0.80% ( p = 0.0034), however, grazing remarkably
increased the 0-5, 5-10, 10-20, 20-30 cm soil ACa by 188.76% (p = 7.9e-05), 93.24% (p = 0.0177) ,84.18%
(p = 0.00067), and 38.77% (p = 0.01368), the 0-5, 5-10 cm soil AMg by 186.69% ( p = 0.0016), 78.89%
(p = 0.0109), t he 0-5, 5-10, 1 0-20 c m s oil pH b y 0 .51 ( p = 0.0013), 0.37 (p = 0.0006), and
0.27 (p = 0.0114) units, the 0 -5, 5-10, 10-20 cm soil BD by 59.03% ( p = 0.0077), 44.14% ( p = 0.0147),
and 35.55% (p = 0.0071), the 30-50 cm soil WC by 22.88% (p = 0.0241), the 0-5 cm soil βGC by 89.49%
(p = 0.0011), the 0-5, 5-10 cm soil ACP by 7.87% (p = 0.0300), 6.57% (p = 0.0240), respectively. Grazing
exacerbated the microbial C limitation of 0-5 and 10-20 cm soils by 20.51% (p = 0.0078) and 40.38%
(p = 0.0209) and switched the soil microbiome from under N limitation to under P limitation at 5-10 cm
(p = 0.0390). Specific soil available cations were identified as the important factors that significantly
explained the variation of soil ecto-enzyme activities and soil microbial carbon and nutrient limitations. These findings present basic information for the future improvement management of subtropical
grassland and understanding the impact of grazing on microbial element limitation.