Research on the Effect of Seasonal Freeze-Thaw Cycles and Different
Salinity Gradients on Microbial Abundance
- Yue-Fa YANG,
- Chun-Xia WANG,
- He Xin He Xin Lin,
- Hong-Xin WANG,
- Yuan WANG,
- Fang-Yuan ZHOU,
- Da QIN,
- Zi-Kang FAN
Yue-Fa YANG
Shihezi University School of Water Conservancy and Civil Engineering
Author ProfileChun-Xia WANG
Shihezi University School of Water Conservancy and Civil Engineering
Corresponding Author:wangchunxia1979@139.com
Author ProfileHe Xin He Xin Lin
Shihezi University School of Water Conservancy and Civil Engineering
Author ProfileHong-Xin WANG
Shihezi University School of Water Conservancy and Civil Engineering
Author ProfileYuan WANG
Shihezi University School of Water Conservancy and Civil Engineering
Author ProfileFang-Yuan ZHOU
Shihezi University School of Water Conservancy and Civil Engineering
Author ProfileDa QIN
Shihezi University School of Water Conservancy and Civil Engineering
Author ProfileZi-Kang FAN
Shihezi University School of Water Conservancy and Civil Engineering
Author ProfileAbstract
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Salinization severely impacts soil health. The seasonal freeze-thaw
period is a crucial time for the restoration of soil fertility, and soil
microorganisms play an important role in the cycling of soil ecosystems.
Therefore, it is essential to determine the changes in microbial
abundance under the influence of soil salinity gradients during the
seasonal freeze-thaw period and to understand their relationships with
soil environmental factors.This study designed 19 different gradients of
chloride and sulfate salts. Soil samples were collected after the
seasonal freeze-thaw period to examine the abundance of soil
microorganisms and soil environmental factors, followed by correlation
analysis. We found that with increasing salinity, the abundance of soil
bacteria and fungi significantly decreased, but chloride and sulfate
concentrations at 3 g/kg promoted fungal proliferation.We also observed
that during the seasonal freeze-thaw period under the chloride gradient:
in the 0-5 cm soil layer, soil bacteria and fungi exhibited a symbiotic
relationship, with the abundance of soil bacteria primarily influenced
by soil pH, Na +, Ca 2+, Cl
-, organic matter, and nitrate nitrogen; the abundance
of soil fungi was mainly affected by soil pH. In the 5-20 cm soil layer,
the abundance of soil bacteria was mainly influenced by soil salinity,
soil pH, Ca 2+, Cl -, and nitrate
nitrogen, while the abundance of soil fungi was affected by soil
salinity, soil pH, Na +, Ca 2+, Cl
-, and nitrate nitrogen.We also found that under the
sulfate gradient during the seasonal freeze-thaw period: in the 0-5 cm
soil layer, the abundance of soil bacteria was not significantly
correlated with various soil indicators, and the abundance of soil fungi
was mainly influenced by Na +, Ca
2+, Cl -, and SO 4
2-; in the 5-20 cm soil layer, the abundance of soil
bacteria was influenced by soil pH, Na +, Ca
2+, Cl -, and SO 4
2-, while the abundance of soil fungi was affected by
nitrate nitrogen. The thresholds for chloride and sulfate concentrations
were 5.5 g/kg and 6.5 g/kg, respectively.